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href="https://www.academia.edu/96354885/Raw_data_for_Biomechanical_demands_of_percussive_techniques_in_the_context_of_early_stone_toolmaking"><img alt="Research paper thumbnail of Raw data for: Biomechanical demands of percussive techniques in the context of early stone toolmaking" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354885/Raw_data_for_Biomechanical_demands_of_percussive_techniques_in_the_context_of_early_stone_toolmaking">Raw data for: Biomechanical demands of percussive techniques in the context of early stone toolmaking</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Recent discoveries in archaeology and palaeoanthropology highlight that stone stool knapping coul...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Recent discoveries in archaeology and palaeoanthropology highlight that stone stool knapping could have emerged first within the genera Australopithecus or Kenyanthropus rather than Homo. To explore the implications of this hypothesis determining the physical demands and motor control needed for performing the percussive movements during the oldest stone toolmaking technology (i.e. Lomekwian) would help. We analysed the joint-angle patterns and muscle activity of a knapping expert using three stone tool replication techniques: unipolar flaking on passive hammer (PH), bipolar flaking on anvil (BP), multidirectional and multifacial flaking with free hand (FH). PH presents high levels of activity for Biceps brachii and the wrist extensors and flexors. By contrast, BP and FH are characterised by high solicitation of forearm pronation. The synergy analyses depict a high muscular and kinematic coordination. Whereas the muscle pattern is very close between the techniques, kinematic pattern...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354885"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354885"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354885; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354885]").text(description); $(".js-view-count[data-work-id=96354885]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354885; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354885']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354885, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354885]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354885,"title":"Raw data for: Biomechanical demands of percussive techniques in the context of early stone toolmaking","translated_title":"","metadata":{"abstract":"Recent discoveries in archaeology and palaeoanthropology highlight that stone stool knapping could have emerged first within the genera Australopithecus or Kenyanthropus rather than Homo. 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L'archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d'enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2ac0a1d641caa09b3c934c7db72cf881" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":98275615,"asset_id":96354846,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/98275615/download_file?st=MTczMzkwNDgxMSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354846"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354846"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354846; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354846]").text(description); $(".js-view-count[data-work-id=96354846]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354846; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354846']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354846, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "2ac0a1d641caa09b3c934c7db72cf881" } } $('.js-work-strip[data-work-id=96354846]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354846,"title":"The teeth of H. luzonensis: a diagnostic taxonomic element","translated_title":"","metadata":{"ai_title_tag":"Diagnostic Features of H. luzonensis Teeth","grobid_abstract":"HAL is a multidisciplinary open access archive for the deposit and dissemination of scientific research documents, whether they are published or not. 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The repository is the National Museum of the Philippines, Manila. &lt;i&gt;Homo luzonensis&lt;/i&gt; has been deposited in the ZooBank database (<a href="http://zoobank.org/" rel="nofollow">http://zoobank.org/</a>) with Life Science Identifier urn:lsid:zoobank. org:act: 4F743862-662F-4E6B-9812-8 A05533 C1347. &lt;b&gt;Paratypes.&lt;/b&gt; Recovered in 2007, 2011 and 2015 from the same excavation area and layer as the holotype: CCH1, a right third metatarsal 1; CCH2 and CCH5, two manual phalanges; CCH3 and CCH4, two pedal phalanges; CCH8, a left upper third or fourth premolar (P 3/4); and CCH9, a right M 3 (all specimens are housed at the National Museum of the Philippines, Manila). &lt;b&gt;Referred material.&lt;/b&gt; CCH7, a femoral shaft that belonged to a juvenile individual (housed at the National Museum of the Philippines, Manila). &lt;b&gt;Locality.&lt;/b&gt; The type locality is Callao Cave, in the Callao Limestone formation in the Peñablanca region of northern Luzon, the Philippines, at coordinates 17° 42′ 11.7″ N, 121° 49′ 25.5″ E. &lt;b&gt;Diagnosis.&lt;/b&gt; Postcanine maxillary teeth of small size that are mesiodistally compressed, with a premolar:molar crown size ratio that is high compared to other species in the genus &lt;i&gt;Homo&lt;/i&gt;. Upper premolars with two or three roots, a mesio-distally expanded lingual crown, strong buccal grooves, partial or continuous transverse crest, and an enameldentine junction (EDJ) shape that is distinct from that of &lt;i&gt;H. sapiens&lt;/i&gt;, &lt;i&gt;Homo neanderthalensis&lt;/i&gt; and Asian &lt;i&gt;Homo erectus&lt;/i&gt;. Very small upper molars, with a M 1 &amp;gt; M 2 &amp;gt; M 3 crown size pattern, a simplified occlusal morphology with reduced metacone and hypocone, no crenulation on the EDJ, and EDJ shape affinities with that of &lt;i&gt;H. sapiens&lt;/i&gt; and Asian &lt;i&gt;H. erectus&lt;/i&gt;. Intermediate manual phalanx (rays 2–4) that is long and narrow (u [...]</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354844"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354844"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354844; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354844]").text(description); $(".js-view-count[data-work-id=96354844]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354844; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354844']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354844, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354844]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354844,"title":"Homo luzonensis Détroit \u0026 Mijares \u0026 Corny \u0026 Daver \u0026 Zanolli \u0026 Dizon \u0026 Robles \u0026 Grün \u0026 Piper 2019, sp. nov","translated_title":"","metadata":{"abstract":"\u0026lt;i\u0026gt;Homo luzonensis\u0026lt;/i\u0026gt; sp. nov. \u0026lt;b\u0026gt;Etymology.\u0026lt;/b\u0026gt; The species name is derived from the island of Luzon, where the specimens were discovered. \u0026lt;b\u0026gt;Holotype.\u0026lt;/b\u0026gt; CCH6 (CCH6-a to CCH6-e), maxillary right postcanine dentition of a single individual discovered on 24 August 2011. The repository is the National Museum of the Philippines, Manila. \u0026lt;i\u0026gt;Homo luzonensis\u0026lt;/i\u0026gt; has been deposited in the ZooBank database (http://zoobank.org/) with Life Science Identifier urn:lsid:zoobank. org:act: 4F743862-662F-4E6B-9812-8 A05533 C1347. \u0026lt;b\u0026gt;Paratypes.\u0026lt;/b\u0026gt; Recovered in 2007, 2011 and 2015 from the same excavation area and layer as the holotype: CCH1, a right third metatarsal 1; CCH2 and CCH5, two manual phalanges; CCH3 and CCH4, two pedal phalanges; CCH8, a left upper third or fourth premolar (P 3/4); and CCH9, a right M 3 (all specimens are housed at the National Museum of the Philippines, Manila). \u0026lt;b\u0026gt;Referred material.\u0026lt;/b\u0026gt; CCH7, a femoral shaft that belonged to a juvenile individual (housed at the National Museum of the Philippines, Manila). \u0026lt;b\u0026gt;Locality.\u0026lt;/b\u0026gt; The type locality is Callao Cave, in the Callao Limestone formation in the Peñablanca region of northern Luzon, the Philippines, at coordinates 17° 42′ 11.7″ N, 121° 49′ 25.5″ E. \u0026lt;b\u0026gt;Diagnosis.\u0026lt;/b\u0026gt; Postcanine maxillary teeth of small size that are mesiodistally compressed, with a premolar:molar crown size ratio that is high compared to other species in the genus \u0026lt;i\u0026gt;Homo\u0026lt;/i\u0026gt;. Upper premolars with two or three roots, a mesio-distally expanded lingual crown, strong buccal grooves, partial or continuous transverse crest, and an enameldentine junction (EDJ) shape that is distinct from that of \u0026lt;i\u0026gt;H. sapiens\u0026lt;/i\u0026gt;, \u0026lt;i\u0026gt;Homo neanderthalensis\u0026lt;/i\u0026gt; and Asian \u0026lt;i\u0026gt;Homo erectus\u0026lt;/i\u0026gt;. Very small upper molars, with a M 1 \u0026amp;gt; M 2 \u0026amp;gt; M 3 crown size pattern, a simplified occlusal morphology with reduced metacone and hypocone, no crenulation on the EDJ, and EDJ shape affinities with that of \u0026lt;i\u0026gt;H. sapiens\u0026lt;/i\u0026gt; and Asian \u0026lt;i\u0026gt;H. erectus\u0026lt;/i\u0026gt;. Intermediate manual phalanx (rays 2–4) that is long and narrow (u [...]","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"\u0026lt;i\u0026gt;Homo luzonensis\u0026lt;/i\u0026gt; sp. nov. \u0026lt;b\u0026gt;Etymology.\u0026lt;/b\u0026gt; The species name is derived from the island of Luzon, where the specimens were discovered. \u0026lt;b\u0026gt;Holotype.\u0026lt;/b\u0026gt; CCH6 (CCH6-a to CCH6-e), maxillary right postcanine dentition of a single individual discovered on 24 August 2011. The repository is the National Museum of the Philippines, Manila. \u0026lt;i\u0026gt;Homo luzonensis\u0026lt;/i\u0026gt; has been deposited in the ZooBank database (http://zoobank.org/) with Life Science Identifier urn:lsid:zoobank. org:act: 4F743862-662F-4E6B-9812-8 A05533 C1347. \u0026lt;b\u0026gt;Paratypes.\u0026lt;/b\u0026gt; Recovered in 2007, 2011 and 2015 from the same excavation area and layer as the holotype: CCH1, a right third metatarsal 1; CCH2 and CCH5, two manual phalanges; CCH3 and CCH4, two pedal phalanges; CCH8, a left upper third or fourth premolar (P 3/4); and CCH9, a right M 3 (all specimens are housed at the National Museum of the Philippines, Manila). \u0026lt;b\u0026gt;Referred material.\u0026lt;/b\u0026gt; CCH7, a femoral shaft that belonged to a juvenile individual (housed at the National Museum of the Philippines, Manila). \u0026lt;b\u0026gt;Locality.\u0026lt;/b\u0026gt; The type locality is Callao Cave, in the Callao Limestone formation in the Peñablanca region of northern Luzon, the Philippines, at coordinates 17° 42′ 11.7″ N, 121° 49′ 25.5″ E. \u0026lt;b\u0026gt;Diagnosis.\u0026lt;/b\u0026gt; Postcanine maxillary teeth of small size that are mesiodistally compressed, with a premolar:molar crown size ratio that is high compared to other species in the genus \u0026lt;i\u0026gt;Homo\u0026lt;/i\u0026gt;. Upper premolars with two or three roots, a mesio-distally expanded lingual crown, strong buccal grooves, partial or continuous transverse crest, and an enameldentine junction (EDJ) shape that is distinct from that of \u0026lt;i\u0026gt;H. sapiens\u0026lt;/i\u0026gt;, \u0026lt;i\u0026gt;Homo neanderthalensis\u0026lt;/i\u0026gt; and Asian \u0026lt;i\u0026gt;Homo erectus\u0026lt;/i\u0026gt;. Very small upper molars, with a M 1 \u0026amp;gt; M 2 \u0026amp;gt; M 3 crown size pattern, a simplified occlusal morphology with reduced metacone and hypocone, no crenulation on the EDJ, and EDJ shape affinities with that of \u0026lt;i\u0026gt;H. sapiens\u0026lt;/i\u0026gt; and Asian \u0026lt;i\u0026gt;H. erectus\u0026lt;/i\u0026gt;. Intermediate manual phalanx (rays 2–4) that is long and narrow (u [...]","internal_url":"https://www.academia.edu/96354844/Homo_luzonensis_D%C3%A9troit_and_Mijares_and_Corny_and_Daver_and_Zanolli_and_Dizon_and_Robles_and_Gr%C3%BCn_and_Piper_2019_sp_nov","translated_internal_url":"","created_at":"2023-02-05T12:27:26.945-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Homo_luzonensis_Détroit_and_Mijares_and_Corny_and_Daver_and_Zanolli_and_Dizon_and_Robles_and_Grün_and_Piper_2019_sp_nov","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"\u0026lt;i\u0026gt;Homo luzonensis\u0026lt;/i\u0026gt; sp. nov. \u0026lt;b\u0026gt;Etymology.\u0026lt;/b\u0026gt; The species name is derived from the island of Luzon, where the specimens were discovered. \u0026lt;b\u0026gt;Holotype.\u0026lt;/b\u0026gt; CCH6 (CCH6-a to CCH6-e), maxillary right postcanine dentition of a single individual discovered on 24 August 2011. The repository is the National Museum of the Philippines, Manila. \u0026lt;i\u0026gt;Homo luzonensis\u0026lt;/i\u0026gt; has been deposited in the ZooBank database (http://zoobank.org/) with Life Science Identifier urn:lsid:zoobank. org:act: 4F743862-662F-4E6B-9812-8 A05533 C1347. \u0026lt;b\u0026gt;Paratypes.\u0026lt;/b\u0026gt; Recovered in 2007, 2011 and 2015 from the same excavation area and layer as the holotype: CCH1, a right third metatarsal 1; CCH2 and CCH5, two manual phalanges; CCH3 and CCH4, two pedal phalanges; CCH8, a left upper third or fourth premolar (P 3/4); and CCH9, a right M 3 (all specimens are housed at the National Museum of the Philippines, Manila). \u0026lt;b\u0026gt;Referred material.\u0026lt;/b\u0026gt; CCH7, a femoral shaft that belonged to a juvenile individual (housed at the National Museum of the Philippines, Manila). \u0026lt;b\u0026gt;Locality.\u0026lt;/b\u0026gt; The type locality is Callao Cave, in the Callao Limestone formation in the Peñablanca region of northern Luzon, the Philippines, at coordinates 17° 42′ 11.7″ N, 121° 49′ 25.5″ E. \u0026lt;b\u0026gt;Diagnosis.\u0026lt;/b\u0026gt; Postcanine maxillary teeth of small size that are mesiodistally compressed, with a premolar:molar crown size ratio that is high compared to other species in the genus \u0026lt;i\u0026gt;Homo\u0026lt;/i\u0026gt;. Upper premolars with two or three roots, a mesio-distally expanded lingual crown, strong buccal grooves, partial or continuous transverse crest, and an enameldentine junction (EDJ) shape that is distinct from that of \u0026lt;i\u0026gt;H. sapiens\u0026lt;/i\u0026gt;, \u0026lt;i\u0026gt;Homo neanderthalensis\u0026lt;/i\u0026gt; and Asian \u0026lt;i\u0026gt;Homo erectus\u0026lt;/i\u0026gt;. Very small upper molars, with a M 1 \u0026amp;gt; M 2 \u0026amp;gt; M 3 crown size pattern, a simplified occlusal morphology with reduced metacone and hypocone, no crenulation on the EDJ, and EDJ shape affinities with that of \u0026lt;i\u0026gt;H. sapiens\u0026lt;/i\u0026gt; and Asian \u0026lt;i\u0026gt;H. erectus\u0026lt;/i\u0026gt;. Intermediate manual phalanx (rays 2–4) that is long and narrow (u [...]","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354843"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354843/Extended_Data_Fig_10_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Extended Data Fig. 10 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354843/Extended_Data_Fig_10_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Extended Data Fig. 10 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Extended Data Fig. 10 | CCH7, femoral shaft of a juvenile individual of H. luzonensis. a, Photogr...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Extended Data Fig. 10 | CCH7, femoral shaft of a juvenile individual of H. luzonensis. a, Photograph of the original specimen CCH7 (posterior aspect). b, Three-dimensional rendering of CCH7. From left to right: anterior, medial, posterior and lateral aspects. Scale bar, 20 mm. c, Transverse micro-CT slices of CCH7 at proximal diaphysis (top), midshaft (middle) and distal diaphysis (bottom), and posterior aspect of the three-dimensional rendering of the femoral shaft, during the segmentation process (orientation of slices: anterior is up, posterior is down, lateral is left, medial is right).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354843"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354843"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354843; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354843]").text(description); $(".js-view-count[data-work-id=96354843]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354843; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354843']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354843, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354843]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354843,"title":"Extended Data Fig. 10 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Extended Data Fig. 10 | CCH7, femoral shaft of a juvenile individual of H. luzonensis. a, Photograph of the original specimen CCH7 (posterior aspect). b, Three-dimensional rendering of CCH7. From left to right: anterior, medial, posterior and lateral aspects. Scale bar, 20 mm. c, Transverse micro-CT slices of CCH7 at proximal diaphysis (top), midshaft (middle) and distal diaphysis (bottom), and posterior aspect of the three-dimensional rendering of the femoral shaft, during the segmentation process (orientation of slices: anterior is up, posterior is down, lateral is left, medial is right).","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Extended Data Fig. 10 | CCH7, femoral shaft of a juvenile individual of H. luzonensis. a, Photograph of the original specimen CCH7 (posterior aspect). b, Three-dimensional rendering of CCH7. From left to right: anterior, medial, posterior and lateral aspects. Scale bar, 20 mm. c, Transverse micro-CT slices of CCH7 at proximal diaphysis (top), midshaft (middle) and distal diaphysis (bottom), and posterior aspect of the three-dimensional rendering of the femoral shaft, during the segmentation process (orientation of slices: anterior is up, posterior is down, lateral is left, medial is right).","internal_url":"https://www.academia.edu/96354843/Extended_Data_Fig_10_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:26.811-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Extended_Data_Fig_10_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Extended Data Fig. 10 | CCH7, femoral shaft of a juvenile individual of H. luzonensis. a, Photograph of the original specimen CCH7 (posterior aspect). b, Three-dimensional rendering of CCH7. From left to right: anterior, medial, posterior and lateral aspects. Scale bar, 20 mm. c, Transverse micro-CT slices of CCH7 at proximal diaphysis (top), midshaft (middle) and distal diaphysis (bottom), and posterior aspect of the three-dimensional rendering of the femoral shaft, during the segmentation process (orientation of slices: anterior is up, posterior is down, lateral is left, medial is right).","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354842"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354842/Extended_Data_Fig_9_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Extended Data Fig. 9 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354842/Extended_Data_Fig_9_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Extended Data Fig. 9 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Extended Data Fig. 9 | CCH3, intermediate pedal phalanx of H. luzonensis. a, Photograph of the or...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Extended Data Fig. 9 | CCH3, intermediate pedal phalanx of H. luzonensis. a, Photograph of the original specimen CCH3 in plantar view. b, Three-dimensional rendering of CCH3. From left to right: plantar, medial, dorsal, lateral, distal (top), proximal (bottom), disto-medial and proximo-medial aspects. c, Comparison of CCH3 with Pliocene (A.L.333- 21a, unknown side and rays 2–5, and A.L.333-115k, fourth intermediate phalanx), Upper Pleistocene (LB1/56, LB1-15 and LB1/39: unknown side and rays 2–5) and recent (PAPO-74-150) intermediate pedal phalanges in plantar (top) and side (bottom) views. Note the variation in shape and size both between taxa (for example, H. sapiens and H. floresiensis) and in the same individual (for example, LB1 and PAPO-74-150). A detailed list of specimens can be found in Supplementary Table 12. Scale bars, 10 mm.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354842"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354842"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354842; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354842]").text(description); $(".js-view-count[data-work-id=96354842]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354842; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354842']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354842, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354842]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354842,"title":"Extended Data Fig. 9 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Extended Data Fig. 9 | CCH3, intermediate pedal phalanx of H. luzonensis. a, Photograph of the original specimen CCH3 in plantar view. b, Three-dimensional rendering of CCH3. From left to right: plantar, medial, dorsal, lateral, distal (top), proximal (bottom), disto-medial and proximo-medial aspects. c, Comparison of CCH3 with Pliocene (A.L.333- 21a, unknown side and rays 2–5, and A.L.333-115k, fourth intermediate phalanx), Upper Pleistocene (LB1/56, LB1-15 and LB1/39: unknown side and rays 2–5) and recent (PAPO-74-150) intermediate pedal phalanges in plantar (top) and side (bottom) views. Note the variation in shape and size both between taxa (for example, H. sapiens and H. floresiensis) and in the same individual (for example, LB1 and PAPO-74-150). A detailed list of specimens can be found in Supplementary Table 12. Scale bars, 10 mm.","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Extended Data Fig. 9 | CCH3, intermediate pedal phalanx of H. luzonensis. a, Photograph of the original specimen CCH3 in plantar view. b, Three-dimensional rendering of CCH3. From left to right: plantar, medial, dorsal, lateral, distal (top), proximal (bottom), disto-medial and proximo-medial aspects. c, Comparison of CCH3 with Pliocene (A.L.333- 21a, unknown side and rays 2–5, and A.L.333-115k, fourth intermediate phalanx), Upper Pleistocene (LB1/56, LB1-15 and LB1/39: unknown side and rays 2–5) and recent (PAPO-74-150) intermediate pedal phalanges in plantar (top) and side (bottom) views. Note the variation in shape and size both between taxa (for example, H. sapiens and H. floresiensis) and in the same individual (for example, LB1 and PAPO-74-150). A detailed list of specimens can be found in Supplementary Table 12. Scale bars, 10 mm.","internal_url":"https://www.academia.edu/96354842/Extended_Data_Fig_9_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:26.672-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Extended_Data_Fig_9_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Extended Data Fig. 9 | CCH3, intermediate pedal phalanx of H. luzonensis. a, Photograph of the original specimen CCH3 in plantar view. b, Three-dimensional rendering of CCH3. From left to right: plantar, medial, dorsal, lateral, distal (top), proximal (bottom), disto-medial and proximo-medial aspects. c, Comparison of CCH3 with Pliocene (A.L.333- 21a, unknown side and rays 2–5, and A.L.333-115k, fourth intermediate phalanx), Upper Pleistocene (LB1/56, LB1-15 and LB1/39: unknown side and rays 2–5) and recent (PAPO-74-150) intermediate pedal phalanges in plantar (top) and side (bottom) views. Note the variation in shape and size both between taxa (for example, H. sapiens and H. floresiensis) and in the same individual (for example, LB1 and PAPO-74-150). A detailed list of specimens can be found in Supplementary Table 12. Scale bars, 10 mm.","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354841"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354841/Extended_Data_Fig_6_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Extended Data Fig. 6 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354841/Extended_Data_Fig_6_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Extended Data Fig. 6 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Extended Data Fig. 6 | Procrustes analyses of the intermediate manual phalanx of H. luzonensis. C...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Extended Data Fig. 6 | Procrustes analyses of the intermediate manual phalanx of H. luzonensis. CCH2 compared to specimens attributed to Australopithecus (A. afarensis, n = 1; A. africanus, n = 1; A. sediba, n = 2), Paranthropus/early Homo (Swartkrans, Member 1, n = 3; Member 3, n = 2), H. naledi (Hand 1, n = 2), H. floresiensis (LB1/48 and LB6/9) and recent H. sapiens separated into 3 samples corresponding to ray number (n = 15, 21 and 19 for rays 2, 3 and 4, respectively). A detailed list of specimens can be found in Supplementary Table 9. a–c, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 3 only): scatter plot of individual scores for bgPC1 versus bgPC2 (a); scatter plot of individual scores for bgPC2 versus bgPC3 (b); shape variation associated with bgPC1, bgPC2 and bgPC3 (c). d, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 4 only): scatter plot of individual scores for bgPC1 versus bgPC2....</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354841"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354841"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354841; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354841]").text(description); $(".js-view-count[data-work-id=96354841]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354841; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354841']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354841, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354841]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354841,"title":"Extended Data Fig. 6 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Extended Data Fig. 6 | Procrustes analyses of the intermediate manual phalanx of H. luzonensis. CCH2 compared to specimens attributed to Australopithecus (A. afarensis, n = 1; A. africanus, n = 1; A. sediba, n = 2), Paranthropus/early Homo (Swartkrans, Member 1, n = 3; Member 3, n = 2), H. naledi (Hand 1, n = 2), H. floresiensis (LB1/48 and LB6/9) and recent H. sapiens separated into 3 samples corresponding to ray number (n = 15, 21 and 19 for rays 2, 3 and 4, respectively). A detailed list of specimens can be found in Supplementary Table 9. a–c, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 3 only): scatter plot of individual scores for bgPC1 versus bgPC2 (a); scatter plot of individual scores for bgPC2 versus bgPC3 (b); shape variation associated with bgPC1, bgPC2 and bgPC3 (c). d, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 4 only): scatter plot of individual scores for bgPC1 versus bgPC2....","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Extended Data Fig. 6 | Procrustes analyses of the intermediate manual phalanx of H. luzonensis. CCH2 compared to specimens attributed to Australopithecus (A. afarensis, n = 1; A. africanus, n = 1; A. sediba, n = 2), Paranthropus/early Homo (Swartkrans, Member 1, n = 3; Member 3, n = 2), H. naledi (Hand 1, n = 2), H. floresiensis (LB1/48 and LB6/9) and recent H. sapiens separated into 3 samples corresponding to ray number (n = 15, 21 and 19 for rays 2, 3 and 4, respectively). A detailed list of specimens can be found in Supplementary Table 9. a–c, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 3 only): scatter plot of individual scores for bgPC1 versus bgPC2 (a); scatter plot of individual scores for bgPC2 versus bgPC3 (b); shape variation associated with bgPC1, bgPC2 and bgPC3 (c). d, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 4 only): scatter plot of individual scores for bgPC1 versus bgPC2....","internal_url":"https://www.academia.edu/96354841/Extended_Data_Fig_6_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:26.536-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Extended_Data_Fig_6_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Extended Data Fig. 6 | Procrustes analyses of the intermediate manual phalanx of H. luzonensis. CCH2 compared to specimens attributed to Australopithecus (A. afarensis, n = 1; A. africanus, n = 1; A. sediba, n = 2), Paranthropus/early Homo (Swartkrans, Member 1, n = 3; Member 3, n = 2), H. naledi (Hand 1, n = 2), H. floresiensis (LB1/48 and LB6/9) and recent H. sapiens separated into 3 samples corresponding to ray number (n = 15, 21 and 19 for rays 2, 3 and 4, respectively). A detailed list of specimens can be found in Supplementary Table 9. a–c, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 3 only): scatter plot of individual scores for bgPC1 versus bgPC2 (a); scatter plot of individual scores for bgPC2 versus bgPC3 (b); shape variation associated with bgPC1, bgPC2 and bgPC3 (c). d, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 4 only): scatter plot of individual scores for bgPC1 versus bgPC2....","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354840"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354840/Extended_Data_Fig_3_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Extended Data Fig. 3 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354840/Extended_Data_Fig_3_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Extended Data Fig. 3 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Extended Data Fig. 3 | Elliptic Fourier analysis of M1 crown contour. CCH6-c compared to the holo...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Extended Data Fig. 3 | Elliptic Fourier analysis of M1 crown contour. CCH6-c compared to the holotype of H. floresiensis (LB1) and large samples of archaeological and recent H. sapiens individuals. a, PCA of shape data for all specimens, scatter plot of individual scores for PC1 versus PC2 (see Methods; elliptic Fourier descriptors applied to Procrustes-aligned outlines, ten harmonics included). LGM, Last Glacial Maximum. Sample sizes: H. luzonensis, n = 1; H. floresiensis, n = 2; pre- LGM, n = 2; pre-Neolithic post-LGM, n = 12; Neolithic/post-Neolithic, n = 232; recent &#39;Negritos&#39;, n = 19. A detailed list of specimens can be found in Supplementary Table 5. b, Bar plot of eigenvalues (%) of PC1–PC6. c, Extreme shape variations along PC1 and PC2. The scores of H. luzonensis M1 along PC1 and PC2 reflects a crown outline shape that is mesio-distally compressed, but not as much as that of H. floresiensis (two versions of the LB1 right M 1). d, Right M 1 of the holotype of H. flor...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354840"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354840"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354840; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354840]").text(description); $(".js-view-count[data-work-id=96354840]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354840; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354840']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354840, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354840]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354840,"title":"Extended Data Fig. 3 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Extended Data Fig. 3 | Elliptic Fourier analysis of M1 crown contour. CCH6-c compared to the holotype of H. floresiensis (LB1) and large samples of archaeological and recent H. sapiens individuals. a, PCA of shape data for all specimens, scatter plot of individual scores for PC1 versus PC2 (see Methods; elliptic Fourier descriptors applied to Procrustes-aligned outlines, ten harmonics included). LGM, Last Glacial Maximum. Sample sizes: H. luzonensis, n = 1; H. floresiensis, n = 2; pre- LGM, n = 2; pre-Neolithic post-LGM, n = 12; Neolithic/post-Neolithic, n = 232; recent \u0026#39;Negritos\u0026#39;, n = 19. A detailed list of specimens can be found in Supplementary Table 5. b, Bar plot of eigenvalues (%) of PC1–PC6. c, Extreme shape variations along PC1 and PC2. The scores of H. luzonensis M1 along PC1 and PC2 reflects a crown outline shape that is mesio-distally compressed, but not as much as that of H. floresiensis (two versions of the LB1 right M 1). d, Right M 1 of the holotype of H. flor...","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Extended Data Fig. 3 | Elliptic Fourier analysis of M1 crown contour. CCH6-c compared to the holotype of H. floresiensis (LB1) and large samples of archaeological and recent H. sapiens individuals. a, PCA of shape data for all specimens, scatter plot of individual scores for PC1 versus PC2 (see Methods; elliptic Fourier descriptors applied to Procrustes-aligned outlines, ten harmonics included). LGM, Last Glacial Maximum. Sample sizes: H. luzonensis, n = 1; H. floresiensis, n = 2; pre- LGM, n = 2; pre-Neolithic post-LGM, n = 12; Neolithic/post-Neolithic, n = 232; recent \u0026#39;Negritos\u0026#39;, n = 19. A detailed list of specimens can be found in Supplementary Table 5. b, Bar plot of eigenvalues (%) of PC1–PC6. c, Extreme shape variations along PC1 and PC2. The scores of H. luzonensis M1 along PC1 and PC2 reflects a crown outline shape that is mesio-distally compressed, but not as much as that of H. floresiensis (two versions of the LB1 right M 1). d, Right M 1 of the holotype of H. flor...","internal_url":"https://www.academia.edu/96354840/Extended_Data_Fig_3_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:26.395-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Extended_Data_Fig_3_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Extended Data Fig. 3 | Elliptic Fourier analysis of M1 crown contour. CCH6-c compared to the holotype of H. floresiensis (LB1) and large samples of archaeological and recent H. sapiens individuals. a, PCA of shape data for all specimens, scatter plot of individual scores for PC1 versus PC2 (see Methods; elliptic Fourier descriptors applied to Procrustes-aligned outlines, ten harmonics included). LGM, Last Glacial Maximum. Sample sizes: H. luzonensis, n = 1; H. floresiensis, n = 2; pre- LGM, n = 2; pre-Neolithic post-LGM, n = 12; Neolithic/post-Neolithic, n = 232; recent \u0026#39;Negritos\u0026#39;, n = 19. A detailed list of specimens can be found in Supplementary Table 5. b, Bar plot of eigenvalues (%) of PC1–PC6. c, Extreme shape variations along PC1 and PC2. The scores of H. luzonensis M1 along PC1 and PC2 reflects a crown outline shape that is mesio-distally compressed, but not as much as that of H. floresiensis (two versions of the LB1 right M 1). d, Right M 1 of the holotype of H. flor...","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354839"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354839/Extended_Data_Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Extended Data Fig. 1 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354839/Extended_Data_Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Extended Data Fig. 1 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Extended Data Fig. 1 | Inventory of the fossil elements attributed to H. luzonensis and detailed ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Extended Data Fig. 1 | Inventory of the fossil elements attributed to H. luzonensis and detailed views of the dental remains. a, The hominin fossils recovered from Callao Cave. R, right; L, left; P, premolar; M, molar. b, Three-dimensional rendering of the postcanine maxillary teeth CCH6-b to CCH6-e (M 2 –P 3): occlusal (top row) and buccal (bottom row) aspects. Enamel is shown in dark blue, dentine and cement in light brown and pulp cavity in dark grey. In all views, mesial is to the right, distal to the left. c, CCH6-a, right M 3: occlusal, buccal, lingual, mesial and distal aspects (from top to bottom and left to right). Occlusal view: mesial is to the right, distal to the left. d, CCH6-a to CCH6-e, right M 3 –P 3: photograph of occlusal aspect. Mesial is to the right, distal to the left. The numbers indicate the locations of the detailed views of the inter-proximal contact facets (IPCFs): P 3 (CCH6-e), mesial IPCF 1: note the small size of this IPCF, indicating that the canine w...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354839"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354839"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354839; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354839]").text(description); $(".js-view-count[data-work-id=96354839]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354839; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354839']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354839, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354839]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354839,"title":"Extended Data Fig. 1 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Extended Data Fig. 1 | Inventory of the fossil elements attributed to H. luzonensis and detailed views of the dental remains. a, The hominin fossils recovered from Callao Cave. R, right; L, left; P, premolar; M, molar. b, Three-dimensional rendering of the postcanine maxillary teeth CCH6-b to CCH6-e (M 2 –P 3): occlusal (top row) and buccal (bottom row) aspects. Enamel is shown in dark blue, dentine and cement in light brown and pulp cavity in dark grey. In all views, mesial is to the right, distal to the left. c, CCH6-a, right M 3: occlusal, buccal, lingual, mesial and distal aspects (from top to bottom and left to right). Occlusal view: mesial is to the right, distal to the left. d, CCH6-a to CCH6-e, right M 3 –P 3: photograph of occlusal aspect. Mesial is to the right, distal to the left. The numbers indicate the locations of the detailed views of the inter-proximal contact facets (IPCFs): P 3 (CCH6-e), mesial IPCF 1: note the small size of this IPCF, indicating that the canine w...","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Extended Data Fig. 1 | Inventory of the fossil elements attributed to H. luzonensis and detailed views of the dental remains. a, The hominin fossils recovered from Callao Cave. R, right; L, left; P, premolar; M, molar. b, Three-dimensional rendering of the postcanine maxillary teeth CCH6-b to CCH6-e (M 2 –P 3): occlusal (top row) and buccal (bottom row) aspects. Enamel is shown in dark blue, dentine and cement in light brown and pulp cavity in dark grey. In all views, mesial is to the right, distal to the left. c, CCH6-a, right M 3: occlusal, buccal, lingual, mesial and distal aspects (from top to bottom and left to right). Occlusal view: mesial is to the right, distal to the left. d, CCH6-a to CCH6-e, right M 3 –P 3: photograph of occlusal aspect. Mesial is to the right, distal to the left. The numbers indicate the locations of the detailed views of the inter-proximal contact facets (IPCFs): P 3 (CCH6-e), mesial IPCF 1: note the small size of this IPCF, indicating that the canine w...","internal_url":"https://www.academia.edu/96354839/Extended_Data_Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:25.851-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Extended_Data_Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Extended Data Fig. 1 | Inventory of the fossil elements attributed to H. luzonensis and detailed views of the dental remains. a, The hominin fossils recovered from Callao Cave. R, right; L, left; P, premolar; M, molar. b, Three-dimensional rendering of the postcanine maxillary teeth CCH6-b to CCH6-e (M 2 –P 3): occlusal (top row) and buccal (bottom row) aspects. Enamel is shown in dark blue, dentine and cement in light brown and pulp cavity in dark grey. In all views, mesial is to the right, distal to the left. c, CCH6-a, right M 3: occlusal, buccal, lingual, mesial and distal aspects (from top to bottom and left to right). Occlusal view: mesial is to the right, distal to the left. d, CCH6-a to CCH6-e, right M 3 –P 3: photograph of occlusal aspect. Mesial is to the right, distal to the left. The numbers indicate the locations of the detailed views of the inter-proximal contact facets (IPCFs): P 3 (CCH6-e), mesial IPCF 1: note the small size of this IPCF, indicating that the canine w...","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354838"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354838/Fig_4_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Fig. 4 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354838/Fig_4_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Fig. 4 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Fig. 4 | Premolar EDJ of H. luzonensis. a, EDJ of the P 3 of H. luzonensis (CCH6-e) compared to t...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Fig. 4 | Premolar EDJ of H. luzonensis. a, EDJ of the P 3 of H. luzonensis (CCH6-e) compared to the EDJs of H. floresiensis (Liang Bua 1 (LB1)), H. sapiens, H. erectus (Sangiran 4) and H. neanderthalensis (KRD 53). Horns of dentine were reconstructed for CCH6-e, LB1 and Sangiran 4; see Methods. Scale bar, 5 mm. b, c, Between-group principal component analyses (bgPCAs) of the three-dimensional landmark Procrustes- registered shape coordinates of the P 3 s (b) and P 4 s (c). Sample sizes for b, c, respectively: H. erectus, n = 2, 3; H. neanderthalensis, n = 5, 6; fossil H. sapiens, n = 3, 3; extant H. sapiens, n = 8, 9; H. floresiensis, n = 1, 0; H. luzonensis, n = 2, 2. A detailed list of specimens can be found in Supplementary Table 6</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354838"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354838"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354838; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354838]").text(description); $(".js-view-count[data-work-id=96354838]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354838; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354838']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354838, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354838]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354838,"title":"Fig. 4 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Fig. 4 | Premolar EDJ of H. luzonensis. a, EDJ of the P 3 of H. luzonensis (CCH6-e) compared to the EDJs of H. floresiensis (Liang Bua 1 (LB1)), H. sapiens, H. erectus (Sangiran 4) and H. neanderthalensis (KRD 53). Horns of dentine were reconstructed for CCH6-e, LB1 and Sangiran 4; see Methods. Scale bar, 5 mm. b, c, Between-group principal component analyses (bgPCAs) of the three-dimensional landmark Procrustes- registered shape coordinates of the P 3 s (b) and P 4 s (c). Sample sizes for b, c, respectively: H. erectus, n = 2, 3; H. neanderthalensis, n = 5, 6; fossil H. sapiens, n = 3, 3; extant H. sapiens, n = 8, 9; H. floresiensis, n = 1, 0; H. luzonensis, n = 2, 2. A detailed list of specimens can be found in Supplementary Table 6","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Fig. 4 | Premolar EDJ of H. luzonensis. a, EDJ of the P 3 of H. luzonensis (CCH6-e) compared to the EDJs of H. floresiensis (Liang Bua 1 (LB1)), H. sapiens, H. erectus (Sangiran 4) and H. neanderthalensis (KRD 53). Horns of dentine were reconstructed for CCH6-e, LB1 and Sangiran 4; see Methods. Scale bar, 5 mm. b, c, Between-group principal component analyses (bgPCAs) of the three-dimensional landmark Procrustes- registered shape coordinates of the P 3 s (b) and P 4 s (c). Sample sizes for b, c, respectively: H. erectus, n = 2, 3; H. neanderthalensis, n = 5, 6; fossil H. sapiens, n = 3, 3; extant H. sapiens, n = 8, 9; H. floresiensis, n = 1, 0; H. luzonensis, n = 2, 2. A detailed list of specimens can be found in Supplementary Table 6","internal_url":"https://www.academia.edu/96354838/Fig_4_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:25.700-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Fig_4_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Fig. 4 | Premolar EDJ of H. luzonensis. a, EDJ of the P 3 of H. luzonensis (CCH6-e) compared to the EDJs of H. floresiensis (Liang Bua 1 (LB1)), H. sapiens, H. erectus (Sangiran 4) and H. neanderthalensis (KRD 53). Horns of dentine were reconstructed for CCH6-e, LB1 and Sangiran 4; see Methods. Scale bar, 5 mm. b, c, Between-group principal component analyses (bgPCAs) of the three-dimensional landmark Procrustes- registered shape coordinates of the P 3 s (b) and P 4 s (c). Sample sizes for b, c, respectively: H. erectus, n = 2, 3; H. neanderthalensis, n = 5, 6; fossil H. sapiens, n = 3, 3; extant H. sapiens, n = 8, 9; H. floresiensis, n = 1, 0; H. luzonensis, n = 2, 2. A detailed list of specimens can be found in Supplementary Table 6","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354837"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354837/Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Fig. 1 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354837/Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Fig. 1 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Fig. 1 | Geographical location of Callao Cave. Map showing the location of Callao Cave on Luzon I...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Fig. 1 | Geographical location of Callao Cave. Map showing the location of Callao Cave on Luzon Island (the Philippines), emerged lands at 50 and 120 m below present sea level (adapted from ref. 46, H. K. Voris, Field Museum of Natural History) and the major biogeographical boundaries recognized in the area. A, Wallace&#39;s Line modified by Huxley; B, Wallace&#39;s Line; C, Lydekker&#39;s Line. Luzon Island lies in between the original Wallace&#39;s Line and the Wallace&#39;s Line modified by Huxley and was never connected to mainland Asia during the Quaternary.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354837"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354837"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354837; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354837]").text(description); $(".js-view-count[data-work-id=96354837]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354837; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354837']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354837, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354837]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354837,"title":"Fig. 1 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Fig. 1 | Geographical location of Callao Cave. Map showing the location of Callao Cave on Luzon Island (the Philippines), emerged lands at 50 and 120 m below present sea level (adapted from ref. 46, H. K. Voris, Field Museum of Natural History) and the major biogeographical boundaries recognized in the area. A, Wallace\u0026#39;s Line modified by Huxley; B, Wallace\u0026#39;s Line; C, Lydekker\u0026#39;s Line. Luzon Island lies in between the original Wallace\u0026#39;s Line and the Wallace\u0026#39;s Line modified by Huxley and was never connected to mainland Asia during the Quaternary.","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Fig. 1 | Geographical location of Callao Cave. Map showing the location of Callao Cave on Luzon Island (the Philippines), emerged lands at 50 and 120 m below present sea level (adapted from ref. 46, H. K. Voris, Field Museum of Natural History) and the major biogeographical boundaries recognized in the area. A, Wallace\u0026#39;s Line modified by Huxley; B, Wallace\u0026#39;s Line; C, Lydekker\u0026#39;s Line. Luzon Island lies in between the original Wallace\u0026#39;s Line and the Wallace\u0026#39;s Line modified by Huxley and was never connected to mainland Asia during the Quaternary.","internal_url":"https://www.academia.edu/96354837/Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:25.567-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Fig. 1 | Geographical location of Callao Cave. Map showing the location of Callao Cave on Luzon Island (the Philippines), emerged lands at 50 and 120 m below present sea level (adapted from ref. 46, H. K. Voris, Field Museum of Natural History) and the major biogeographical boundaries recognized in the area. A, Wallace\u0026#39;s Line modified by Huxley; B, Wallace\u0026#39;s Line; C, Lydekker\u0026#39;s Line. Luzon Island lies in between the original Wallace\u0026#39;s Line and the Wallace\u0026#39;s Line modified by Huxley and was never connected to mainland Asia during the Quaternary.","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354836"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354836/Rhinocerotidae_and_Chalicotheriidae_Perissodactyla_Tapiromorpha_"><img alt="Research paper thumbnail of Rhinocerotidae and Chalicotheriidae (Perissodactyla, Tapiromorpha)" class="work-thumbnail" src="https://attachments.academia-assets.com/98275637/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354836/Rhinocerotidae_and_Chalicotheriidae_Perissodactyla_Tapiromorpha_">Rhinocerotidae and Chalicotheriidae (Perissodactyla, Tapiromorpha)</a></div><div class="wp-workCard_item"><span>Geodiversitas</span><span>, 2016</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Here we describe mandibular, dental, and postcranial remains referable to Rhinocerotidae and Chal...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Here we describe mandibular, dental, and postcranial remains referable to Rhinocerotidae and Chalicotheriidae (Perissodactyla) originating from the vertebrate localities of Küçükçekmece East and Küçükçekmece West, in Thrace (European Turkey). The four rhinocerotids recognized comprise the early diverging Ronzotherium sp. (one lower molar, reworked from Oligocene deposits; Küçükçekmece West), the two-horned rhinocerotine Ceratotherium neumayri (Osborn, 1900), and two small chilothere aceratheriines: Chilotherium schlosseri (Weber, 1905) and Persiatherium sp. A chalicotheriine chalicotheriid, Kalimantsia sp., is documented by two tooth fragments and an unfused second phalanx of undoubtful affinities in Küçükçekmece West. This occurrence substantiates the record of Kalimantsia, previously restricted to the type locality Kalimantsi-Pehsata, in SW Bulgaria, and allows notably for the first recognition of postcranial remains for this taxon. Although distinct in terms of taxonomic composition and relative abundance, the rhinocerotid assemblages of Küçükçekmece East and Küçükçekmece West are in total agreement with a single biostratigraphical age, estimated to be correlated with the late Vallesian MN10 zone.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="753bbba57989829a16ef6c80e9788fd7" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":98275637,"asset_id":96354836,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/98275637/download_file?st=MTczMzkwNDgxMiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354836"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354836"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354836; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354836]").text(description); $(".js-view-count[data-work-id=96354836]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354836; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354836']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354836, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "753bbba57989829a16ef6c80e9788fd7" } } $('.js-work-strip[data-work-id=96354836]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354836,"title":"Rhinocerotidae and Chalicotheriidae (Perissodactyla, Tapiromorpha)","translated_title":"","metadata":{"publisher":"Museum National d'Histoire Naturelle, Paris, France","ai_title_tag":"Fossil Remains of Rhinocerotidae and Chalicotheriidae in Turkey","grobid_abstract":"Here we describe mandibular, dental, and postcranial remains referable to Rhinocerotidae and Chalicotheriidae (Perissodactyla) originating from the vertebrate localities of Küçükçekmece East and Küçükçekmece West, in Thrace (European Turkey). The four rhinocerotids recognized comprise the early diverging Ronzotherium sp. (one lower molar, reworked from Oligocene deposits; Küçükçekmece West), the two-horned rhinocerotine Ceratotherium neumayri (Osborn, 1900), and two small chilothere aceratheriines: Chilotherium schlosseri (Weber, 1905) and Persiatherium sp. A chalicotheriine chalicotheriid, Kalimantsia sp., is documented by two tooth fragments and an unfused second phalanx of undoubtful affinities in Küçükçekmece West. This occurrence substantiates the record of Kalimantsia, previously restricted to the type locality Kalimantsi-Pehsata, in SW Bulgaria, and allows notably for the first recognition of postcranial remains for this taxon. Although distinct in terms of taxonomic composition and relative abundance, the rhinocerotid assemblages of Küçükçekmece East and Küçükçekmece West are in total agreement with a single biostratigraphical age, estimated to be correlated with the late Vallesian MN10 zone.","publication_date":{"day":null,"month":null,"year":2016,"errors":{}},"publication_name":"Geodiversitas","grobid_abstract_attachment_id":98275637},"translated_abstract":null,"internal_url":"https://www.academia.edu/96354836/Rhinocerotidae_and_Chalicotheriidae_Perissodactyla_Tapiromorpha_","translated_internal_url":"","created_at":"2023-02-05T12:27:25.409-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":98275637,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/98275637/thumbnails/1.jpg","file_name":"Antoine_20__20Sen_202016_20Geodiversitas.pdf","download_url":"https://www.academia.edu/attachments/98275637/download_file?st=MTczMzkwNDgxMiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Rhinocerotidae_and_Chalicotheriidae_Peri.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/98275637/Antoine_20__20Sen_202016_20Geodiversitas-libre.pdf?1675630162=\u0026response-content-disposition=attachment%3B+filename%3DRhinocerotidae_and_Chalicotheriidae_Peri.pdf\u0026Expires=1733908412\u0026Signature=gAoNcvnw9RitYg--2Fv4~hxpRt5xhvnrIs01xcHQ4avHeqw9oFB7Jdb2oP67WN6WMIGBFu0MuaO2RSFPR2H2j1gBSv58Htpx-FIb4wsom1H2vkT6wEZ8k0cYeIylZAQ92EO8OTN2KE34icLJN50Xh6UbaRyiRgtgUpTk5vYmy3Ki8EKLaPezJ1F5BpzAyejGkp9vhF-18b0a-Ugyrw7Srzu~846RKqY9opnBwKByVl6Twou0QTviYa8AnRzr~VgsfSm2YDJwpqS6Ec9DSxZgiZYIgr-8mYps7lg8MFX-TLj2cZNc0EY~f6sSnOJLJeVfPvZscH7rPADa3EOqA543sA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Rhinocerotidae_and_Chalicotheriidae_Perissodactyla_Tapiromorpha_","translated_slug":"","page_count":16,"language":"en","content_type":"Work","summary":"Here we describe mandibular, dental, and postcranial remains referable to Rhinocerotidae and Chalicotheriidae (Perissodactyla) originating from the vertebrate localities of Küçükçekmece East and Küçükçekmece West, in Thrace (European Turkey). The four rhinocerotids recognized comprise the early diverging Ronzotherium sp. (one lower molar, reworked from Oligocene deposits; Küçükçekmece West), the two-horned rhinocerotine Ceratotherium neumayri (Osborn, 1900), and two small chilothere aceratheriines: Chilotherium schlosseri (Weber, 1905) and Persiatherium sp. A chalicotheriine chalicotheriid, Kalimantsia sp., is documented by two tooth fragments and an unfused second phalanx of undoubtful affinities in Küçükçekmece West. This occurrence substantiates the record of Kalimantsia, previously restricted to the type locality Kalimantsi-Pehsata, in SW Bulgaria, and allows notably for the first recognition of postcranial remains for this taxon. Although distinct in terms of taxonomic composition and relative abundance, the rhinocerotid assemblages of Küçükçekmece East and Küçükçekmece West are in total agreement with a single biostratigraphical age, estimated to be correlated with the late Vallesian MN10 zone.","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[{"id":98275637,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/98275637/thumbnails/1.jpg","file_name":"Antoine_20__20Sen_202016_20Geodiversitas.pdf","download_url":"https://www.academia.edu/attachments/98275637/download_file?st=MTczMzkwNDgxMiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Rhinocerotidae_and_Chalicotheriidae_Peri.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/98275637/Antoine_20__20Sen_202016_20Geodiversitas-libre.pdf?1675630162=\u0026response-content-disposition=attachment%3B+filename%3DRhinocerotidae_and_Chalicotheriidae_Peri.pdf\u0026Expires=1733908412\u0026Signature=gAoNcvnw9RitYg--2Fv4~hxpRt5xhvnrIs01xcHQ4avHeqw9oFB7Jdb2oP67WN6WMIGBFu0MuaO2RSFPR2H2j1gBSv58Htpx-FIb4wsom1H2vkT6wEZ8k0cYeIylZAQ92EO8OTN2KE34icLJN50Xh6UbaRyiRgtgUpTk5vYmy3Ki8EKLaPezJ1F5BpzAyejGkp9vhF-18b0a-Ugyrw7Srzu~846RKqY9opnBwKByVl6Twou0QTviYa8AnRzr~VgsfSm2YDJwpqS6Ec9DSxZgiZYIgr-8mYps7lg8MFX-TLj2cZNc0EY~f6sSnOJLJeVfPvZscH7rPADa3EOqA543sA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":29521,"name":"Paleobiogeography","url":"https://www.academia.edu/Documents/in/Paleobiogeography"},{"id":77537,"name":"Rhinocerotidae","url":"https://www.academia.edu/Documents/in/Rhinocerotidae"},{"id":128561,"name":"Rhinoceros","url":"https://www.academia.edu/Documents/in/Rhinoceros"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354835"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354835/Proconsul_heseloni_distal_radial_and_ulnar_epiphyses_from_the_Kaswanga_Primate_Site_Rusinga_Island_Kenya"><img alt="Research paper thumbnail of Proconsul heseloni distal radial and ulnar epiphyses from the Kaswanga Primate Site, Rusinga Island, Kenya" class="work-thumbnail" src="https://attachments.academia-assets.com/98275671/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354835/Proconsul_heseloni_distal_radial_and_ulnar_epiphyses_from_the_Kaswanga_Primate_Site_Rusinga_Island_Kenya">Proconsul heseloni distal radial and ulnar epiphyses from the Kaswanga Primate Site, Rusinga Island, Kenya</a></div><div class="wp-workCard_item"><span>Journal of human evolution</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Only two distal epiphyses of a radius and ulna are consensually attributed to the holotype skelet...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Only two distal epiphyses of a radius and ulna are consensually attributed to the holotype skeleton of Proconsul heseloni, KNM-RU 2036. Here, we describe seven adult and immature distal antebrachial (radial and ulnar) epiphyses from two other individuals of P. heseloni from the Lower Miocene deposits of the Kaswanga Primate Site (KPS), Rusinga Island, Kenya. Because KNM-RU 2036 and KNM-KPS individuals III and VIII are conspecific and penecontemporaneous, their comparison provides the opportunity i) to characterize, for the first time, the morphological variation of the distal radioulnar joint in a Miocene ape, P. heseloni, and ii) to investigate the functional and evolutionary implications. Our results show that the distal antebrachial epiphyses of KNM-KPS III and VIII correspond to stages of bone maturation that are more advanced than those of KNM-RU 2036 (larger articulations and sharper articular borders and ligament attachments that are more developed). Accordingly, functional i...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="7338e4c4d68272d5bcecfd74b54ee15e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":98275671,"asset_id":96354835,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/98275671/download_file?st=MTczMzkwNDgxMiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354835"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354835"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354835; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354835]").text(description); $(".js-view-count[data-work-id=96354835]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354835; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354835']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354835, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "7338e4c4d68272d5bcecfd74b54ee15e" } } $('.js-work-strip[data-work-id=96354835]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354835,"title":"Proconsul heseloni distal radial and ulnar epiphyses from the Kaswanga Primate Site, Rusinga Island, Kenya","translated_title":"","metadata":{"abstract":"Only two distal epiphyses of a radius and ulna are consensually attributed to the holotype skeleton of Proconsul heseloni, KNM-RU 2036. Here, we describe seven adult and immature distal antebrachial (radial and ulnar) epiphyses from two other individuals of P. heseloni from the Lower Miocene deposits of the Kaswanga Primate Site (KPS), Rusinga Island, Kenya. Because KNM-RU 2036 and KNM-KPS individuals III and VIII are conspecific and penecontemporaneous, their comparison provides the opportunity i) to characterize, for the first time, the morphological variation of the distal radioulnar joint in a Miocene ape, P. heseloni, and ii) to investigate the functional and evolutionary implications. Our results show that the distal antebrachial epiphyses of KNM-KPS III and VIII correspond to stages of bone maturation that are more advanced than those of KNM-RU 2036 (larger articulations and sharper articular borders and ligament attachments that are more developed). Accordingly, functional i...","ai_title_tag":"Morphological Variation of Distal Epiphyses in Proconsul heseloni","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"Journal of human evolution"},"translated_abstract":"Only two distal epiphyses of a radius and ulna are consensually attributed to the holotype skeleton of Proconsul heseloni, KNM-RU 2036. Here, we describe seven adult and immature distal antebrachial (radial and ulnar) epiphyses from two other individuals of P. heseloni from the Lower Miocene deposits of the Kaswanga Primate Site (KPS), Rusinga Island, Kenya. Because KNM-RU 2036 and KNM-KPS individuals III and VIII are conspecific and penecontemporaneous, their comparison provides the opportunity i) to characterize, for the first time, the morphological variation of the distal radioulnar joint in a Miocene ape, P. heseloni, and ii) to investigate the functional and evolutionary implications. Our results show that the distal antebrachial epiphyses of KNM-KPS III and VIII correspond to stages of bone maturation that are more advanced than those of KNM-RU 2036 (larger articulations and sharper articular borders and ligament attachments that are more developed). 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Here, we describe seven adult and immature distal antebrachial (radial and ulnar) epiphyses from two other individuals of P. heseloni from the Lower Miocene deposits of the Kaswanga Primate Site (KPS), Rusinga Island, Kenya. Because KNM-RU 2036 and KNM-KPS individuals III and VIII are conspecific and penecontemporaneous, their comparison provides the opportunity i) to characterize, for the first time, the morphological variation of the distal radioulnar joint in a Miocene ape, P. heseloni, and ii) to investigate the functional and evolutionary implications. Our results show that the distal antebrachial epiphyses of KNM-KPS III and VIII correspond to stages of bone maturation that are more advanced than those of KNM-RU 2036 (larger articulations and sharper articular borders and ligament attachments that are more developed). 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Developments in Primatology: Progress and Prospects. Edited by Kristiaan D'Août and Evie E. Vereecke. New York: Springer. $179.00. xvi + 364 p.; ill.; index. ISBN: 978-1-4419-1419-4 (hc); 978-1-4419-1420-0 (eb). 2011" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354834/Primate_Locomotion_Linking_Field_and_Laboratory_Research_Developments_in_Primatology_Progress_and_Prospects_Edited_by_Kristiaan_DAo%C3%BBt_and_Evie_E_Vereecke_New_York_Springer_179_00_xvi_364_p_ill_index_ISBN_978_1_4419_1419_4_hc_978_1_4419_1420_0_eb_2011">Primate Locomotion: Linking Field and Laboratory Research. Developments in Primatology: Progress and Prospects. Edited by Kristiaan D'Août and Evie E. Vereecke. New York: Springer. $179.00. xvi + 364 p.; ill.; index. ISBN: 978-1-4419-1419-4 (hc); 978-1-4419-1420-0 (eb). 2011</a></div><div class="wp-workCard_item"><span>The Quarterly Review of Biology</span><span>, 2012</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354834"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354834"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354834; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354834]").text(description); $(".js-view-count[data-work-id=96354834]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354834; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354834']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354834, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354834]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354834,"title":"Primate Locomotion: Linking Field and Laboratory Research. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="15205662" id="papers"><div class="js-work-strip profile--work_container" data-work-id="96354885"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354885/Raw_data_for_Biomechanical_demands_of_percussive_techniques_in_the_context_of_early_stone_toolmaking"><img alt="Research paper thumbnail of Raw data for: Biomechanical demands of percussive techniques in the context of early stone toolmaking" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354885/Raw_data_for_Biomechanical_demands_of_percussive_techniques_in_the_context_of_early_stone_toolmaking">Raw data for: Biomechanical demands of percussive techniques in the context of early stone toolmaking</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Recent discoveries in archaeology and palaeoanthropology highlight that stone stool knapping coul...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Recent discoveries in archaeology and palaeoanthropology highlight that stone stool knapping could have emerged first within the genera Australopithecus or Kenyanthropus rather than Homo. To explore the implications of this hypothesis determining the physical demands and motor control needed for performing the percussive movements during the oldest stone toolmaking technology (i.e. Lomekwian) would help. We analysed the joint-angle patterns and muscle activity of a knapping expert using three stone tool replication techniques: unipolar flaking on passive hammer (PH), bipolar flaking on anvil (BP), multidirectional and multifacial flaking with free hand (FH). PH presents high levels of activity for Biceps brachii and the wrist extensors and flexors. By contrast, BP and FH are characterised by high solicitation of forearm pronation. The synergy analyses depict a high muscular and kinematic coordination. Whereas the muscle pattern is very close between the techniques, kinematic pattern...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354885"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354885"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354885; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354885]").text(description); $(".js-view-count[data-work-id=96354885]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354885; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354885']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354885, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354885]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354885,"title":"Raw data for: Biomechanical demands of percussive techniques in the context of early stone toolmaking","translated_title":"","metadata":{"abstract":"Recent discoveries in archaeology and palaeoanthropology highlight that stone stool knapping could have emerged first within the genera Australopithecus or Kenyanthropus rather than Homo. 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By contrast, BP and FH are characterised by high solicitation of forearm pronation. The synergy analyses depict a high muscular and kinematic coordination. 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The repository is the National Museum of the Philippines, Manila. &lt;i&gt;Homo luzonensis&lt;/i&gt; has been deposited in the ZooBank database (<a href="http://zoobank.org/" rel="nofollow">http://zoobank.org/</a>) with Life Science Identifier urn:lsid:zoobank. org:act: 4F743862-662F-4E6B-9812-8 A05533 C1347. &lt;b&gt;Paratypes.&lt;/b&gt; Recovered in 2007, 2011 and 2015 from the same excavation area and layer as the holotype: CCH1, a right third metatarsal 1; CCH2 and CCH5, two manual phalanges; CCH3 and CCH4, two pedal phalanges; CCH8, a left upper third or fourth premolar (P 3/4); and CCH9, a right M 3 (all specimens are housed at the National Museum of the Philippines, Manila). &lt;b&gt;Referred material.&lt;/b&gt; CCH7, a femoral shaft that belonged to a juvenile individual (housed at the National Museum of the Philippines, Manila). &lt;b&gt;Locality.&lt;/b&gt; The type locality is Callao Cave, in the Callao Limestone formation in the Peñablanca region of northern Luzon, the Philippines, at coordinates 17° 42′ 11.7″ N, 121° 49′ 25.5″ E. &lt;b&gt;Diagnosis.&lt;/b&gt; Postcanine maxillary teeth of small size that are mesiodistally compressed, with a premolar:molar crown size ratio that is high compared to other species in the genus &lt;i&gt;Homo&lt;/i&gt;. Upper premolars with two or three roots, a mesio-distally expanded lingual crown, strong buccal grooves, partial or continuous transverse crest, and an enameldentine junction (EDJ) shape that is distinct from that of &lt;i&gt;H. sapiens&lt;/i&gt;, &lt;i&gt;Homo neanderthalensis&lt;/i&gt; and Asian &lt;i&gt;Homo erectus&lt;/i&gt;. Very small upper molars, with a M 1 &amp;gt; M 2 &amp;gt; M 3 crown size pattern, a simplified occlusal morphology with reduced metacone and hypocone, no crenulation on the EDJ, and EDJ shape affinities with that of &lt;i&gt;H. sapiens&lt;/i&gt; and Asian &lt;i&gt;H. erectus&lt;/i&gt;. Intermediate manual phalanx (rays 2–4) that is long and narrow (u [...]</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354844"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354844"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354844; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354844]").text(description); $(".js-view-count[data-work-id=96354844]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354844; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354844']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354844, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354844]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354844,"title":"Homo luzonensis Détroit \u0026 Mijares \u0026 Corny \u0026 Daver \u0026 Zanolli \u0026 Dizon \u0026 Robles \u0026 Grün \u0026 Piper 2019, sp. nov","translated_title":"","metadata":{"abstract":"\u0026lt;i\u0026gt;Homo luzonensis\u0026lt;/i\u0026gt; sp. nov. \u0026lt;b\u0026gt;Etymology.\u0026lt;/b\u0026gt; The species name is derived from the island of Luzon, where the specimens were discovered. \u0026lt;b\u0026gt;Holotype.\u0026lt;/b\u0026gt; CCH6 (CCH6-a to CCH6-e), maxillary right postcanine dentition of a single individual discovered on 24 August 2011. The repository is the National Museum of the Philippines, Manila. \u0026lt;i\u0026gt;Homo luzonensis\u0026lt;/i\u0026gt; has been deposited in the ZooBank database (http://zoobank.org/) with Life Science Identifier urn:lsid:zoobank. org:act: 4F743862-662F-4E6B-9812-8 A05533 C1347. \u0026lt;b\u0026gt;Paratypes.\u0026lt;/b\u0026gt; Recovered in 2007, 2011 and 2015 from the same excavation area and layer as the holotype: CCH1, a right third metatarsal 1; CCH2 and CCH5, two manual phalanges; CCH3 and CCH4, two pedal phalanges; CCH8, a left upper third or fourth premolar (P 3/4); and CCH9, a right M 3 (all specimens are housed at the National Museum of the Philippines, Manila). \u0026lt;b\u0026gt;Referred material.\u0026lt;/b\u0026gt; CCH7, a femoral shaft that belonged to a juvenile individual (housed at the National Museum of the Philippines, Manila). \u0026lt;b\u0026gt;Locality.\u0026lt;/b\u0026gt; The type locality is Callao Cave, in the Callao Limestone formation in the Peñablanca region of northern Luzon, the Philippines, at coordinates 17° 42′ 11.7″ N, 121° 49′ 25.5″ E. \u0026lt;b\u0026gt;Diagnosis.\u0026lt;/b\u0026gt; Postcanine maxillary teeth of small size that are mesiodistally compressed, with a premolar:molar crown size ratio that is high compared to other species in the genus \u0026lt;i\u0026gt;Homo\u0026lt;/i\u0026gt;. Upper premolars with two or three roots, a mesio-distally expanded lingual crown, strong buccal grooves, partial or continuous transverse crest, and an enameldentine junction (EDJ) shape that is distinct from that of \u0026lt;i\u0026gt;H. sapiens\u0026lt;/i\u0026gt;, \u0026lt;i\u0026gt;Homo neanderthalensis\u0026lt;/i\u0026gt; and Asian \u0026lt;i\u0026gt;Homo erectus\u0026lt;/i\u0026gt;. Very small upper molars, with a M 1 \u0026amp;gt; M 2 \u0026amp;gt; M 3 crown size pattern, a simplified occlusal morphology with reduced metacone and hypocone, no crenulation on the EDJ, and EDJ shape affinities with that of \u0026lt;i\u0026gt;H. sapiens\u0026lt;/i\u0026gt; and Asian \u0026lt;i\u0026gt;H. erectus\u0026lt;/i\u0026gt;. Intermediate manual phalanx (rays 2–4) that is long and narrow (u [...]","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"\u0026lt;i\u0026gt;Homo luzonensis\u0026lt;/i\u0026gt; sp. nov. \u0026lt;b\u0026gt;Etymology.\u0026lt;/b\u0026gt; The species name is derived from the island of Luzon, where the specimens were discovered. \u0026lt;b\u0026gt;Holotype.\u0026lt;/b\u0026gt; CCH6 (CCH6-a to CCH6-e), maxillary right postcanine dentition of a single individual discovered on 24 August 2011. The repository is the National Museum of the Philippines, Manila. \u0026lt;i\u0026gt;Homo luzonensis\u0026lt;/i\u0026gt; has been deposited in the ZooBank database (http://zoobank.org/) with Life Science Identifier urn:lsid:zoobank. org:act: 4F743862-662F-4E6B-9812-8 A05533 C1347. \u0026lt;b\u0026gt;Paratypes.\u0026lt;/b\u0026gt; Recovered in 2007, 2011 and 2015 from the same excavation area and layer as the holotype: CCH1, a right third metatarsal 1; CCH2 and CCH5, two manual phalanges; CCH3 and CCH4, two pedal phalanges; CCH8, a left upper third or fourth premolar (P 3/4); and CCH9, a right M 3 (all specimens are housed at the National Museum of the Philippines, Manila). \u0026lt;b\u0026gt;Referred material.\u0026lt;/b\u0026gt; CCH7, a femoral shaft that belonged to a juvenile individual (housed at the National Museum of the Philippines, Manila). \u0026lt;b\u0026gt;Locality.\u0026lt;/b\u0026gt; The type locality is Callao Cave, in the Callao Limestone formation in the Peñablanca region of northern Luzon, the Philippines, at coordinates 17° 42′ 11.7″ N, 121° 49′ 25.5″ E. \u0026lt;b\u0026gt;Diagnosis.\u0026lt;/b\u0026gt; Postcanine maxillary teeth of small size that are mesiodistally compressed, with a premolar:molar crown size ratio that is high compared to other species in the genus \u0026lt;i\u0026gt;Homo\u0026lt;/i\u0026gt;. Upper premolars with two or three roots, a mesio-distally expanded lingual crown, strong buccal grooves, partial or continuous transverse crest, and an enameldentine junction (EDJ) shape that is distinct from that of \u0026lt;i\u0026gt;H. sapiens\u0026lt;/i\u0026gt;, \u0026lt;i\u0026gt;Homo neanderthalensis\u0026lt;/i\u0026gt; and Asian \u0026lt;i\u0026gt;Homo erectus\u0026lt;/i\u0026gt;. Very small upper molars, with a M 1 \u0026amp;gt; M 2 \u0026amp;gt; M 3 crown size pattern, a simplified occlusal morphology with reduced metacone and hypocone, no crenulation on the EDJ, and EDJ shape affinities with that of \u0026lt;i\u0026gt;H. sapiens\u0026lt;/i\u0026gt; and Asian \u0026lt;i\u0026gt;H. erectus\u0026lt;/i\u0026gt;. Intermediate manual phalanx (rays 2–4) that is long and narrow (u [...]","internal_url":"https://www.academia.edu/96354844/Homo_luzonensis_D%C3%A9troit_and_Mijares_and_Corny_and_Daver_and_Zanolli_and_Dizon_and_Robles_and_Gr%C3%BCn_and_Piper_2019_sp_nov","translated_internal_url":"","created_at":"2023-02-05T12:27:26.945-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Homo_luzonensis_Détroit_and_Mijares_and_Corny_and_Daver_and_Zanolli_and_Dizon_and_Robles_and_Grün_and_Piper_2019_sp_nov","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"\u0026lt;i\u0026gt;Homo luzonensis\u0026lt;/i\u0026gt; sp. nov. \u0026lt;b\u0026gt;Etymology.\u0026lt;/b\u0026gt; The species name is derived from the island of Luzon, where the specimens were discovered. \u0026lt;b\u0026gt;Holotype.\u0026lt;/b\u0026gt; CCH6 (CCH6-a to CCH6-e), maxillary right postcanine dentition of a single individual discovered on 24 August 2011. The repository is the National Museum of the Philippines, Manila. \u0026lt;i\u0026gt;Homo luzonensis\u0026lt;/i\u0026gt; has been deposited in the ZooBank database (http://zoobank.org/) with Life Science Identifier urn:lsid:zoobank. org:act: 4F743862-662F-4E6B-9812-8 A05533 C1347. \u0026lt;b\u0026gt;Paratypes.\u0026lt;/b\u0026gt; Recovered in 2007, 2011 and 2015 from the same excavation area and layer as the holotype: CCH1, a right third metatarsal 1; CCH2 and CCH5, two manual phalanges; CCH3 and CCH4, two pedal phalanges; CCH8, a left upper third or fourth premolar (P 3/4); and CCH9, a right M 3 (all specimens are housed at the National Museum of the Philippines, Manila). \u0026lt;b\u0026gt;Referred material.\u0026lt;/b\u0026gt; CCH7, a femoral shaft that belonged to a juvenile individual (housed at the National Museum of the Philippines, Manila). \u0026lt;b\u0026gt;Locality.\u0026lt;/b\u0026gt; The type locality is Callao Cave, in the Callao Limestone formation in the Peñablanca region of northern Luzon, the Philippines, at coordinates 17° 42′ 11.7″ N, 121° 49′ 25.5″ E. \u0026lt;b\u0026gt;Diagnosis.\u0026lt;/b\u0026gt; Postcanine maxillary teeth of small size that are mesiodistally compressed, with a premolar:molar crown size ratio that is high compared to other species in the genus \u0026lt;i\u0026gt;Homo\u0026lt;/i\u0026gt;. Upper premolars with two or three roots, a mesio-distally expanded lingual crown, strong buccal grooves, partial or continuous transverse crest, and an enameldentine junction (EDJ) shape that is distinct from that of \u0026lt;i\u0026gt;H. sapiens\u0026lt;/i\u0026gt;, \u0026lt;i\u0026gt;Homo neanderthalensis\u0026lt;/i\u0026gt; and Asian \u0026lt;i\u0026gt;Homo erectus\u0026lt;/i\u0026gt;. Very small upper molars, with a M 1 \u0026amp;gt; M 2 \u0026amp;gt; M 3 crown size pattern, a simplified occlusal morphology with reduced metacone and hypocone, no crenulation on the EDJ, and EDJ shape affinities with that of \u0026lt;i\u0026gt;H. sapiens\u0026lt;/i\u0026gt; and Asian \u0026lt;i\u0026gt;H. erectus\u0026lt;/i\u0026gt;. Intermediate manual phalanx (rays 2–4) that is long and narrow (u [...]","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354843"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354843/Extended_Data_Fig_10_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Extended Data Fig. 10 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354843/Extended_Data_Fig_10_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Extended Data Fig. 10 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Extended Data Fig. 10 | CCH7, femoral shaft of a juvenile individual of H. luzonensis. a, Photogr...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Extended Data Fig. 10 | CCH7, femoral shaft of a juvenile individual of H. luzonensis. a, Photograph of the original specimen CCH7 (posterior aspect). b, Three-dimensional rendering of CCH7. From left to right: anterior, medial, posterior and lateral aspects. Scale bar, 20 mm. c, Transverse micro-CT slices of CCH7 at proximal diaphysis (top), midshaft (middle) and distal diaphysis (bottom), and posterior aspect of the three-dimensional rendering of the femoral shaft, during the segmentation process (orientation of slices: anterior is up, posterior is down, lateral is left, medial is right).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354843"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354843"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354843; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354843]").text(description); $(".js-view-count[data-work-id=96354843]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354843; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354843']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354843, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354843]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354843,"title":"Extended Data Fig. 10 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Extended Data Fig. 10 | CCH7, femoral shaft of a juvenile individual of H. luzonensis. a, Photograph of the original specimen CCH7 (posterior aspect). b, Three-dimensional rendering of CCH7. From left to right: anterior, medial, posterior and lateral aspects. Scale bar, 20 mm. c, Transverse micro-CT slices of CCH7 at proximal diaphysis (top), midshaft (middle) and distal diaphysis (bottom), and posterior aspect of the three-dimensional rendering of the femoral shaft, during the segmentation process (orientation of slices: anterior is up, posterior is down, lateral is left, medial is right).","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Extended Data Fig. 10 | CCH7, femoral shaft of a juvenile individual of H. luzonensis. a, Photograph of the original specimen CCH7 (posterior aspect). b, Three-dimensional rendering of CCH7. From left to right: anterior, medial, posterior and lateral aspects. Scale bar, 20 mm. c, Transverse micro-CT slices of CCH7 at proximal diaphysis (top), midshaft (middle) and distal diaphysis (bottom), and posterior aspect of the three-dimensional rendering of the femoral shaft, during the segmentation process (orientation of slices: anterior is up, posterior is down, lateral is left, medial is right).","internal_url":"https://www.academia.edu/96354843/Extended_Data_Fig_10_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:26.811-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Extended_Data_Fig_10_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Extended Data Fig. 10 | CCH7, femoral shaft of a juvenile individual of H. luzonensis. a, Photograph of the original specimen CCH7 (posterior aspect). b, Three-dimensional rendering of CCH7. From left to right: anterior, medial, posterior and lateral aspects. Scale bar, 20 mm. c, Transverse micro-CT slices of CCH7 at proximal diaphysis (top), midshaft (middle) and distal diaphysis (bottom), and posterior aspect of the three-dimensional rendering of the femoral shaft, during the segmentation process (orientation of slices: anterior is up, posterior is down, lateral is left, medial is right).","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354842"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354842/Extended_Data_Fig_9_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Extended Data Fig. 9 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354842/Extended_Data_Fig_9_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Extended Data Fig. 9 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Extended Data Fig. 9 | CCH3, intermediate pedal phalanx of H. luzonensis. a, Photograph of the or...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Extended Data Fig. 9 | CCH3, intermediate pedal phalanx of H. luzonensis. a, Photograph of the original specimen CCH3 in plantar view. b, Three-dimensional rendering of CCH3. From left to right: plantar, medial, dorsal, lateral, distal (top), proximal (bottom), disto-medial and proximo-medial aspects. c, Comparison of CCH3 with Pliocene (A.L.333- 21a, unknown side and rays 2–5, and A.L.333-115k, fourth intermediate phalanx), Upper Pleistocene (LB1/56, LB1-15 and LB1/39: unknown side and rays 2–5) and recent (PAPO-74-150) intermediate pedal phalanges in plantar (top) and side (bottom) views. Note the variation in shape and size both between taxa (for example, H. sapiens and H. floresiensis) and in the same individual (for example, LB1 and PAPO-74-150). A detailed list of specimens can be found in Supplementary Table 12. Scale bars, 10 mm.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354842"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354842"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354842; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354842]").text(description); $(".js-view-count[data-work-id=96354842]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354842; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354842']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354842, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354842]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354842,"title":"Extended Data Fig. 9 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Extended Data Fig. 9 | CCH3, intermediate pedal phalanx of H. luzonensis. a, Photograph of the original specimen CCH3 in plantar view. b, Three-dimensional rendering of CCH3. From left to right: plantar, medial, dorsal, lateral, distal (top), proximal (bottom), disto-medial and proximo-medial aspects. c, Comparison of CCH3 with Pliocene (A.L.333- 21a, unknown side and rays 2–5, and A.L.333-115k, fourth intermediate phalanx), Upper Pleistocene (LB1/56, LB1-15 and LB1/39: unknown side and rays 2–5) and recent (PAPO-74-150) intermediate pedal phalanges in plantar (top) and side (bottom) views. Note the variation in shape and size both between taxa (for example, H. sapiens and H. floresiensis) and in the same individual (for example, LB1 and PAPO-74-150). A detailed list of specimens can be found in Supplementary Table 12. Scale bars, 10 mm.","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Extended Data Fig. 9 | CCH3, intermediate pedal phalanx of H. luzonensis. a, Photograph of the original specimen CCH3 in plantar view. b, Three-dimensional rendering of CCH3. From left to right: plantar, medial, dorsal, lateral, distal (top), proximal (bottom), disto-medial and proximo-medial aspects. c, Comparison of CCH3 with Pliocene (A.L.333- 21a, unknown side and rays 2–5, and A.L.333-115k, fourth intermediate phalanx), Upper Pleistocene (LB1/56, LB1-15 and LB1/39: unknown side and rays 2–5) and recent (PAPO-74-150) intermediate pedal phalanges in plantar (top) and side (bottom) views. Note the variation in shape and size both between taxa (for example, H. sapiens and H. floresiensis) and in the same individual (for example, LB1 and PAPO-74-150). A detailed list of specimens can be found in Supplementary Table 12. Scale bars, 10 mm.","internal_url":"https://www.academia.edu/96354842/Extended_Data_Fig_9_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:26.672-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Extended_Data_Fig_9_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Extended Data Fig. 9 | CCH3, intermediate pedal phalanx of H. luzonensis. a, Photograph of the original specimen CCH3 in plantar view. b, Three-dimensional rendering of CCH3. From left to right: plantar, medial, dorsal, lateral, distal (top), proximal (bottom), disto-medial and proximo-medial aspects. c, Comparison of CCH3 with Pliocene (A.L.333- 21a, unknown side and rays 2–5, and A.L.333-115k, fourth intermediate phalanx), Upper Pleistocene (LB1/56, LB1-15 and LB1/39: unknown side and rays 2–5) and recent (PAPO-74-150) intermediate pedal phalanges in plantar (top) and side (bottom) views. Note the variation in shape and size both between taxa (for example, H. sapiens and H. floresiensis) and in the same individual (for example, LB1 and PAPO-74-150). A detailed list of specimens can be found in Supplementary Table 12. Scale bars, 10 mm.","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354841"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354841/Extended_Data_Fig_6_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Extended Data Fig. 6 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354841/Extended_Data_Fig_6_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Extended Data Fig. 6 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Extended Data Fig. 6 | Procrustes analyses of the intermediate manual phalanx of H. luzonensis. C...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Extended Data Fig. 6 | Procrustes analyses of the intermediate manual phalanx of H. luzonensis. CCH2 compared to specimens attributed to Australopithecus (A. afarensis, n = 1; A. africanus, n = 1; A. sediba, n = 2), Paranthropus/early Homo (Swartkrans, Member 1, n = 3; Member 3, n = 2), H. naledi (Hand 1, n = 2), H. floresiensis (LB1/48 and LB6/9) and recent H. sapiens separated into 3 samples corresponding to ray number (n = 15, 21 and 19 for rays 2, 3 and 4, respectively). A detailed list of specimens can be found in Supplementary Table 9. a–c, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 3 only): scatter plot of individual scores for bgPC1 versus bgPC2 (a); scatter plot of individual scores for bgPC2 versus bgPC3 (b); shape variation associated with bgPC1, bgPC2 and bgPC3 (c). d, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 4 only): scatter plot of individual scores for bgPC1 versus bgPC2....</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354841"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354841"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354841; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354841]").text(description); $(".js-view-count[data-work-id=96354841]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354841; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354841']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354841, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354841]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354841,"title":"Extended Data Fig. 6 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Extended Data Fig. 6 | Procrustes analyses of the intermediate manual phalanx of H. luzonensis. CCH2 compared to specimens attributed to Australopithecus (A. afarensis, n = 1; A. africanus, n = 1; A. sediba, n = 2), Paranthropus/early Homo (Swartkrans, Member 1, n = 3; Member 3, n = 2), H. naledi (Hand 1, n = 2), H. floresiensis (LB1/48 and LB6/9) and recent H. sapiens separated into 3 samples corresponding to ray number (n = 15, 21 and 19 for rays 2, 3 and 4, respectively). A detailed list of specimens can be found in Supplementary Table 9. a–c, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 3 only): scatter plot of individual scores for bgPC1 versus bgPC2 (a); scatter plot of individual scores for bgPC2 versus bgPC3 (b); shape variation associated with bgPC1, bgPC2 and bgPC3 (c). d, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 4 only): scatter plot of individual scores for bgPC1 versus bgPC2....","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Extended Data Fig. 6 | Procrustes analyses of the intermediate manual phalanx of H. luzonensis. CCH2 compared to specimens attributed to Australopithecus (A. afarensis, n = 1; A. africanus, n = 1; A. sediba, n = 2), Paranthropus/early Homo (Swartkrans, Member 1, n = 3; Member 3, n = 2), H. naledi (Hand 1, n = 2), H. floresiensis (LB1/48 and LB6/9) and recent H. sapiens separated into 3 samples corresponding to ray number (n = 15, 21 and 19 for rays 2, 3 and 4, respectively). 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CCH2 compared to specimens attributed to Australopithecus (A. afarensis, n = 1; A. africanus, n = 1; A. sediba, n = 2), Paranthropus/early Homo (Swartkrans, Member 1, n = 3; Member 3, n = 2), H. naledi (Hand 1, n = 2), H. floresiensis (LB1/48 and LB6/9) and recent H. sapiens separated into 3 samples corresponding to ray number (n = 15, 21 and 19 for rays 2, 3 and 4, respectively). A detailed list of specimens can be found in Supplementary Table 9. a–c, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 3 only): scatter plot of individual scores for bgPC1 versus bgPC2 (a); scatter plot of individual scores for bgPC2 versus bgPC3 (b); shape variation associated with bgPC1, bgPC2 and bgPC3 (c). d, bgPCA of Procrustes-registered landmarks and semilandmarks (H. sapiens sample includes ray 4 only): scatter plot of individual scores for bgPC1 versus bgPC2....","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354840"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354840/Extended_Data_Fig_3_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Extended Data Fig. 3 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354840/Extended_Data_Fig_3_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Extended Data Fig. 3 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Extended Data Fig. 3 | Elliptic Fourier analysis of M1 crown contour. CCH6-c compared to the holo...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Extended Data Fig. 3 | Elliptic Fourier analysis of M1 crown contour. CCH6-c compared to the holotype of H. floresiensis (LB1) and large samples of archaeological and recent H. sapiens individuals. a, PCA of shape data for all specimens, scatter plot of individual scores for PC1 versus PC2 (see Methods; elliptic Fourier descriptors applied to Procrustes-aligned outlines, ten harmonics included). LGM, Last Glacial Maximum. Sample sizes: H. luzonensis, n = 1; H. floresiensis, n = 2; pre- LGM, n = 2; pre-Neolithic post-LGM, n = 12; Neolithic/post-Neolithic, n = 232; recent &#39;Negritos&#39;, n = 19. A detailed list of specimens can be found in Supplementary Table 5. b, Bar plot of eigenvalues (%) of PC1–PC6. c, Extreme shape variations along PC1 and PC2. The scores of H. luzonensis M1 along PC1 and PC2 reflects a crown outline shape that is mesio-distally compressed, but not as much as that of H. floresiensis (two versions of the LB1 right M 1). d, Right M 1 of the holotype of H. flor...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354840"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354840"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354840; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354840]").text(description); $(".js-view-count[data-work-id=96354840]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354840; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354840']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354840, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354840]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354840,"title":"Extended Data Fig. 3 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Extended Data Fig. 3 | Elliptic Fourier analysis of M1 crown contour. CCH6-c compared to the holotype of H. floresiensis (LB1) and large samples of archaeological and recent H. sapiens individuals. a, PCA of shape data for all specimens, scatter plot of individual scores for PC1 versus PC2 (see Methods; elliptic Fourier descriptors applied to Procrustes-aligned outlines, ten harmonics included). LGM, Last Glacial Maximum. Sample sizes: H. luzonensis, n = 1; H. floresiensis, n = 2; pre- LGM, n = 2; pre-Neolithic post-LGM, n = 12; Neolithic/post-Neolithic, n = 232; recent \u0026#39;Negritos\u0026#39;, n = 19. A detailed list of specimens can be found in Supplementary Table 5. b, Bar plot of eigenvalues (%) of PC1–PC6. c, Extreme shape variations along PC1 and PC2. The scores of H. luzonensis M1 along PC1 and PC2 reflects a crown outline shape that is mesio-distally compressed, but not as much as that of H. floresiensis (two versions of the LB1 right M 1). d, Right M 1 of the holotype of H. flor...","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Extended Data Fig. 3 | Elliptic Fourier analysis of M1 crown contour. CCH6-c compared to the holotype of H. floresiensis (LB1) and large samples of archaeological and recent H. sapiens individuals. a, PCA of shape data for all specimens, scatter plot of individual scores for PC1 versus PC2 (see Methods; elliptic Fourier descriptors applied to Procrustes-aligned outlines, ten harmonics included). LGM, Last Glacial Maximum. Sample sizes: H. luzonensis, n = 1; H. floresiensis, n = 2; pre- LGM, n = 2; pre-Neolithic post-LGM, n = 12; Neolithic/post-Neolithic, n = 232; recent \u0026#39;Negritos\u0026#39;, n = 19. A detailed list of specimens can be found in Supplementary Table 5. b, Bar plot of eigenvalues (%) of PC1–PC6. c, Extreme shape variations along PC1 and PC2. The scores of H. luzonensis M1 along PC1 and PC2 reflects a crown outline shape that is mesio-distally compressed, but not as much as that of H. floresiensis (two versions of the LB1 right M 1). d, Right M 1 of the holotype of H. flor...","internal_url":"https://www.academia.edu/96354840/Extended_Data_Fig_3_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:26.395-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Extended_Data_Fig_3_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Extended Data Fig. 3 | Elliptic Fourier analysis of M1 crown contour. CCH6-c compared to the holotype of H. floresiensis (LB1) and large samples of archaeological and recent H. sapiens individuals. a, PCA of shape data for all specimens, scatter plot of individual scores for PC1 versus PC2 (see Methods; elliptic Fourier descriptors applied to Procrustes-aligned outlines, ten harmonics included). LGM, Last Glacial Maximum. Sample sizes: H. luzonensis, n = 1; H. floresiensis, n = 2; pre- LGM, n = 2; pre-Neolithic post-LGM, n = 12; Neolithic/post-Neolithic, n = 232; recent \u0026#39;Negritos\u0026#39;, n = 19. A detailed list of specimens can be found in Supplementary Table 5. b, Bar plot of eigenvalues (%) of PC1–PC6. c, Extreme shape variations along PC1 and PC2. The scores of H. luzonensis M1 along PC1 and PC2 reflects a crown outline shape that is mesio-distally compressed, but not as much as that of H. floresiensis (two versions of the LB1 right M 1). d, Right M 1 of the holotype of H. flor...","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354839"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354839/Extended_Data_Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Extended Data Fig. 1 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354839/Extended_Data_Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Extended Data Fig. 1 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Extended Data Fig. 1 | Inventory of the fossil elements attributed to H. luzonensis and detailed ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Extended Data Fig. 1 | Inventory of the fossil elements attributed to H. luzonensis and detailed views of the dental remains. a, The hominin fossils recovered from Callao Cave. R, right; L, left; P, premolar; M, molar. b, Three-dimensional rendering of the postcanine maxillary teeth CCH6-b to CCH6-e (M 2 –P 3): occlusal (top row) and buccal (bottom row) aspects. Enamel is shown in dark blue, dentine and cement in light brown and pulp cavity in dark grey. In all views, mesial is to the right, distal to the left. c, CCH6-a, right M 3: occlusal, buccal, lingual, mesial and distal aspects (from top to bottom and left to right). Occlusal view: mesial is to the right, distal to the left. d, CCH6-a to CCH6-e, right M 3 –P 3: photograph of occlusal aspect. Mesial is to the right, distal to the left. The numbers indicate the locations of the detailed views of the inter-proximal contact facets (IPCFs): P 3 (CCH6-e), mesial IPCF 1: note the small size of this IPCF, indicating that the canine w...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354839"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354839"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354839; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354839]").text(description); $(".js-view-count[data-work-id=96354839]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354839; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354839']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354839, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354839]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354839,"title":"Extended Data Fig. 1 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Extended Data Fig. 1 | Inventory of the fossil elements attributed to H. luzonensis and detailed views of the dental remains. a, The hominin fossils recovered from Callao Cave. R, right; L, left; P, premolar; M, molar. b, Three-dimensional rendering of the postcanine maxillary teeth CCH6-b to CCH6-e (M 2 –P 3): occlusal (top row) and buccal (bottom row) aspects. Enamel is shown in dark blue, dentine and cement in light brown and pulp cavity in dark grey. In all views, mesial is to the right, distal to the left. c, CCH6-a, right M 3: occlusal, buccal, lingual, mesial and distal aspects (from top to bottom and left to right). Occlusal view: mesial is to the right, distal to the left. d, CCH6-a to CCH6-e, right M 3 –P 3: photograph of occlusal aspect. Mesial is to the right, distal to the left. The numbers indicate the locations of the detailed views of the inter-proximal contact facets (IPCFs): P 3 (CCH6-e), mesial IPCF 1: note the small size of this IPCF, indicating that the canine w...","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Extended Data Fig. 1 | Inventory of the fossil elements attributed to H. luzonensis and detailed views of the dental remains. a, The hominin fossils recovered from Callao Cave. R, right; L, left; P, premolar; M, molar. b, Three-dimensional rendering of the postcanine maxillary teeth CCH6-b to CCH6-e (M 2 –P 3): occlusal (top row) and buccal (bottom row) aspects. Enamel is shown in dark blue, dentine and cement in light brown and pulp cavity in dark grey. In all views, mesial is to the right, distal to the left. c, CCH6-a, right M 3: occlusal, buccal, lingual, mesial and distal aspects (from top to bottom and left to right). Occlusal view: mesial is to the right, distal to the left. d, CCH6-a to CCH6-e, right M 3 –P 3: photograph of occlusal aspect. Mesial is to the right, distal to the left. The numbers indicate the locations of the detailed views of the inter-proximal contact facets (IPCFs): P 3 (CCH6-e), mesial IPCF 1: note the small size of this IPCF, indicating that the canine w...","internal_url":"https://www.academia.edu/96354839/Extended_Data_Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:25.851-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Extended_Data_Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Extended Data Fig. 1 | Inventory of the fossil elements attributed to H. luzonensis and detailed views of the dental remains. a, The hominin fossils recovered from Callao Cave. R, right; L, left; P, premolar; M, molar. b, Three-dimensional rendering of the postcanine maxillary teeth CCH6-b to CCH6-e (M 2 –P 3): occlusal (top row) and buccal (bottom row) aspects. Enamel is shown in dark blue, dentine and cement in light brown and pulp cavity in dark grey. In all views, mesial is to the right, distal to the left. c, CCH6-a, right M 3: occlusal, buccal, lingual, mesial and distal aspects (from top to bottom and left to right). Occlusal view: mesial is to the right, distal to the left. d, CCH6-a to CCH6-e, right M 3 –P 3: photograph of occlusal aspect. Mesial is to the right, distal to the left. The numbers indicate the locations of the detailed views of the inter-proximal contact facets (IPCFs): P 3 (CCH6-e), mesial IPCF 1: note the small size of this IPCF, indicating that the canine w...","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354838"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354838/Fig_4_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Fig. 4 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354838/Fig_4_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Fig. 4 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Fig. 4 | Premolar EDJ of H. luzonensis. a, EDJ of the P 3 of H. luzonensis (CCH6-e) compared to t...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Fig. 4 | Premolar EDJ of H. luzonensis. a, EDJ of the P 3 of H. luzonensis (CCH6-e) compared to the EDJs of H. floresiensis (Liang Bua 1 (LB1)), H. sapiens, H. erectus (Sangiran 4) and H. neanderthalensis (KRD 53). Horns of dentine were reconstructed for CCH6-e, LB1 and Sangiran 4; see Methods. Scale bar, 5 mm. b, c, Between-group principal component analyses (bgPCAs) of the three-dimensional landmark Procrustes- registered shape coordinates of the P 3 s (b) and P 4 s (c). Sample sizes for b, c, respectively: H. erectus, n = 2, 3; H. neanderthalensis, n = 5, 6; fossil H. sapiens, n = 3, 3; extant H. sapiens, n = 8, 9; H. floresiensis, n = 1, 0; H. luzonensis, n = 2, 2. A detailed list of specimens can be found in Supplementary Table 6</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354838"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354838"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354838; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354838]").text(description); $(".js-view-count[data-work-id=96354838]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354838; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354838']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354838, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354838]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354838,"title":"Fig. 4 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Fig. 4 | Premolar EDJ of H. luzonensis. a, EDJ of the P 3 of H. luzonensis (CCH6-e) compared to the EDJs of H. floresiensis (Liang Bua 1 (LB1)), H. sapiens, H. erectus (Sangiran 4) and H. neanderthalensis (KRD 53). Horns of dentine were reconstructed for CCH6-e, LB1 and Sangiran 4; see Methods. Scale bar, 5 mm. b, c, Between-group principal component analyses (bgPCAs) of the three-dimensional landmark Procrustes- registered shape coordinates of the P 3 s (b) and P 4 s (c). Sample sizes for b, c, respectively: H. erectus, n = 2, 3; H. neanderthalensis, n = 5, 6; fossil H. sapiens, n = 3, 3; extant H. sapiens, n = 8, 9; H. floresiensis, n = 1, 0; H. luzonensis, n = 2, 2. A detailed list of specimens can be found in Supplementary Table 6","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Fig. 4 | Premolar EDJ of H. luzonensis. a, EDJ of the P 3 of H. luzonensis (CCH6-e) compared to the EDJs of H. floresiensis (Liang Bua 1 (LB1)), H. sapiens, H. erectus (Sangiran 4) and H. neanderthalensis (KRD 53). Horns of dentine were reconstructed for CCH6-e, LB1 and Sangiran 4; see Methods. Scale bar, 5 mm. b, c, Between-group principal component analyses (bgPCAs) of the three-dimensional landmark Procrustes- registered shape coordinates of the P 3 s (b) and P 4 s (c). Sample sizes for b, c, respectively: H. erectus, n = 2, 3; H. neanderthalensis, n = 5, 6; fossil H. sapiens, n = 3, 3; extant H. sapiens, n = 8, 9; H. floresiensis, n = 1, 0; H. luzonensis, n = 2, 2. A detailed list of specimens can be found in Supplementary Table 6","internal_url":"https://www.academia.edu/96354838/Fig_4_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:25.700-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Fig_4_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Fig. 4 | Premolar EDJ of H. luzonensis. a, EDJ of the P 3 of H. luzonensis (CCH6-e) compared to the EDJs of H. floresiensis (Liang Bua 1 (LB1)), H. sapiens, H. erectus (Sangiran 4) and H. neanderthalensis (KRD 53). Horns of dentine were reconstructed for CCH6-e, LB1 and Sangiran 4; see Methods. Scale bar, 5 mm. b, c, Between-group principal component analyses (bgPCAs) of the three-dimensional landmark Procrustes- registered shape coordinates of the P 3 s (b) and P 4 s (c). Sample sizes for b, c, respectively: H. erectus, n = 2, 3; H. neanderthalensis, n = 5, 6; fossil H. sapiens, n = 3, 3; extant H. sapiens, n = 8, 9; H. floresiensis, n = 1, 0; H. luzonensis, n = 2, 2. A detailed list of specimens can be found in Supplementary Table 6","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354837"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354837/Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines"><img alt="Research paper thumbnail of Fig. 1 in A new species of Homo from the Late Pleistocene of the Philippines" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354837/Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines">Fig. 1 in A new species of Homo from the Late Pleistocene of the Philippines</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Fig. 1 | Geographical location of Callao Cave. Map showing the location of Callao Cave on Luzon I...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Fig. 1 | Geographical location of Callao Cave. Map showing the location of Callao Cave on Luzon Island (the Philippines), emerged lands at 50 and 120 m below present sea level (adapted from ref. 46, H. K. Voris, Field Museum of Natural History) and the major biogeographical boundaries recognized in the area. A, Wallace&#39;s Line modified by Huxley; B, Wallace&#39;s Line; C, Lydekker&#39;s Line. Luzon Island lies in between the original Wallace&#39;s Line and the Wallace&#39;s Line modified by Huxley and was never connected to mainland Asia during the Quaternary.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354837"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354837"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354837; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354837]").text(description); $(".js-view-count[data-work-id=96354837]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354837; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354837']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354837, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=96354837]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354837,"title":"Fig. 1 in A new species of Homo from the Late Pleistocene of the Philippines","translated_title":"","metadata":{"abstract":"Fig. 1 | Geographical location of Callao Cave. Map showing the location of Callao Cave on Luzon Island (the Philippines), emerged lands at 50 and 120 m below present sea level (adapted from ref. 46, H. K. Voris, Field Museum of Natural History) and the major biogeographical boundaries recognized in the area. A, Wallace\u0026#39;s Line modified by Huxley; B, Wallace\u0026#39;s Line; C, Lydekker\u0026#39;s Line. Luzon Island lies in between the original Wallace\u0026#39;s Line and the Wallace\u0026#39;s Line modified by Huxley and was never connected to mainland Asia during the Quaternary.","publisher":"Zenodo","publication_date":{"day":10,"month":4,"year":2019,"errors":{}}},"translated_abstract":"Fig. 1 | Geographical location of Callao Cave. Map showing the location of Callao Cave on Luzon Island (the Philippines), emerged lands at 50 and 120 m below present sea level (adapted from ref. 46, H. K. Voris, Field Museum of Natural History) and the major biogeographical boundaries recognized in the area. A, Wallace\u0026#39;s Line modified by Huxley; B, Wallace\u0026#39;s Line; C, Lydekker\u0026#39;s Line. Luzon Island lies in between the original Wallace\u0026#39;s Line and the Wallace\u0026#39;s Line modified by Huxley and was never connected to mainland Asia during the Quaternary.","internal_url":"https://www.academia.edu/96354837/Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_internal_url":"","created_at":"2023-02-05T12:27:25.567-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Fig_1_in_A_new_species_of_Homo_from_the_Late_Pleistocene_of_the_Philippines","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"Fig. 1 | Geographical location of Callao Cave. Map showing the location of Callao Cave on Luzon Island (the Philippines), emerged lands at 50 and 120 m below present sea level (adapted from ref. 46, H. K. Voris, Field Museum of Natural History) and the major biogeographical boundaries recognized in the area. A, Wallace\u0026#39;s Line modified by Huxley; B, Wallace\u0026#39;s Line; C, Lydekker\u0026#39;s Line. Luzon Island lies in between the original Wallace\u0026#39;s Line and the Wallace\u0026#39;s Line modified by Huxley and was never connected to mainland Asia during the Quaternary.","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354836"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354836/Rhinocerotidae_and_Chalicotheriidae_Perissodactyla_Tapiromorpha_"><img alt="Research paper thumbnail of Rhinocerotidae and Chalicotheriidae (Perissodactyla, Tapiromorpha)" class="work-thumbnail" src="https://attachments.academia-assets.com/98275637/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354836/Rhinocerotidae_and_Chalicotheriidae_Perissodactyla_Tapiromorpha_">Rhinocerotidae and Chalicotheriidae (Perissodactyla, Tapiromorpha)</a></div><div class="wp-workCard_item"><span>Geodiversitas</span><span>, 2016</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Here we describe mandibular, dental, and postcranial remains referable to Rhinocerotidae and Chal...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Here we describe mandibular, dental, and postcranial remains referable to Rhinocerotidae and Chalicotheriidae (Perissodactyla) originating from the vertebrate localities of Küçükçekmece East and Küçükçekmece West, in Thrace (European Turkey). The four rhinocerotids recognized comprise the early diverging Ronzotherium sp. (one lower molar, reworked from Oligocene deposits; Küçükçekmece West), the two-horned rhinocerotine Ceratotherium neumayri (Osborn, 1900), and two small chilothere aceratheriines: Chilotherium schlosseri (Weber, 1905) and Persiatherium sp. A chalicotheriine chalicotheriid, Kalimantsia sp., is documented by two tooth fragments and an unfused second phalanx of undoubtful affinities in Küçükçekmece West. This occurrence substantiates the record of Kalimantsia, previously restricted to the type locality Kalimantsi-Pehsata, in SW Bulgaria, and allows notably for the first recognition of postcranial remains for this taxon. Although distinct in terms of taxonomic composition and relative abundance, the rhinocerotid assemblages of Küçükçekmece East and Küçükçekmece West are in total agreement with a single biostratigraphical age, estimated to be correlated with the late Vallesian MN10 zone.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="753bbba57989829a16ef6c80e9788fd7" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":98275637,"asset_id":96354836,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/98275637/download_file?st=MTczMzkwNDgxMyw4LjIyMi4yMDguMTQ2&st=MTczMzkwNDgxMiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354836"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354836"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354836; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354836]").text(description); $(".js-view-count[data-work-id=96354836]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354836; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354836']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354836, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "753bbba57989829a16ef6c80e9788fd7" } } $('.js-work-strip[data-work-id=96354836]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354836,"title":"Rhinocerotidae and Chalicotheriidae (Perissodactyla, Tapiromorpha)","translated_title":"","metadata":{"publisher":"Museum National d'Histoire Naturelle, Paris, France","ai_title_tag":"Fossil Remains of Rhinocerotidae and Chalicotheriidae in Turkey","grobid_abstract":"Here we describe mandibular, dental, and postcranial remains referable to Rhinocerotidae and Chalicotheriidae (Perissodactyla) originating from the vertebrate localities of Küçükçekmece East and Küçükçekmece West, in Thrace (European Turkey). The four rhinocerotids recognized comprise the early diverging Ronzotherium sp. (one lower molar, reworked from Oligocene deposits; Küçükçekmece West), the two-horned rhinocerotine Ceratotherium neumayri (Osborn, 1900), and two small chilothere aceratheriines: Chilotherium schlosseri (Weber, 1905) and Persiatherium sp. A chalicotheriine chalicotheriid, Kalimantsia sp., is documented by two tooth fragments and an unfused second phalanx of undoubtful affinities in Küçükçekmece West. This occurrence substantiates the record of Kalimantsia, previously restricted to the type locality Kalimantsi-Pehsata, in SW Bulgaria, and allows notably for the first recognition of postcranial remains for this taxon. Although distinct in terms of taxonomic composition and relative abundance, the rhinocerotid assemblages of Küçükçekmece East and Küçükçekmece West are in total agreement with a single biostratigraphical age, estimated to be correlated with the late Vallesian MN10 zone.","publication_date":{"day":null,"month":null,"year":2016,"errors":{}},"publication_name":"Geodiversitas","grobid_abstract_attachment_id":98275637},"translated_abstract":null,"internal_url":"https://www.academia.edu/96354836/Rhinocerotidae_and_Chalicotheriidae_Perissodactyla_Tapiromorpha_","translated_internal_url":"","created_at":"2023-02-05T12:27:25.409-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":98275637,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/98275637/thumbnails/1.jpg","file_name":"Antoine_20__20Sen_202016_20Geodiversitas.pdf","download_url":"https://www.academia.edu/attachments/98275637/download_file?st=MTczMzkwNDgxMyw4LjIyMi4yMDguMTQ2&st=MTczMzkwNDgxMiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Rhinocerotidae_and_Chalicotheriidae_Peri.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/98275637/Antoine_20__20Sen_202016_20Geodiversitas-libre.pdf?1675630162=\u0026response-content-disposition=attachment%3B+filename%3DRhinocerotidae_and_Chalicotheriidae_Peri.pdf\u0026Expires=1733908412\u0026Signature=gAoNcvnw9RitYg--2Fv4~hxpRt5xhvnrIs01xcHQ4avHeqw9oFB7Jdb2oP67WN6WMIGBFu0MuaO2RSFPR2H2j1gBSv58Htpx-FIb4wsom1H2vkT6wEZ8k0cYeIylZAQ92EO8OTN2KE34icLJN50Xh6UbaRyiRgtgUpTk5vYmy3Ki8EKLaPezJ1F5BpzAyejGkp9vhF-18b0a-Ugyrw7Srzu~846RKqY9opnBwKByVl6Twou0QTviYa8AnRzr~VgsfSm2YDJwpqS6Ec9DSxZgiZYIgr-8mYps7lg8MFX-TLj2cZNc0EY~f6sSnOJLJeVfPvZscH7rPADa3EOqA543sA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Rhinocerotidae_and_Chalicotheriidae_Perissodactyla_Tapiromorpha_","translated_slug":"","page_count":16,"language":"en","content_type":"Work","summary":"Here we describe mandibular, dental, and postcranial remains referable to Rhinocerotidae and Chalicotheriidae (Perissodactyla) originating from the vertebrate localities of Küçükçekmece East and Küçükçekmece West, in Thrace (European Turkey). The four rhinocerotids recognized comprise the early diverging Ronzotherium sp. (one lower molar, reworked from Oligocene deposits; Küçükçekmece West), the two-horned rhinocerotine Ceratotherium neumayri (Osborn, 1900), and two small chilothere aceratheriines: Chilotherium schlosseri (Weber, 1905) and Persiatherium sp. A chalicotheriine chalicotheriid, Kalimantsia sp., is documented by two tooth fragments and an unfused second phalanx of undoubtful affinities in Küçükçekmece West. This occurrence substantiates the record of Kalimantsia, previously restricted to the type locality Kalimantsi-Pehsata, in SW Bulgaria, and allows notably for the first recognition of postcranial remains for this taxon. Although distinct in terms of taxonomic composition and relative abundance, the rhinocerotid assemblages of Küçükçekmece East and Küçükçekmece West are in total agreement with a single biostratigraphical age, estimated to be correlated with the late Vallesian MN10 zone.","owner":{"id":156116780,"first_name":"guillaume","middle_initials":null,"last_name":"daver","page_name":"gdaver","domain_name":"independent","created_at":"2020-04-29T03:42:46.837-07:00","display_name":"guillaume daver","url":"https://independent.academia.edu/gdaver"},"attachments":[{"id":98275637,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/98275637/thumbnails/1.jpg","file_name":"Antoine_20__20Sen_202016_20Geodiversitas.pdf","download_url":"https://www.academia.edu/attachments/98275637/download_file?st=MTczMzkwNDgxMyw4LjIyMi4yMDguMTQ2&st=MTczMzkwNDgxMiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Rhinocerotidae_and_Chalicotheriidae_Peri.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/98275637/Antoine_20__20Sen_202016_20Geodiversitas-libre.pdf?1675630162=\u0026response-content-disposition=attachment%3B+filename%3DRhinocerotidae_and_Chalicotheriidae_Peri.pdf\u0026Expires=1733908412\u0026Signature=gAoNcvnw9RitYg--2Fv4~hxpRt5xhvnrIs01xcHQ4avHeqw9oFB7Jdb2oP67WN6WMIGBFu0MuaO2RSFPR2H2j1gBSv58Htpx-FIb4wsom1H2vkT6wEZ8k0cYeIylZAQ92EO8OTN2KE34icLJN50Xh6UbaRyiRgtgUpTk5vYmy3Ki8EKLaPezJ1F5BpzAyejGkp9vhF-18b0a-Ugyrw7Srzu~846RKqY9opnBwKByVl6Twou0QTviYa8AnRzr~VgsfSm2YDJwpqS6Ec9DSxZgiZYIgr-8mYps7lg8MFX-TLj2cZNc0EY~f6sSnOJLJeVfPvZscH7rPADa3EOqA543sA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":29521,"name":"Paleobiogeography","url":"https://www.academia.edu/Documents/in/Paleobiogeography"},{"id":77537,"name":"Rhinocerotidae","url":"https://www.academia.edu/Documents/in/Rhinocerotidae"},{"id":128561,"name":"Rhinoceros","url":"https://www.academia.edu/Documents/in/Rhinoceros"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="96354835"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/96354835/Proconsul_heseloni_distal_radial_and_ulnar_epiphyses_from_the_Kaswanga_Primate_Site_Rusinga_Island_Kenya"><img alt="Research paper thumbnail of Proconsul heseloni distal radial and ulnar epiphyses from the Kaswanga Primate Site, Rusinga Island, Kenya" class="work-thumbnail" src="https://attachments.academia-assets.com/98275671/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354835/Proconsul_heseloni_distal_radial_and_ulnar_epiphyses_from_the_Kaswanga_Primate_Site_Rusinga_Island_Kenya">Proconsul heseloni distal radial and ulnar epiphyses from the Kaswanga Primate Site, Rusinga Island, Kenya</a></div><div class="wp-workCard_item"><span>Journal of human evolution</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Only two distal epiphyses of a radius and ulna are consensually attributed to the holotype skelet...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Only two distal epiphyses of a radius and ulna are consensually attributed to the holotype skeleton of Proconsul heseloni, KNM-RU 2036. Here, we describe seven adult and immature distal antebrachial (radial and ulnar) epiphyses from two other individuals of P. heseloni from the Lower Miocene deposits of the Kaswanga Primate Site (KPS), Rusinga Island, Kenya. Because KNM-RU 2036 and KNM-KPS individuals III and VIII are conspecific and penecontemporaneous, their comparison provides the opportunity i) to characterize, for the first time, the morphological variation of the distal radioulnar joint in a Miocene ape, P. heseloni, and ii) to investigate the functional and evolutionary implications. Our results show that the distal antebrachial epiphyses of KNM-KPS III and VIII correspond to stages of bone maturation that are more advanced than those of KNM-RU 2036 (larger articulations and sharper articular borders and ligament attachments that are more developed). Accordingly, functional i...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="7338e4c4d68272d5bcecfd74b54ee15e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":98275671,"asset_id":96354835,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/98275671/download_file?st=MTczMzkwNDgxMyw4LjIyMi4yMDguMTQ2&st=MTczMzkwNDgxMiw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="96354835"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="96354835"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 96354835; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=96354835]").text(description); $(".js-view-count[data-work-id=96354835]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 96354835; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='96354835']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 96354835, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "7338e4c4d68272d5bcecfd74b54ee15e" } } $('.js-work-strip[data-work-id=96354835]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":96354835,"title":"Proconsul heseloni distal radial and ulnar epiphyses from the Kaswanga Primate Site, Rusinga Island, Kenya","translated_title":"","metadata":{"abstract":"Only two distal epiphyses of a radius and ulna are consensually attributed to the holotype skeleton of Proconsul heseloni, KNM-RU 2036. Here, we describe seven adult and immature distal antebrachial (radial and ulnar) epiphyses from two other individuals of P. heseloni from the Lower Miocene deposits of the Kaswanga Primate Site (KPS), Rusinga Island, Kenya. Because KNM-RU 2036 and KNM-KPS individuals III and VIII are conspecific and penecontemporaneous, their comparison provides the opportunity i) to characterize, for the first time, the morphological variation of the distal radioulnar joint in a Miocene ape, P. heseloni, and ii) to investigate the functional and evolutionary implications. Our results show that the distal antebrachial epiphyses of KNM-KPS III and VIII correspond to stages of bone maturation that are more advanced than those of KNM-RU 2036 (larger articulations and sharper articular borders and ligament attachments that are more developed). Accordingly, functional i...","ai_title_tag":"Morphological Variation of Distal Epiphyses in Proconsul heseloni","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"Journal of human evolution"},"translated_abstract":"Only two distal epiphyses of a radius and ulna are consensually attributed to the holotype skeleton of Proconsul heseloni, KNM-RU 2036. Here, we describe seven adult and immature distal antebrachial (radial and ulnar) epiphyses from two other individuals of P. heseloni from the Lower Miocene deposits of the Kaswanga Primate Site (KPS), Rusinga Island, Kenya. Because KNM-RU 2036 and KNM-KPS individuals III and VIII are conspecific and penecontemporaneous, their comparison provides the opportunity i) to characterize, for the first time, the morphological variation of the distal radioulnar joint in a Miocene ape, P. heseloni, and ii) to investigate the functional and evolutionary implications. Our results show that the distal antebrachial epiphyses of KNM-KPS III and VIII correspond to stages of bone maturation that are more advanced than those of KNM-RU 2036 (larger articulations and sharper articular borders and ligament attachments that are more developed). Accordingly, functional i...","internal_url":"https://www.academia.edu/96354835/Proconsul_heseloni_distal_radial_and_ulnar_epiphyses_from_the_Kaswanga_Primate_Site_Rusinga_Island_Kenya","translated_internal_url":"","created_at":"2023-02-05T12:27:25.280-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":156116780,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":98275671,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/98275671/thumbnails/1.jpg","file_name":"j.jhevol.2014.06.02120230205-1-4rcn1q.pdf","download_url":"https://www.academia.edu/attachments/98275671/download_file?st=MTczMzkwNDgxMyw4LjIyMi4yMDguMTQ2&st=MTczMzkwNDgxMiw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Proconsul_heseloni_distal_radial_and_uln.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/98275671/j.jhevol.2014.06.02120230205-1-4rcn1q-libre.pdf?1675630145=\u0026response-content-disposition=attachment%3B+filename%3DProconsul_heseloni_distal_radial_and_uln.pdf\u0026Expires=1733908412\u0026Signature=UU1OVrSKEIG~0fAM0xgb0dd6R3Qg35ppA5q1ty2ZDfEEg~ewuJg34Nq3DqHEvcKJJLSnC5Kw4alEPByzquw~qjY-5HUEhhBXQeVWMLvoS9LXENN3rmf3yXneoMjAjjaVuWSsKBQKYVz~soAmAoJDnLgLL5I1cCK5~DL7aFBhxGaKsy9oR-yRxzpJfqn3rkuH4AQpDRctWO2VAYsgP1K5dfGwGty9RhGv0Yt09Tmxp9r70GK5M75R0C-dByql6voLtBo1OgckhLipE-bI8Wv9Q-rl7jql2hZUTHCDFXYrd0uHNsTneh16I54X~2Nk104LqiSuUsAlBe-jWOXNXzVpbA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Proconsul_heseloni_distal_radial_and_ulnar_epiphyses_from_the_Kaswanga_Primate_Site_Rusinga_Island_Kenya","translated_slug":"","page_count":17,"language":"en","content_type":"Work","summary":"Only two distal epiphyses of a radius and ulna are consensually attributed to the holotype skeleton of Proconsul heseloni, KNM-RU 2036. 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Developments in Primatology: Progress and Prospects. Edited by Kristiaan D'Août and Evie E. Vereecke. New York: Springer. $179.00. xvi + 364 p.; ill.; index. ISBN: 978-1-4419-1419-4 (hc); 978-1-4419-1420-0 (eb). 2011" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/96354834/Primate_Locomotion_Linking_Field_and_Laboratory_Research_Developments_in_Primatology_Progress_and_Prospects_Edited_by_Kristiaan_DAo%C3%BBt_and_Evie_E_Vereecke_New_York_Springer_179_00_xvi_364_p_ill_index_ISBN_978_1_4419_1419_4_hc_978_1_4419_1420_0_eb_2011">Primate Locomotion: Linking Field and Laboratory Research. Developments in Primatology: Progress and Prospects. Edited by Kristiaan D'Août and Evie E. Vereecke. New York: Springer. $179.00. xvi + 364 p.; ill.; index. 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