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class="js-profile-view-count"></span></p></div></span></div><div class="user-bio-container"><div class="profile-bio fake-truncate js-profile-about" style="margin: 0px;">I am a  professional researcher retired but still interested in keeping with updated published papers in paleoanthropology , human origin and past vegetation and palaeoenvironmemt<br /><div class="js-profile-less-about u-linkUnstyled u-tcGrayDarker u-textDecorationUnderline u-displayNone">less</div></div></div><div class="ri-section"><div class="ri-section-header"><span>Interests</span></div><div class="ri-tags-container"><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="49112639" href="https://www.academia.edu/Documents/in/Miocene"><div id="js-react-on-rails-context" style="display:none" 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$(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="120775371"><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/120775371/Variability_in_the_Mountain_Environment_at_Melka_Kunture_Archaeological_Site_Ethiopia_During_the_Early_Pleistocene_1_7_Ma_and_the_Mid_Pleistocene_Transition_0_9_0_6_Ma_"><img alt="Research paper thumbnail of Variability in the Mountain Environment at Melka Kunture Archaeological Site, Ethiopia, During the Early Pleistocene (~1.7 Ma) and the Mid-Pleistocene Transition (0.9–0.6 Ma)" 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/120775371/Variability_in_the_Mountain_Environment_at_Melka_Kunture_Archaeological_Site_Ethiopia_During_the_Early_Pleistocene_1_7_Ma_and_the_Mid_Pleistocene_Transition_0_9_0_6_Ma_">Variability in the Mountain Environment at Melka Kunture Archaeological Site, Ethiopia, During the Early Pleistocene (~1.7 Ma) and the Mid-Pleistocene Transition (0.9–0.6 Ma)</a></div><div class="wp-workCard_item"><span>Vertebrate paleobiology and paleoanthropology series</span><span>, 2018</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In this paper, we present and discuss pollen data from the Early Pleistocene (1.8 to 1.6 Ma) – we...</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">In this paper, we present and discuss pollen data from the Early Pleistocene (1.8 to 1.6 Ma) – we use the revised timescale approved by IUGS, in which the base of the Pleistocene is defined by the GSSP of the Gelasian Stage at 2.588 (2.6) Ma (Gibbard et al. 2010) – and from the Mid-Pleistocene Transition (0.9 to 0.6 Ma) at Melka Kunture (Upper Awash, Ethiopia). At 2000 m asl in the Ethiopian highlands, these deposits yield many rich and successive archaeological sites, notably documenting the late Oldowan, the emergence of the Acheulean and the middle Acheulean. The stratigraphic position of the fifteen pollen samples is checked by 40Ar/39Ar dating and by geological investigation. Furthermore, they are now correlated to archaeological layers whose excavated lithic industries have been reinterpreted. Our study shows that mountain forest trees belonging to the present-day Afromontane complex were already established in Ethiopia at ~1.8 Ma and that the knappers of the Oldowan and early Acheulean could cope with mountain climatic conditions that had a large diurnal temperature range. Moreover, the new interpretation of pollen results emphasizes changes that occurred in the vegetation cover at 200- or 300-thousand-year snapshot intervals, one during the Early Pleistocene and another one later on, during the Mid-Pleistocene Transition. These changes concerned plant species and their respective abundance and appear to have been related to rainfall and temperature variability. The proportion of forest trees increased during wet episodes, whereas the influence of Afroalpine grassland indicators increased during cool and dry episodes. Variations in Early Pleistocene pollen data from Melka Kunture at ~1.8–1.6 Ma are consistent with isotopic evidence of precession variability as recorded at Olduvai and Turkana archaeological sites at ~2–1.8 Ma. For the Mid-Pleistocene Transition, variations in pollen data seem to match the climatic variability of isotopic and long pollen records from the Mediterranean region, notably upon the onset of dominant 100 ka-long glacial/interglacial cycles.</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="120775371"><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="120775371"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 120775371; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=120775371]").text(description); $(".js-view-count[data-work-id=120775371]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 120775371; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='120775371']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 120775371, 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" } } $('.js-work-strip[data-work-id=120775371]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":120775371,"title":"Variability in the Mountain Environment at Melka Kunture Archaeological Site, Ethiopia, During the Early Pleistocene (~1.7 Ma) and the Mid-Pleistocene Transition (0.9–0.6 Ma)","translated_title":"","metadata":{"abstract":"In this paper, we present and discuss pollen data from the Early Pleistocene (1.8 to 1.6 Ma) – we use the revised timescale approved by IUGS, in which the base of the Pleistocene is defined by the GSSP of the Gelasian Stage at 2.588 (2.6) Ma (Gibbard et al. 2010) – and from the Mid-Pleistocene Transition (0.9 to 0.6 Ma) at Melka Kunture (Upper Awash, Ethiopia). At 2000 m asl in the Ethiopian highlands, these deposits yield many rich and successive archaeological sites, notably documenting the late Oldowan, the emergence of the Acheulean and the middle Acheulean. The stratigraphic position of the fifteen pollen samples is checked by 40Ar/39Ar dating and by geological investigation. Furthermore, they are now correlated to archaeological layers whose excavated lithic industries have been reinterpreted. Our study shows that mountain forest trees belonging to the present-day Afromontane complex were already established in Ethiopia at ~1.8 Ma and that the knappers of the Oldowan and early Acheulean could cope with mountain climatic conditions that had a large diurnal temperature range. Moreover, the new interpretation of pollen results emphasizes changes that occurred in the vegetation cover at 200- or 300-thousand-year snapshot intervals, one during the Early Pleistocene and another one later on, during the Mid-Pleistocene Transition. These changes concerned plant species and their respective abundance and appear to have been related to rainfall and temperature variability. The proportion of forest trees increased during wet episodes, whereas the influence of Afroalpine grassland indicators increased during cool and dry episodes. Variations in Early Pleistocene pollen data from Melka Kunture at ~1.8–1.6 Ma are consistent with isotopic evidence of precession variability as recorded at Olduvai and Turkana archaeological sites at ~2–1.8 Ma. For the Mid-Pleistocene Transition, variations in pollen data seem to match the climatic variability of isotopic and long pollen records from the Mediterranean region, notably upon the onset of dominant 100 ka-long glacial/interglacial cycles.","publisher":"Springer Nature (Netherlands)","publication_date":{"day":null,"month":null,"year":2018,"errors":{}},"publication_name":"Vertebrate paleobiology and paleoanthropology series"},"translated_abstract":"In this paper, we present and discuss pollen data from the Early Pleistocene (1.8 to 1.6 Ma) – we use the revised timescale approved by IUGS, in which the base of the Pleistocene is defined by the GSSP of the Gelasian Stage at 2.588 (2.6) Ma (Gibbard et al. 2010) – and from the Mid-Pleistocene Transition (0.9 to 0.6 Ma) at Melka Kunture (Upper Awash, Ethiopia). At 2000 m asl in the Ethiopian highlands, these deposits yield many rich and successive archaeological sites, notably documenting the late Oldowan, the emergence of the Acheulean and the middle Acheulean. The stratigraphic position of the fifteen pollen samples is checked by 40Ar/39Ar dating and by geological investigation. Furthermore, they are now correlated to archaeological layers whose excavated lithic industries have been reinterpreted. Our study shows that mountain forest trees belonging to the present-day Afromontane complex were already established in Ethiopia at ~1.8 Ma and that the knappers of the Oldowan and early Acheulean could cope with mountain climatic conditions that had a large diurnal temperature range. Moreover, the new interpretation of pollen results emphasizes changes that occurred in the vegetation cover at 200- or 300-thousand-year snapshot intervals, one during the Early Pleistocene and another one later on, during the Mid-Pleistocene Transition. These changes concerned plant species and their respective abundance and appear to have been related to rainfall and temperature variability. The proportion of forest trees increased during wet episodes, whereas the influence of Afroalpine grassland indicators increased during cool and dry episodes. Variations in Early Pleistocene pollen data from Melka Kunture at ~1.8–1.6 Ma are consistent with isotopic evidence of precession variability as recorded at Olduvai and Turkana archaeological sites at ~2–1.8 Ma. For the Mid-Pleistocene Transition, variations in pollen data seem to match the climatic variability of isotopic and long pollen records from the Mediterranean region, notably upon the onset of dominant 100 ka-long glacial/interglacial cycles.","internal_url":"https://www.academia.edu/120775371/Variability_in_the_Mountain_Environment_at_Melka_Kunture_Archaeological_Site_Ethiopia_During_the_Early_Pleistocene_1_7_Ma_and_the_Mid_Pleistocene_Transition_0_9_0_6_Ma_","translated_internal_url":"","created_at":"2024-06-09T09:16:10.733-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":49112639,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Variability_in_the_Mountain_Environment_at_Melka_Kunture_Archaeological_Site_Ethiopia_During_the_Early_Pleistocene_1_7_Ma_and_the_Mid_Pleistocene_Transition_0_9_0_6_Ma_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":49112639,"first_name":"raymonde","middle_initials":null,"last_name":"Bonnefille","page_name":"rBonnefille","domain_name":"independent","created_at":"2016-05-23T02:32:27.321-07:00","display_name":"raymonde Bonnefille","url":"https://independent.academia.edu/rBonnefille"},"attachments":[],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":392,"name":"Archaeology","url":"https://www.academia.edu/Documents/in/Archaeology"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":30254,"name":"Pleistocene","url":"https://www.academia.edu/Documents/in/Pleistocene"},{"id":77502,"name":"Early Pleistocene","url":"https://www.academia.edu/Documents/in/Early_Pleistocene"},{"id":3647879,"name":"Springer Ebooks","url":"https://www.academia.edu/Documents/in/Springer_Ebooks"}],"urls":[{"id":42791705,"url":"https://doi.org/10.1007/978-3-319-75985-2_5"}]}, 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="120775368"><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/120775368/Modern_pollen_rain_from_the_Biligirirangan_Melagiri_hills_of_southern_Eastern_Ghats_India"><img alt="Research paper thumbnail of Modern pollen rain from the Biligirirangan–Melagiri hills of southern Eastern Ghats, India" class="work-thumbnail" src="https://attachments.academia-assets.com/115879254/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/120775368/Modern_pollen_rain_from_the_Biligirirangan_Melagiri_hills_of_southern_Eastern_Ghats_India">Modern pollen rain from the Biligirirangan–Melagiri hills of southern Eastern Ghats, India</a></div><div class="wp-workCard_item"><span>Review of Palaeobotany and Palynology</span><span>, 2000</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A total of 39 soil surface samples collected between 11 degrees 30&amp;amp;amp;amp;amp;amp;amp;am...</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">A total of 39 soil surface samples collected between 11 degrees 30&amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;N 76 degrees 45&amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;E and 12 degrees 45&amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;N 78 degrees 15&amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;E from the mainly deciduous forests in the Biligirirangan-Melagiri hills of the southern Eastern Ghats were analysed for their pollen content. The samples are distributed among four different deciduous and evergreen vegetation types between 210 and 1700m altitudes and fall within three distinct rainfall regimes. The aims of this paper are to provide new data on the modern pollen rain from the Southern Eastern Ghats, a region characterized by a unique and complex climate and vegetation, and to interpret these data using multivariate statistics and the diagram of pollen percentages. We could distinguish first between the deciduous and the evergreen forests and then also between different types of deciduous forest. The distinction between the evergreen and deciduous forests was based on a humidity gradient and that among the deciduous forests on a physiognomic gradient identified through correspondence analysis. The above analysis also allowed us to identify a set of 14 pollen taxa markers and 11 associated pollen taxa that help differentiate the evergreen from deciduous forests. Similarly, a set of 12 pollen taxa markers and six associated pollen taxa was demarcated to help distinguish woodland formations from scrub and thicket formations, among the deciduous vegetation. We could also differentiate amongst the four distinct vegetation types sampled, on the basis of distinct associations of both tree and herb pollen taxa according to their relative abundance in the pollen diagram as well as on the proportion of total arboreal pollen. The ground cover of grasses and other herbaceous plants in the deciduous forests is effectively demonstrated by percentages of non-arboreal pollen varying between 40 and 70%. The 1000m altitude limit reflecting a gradient of humidity and the physiognomic gradient among deciduous forests seem to be important in this region.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1f9a3e7b335313799ba618fbc1772fc7" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":115879254,"asset_id":120775368,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/115879254/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&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="120775368"><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="120775368"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 120775368; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=120775368]").text(description); $(".js-view-count[data-work-id=120775368]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 120775368; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='120775368']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 120775368, 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: "1f9a3e7b335313799ba618fbc1772fc7" } } $('.js-work-strip[data-work-id=120775368]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":120775368,"title":"Modern pollen rain from the Biligirirangan–Melagiri hills of southern Eastern Ghats, India","translated_title":"","metadata":{"abstract":"A total of 39 soil surface samples collected between 11 degrees 30\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;N 76 degrees 45\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;E and 12 degrees 45\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;N 78 degrees 15\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;E from the mainly deciduous forests in the Biligirirangan-Melagiri hills of the southern Eastern Ghats were analysed for their pollen content. The samples are distributed among four different deciduous and evergreen vegetation types between 210 and 1700m altitudes and fall within three distinct rainfall regimes. The aims of this paper are to provide new data on the modern pollen rain from the Southern Eastern Ghats, a region characterized by a unique and complex climate and vegetation, and to interpret these data using multivariate statistics and the diagram of pollen percentages. We could distinguish first between the deciduous and the evergreen forests and then also between different types of deciduous forest. The distinction between the evergreen and deciduous forests was based on a humidity gradient and that among the deciduous forests on a physiognomic gradient identified through correspondence analysis. The above analysis also allowed us to identify a set of 14 pollen taxa markers and 11 associated pollen taxa that help differentiate the evergreen from deciduous forests. Similarly, a set of 12 pollen taxa markers and six associated pollen taxa was demarcated to help distinguish woodland formations from scrub and thicket formations, among the deciduous vegetation. We could also differentiate amongst the four distinct vegetation types sampled, on the basis of distinct associations of both tree and herb pollen taxa according to their relative abundance in the pollen diagram as well as on the proportion of total arboreal pollen. The ground cover of grasses and other herbaceous plants in the deciduous forests is effectively demonstrated by percentages of non-arboreal pollen varying between 40 and 70%. The 1000m altitude limit reflecting a gradient of humidity and the physiognomic gradient among deciduous forests seem to be important in this region.","publisher":"Elsevier BV","publication_date":{"day":null,"month":null,"year":2000,"errors":{}},"publication_name":"Review of Palaeobotany and Palynology"},"translated_abstract":"A total of 39 soil surface samples collected between 11 degrees 30\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;N 76 degrees 45\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;E and 12 degrees 45\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;N 78 degrees 15\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;E from the mainly deciduous forests in the Biligirirangan-Melagiri hills of the southern Eastern Ghats were analysed for their pollen content. The samples are distributed among four different deciduous and evergreen vegetation types between 210 and 1700m altitudes and fall within three distinct rainfall regimes. The aims of this paper are to provide new data on the modern pollen rain from the Southern Eastern Ghats, a region characterized by a unique and complex climate and vegetation, and to interpret these data using multivariate statistics and the diagram of pollen percentages. We could distinguish first between the deciduous and the evergreen forests and then also between different types of deciduous forest. The distinction between the evergreen and deciduous forests was based on a humidity gradient and that among the deciduous forests on a physiognomic gradient identified through correspondence analysis. The above analysis also allowed us to identify a set of 14 pollen taxa markers and 11 associated pollen taxa that help differentiate the evergreen from deciduous forests. Similarly, a set of 12 pollen taxa markers and six associated pollen taxa was demarcated to help distinguish woodland formations from scrub and thicket formations, among the deciduous vegetation. We could also differentiate amongst the four distinct vegetation types sampled, on the basis of distinct associations of both tree and herb pollen taxa according to their relative abundance in the pollen diagram as well as on the proportion of total arboreal pollen. The ground cover of grasses and other herbaceous plants in the deciduous forests is effectively demonstrated by percentages of non-arboreal pollen varying between 40 and 70%. The 1000m altitude limit reflecting a gradient of humidity and the physiognomic gradient among deciduous forests seem to be important in this region.","internal_url":"https://www.academia.edu/120775368/Modern_pollen_rain_from_the_Biligirirangan_Melagiri_hills_of_southern_Eastern_Ghats_India","translated_internal_url":"","created_at":"2024-06-09T09:16:10.505-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":49112639,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":115879254,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/115879254/thumbnails/1.jpg","file_name":"Anupamaetal2000.pdf","download_url":"https://www.academia.edu/attachments/115879254/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modern_pollen_rain_from_the_Biligirirang.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/115879254/Anupamaetal2000-libre.pdf?1718099157=\u0026response-content-disposition=attachment%3B+filename%3DModern_pollen_rain_from_the_Biligirirang.pdf\u0026Expires=1732549234\u0026Signature=SuoDjDOxPyRGZfJFYTCAfYaSv4RQnI7Q9QqF7iVdyLFX-hi43v-kVd0IebP1qSOlfXbECuoYBn~iZBH4SIhKyUOvRLHS-RX2rcEsCjdP~Wq8R~4mzm3Jf4WWF2uoLjVDGr4DmsagFs9SIdtAxi~b6gYBdn41B3~71QnDX91Ld06k8VREwSgbAEUHEL15Yf~ngew8W7ngdmb0EDERsWwi7w~QEafaNAYD2~HhaaCoMeH3fIkEaBFv43ZA5cYw-c8snshr0Fmm-i97ABq~-sr~eoMFFqIbyxZq1mGacFibzd0tJmXCLcH16J9J6M04s2VhECmIBOcdgGlsrPdMn1T5lA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Modern_pollen_rain_from_the_Biligirirangan_Melagiri_hills_of_southern_Eastern_Ghats_India","translated_slug":"","page_count":22,"language":"en","content_type":"Work","owner":{"id":49112639,"first_name":"raymonde","middle_initials":null,"last_name":"Bonnefille","page_name":"rBonnefille","domain_name":"independent","created_at":"2016-05-23T02:32:27.321-07:00","display_name":"raymonde Bonnefille","url":"https://independent.academia.edu/rBonnefille"},"attachments":[{"id":115879254,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/115879254/thumbnails/1.jpg","file_name":"Anupamaetal2000.pdf","download_url":"https://www.academia.edu/attachments/115879254/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modern_pollen_rain_from_the_Biligirirang.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/115879254/Anupamaetal2000-libre.pdf?1718099157=\u0026response-content-disposition=attachment%3B+filename%3DModern_pollen_rain_from_the_Biligirirang.pdf\u0026Expires=1732549234\u0026Signature=SuoDjDOxPyRGZfJFYTCAfYaSv4RQnI7Q9QqF7iVdyLFX-hi43v-kVd0IebP1qSOlfXbECuoYBn~iZBH4SIhKyUOvRLHS-RX2rcEsCjdP~Wq8R~4mzm3Jf4WWF2uoLjVDGr4DmsagFs9SIdtAxi~b6gYBdn41B3~71QnDX91Ld06k8VREwSgbAEUHEL15Yf~ngew8W7ngdmb0EDERsWwi7w~QEafaNAYD2~HhaaCoMeH3fIkEaBFv43ZA5cYw-c8snshr0Fmm-i97ABq~-sr~eoMFFqIbyxZq1mGacFibzd0tJmXCLcH16J9J6M04s2VhECmIBOcdgGlsrPdMn1T5lA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":1352,"name":"Multivariate Statistics","url":"https://www.academia.edu/Documents/in/Multivariate_Statistics"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":26327,"name":"Medicine","url":"https://www.academia.edu/Documents/in/Medicine"},{"id":28230,"name":"Correspondence Analysis","url":"https://www.academia.edu/Documents/in/Correspondence_Analysis"},{"id":32759,"name":"Palaeobotany","url":"https://www.academia.edu/Documents/in/Palaeobotany"},{"id":83086,"name":"Pollen","url":"https://www.academia.edu/Documents/in/Pollen"},{"id":372637,"name":"Deciduous","url":"https://www.academia.edu/Documents/in/Deciduous"},{"id":745347,"name":"Relative Abundance","url":"https://www.academia.edu/Documents/in/Relative_Abundance"},{"id":843041,"name":"Evergreen","url":"https://www.academia.edu/Documents/in/Evergreen"},{"id":1004965,"name":"Deciduous Forest","url":"https://www.academia.edu/Documents/in/Deciduous_Forest"}],"urls":[{"id":42791703,"url":"https://api.elsevier.com/content/article/PII:S0034666799000391?httpAccept=text/xml"}]}, 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="120775365"><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/120775365/Modern_pollen_spectra_from_tropical_South_India_and_Sri_Lanka_altitudinal_distribution"><img alt="Research paper thumbnail of Modern pollen spectra from tropical South India and Sri Lanka: altitudinal distribution" class="work-thumbnail" src="https://attachments.academia-assets.com/115878973/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/120775365/Modern_pollen_spectra_from_tropical_South_India_and_Sri_Lanka_altitudinal_distribution">Modern pollen spectra from tropical South India and Sri Lanka: altitudinal distribution</a></div><div class="wp-workCard_item"><span>Journal of Biogeography</span><span>, 1999</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">SummaryWe analysed the pollen content of 106 surface soil samples from evergreen and deciduous tr...</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">SummaryWe analysed the pollen content of 106 surface soil samples from evergreen and deciduous tropical forests distributed between 6° and 13° of latitude north in South India and Sri Lanka. The samples were collected along altitudinal gradients, ranging from 50 to 2420 m, in five regions that experience different rainfall regimes. Original pollen data from tropical vegetation subjected to seasonal monsoon rains are presented along altitude/temperature gradients. This paper includes a summarized description of the vegetation types mapped in the area.The pollen results are presented in the form of quantitative pollen diagrams and correspondence analyses. They show clear distinct pollen assemblages and markers for all types of vegetation in deciduous and evergreen vegetation. Forests are well identified by percentages of Arboreal Pollen greater than 50%, despite the fact that Dipterocarpaceae and Lauraceae are hardly recorded by pollen.The pollen distinction between low, medium and hi...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="8f0eb9763ca8561378df20f55cde8be8" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":115878973,"asset_id":120775365,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/115878973/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&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="120775365"><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="120775365"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 120775365; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=120775365]").text(description); $(".js-view-count[data-work-id=120775365]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 120775365; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='120775365']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 120775365, 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: "8f0eb9763ca8561378df20f55cde8be8" } } $('.js-work-strip[data-work-id=120775365]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":120775365,"title":"Modern pollen spectra from tropical South India and Sri Lanka: altitudinal distribution","translated_title":"","metadata":{"abstract":"SummaryWe analysed the pollen content of 106 surface soil samples from evergreen and deciduous tropical forests distributed between 6° and 13° of latitude north in South India and Sri Lanka. The samples were collected along altitudinal gradients, ranging from 50 to 2420 m, in five regions that experience different rainfall regimes. Original pollen data from tropical vegetation subjected to seasonal monsoon rains are presented along altitude/temperature gradients. This paper includes a summarized description of the vegetation types mapped in the area.The pollen results are presented in the form of quantitative pollen diagrams and correspondence analyses. They show clear distinct pollen assemblages and markers for all types of vegetation in deciduous and evergreen vegetation. Forests are well identified by percentages of Arboreal Pollen greater than 50%, despite the fact that Dipterocarpaceae and Lauraceae are hardly recorded by pollen.The pollen distinction between low, medium and hi...","publisher":"Wiley","publication_date":{"day":null,"month":null,"year":1999,"errors":{}},"publication_name":"Journal of Biogeography"},"translated_abstract":"SummaryWe analysed the pollen content of 106 surface soil samples from evergreen and deciduous tropical forests distributed between 6° and 13° of latitude north in South India and Sri Lanka. The samples were collected along altitudinal gradients, ranging from 50 to 2420 m, in five regions that experience different rainfall regimes. Original pollen data from tropical vegetation subjected to seasonal monsoon rains are presented along altitude/temperature gradients. This paper includes a summarized description of the vegetation types mapped in the area.The pollen results are presented in the form of quantitative pollen diagrams and correspondence analyses. They show clear distinct pollen assemblages and markers for all types of vegetation in deciduous and evergreen vegetation. Forests are well identified by percentages of Arboreal Pollen greater than 50%, despite the fact that Dipterocarpaceae and Lauraceae are hardly recorded by pollen.The pollen distinction between low, medium and hi...","internal_url":"https://www.academia.edu/120775365/Modern_pollen_spectra_from_tropical_South_India_and_Sri_Lanka_altitudinal_distribution","translated_internal_url":"","created_at":"2024-06-09T09:16:09.273-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":49112639,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":115878973,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/115878973/thumbnails/1.jpg","file_name":"1999_Bonnefille_et_al_JBIO.pdf","download_url":"https://www.academia.edu/attachments/115878973/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modern_pollen_spectra_from_tropical_Sout.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/115878973/1999_Bonnefille_et_al_JBIO-libre.pdf?1718099189=\u0026response-content-disposition=attachment%3B+filename%3DModern_pollen_spectra_from_tropical_Sout.pdf\u0026Expires=1732549234\u0026Signature=Buc0Q7jYQvSiC66Hft0UPR6-WMJloghoZa0tCrmDmtUrSNfR-VID2tLqz7Bj9INkleYxk~LwJsiIZgIDcSOlbpqmhjC7HCrFcTgJNosaQH8NDewKewkJde3XFHq6XvOdUg9h3ohd0pp4jZIHnThHwljl~CpS6oy2l8ByDoX6mRJxIeERxA~JNKKpu~GS7J1MIqKil9HbpM8qrr~-LkeVDpip2u7TpDVHP0L0Dr2JM3jQXfD9oPp0OBl6YWKL28vjAmP06SQc-8tEhQ0hBmsxH99dPCqNVyFwVMlH~O8Y14aG0GHE5m3O0ZHs473KyloT593hUQHLPK3vcDJ~yu2mZQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Modern_pollen_spectra_from_tropical_South_India_and_Sri_Lanka_altitudinal_distribution","translated_slug":"","page_count":27,"language":"en","content_type":"Work","owner":{"id":49112639,"first_name":"raymonde","middle_initials":null,"last_name":"Bonnefille","page_name":"rBonnefille","domain_name":"independent","created_at":"2016-05-23T02:32:27.321-07:00","display_name":"raymonde Bonnefille","url":"https://independent.academia.edu/rBonnefille"},"attachments":[{"id":115878973,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/115878973/thumbnails/1.jpg","file_name":"1999_Bonnefille_et_al_JBIO.pdf","download_url":"https://www.academia.edu/attachments/115878973/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modern_pollen_spectra_from_tropical_Sout.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/115878973/1999_Bonnefille_et_al_JBIO-libre.pdf?1718099189=\u0026response-content-disposition=attachment%3B+filename%3DModern_pollen_spectra_from_tropical_Sout.pdf\u0026Expires=1732549234\u0026Signature=Buc0Q7jYQvSiC66Hft0UPR6-WMJloghoZa0tCrmDmtUrSNfR-VID2tLqz7Bj9INkleYxk~LwJsiIZgIDcSOlbpqmhjC7HCrFcTgJNosaQH8NDewKewkJde3XFHq6XvOdUg9h3ohd0pp4jZIHnThHwljl~CpS6oy2l8ByDoX6mRJxIeERxA~JNKKpu~GS7J1MIqKil9HbpM8qrr~-LkeVDpip2u7TpDVHP0L0Dr2JM3jQXfD9oPp0OBl6YWKL28vjAmP06SQc-8tEhQ0hBmsxH99dPCqNVyFwVMlH~O8Y14aG0GHE5m3O0ZHs473KyloT593hUQHLPK3vcDJ~yu2mZQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":9850,"name":"Sri Lanka","url":"https://www.academia.edu/Documents/in/Sri_Lanka"},{"id":17823,"name":"Biogeography","url":"https://www.academia.edu/Documents/in/Biogeography"},{"id":20771,"name":"South India","url":"https://www.academia.edu/Documents/in/South_India"},{"id":43838,"name":"India","url":"https://www.academia.edu/Documents/in/India"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":76763,"name":"Tropics","url":"https://www.academia.edu/Documents/in/Tropics"},{"id":83086,"name":"Pollen","url":"https://www.academia.edu/Documents/in/Pollen"},{"id":168657,"name":"Evergreen Forest","url":"https://www.academia.edu/Documents/in/Evergreen_Forest"},{"id":304559,"name":"Modern pollen rain","url":"https://www.academia.edu/Documents/in/Modern_pollen_rain"},{"id":372637,"name":"Deciduous","url":"https://www.academia.edu/Documents/in/Deciduous"},{"id":564837,"name":"Tropical forests","url":"https://www.academia.edu/Documents/in/Tropical_forests"},{"id":789599,"name":"Biome","url":"https://www.academia.edu/Documents/in/Biome"},{"id":843041,"name":"Evergreen","url":"https://www.academia.edu/Documents/in/Evergreen"},{"id":1299102,"name":"Arboreal Locomotion","url":"https://www.academia.edu/Documents/in/Arboreal_Locomotion"}],"urls":[{"id":42791702,"url":"https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-2699.1999.00359.x"}]}, dispatcherData: dispatcherData }); 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Our aim is to infer the diet, habitat, and environment at both sites and provide a broader paleoecological reconstruction. During the Pleistocene, the vegetation of the highlands of Ethiopia belonged to the \"Dry evergreen Afromontane Forest and grassland complex\", distinct from the savanna of lower elevations in East Africa. Our carbon isotopic results indicate that all the analyzed faunal taxa were grazers, consuming C 4 grasses, while oxygen isotopic results clearly discriminate the taxa according to their semi-aquatic or terrestrial habitats. These results are consistent with the analysis of the faunal assemblages and the palynological results, suggesting extended mountain grasslands in the landscape at Garba IVD. In contrast, the carbon isotopic results do not totally agree with the pollen paleoenvironmental reconstruction at Gombore IB, where the open vegetation was interrupted by forests and bushy vegetation. Stable isotopes and pollen data provide different outcomes (feeding strategies vs. nearby plants) and have different temporal and spatial resolutions. This is relevant when reconstructing past environments by exclusively using independent proxies. Furthermore, isotopic comparisons with other East African archaeological sites of the Lower Pleistocene age indicate that all the analyzed taxa fed on C 4 grasses, and that their dietary strategies were not affected by differences linked to various elevations.","publication_date":{"day":17,"month":10,"year":2022,"errors":{}},"publication_name":"Research Square (Research 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I. Vegetation, lake-levels and geochemistry" class="work-thumbnail" src="https://attachments.academia-assets.com/118740219/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/124533163/Tropical_climates_at_the_Last_Glacial_Maximum_a_new_synthesis_of_terrestrial_palaeoclimate_data_I_Vegetation_lake_levels_and_geochemistry">Tropical climates at the Last Glacial Maximum: a new synthesis of terrestrial palaeoclimate data. I. Vegetation, lake-levels and geochemistry</a></div><div class="wp-workCard_item"><span>Climate Dynamics</span><span>, 1999</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f60ff8919b4b4ed5414d3374e9715bb1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":118740219,"asset_id":124533163,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/118740219/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&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="124533163"><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="124533163"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124533163; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124533163]").text(description); $(".js-view-count[data-work-id=124533163]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124533163; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124533163']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124533163, 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: "f60ff8919b4b4ed5414d3374e9715bb1" } } $('.js-work-strip[data-work-id=124533163]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124533163,"title":"Tropical climates at the Last Glacial Maximum: a new synthesis of terrestrial palaeoclimate data. 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$(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="120775371"><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/120775371/Variability_in_the_Mountain_Environment_at_Melka_Kunture_Archaeological_Site_Ethiopia_During_the_Early_Pleistocene_1_7_Ma_and_the_Mid_Pleistocene_Transition_0_9_0_6_Ma_"><img alt="Research paper thumbnail of Variability in the Mountain Environment at Melka Kunture Archaeological Site, Ethiopia, During the Early Pleistocene (~1.7 Ma) and the Mid-Pleistocene Transition (0.9–0.6 Ma)" 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/120775371/Variability_in_the_Mountain_Environment_at_Melka_Kunture_Archaeological_Site_Ethiopia_During_the_Early_Pleistocene_1_7_Ma_and_the_Mid_Pleistocene_Transition_0_9_0_6_Ma_">Variability in the Mountain Environment at Melka Kunture Archaeological Site, Ethiopia, During the Early Pleistocene (~1.7 Ma) and the Mid-Pleistocene Transition (0.9–0.6 Ma)</a></div><div class="wp-workCard_item"><span>Vertebrate paleobiology and paleoanthropology series</span><span>, 2018</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In this paper, we present and discuss pollen data from the Early Pleistocene (1.8 to 1.6 Ma) – we...</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">In this paper, we present and discuss pollen data from the Early Pleistocene (1.8 to 1.6 Ma) – we use the revised timescale approved by IUGS, in which the base of the Pleistocene is defined by the GSSP of the Gelasian Stage at 2.588 (2.6) Ma (Gibbard et al. 2010) – and from the Mid-Pleistocene Transition (0.9 to 0.6 Ma) at Melka Kunture (Upper Awash, Ethiopia). At 2000 m asl in the Ethiopian highlands, these deposits yield many rich and successive archaeological sites, notably documenting the late Oldowan, the emergence of the Acheulean and the middle Acheulean. The stratigraphic position of the fifteen pollen samples is checked by 40Ar/39Ar dating and by geological investigation. Furthermore, they are now correlated to archaeological layers whose excavated lithic industries have been reinterpreted. Our study shows that mountain forest trees belonging to the present-day Afromontane complex were already established in Ethiopia at ~1.8 Ma and that the knappers of the Oldowan and early Acheulean could cope with mountain climatic conditions that had a large diurnal temperature range. Moreover, the new interpretation of pollen results emphasizes changes that occurred in the vegetation cover at 200- or 300-thousand-year snapshot intervals, one during the Early Pleistocene and another one later on, during the Mid-Pleistocene Transition. These changes concerned plant species and their respective abundance and appear to have been related to rainfall and temperature variability. The proportion of forest trees increased during wet episodes, whereas the influence of Afroalpine grassland indicators increased during cool and dry episodes. Variations in Early Pleistocene pollen data from Melka Kunture at ~1.8–1.6 Ma are consistent with isotopic evidence of precession variability as recorded at Olduvai and Turkana archaeological sites at ~2–1.8 Ma. For the Mid-Pleistocene Transition, variations in pollen data seem to match the climatic variability of isotopic and long pollen records from the Mediterranean region, notably upon the onset of dominant 100 ka-long glacial/interglacial cycles.</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="120775371"><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="120775371"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 120775371; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=120775371]").text(description); $(".js-view-count[data-work-id=120775371]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 120775371; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='120775371']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 120775371, 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" } } $('.js-work-strip[data-work-id=120775371]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":120775371,"title":"Variability in the Mountain Environment at Melka Kunture Archaeological Site, Ethiopia, During the Early Pleistocene (~1.7 Ma) and the Mid-Pleistocene Transition (0.9–0.6 Ma)","translated_title":"","metadata":{"abstract":"In this paper, we present and discuss pollen data from the Early Pleistocene (1.8 to 1.6 Ma) – we use the revised timescale approved by IUGS, in which the base of the Pleistocene is defined by the GSSP of the Gelasian Stage at 2.588 (2.6) Ma (Gibbard et al. 2010) – and from the Mid-Pleistocene Transition (0.9 to 0.6 Ma) at Melka Kunture (Upper Awash, Ethiopia). At 2000 m asl in the Ethiopian highlands, these deposits yield many rich and successive archaeological sites, notably documenting the late Oldowan, the emergence of the Acheulean and the middle Acheulean. The stratigraphic position of the fifteen pollen samples is checked by 40Ar/39Ar dating and by geological investigation. Furthermore, they are now correlated to archaeological layers whose excavated lithic industries have been reinterpreted. Our study shows that mountain forest trees belonging to the present-day Afromontane complex were already established in Ethiopia at ~1.8 Ma and that the knappers of the Oldowan and early Acheulean could cope with mountain climatic conditions that had a large diurnal temperature range. Moreover, the new interpretation of pollen results emphasizes changes that occurred in the vegetation cover at 200- or 300-thousand-year snapshot intervals, one during the Early Pleistocene and another one later on, during the Mid-Pleistocene Transition. These changes concerned plant species and their respective abundance and appear to have been related to rainfall and temperature variability. The proportion of forest trees increased during wet episodes, whereas the influence of Afroalpine grassland indicators increased during cool and dry episodes. Variations in Early Pleistocene pollen data from Melka Kunture at ~1.8–1.6 Ma are consistent with isotopic evidence of precession variability as recorded at Olduvai and Turkana archaeological sites at ~2–1.8 Ma. 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At 2000 m asl in the Ethiopian highlands, these deposits yield many rich and successive archaeological sites, notably documenting the late Oldowan, the emergence of the Acheulean and the middle Acheulean. The stratigraphic position of the fifteen pollen samples is checked by 40Ar/39Ar dating and by geological investigation. Furthermore, they are now correlated to archaeological layers whose excavated lithic industries have been reinterpreted. Our study shows that mountain forest trees belonging to the present-day Afromontane complex were already established in Ethiopia at ~1.8 Ma and that the knappers of the Oldowan and early Acheulean could cope with mountain climatic conditions that had a large diurnal temperature range. Moreover, the new interpretation of pollen results emphasizes changes that occurred in the vegetation cover at 200- or 300-thousand-year snapshot intervals, one during the Early Pleistocene and another one later on, during the Mid-Pleistocene Transition. These changes concerned plant species and their respective abundance and appear to have been related to rainfall and temperature variability. The proportion of forest trees increased during wet episodes, whereas the influence of Afroalpine grassland indicators increased during cool and dry episodes. Variations in Early Pleistocene pollen data from Melka Kunture at ~1.8–1.6 Ma are consistent with isotopic evidence of precession variability as recorded at Olduvai and Turkana archaeological sites at ~2–1.8 Ma. For the Mid-Pleistocene Transition, variations in pollen data seem to match the climatic variability of isotopic and long pollen records from the Mediterranean region, notably upon the onset of dominant 100 ka-long glacial/interglacial cycles.","internal_url":"https://www.academia.edu/120775371/Variability_in_the_Mountain_Environment_at_Melka_Kunture_Archaeological_Site_Ethiopia_During_the_Early_Pleistocene_1_7_Ma_and_the_Mid_Pleistocene_Transition_0_9_0_6_Ma_","translated_internal_url":"","created_at":"2024-06-09T09:16:10.733-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":49112639,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Variability_in_the_Mountain_Environment_at_Melka_Kunture_Archaeological_Site_Ethiopia_During_the_Early_Pleistocene_1_7_Ma_and_the_Mid_Pleistocene_Transition_0_9_0_6_Ma_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":49112639,"first_name":"raymonde","middle_initials":null,"last_name":"Bonnefille","page_name":"rBonnefille","domain_name":"independent","created_at":"2016-05-23T02:32:27.321-07:00","display_name":"raymonde Bonnefille","url":"https://independent.academia.edu/rBonnefille"},"attachments":[],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":392,"name":"Archaeology","url":"https://www.academia.edu/Documents/in/Archaeology"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":30254,"name":"Pleistocene","url":"https://www.academia.edu/Documents/in/Pleistocene"},{"id":77502,"name":"Early Pleistocene","url":"https://www.academia.edu/Documents/in/Early_Pleistocene"},{"id":3647879,"name":"Springer Ebooks","url":"https://www.academia.edu/Documents/in/Springer_Ebooks"}],"urls":[{"id":42791705,"url":"https://doi.org/10.1007/978-3-319-75985-2_5"}]}, 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="120775368"><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/120775368/Modern_pollen_rain_from_the_Biligirirangan_Melagiri_hills_of_southern_Eastern_Ghats_India"><img alt="Research paper thumbnail of Modern pollen rain from the Biligirirangan–Melagiri hills of southern Eastern Ghats, India" class="work-thumbnail" src="https://attachments.academia-assets.com/115879254/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/120775368/Modern_pollen_rain_from_the_Biligirirangan_Melagiri_hills_of_southern_Eastern_Ghats_India">Modern pollen rain from the Biligirirangan–Melagiri hills of southern Eastern Ghats, India</a></div><div class="wp-workCard_item"><span>Review of Palaeobotany and Palynology</span><span>, 2000</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A total of 39 soil surface samples collected between 11 degrees 30&amp;amp;amp;amp;amp;amp;amp;am...</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">A total of 39 soil surface samples collected between 11 degrees 30&amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;N 76 degrees 45&amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;E and 12 degrees 45&amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;N 78 degrees 15&amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;E from the mainly deciduous forests in the Biligirirangan-Melagiri hills of the southern Eastern Ghats were analysed for their pollen content. The samples are distributed among four different deciduous and evergreen vegetation types between 210 and 1700m altitudes and fall within three distinct rainfall regimes. The aims of this paper are to provide new data on the modern pollen rain from the Southern Eastern Ghats, a region characterized by a unique and complex climate and vegetation, and to interpret these data using multivariate statistics and the diagram of pollen percentages. We could distinguish first between the deciduous and the evergreen forests and then also between different types of deciduous forest. The distinction between the evergreen and deciduous forests was based on a humidity gradient and that among the deciduous forests on a physiognomic gradient identified through correspondence analysis. The above analysis also allowed us to identify a set of 14 pollen taxa markers and 11 associated pollen taxa that help differentiate the evergreen from deciduous forests. Similarly, a set of 12 pollen taxa markers and six associated pollen taxa was demarcated to help distinguish woodland formations from scrub and thicket formations, among the deciduous vegetation. We could also differentiate amongst the four distinct vegetation types sampled, on the basis of distinct associations of both tree and herb pollen taxa according to their relative abundance in the pollen diagram as well as on the proportion of total arboreal pollen. The ground cover of grasses and other herbaceous plants in the deciduous forests is effectively demonstrated by percentages of non-arboreal pollen varying between 40 and 70%. The 1000m altitude limit reflecting a gradient of humidity and the physiognomic gradient among deciduous forests seem to be important in this region.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1f9a3e7b335313799ba618fbc1772fc7" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":115879254,"asset_id":120775368,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/115879254/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&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="120775368"><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="120775368"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 120775368; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=120775368]").text(description); $(".js-view-count[data-work-id=120775368]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 120775368; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='120775368']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 120775368, 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: "1f9a3e7b335313799ba618fbc1772fc7" } } $('.js-work-strip[data-work-id=120775368]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":120775368,"title":"Modern pollen rain from the Biligirirangan–Melagiri hills of southern Eastern Ghats, India","translated_title":"","metadata":{"abstract":"A total of 39 soil surface samples collected between 11 degrees 30\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;N 76 degrees 45\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;E and 12 degrees 45\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;N 78 degrees 15\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;E from the mainly deciduous forests in the Biligirirangan-Melagiri hills of the southern Eastern Ghats were analysed for their pollen content. The samples are distributed among four different deciduous and evergreen vegetation types between 210 and 1700m altitudes and fall within three distinct rainfall regimes. The aims of this paper are to provide new data on the modern pollen rain from the Southern Eastern Ghats, a region characterized by a unique and complex climate and vegetation, and to interpret these data using multivariate statistics and the diagram of pollen percentages. We could distinguish first between the deciduous and the evergreen forests and then also between different types of deciduous forest. The distinction between the evergreen and deciduous forests was based on a humidity gradient and that among the deciduous forests on a physiognomic gradient identified through correspondence analysis. The above analysis also allowed us to identify a set of 14 pollen taxa markers and 11 associated pollen taxa that help differentiate the evergreen from deciduous forests. Similarly, a set of 12 pollen taxa markers and six associated pollen taxa was demarcated to help distinguish woodland formations from scrub and thicket formations, among the deciduous vegetation. We could also differentiate amongst the four distinct vegetation types sampled, on the basis of distinct associations of both tree and herb pollen taxa according to their relative abundance in the pollen diagram as well as on the proportion of total arboreal pollen. The ground cover of grasses and other herbaceous plants in the deciduous forests is effectively demonstrated by percentages of non-arboreal pollen varying between 40 and 70%. The 1000m altitude limit reflecting a gradient of humidity and the physiognomic gradient among deciduous forests seem to be important in this region.","publisher":"Elsevier BV","publication_date":{"day":null,"month":null,"year":2000,"errors":{}},"publication_name":"Review of Palaeobotany and Palynology"},"translated_abstract":"A total of 39 soil surface samples collected between 11 degrees 30\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;N 76 degrees 45\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;E and 12 degrees 45\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;N 78 degrees 15\u0026amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;E from the mainly deciduous forests in the Biligirirangan-Melagiri hills of the southern Eastern Ghats were analysed for their pollen content. The samples are distributed among four different deciduous and evergreen vegetation types between 210 and 1700m altitudes and fall within three distinct rainfall regimes. The aims of this paper are to provide new data on the modern pollen rain from the Southern Eastern Ghats, a region characterized by a unique and complex climate and vegetation, and to interpret these data using multivariate statistics and the diagram of pollen percentages. We could distinguish first between the deciduous and the evergreen forests and then also between different types of deciduous forest. The distinction between the evergreen and deciduous forests was based on a humidity gradient and that among the deciduous forests on a physiognomic gradient identified through correspondence analysis. The above analysis also allowed us to identify a set of 14 pollen taxa markers and 11 associated pollen taxa that help differentiate the evergreen from deciduous forests. Similarly, a set of 12 pollen taxa markers and six associated pollen taxa was demarcated to help distinguish woodland formations from scrub and thicket formations, among the deciduous vegetation. We could also differentiate amongst the four distinct vegetation types sampled, on the basis of distinct associations of both tree and herb pollen taxa according to their relative abundance in the pollen diagram as well as on the proportion of total arboreal pollen. The ground cover of grasses and other herbaceous plants in the deciduous forests is effectively demonstrated by percentages of non-arboreal pollen varying between 40 and 70%. The 1000m altitude limit reflecting a gradient of humidity and the physiognomic gradient among deciduous forests seem to be important in this region.","internal_url":"https://www.academia.edu/120775368/Modern_pollen_rain_from_the_Biligirirangan_Melagiri_hills_of_southern_Eastern_Ghats_India","translated_internal_url":"","created_at":"2024-06-09T09:16:10.505-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":49112639,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":115879254,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/115879254/thumbnails/1.jpg","file_name":"Anupamaetal2000.pdf","download_url":"https://www.academia.edu/attachments/115879254/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modern_pollen_rain_from_the_Biligirirang.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/115879254/Anupamaetal2000-libre.pdf?1718099157=\u0026response-content-disposition=attachment%3B+filename%3DModern_pollen_rain_from_the_Biligirirang.pdf\u0026Expires=1732549234\u0026Signature=SuoDjDOxPyRGZfJFYTCAfYaSv4RQnI7Q9QqF7iVdyLFX-hi43v-kVd0IebP1qSOlfXbECuoYBn~iZBH4SIhKyUOvRLHS-RX2rcEsCjdP~Wq8R~4mzm3Jf4WWF2uoLjVDGr4DmsagFs9SIdtAxi~b6gYBdn41B3~71QnDX91Ld06k8VREwSgbAEUHEL15Yf~ngew8W7ngdmb0EDERsWwi7w~QEafaNAYD2~HhaaCoMeH3fIkEaBFv43ZA5cYw-c8snshr0Fmm-i97ABq~-sr~eoMFFqIbyxZq1mGacFibzd0tJmXCLcH16J9J6M04s2VhECmIBOcdgGlsrPdMn1T5lA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Modern_pollen_rain_from_the_Biligirirangan_Melagiri_hills_of_southern_Eastern_Ghats_India","translated_slug":"","page_count":22,"language":"en","content_type":"Work","owner":{"id":49112639,"first_name":"raymonde","middle_initials":null,"last_name":"Bonnefille","page_name":"rBonnefille","domain_name":"independent","created_at":"2016-05-23T02:32:27.321-07:00","display_name":"raymonde Bonnefille","url":"https://independent.academia.edu/rBonnefille"},"attachments":[{"id":115879254,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/115879254/thumbnails/1.jpg","file_name":"Anupamaetal2000.pdf","download_url":"https://www.academia.edu/attachments/115879254/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modern_pollen_rain_from_the_Biligirirang.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/115879254/Anupamaetal2000-libre.pdf?1718099157=\u0026response-content-disposition=attachment%3B+filename%3DModern_pollen_rain_from_the_Biligirirang.pdf\u0026Expires=1732549234\u0026Signature=SuoDjDOxPyRGZfJFYTCAfYaSv4RQnI7Q9QqF7iVdyLFX-hi43v-kVd0IebP1qSOlfXbECuoYBn~iZBH4SIhKyUOvRLHS-RX2rcEsCjdP~Wq8R~4mzm3Jf4WWF2uoLjVDGr4DmsagFs9SIdtAxi~b6gYBdn41B3~71QnDX91Ld06k8VREwSgbAEUHEL15Yf~ngew8W7ngdmb0EDERsWwi7w~QEafaNAYD2~HhaaCoMeH3fIkEaBFv43ZA5cYw-c8snshr0Fmm-i97ABq~-sr~eoMFFqIbyxZq1mGacFibzd0tJmXCLcH16J9J6M04s2VhECmIBOcdgGlsrPdMn1T5lA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":1352,"name":"Multivariate Statistics","url":"https://www.academia.edu/Documents/in/Multivariate_Statistics"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":26327,"name":"Medicine","url":"https://www.academia.edu/Documents/in/Medicine"},{"id":28230,"name":"Correspondence Analysis","url":"https://www.academia.edu/Documents/in/Correspondence_Analysis"},{"id":32759,"name":"Palaeobotany","url":"https://www.academia.edu/Documents/in/Palaeobotany"},{"id":83086,"name":"Pollen","url":"https://www.academia.edu/Documents/in/Pollen"},{"id":372637,"name":"Deciduous","url":"https://www.academia.edu/Documents/in/Deciduous"},{"id":745347,"name":"Relative Abundance","url":"https://www.academia.edu/Documents/in/Relative_Abundance"},{"id":843041,"name":"Evergreen","url":"https://www.academia.edu/Documents/in/Evergreen"},{"id":1004965,"name":"Deciduous Forest","url":"https://www.academia.edu/Documents/in/Deciduous_Forest"}],"urls":[{"id":42791703,"url":"https://api.elsevier.com/content/article/PII:S0034666799000391?httpAccept=text/xml"}]}, 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="120775365"><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/120775365/Modern_pollen_spectra_from_tropical_South_India_and_Sri_Lanka_altitudinal_distribution"><img alt="Research paper thumbnail of Modern pollen spectra from tropical South India and Sri Lanka: altitudinal distribution" class="work-thumbnail" src="https://attachments.academia-assets.com/115878973/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/120775365/Modern_pollen_spectra_from_tropical_South_India_and_Sri_Lanka_altitudinal_distribution">Modern pollen spectra from tropical South India and Sri Lanka: altitudinal distribution</a></div><div class="wp-workCard_item"><span>Journal of Biogeography</span><span>, 1999</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">SummaryWe analysed the pollen content of 106 surface soil samples from evergreen and deciduous tr...</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">SummaryWe analysed the pollen content of 106 surface soil samples from evergreen and deciduous tropical forests distributed between 6° and 13° of latitude north in South India and Sri Lanka. The samples were collected along altitudinal gradients, ranging from 50 to 2420 m, in five regions that experience different rainfall regimes. Original pollen data from tropical vegetation subjected to seasonal monsoon rains are presented along altitude/temperature gradients. This paper includes a summarized description of the vegetation types mapped in the area.The pollen results are presented in the form of quantitative pollen diagrams and correspondence analyses. They show clear distinct pollen assemblages and markers for all types of vegetation in deciduous and evergreen vegetation. Forests are well identified by percentages of Arboreal Pollen greater than 50%, despite the fact that Dipterocarpaceae and Lauraceae are hardly recorded by pollen.The pollen distinction between low, medium and hi...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="8f0eb9763ca8561378df20f55cde8be8" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":115878973,"asset_id":120775365,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/115878973/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&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="120775365"><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="120775365"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 120775365; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=120775365]").text(description); $(".js-view-count[data-work-id=120775365]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 120775365; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='120775365']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 120775365, 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: "8f0eb9763ca8561378df20f55cde8be8" } } $('.js-work-strip[data-work-id=120775365]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":120775365,"title":"Modern pollen spectra from tropical South India and Sri Lanka: altitudinal distribution","translated_title":"","metadata":{"abstract":"SummaryWe analysed the pollen content of 106 surface soil samples from evergreen and deciduous tropical forests distributed between 6° and 13° of latitude north in South India and Sri Lanka. The samples were collected along altitudinal gradients, ranging from 50 to 2420 m, in five regions that experience different rainfall regimes. Original pollen data from tropical vegetation subjected to seasonal monsoon rains are presented along altitude/temperature gradients. This paper includes a summarized description of the vegetation types mapped in the area.The pollen results are presented in the form of quantitative pollen diagrams and correspondence analyses. They show clear distinct pollen assemblages and markers for all types of vegetation in deciduous and evergreen vegetation. Forests are well identified by percentages of Arboreal Pollen greater than 50%, despite the fact that Dipterocarpaceae and Lauraceae are hardly recorded by pollen.The pollen distinction between low, medium and hi...","publisher":"Wiley","publication_date":{"day":null,"month":null,"year":1999,"errors":{}},"publication_name":"Journal of Biogeography"},"translated_abstract":"SummaryWe analysed the pollen content of 106 surface soil samples from evergreen and deciduous tropical forests distributed between 6° and 13° of latitude north in South India and Sri Lanka. The samples were collected along altitudinal gradients, ranging from 50 to 2420 m, in five regions that experience different rainfall regimes. Original pollen data from tropical vegetation subjected to seasonal monsoon rains are presented along altitude/temperature gradients. This paper includes a summarized description of the vegetation types mapped in the area.The pollen results are presented in the form of quantitative pollen diagrams and correspondence analyses. They show clear distinct pollen assemblages and markers for all types of vegetation in deciduous and evergreen vegetation. Forests are well identified by percentages of Arboreal Pollen greater than 50%, despite the fact that Dipterocarpaceae and Lauraceae are hardly recorded by pollen.The pollen distinction between low, medium and hi...","internal_url":"https://www.academia.edu/120775365/Modern_pollen_spectra_from_tropical_South_India_and_Sri_Lanka_altitudinal_distribution","translated_internal_url":"","created_at":"2024-06-09T09:16:09.273-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":49112639,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":115878973,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/115878973/thumbnails/1.jpg","file_name":"1999_Bonnefille_et_al_JBIO.pdf","download_url":"https://www.academia.edu/attachments/115878973/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modern_pollen_spectra_from_tropical_Sout.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/115878973/1999_Bonnefille_et_al_JBIO-libre.pdf?1718099189=\u0026response-content-disposition=attachment%3B+filename%3DModern_pollen_spectra_from_tropical_Sout.pdf\u0026Expires=1732549234\u0026Signature=Buc0Q7jYQvSiC66Hft0UPR6-WMJloghoZa0tCrmDmtUrSNfR-VID2tLqz7Bj9INkleYxk~LwJsiIZgIDcSOlbpqmhjC7HCrFcTgJNosaQH8NDewKewkJde3XFHq6XvOdUg9h3ohd0pp4jZIHnThHwljl~CpS6oy2l8ByDoX6mRJxIeERxA~JNKKpu~GS7J1MIqKil9HbpM8qrr~-LkeVDpip2u7TpDVHP0L0Dr2JM3jQXfD9oPp0OBl6YWKL28vjAmP06SQc-8tEhQ0hBmsxH99dPCqNVyFwVMlH~O8Y14aG0GHE5m3O0ZHs473KyloT593hUQHLPK3vcDJ~yu2mZQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Modern_pollen_spectra_from_tropical_South_India_and_Sri_Lanka_altitudinal_distribution","translated_slug":"","page_count":27,"language":"en","content_type":"Work","owner":{"id":49112639,"first_name":"raymonde","middle_initials":null,"last_name":"Bonnefille","page_name":"rBonnefille","domain_name":"independent","created_at":"2016-05-23T02:32:27.321-07:00","display_name":"raymonde Bonnefille","url":"https://independent.academia.edu/rBonnefille"},"attachments":[{"id":115878973,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/115878973/thumbnails/1.jpg","file_name":"1999_Bonnefille_et_al_JBIO.pdf","download_url":"https://www.academia.edu/attachments/115878973/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Modern_pollen_spectra_from_tropical_Sout.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/115878973/1999_Bonnefille_et_al_JBIO-libre.pdf?1718099189=\u0026response-content-disposition=attachment%3B+filename%3DModern_pollen_spectra_from_tropical_Sout.pdf\u0026Expires=1732549234\u0026Signature=Buc0Q7jYQvSiC66Hft0UPR6-WMJloghoZa0tCrmDmtUrSNfR-VID2tLqz7Bj9INkleYxk~LwJsiIZgIDcSOlbpqmhjC7HCrFcTgJNosaQH8NDewKewkJde3XFHq6XvOdUg9h3ohd0pp4jZIHnThHwljl~CpS6oy2l8ByDoX6mRJxIeERxA~JNKKpu~GS7J1MIqKil9HbpM8qrr~-LkeVDpip2u7TpDVHP0L0Dr2JM3jQXfD9oPp0OBl6YWKL28vjAmP06SQc-8tEhQ0hBmsxH99dPCqNVyFwVMlH~O8Y14aG0GHE5m3O0ZHs473KyloT593hUQHLPK3vcDJ~yu2mZQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":9850,"name":"Sri Lanka","url":"https://www.academia.edu/Documents/in/Sri_Lanka"},{"id":17823,"name":"Biogeography","url":"https://www.academia.edu/Documents/in/Biogeography"},{"id":20771,"name":"South India","url":"https://www.academia.edu/Documents/in/South_India"},{"id":43838,"name":"India","url":"https://www.academia.edu/Documents/in/India"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":76763,"name":"Tropics","url":"https://www.academia.edu/Documents/in/Tropics"},{"id":83086,"name":"Pollen","url":"https://www.academia.edu/Documents/in/Pollen"},{"id":168657,"name":"Evergreen Forest","url":"https://www.academia.edu/Documents/in/Evergreen_Forest"},{"id":304559,"name":"Modern pollen rain","url":"https://www.academia.edu/Documents/in/Modern_pollen_rain"},{"id":372637,"name":"Deciduous","url":"https://www.academia.edu/Documents/in/Deciduous"},{"id":564837,"name":"Tropical forests","url":"https://www.academia.edu/Documents/in/Tropical_forests"},{"id":789599,"name":"Biome","url":"https://www.academia.edu/Documents/in/Biome"},{"id":843041,"name":"Evergreen","url":"https://www.academia.edu/Documents/in/Evergreen"},{"id":1299102,"name":"Arboreal Locomotion","url":"https://www.academia.edu/Documents/in/Arboreal_Locomotion"}],"urls":[{"id":42791702,"url":"https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-2699.1999.00359.x"}]}, 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="120775310"><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/120775310/Isotopic_insights_into_the_Early_Acheulean_1_95_Ma_1_66_Ma_high_elevation_paleoenvironments_at_Melka_Kunture_Upper_Awash_Ethiopia_"><img alt="Research paper thumbnail of Isotopic insights into the Early Acheulean (1.95 Ma-1.66 Ma) high-elevation paleoenvironments at Melka Kunture (Upper Awash, Ethiopia)" class="work-thumbnail" src="https://attachments.academia-assets.com/115819296/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/120775310/Isotopic_insights_into_the_Early_Acheulean_1_95_Ma_1_66_Ma_high_elevation_paleoenvironments_at_Melka_Kunture_Upper_Awash_Ethiopia_">Isotopic insights into the Early Acheulean (1.95 Ma-1.66 Ma) high-elevation paleoenvironments at Melka Kunture (Upper Awash, Ethiopia)</a></div><div class="wp-workCard_item"><span>Research Square (Research Square)</span><span>, Oct 17, 2022</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3b87842d437148b40edb6bd4244f401c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":115819296,"asset_id":120775310,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/115819296/download_file?st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&st=MTczMjU0NTYzNCw4LjIyMi4yMDguMTQ2&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="120775310"><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="120775310"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 120775310; 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Our aim is to infer the diet, habitat, and environment at both sites and provide a broader paleoecological reconstruction. During the Pleistocene, the vegetation of the highlands of Ethiopia belonged to the \"Dry evergreen Afromontane Forest and grassland complex\", distinct from the savanna of lower elevations in East Africa. Our carbon isotopic results indicate that all the analyzed faunal taxa were grazers, consuming C 4 grasses, while oxygen isotopic results clearly discriminate the taxa according to their semi-aquatic or terrestrial habitats. These results are consistent with the analysis of the faunal assemblages and the palynological results, suggesting extended mountain grasslands in the landscape at Garba IVD. In contrast, the carbon isotopic results do not totally agree with the pollen paleoenvironmental reconstruction at Gombore IB, where the open vegetation was interrupted by forests and bushy vegetation. Stable isotopes and pollen data provide different outcomes (feeding strategies vs. nearby plants) and have different temporal and spatial resolutions. This is relevant when reconstructing past environments by exclusively using independent proxies. Furthermore, isotopic comparisons with other East African archaeological sites of the Lower Pleistocene age indicate that all the analyzed taxa fed on C 4 grasses, and that their dietary strategies were not affected by differences linked to various elevations.","publication_date":{"day":17,"month":10,"year":2022,"errors":{}},"publication_name":"Research Square (Research 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