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class="js-profile-total-view-text">Public Views</span></p><p class="data"><span class="js-profile-view-count"></span></p></div></span></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="32525063" href="https://www.academia.edu/Documents/in/Middle_Stone_Age_Archaeology_"><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://independent.academia.edu/RobertHosfield","location":"/RobertHosfield","scheme":"https","host":"independent.academia.edu","port":null,"pathname":"/RobertHosfield","search":null,"httpAcceptLanguage":null,"serverSide":false}"></div> <div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Middle Stone Age (Archaeology)"]}" data-trace="false" data-dom-id="Pill-react-component-0c47740f-e415-485f-b7ac-8ae02dc6ce8b"></div> <div id="Pill-react-component-0c47740f-e415-485f-b7ac-8ae02dc6ce8b"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="32525063" href="https://www.academia.edu/Documents/in/Flint_Archaeology_"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Flint (Archaeology)"]}" data-trace="false" data-dom-id="Pill-react-component-8de4ea4a-5cdd-4c9c-acbd-a986a3edc945"></div> <div id="Pill-react-component-8de4ea4a-5cdd-4c9c-acbd-a986a3edc945"></div> </a><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="32525063" href="https://www.academia.edu/Documents/in/Australian_Indigenous_Archaeology"><div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Australian Indigenous 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data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/80169597/Beyond_arrows_on_a_map_The_dynamics_of_Homo_sapiens_dispersal_and_occupation_of_Arabia_during_Marine_Isotope_Stage_5"><img alt="Research paper thumbnail of Beyond arrows on a map: The dynamics of Homo sapiens dispersal and occupation of Arabia during Marine Isotope Stage 5" 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/80169597/Beyond_arrows_on_a_map_The_dynamics_of_Homo_sapiens_dispersal_and_occupation_of_Arabia_during_Marine_Isotope_Stage_5">Beyond arrows on a map: The dynamics of Homo sapiens dispersal and occupation of Arabia during Marine Isotope Stage 5</a></div><div class="wp-workCard_item"><span>Journal of Anthropological Archaeology</span><span>, 2021</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Abstract Arabia occupies a crucial central position between Africa and Eurasia. The northward exp...</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">Abstract Arabia occupies a crucial central position between Africa and Eurasia. The northward expansion of the monsoonal rain-belt and the formation of grasslands during Marine Isotope Stage (MIS) 5 provided favourable conditions for Homo sapiens to occupy and traverse now arid areas of Arabia. While “Green Arabia” may have been a crucial stepping-stone on the way to H. sapiens global settlement, the occupation of Arabia is an important area of study in itself and could offer vital perspectives on human-environment interactions. In particular, Green Arabia can offer a unique insight into processes of human dispersal, occupation and extirpation in an environmentally fluctuating landscape. Here we synthesise archaeological, palaeoclimate and ethnographic data to develop a holistic model for the occupation of Green Arabia and offer targets for future research. We suggest that, on broad timescales, the resource availability and carrying capacity of Green Arabia facilitated rapid population expansion and occupation across Arabia. On human time-scales, dispersal was probably a slow process due to the requirements of metapopulation structures, likely consisting of many “micro-dispersals” spanning numerous generations. Transitions to more arid conditions were probably echoed by local hominin extirpations, dispersals into surrounding regions and retraction to resource-retaining core areas.</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="80169597"><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="80169597"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 80169597; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=80169597]").text(description); $(".js-view-count[data-work-id=80169597]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 80169597; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='80169597']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 80169597, 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" } } $('.js-work-strip[data-work-id=80169597]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":80169597,"title":"Beyond arrows on a map: The dynamics of Homo sapiens dispersal and occupation of Arabia during Marine Isotope Stage 5","translated_title":"","metadata":{"abstract":"Abstract Arabia occupies a crucial central position between Africa and Eurasia. The northward expansion of the monsoonal rain-belt and the formation of grasslands during Marine Isotope Stage (MIS) 5 provided favourable conditions for Homo sapiens to occupy and traverse now arid areas of Arabia. While “Green Arabia” may have been a crucial stepping-stone on the way to H. sapiens global settlement, the occupation of Arabia is an important area of study in itself and could offer vital perspectives on human-environment interactions. In particular, Green Arabia can offer a unique insight into processes of human dispersal, occupation and extirpation in an environmentally fluctuating landscape. Here we synthesise archaeological, palaeoclimate and ethnographic data to develop a holistic model for the occupation of Green Arabia and offer targets for future research. We suggest that, on broad timescales, the resource availability and carrying capacity of Green Arabia facilitated rapid population expansion and occupation across Arabia. 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Peak populations are suggested for Marine Isotope Stages (MISs) 13 and 11, and population decline is indicated after MIS 10. 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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="67984991"><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/67984991/Flake_tools_and_handaxes_at_High_Lodge_patterns_in_size_and_shape"><img alt="Research paper thumbnail of Flake tools and handaxes at High Lodge: patterns in size and shape?" class="work-thumbnail" src="https://attachments.academia-assets.com/78626979/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/67984991/Flake_tools_and_handaxes_at_High_Lodge_patterns_in_size_and_shape">Flake tools and handaxes at High Lodge: patterns in size and shape?</a></div><div class="wp-workCard_item"><span>Lithics: The Journal of the Lithic Studies Society</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper explores possible size and shape patterning in Lower Palaeolithic flake tools and hand...</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">This paper explores possible size and shape patterning in Lower Palaeolithic flake tools and handaxes, using the published (Ashton & Cook 1992) primary metrics of the High Lodge Old Collections as a case study. Comparison of coefficient of variation (C.V.) values suggests that while raw artefact metrics and shape proxy values inevitably differ by artefact type, the degree of variability by type is frequently comparable for scrapers, notches and denticulates, flaked flakes, and handaxes. The data from this preliminary investigation therefore suggests that long-standing descriptions of Acheulean flake tools as ad hoc and unstandardised might merit further and fuller re-investigation. Full reference: Hosfield, R.T. 2013. Flake tools and handaxes at High Lodge: patterns in size and shape? Lithics: the Journal of the Lithic Studies Society 34: 23–33 Keywords: Typology, flake tools, Lower Palaeolithic, morphometrics</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="5d1e75c15687fdf9a90573d8ea391171" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":78626979,"asset_id":67984991,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/78626979/download_file?st=MTczMjUyMDg4OSw4LjIyMi4yMDguMTQ2&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="67984991"><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="67984991"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984991; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984991]").text(description); $(".js-view-count[data-work-id=67984991]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984991; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984991']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984991, 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: "5d1e75c15687fdf9a90573d8ea391171" } } $('.js-work-strip[data-work-id=67984991]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984991,"title":"Flake tools and handaxes at High Lodge: patterns in size and shape?","translated_title":"","metadata":{"abstract":"This paper explores possible size and shape patterning in Lower Palaeolithic flake tools and handaxes, using the published (Ashton \u0026 Cook 1992) primary metrics of the High Lodge Old Collections as a case study. 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Lithics: the Journal of the Lithic Studies Society 34: 23–33 Keywords: Typology, flake tools, Lower Palaeolithic, morphometrics","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"Lithics: The Journal of the Lithic Studies Society"},"translated_abstract":"This paper explores possible size and shape patterning in Lower Palaeolithic flake tools and handaxes, using the published (Ashton \u0026 Cook 1992) primary metrics of the High Lodge Old Collections as a case study. Comparison of coefficient of variation (C.V.) values suggests that while raw artefact metrics and shape proxy values inevitably differ by artefact type, the degree of variability by type is frequently comparable for scrapers, notches and denticulates, flaked flakes, and handaxes. The data from this preliminary investigation therefore suggests that long-standing descriptions of Acheulean flake tools as ad hoc and unstandardised might merit further and fuller re-investigation. Full reference: Hosfield, R.T. 2013. Flake tools and handaxes at High Lodge: patterns in size and shape? 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The meeting brought together the increasingly numerous Palaeolithic archaeologists and Pleistocene geologists working in the region to shae and discuss their preliminary results. The papers cover both Pleistocene geological and Palaeolithic archaeological themes and range in scope from regional syntheses and issues to more detailed studies of individual sites. The volume represents both an introduction to the Palaeolithic archaeology and Pleistocene geology of the Solent River and an up-to-date view of current research, as well as signposting directions for future work. Introduction. F.F. Wenban-Smith The Pleistocene geology of the Solent River system. J.K. Dix The Pleistocene evolution and Palaeolithic occupation of the Solent River. 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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="67984987"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/67984987/The_Lower_Palaeolithic_site_of_Broom"><img alt="Research paper thumbnail of The Lower Palaeolithic site of Broom" 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" rel="nofollow" href="https://www.academia.edu/67984987/The_Lower_Palaeolithic_site_of_Broom">The Lower Palaeolithic site of Broom</a></div><div class="wp-workCard_item"><span>Lithics: The Journal of the Lithic Studies Society</span><span>, 2016</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This report presents the results of three seasons’ fieldwork and an initial optical dating progra...</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">This report presents the results of three seasons’ fieldwork and an initial optical dating programme at the Lower Palaeolithic site of Broom (ST 328025 and ST 326020). The site is located in the River Axe valley on the Devon/Dorset border (Hosfield & Terry 2000) and has yielded the largest Acheulean artefact assemblage in southwest Britain. Up to 1800 artefacts, predominantly handaxes, were recovered during the commercial excavation of the Broom gravel pits from the late 19 th century onwards (Green 1988). Chert artefacts are dominant in the extant assemblages, reflecting the Foxmould Chert Beds of Upper Greensand that are incised by the modem River Axe upstream of Broom (Shakesby & Stephens 1984).</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="67984987"><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="67984987"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984987; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984987]").text(description); $(".js-view-count[data-work-id=67984987]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984987; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984987']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984987, 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" } } $('.js-work-strip[data-work-id=67984987]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984987,"title":"The Lower Palaeolithic site of Broom","translated_title":"","metadata":{"abstract":"This report presents the results of three seasons’ fieldwork and an initial optical dating programme at the Lower Palaeolithic site of Broom (ST 328025 and ST 326020). 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Chert artefacts are dominant in the extant assemblages, reflecting the Foxmould Chert Beds of Upper Greensand that are incised by the modem River Axe upstream of Broom (Shakesby \u0026 Stephens 1984).","internal_url":"https://www.academia.edu/67984987/The_Lower_Palaeolithic_site_of_Broom","translated_internal_url":"","created_at":"2022-01-13T10:18:15.935-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":32525063,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"The_Lower_Palaeolithic_site_of_Broom","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":32525063,"first_name":"Robert","middle_initials":null,"last_name":"Hosfield","page_name":"RobertHosfield","domain_name":"independent","created_at":"2015-06-25T02:31:29.760-07:00","display_name":"Robert Hosfield","url":"https://independent.academia.edu/RobertHosfield"},"attachments":[],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="67984986"><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/67984986/Beyond_the_caves_the_palaeolithic_rivers_of_South_West_Britain"><img alt="Research paper thumbnail of Beyond the caves: the palaeolithic rivers of South-West Britain" 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/67984986/Beyond_the_caves_the_palaeolithic_rivers_of_South_West_Britain">Beyond the caves: the palaeolithic rivers of South-West Britain</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper introduces a new English Heritage (Aggregates Levy Sustainability Fund) project The Pa...</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">This paper introduces a new English Heritage (Aggregates Levy Sustainability Fund) project The Palaeolithic Rivers of South-West Britain (project no. 3847), and summarises the results of a first phase resource assessment. The goal of this ongoing project is to develop a new synthesis of the Lower and Middle Palaeolithic occupation of the south-west region, focusing upon river terrace-based archaeology and its implications for hominin landscape use. The resource assessment has reached two preliminary conclusions. Firstly that the region’s earliest Palaeolithic archaeological record is significantly richer than previously believed, and secondly that although find locations have been added in several areas which previously had very few or no finds (e.g.West Cornwall) the overall bias of finds to the south coast is maintained. The project has also revealed that the river terrace resource of South-West England offers potential for geochronological dating, landscape reconstruction, and im...</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="67984986"><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="67984986"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984986; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984986]").text(description); $(".js-view-count[data-work-id=67984986]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984986; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984986']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984986, 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" } } $('.js-work-strip[data-work-id=67984986]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984986,"title":"Beyond the caves: the palaeolithic rivers of South-West Britain","translated_title":"","metadata":{"abstract":"This paper introduces a new English Heritage (Aggregates Levy Sustainability Fund) project The Palaeolithic Rivers of South-West Britain (project no. 3847), and summarises the results of a first phase resource assessment. The goal of this ongoing project is to develop a new synthesis of the Lower and Middle Palaeolithic occupation of the south-west region, focusing upon river terrace-based archaeology and its implications for hominin landscape use. The resource assessment has reached two preliminary conclusions. Firstly that the region’s earliest Palaeolithic archaeological record is significantly richer than previously believed, and secondly that although find locations have been added in several areas which previously had very few or no finds (e.g.West Cornwall) the overall bias of finds to the south coast is maintained. The project has also revealed that the river terrace resource of South-West England offers potential for geochronological dating, landscape reconstruction, and im...","publication_date":{"day":null,"month":null,"year":2006,"errors":{}}},"translated_abstract":"This paper introduces a new English Heritage (Aggregates Levy Sustainability Fund) project The Palaeolithic Rivers of South-West Britain (project no. 3847), and summarises the results of a first phase resource assessment. The goal of this ongoing project is to develop a new synthesis of the Lower and Middle Palaeolithic occupation of the south-west region, focusing upon river terrace-based archaeology and its implications for hominin landscape use. The resource assessment has reached two preliminary conclusions. Firstly that the region’s earliest Palaeolithic archaeological record is significantly richer than previously believed, and secondly that although find locations have been added in several areas which previously had very few or no finds (e.g.West Cornwall) the overall bias of finds to the south coast is maintained. The project has also revealed that the river terrace resource of South-West England offers potential for geochronological dating, landscape reconstruction, and im...","internal_url":"https://www.academia.edu/67984986/Beyond_the_caves_the_palaeolithic_rivers_of_South_West_Britain","translated_internal_url":"","created_at":"2022-01-13T10:18:15.783-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":32525063,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Beyond_the_caves_the_palaeolithic_rivers_of_South_West_Britain","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":32525063,"first_name":"Robert","middle_initials":null,"last_name":"Hosfield","page_name":"RobertHosfield","domain_name":"independent","created_at":"2015-06-25T02:31:29.760-07:00","display_name":"Robert Hosfield","url":"https://independent.academia.edu/RobertHosfield"},"attachments":[],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"}],"urls":[{"id":16361831,"url":"http://ussher.org.uk/journal/00s/2006/Hosfield06-rivers.pdf"}]}, 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="67984985"><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/67984985/Super_volcanic_eruptions_and_impacts_on_hominin_evolution"><img alt="Research paper thumbnail of Super-volcanic eruptions and impacts on hominin evolution" 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/67984985/Super_volcanic_eruptions_and_impacts_on_hominin_evolution">Super-volcanic eruptions and impacts on hominin evolution</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">&lt;p&gt;The impact of super volcanic eruptions (Volcanic Explosivity Index 7-8+) on human evolut...</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">&lt;p&gt;The impact of super volcanic eruptions (Volcanic Explosivity Index 7-8+) on human evolution is a topic that has invited much debate and controversy (Ambrose 1998, Petraglia et al. 2007, 2012; Clarkson et al., 2020), and has typically focused on the impacts on human populations within the last 100-200kya (e.g. Groucutt 2020). What is less well understood is whether there is any clear evidence to show how super-volcanic eruptions, and their subsequent impacts on paleo-environments and climates, may have influenced hominin evolution over the last c. 5mya. Previous studies using first and last hominin appearance dates have suggested that orbitally-induced climatic cycles (eccentricity, obliquity and precession) may play a role in hominin speciation events, but that only obliquity shows any significant relationship with extinction events (Grove 2012a). Firth and Cole (2015) subsequently suggested that selected super-eruptions may have acted as critical enhancers to particular orbital forcing events.&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;This paper revisits the Firth and Cole (2015) study and presents a comparison of super volcanic eruptions against first and last hominin appearance dates; orbitally induced climatic cycles; global temperature (measured using the LR04 Benthic Stack &amp;#8211; Lisiecki and Raymo 2005); and broad technological behavioural changes in order to assess to what extent such eruptions may have impacted, either directly or indirectly, on human evolution at different temporal and geographic scales. Such large eruptive events certainly do seem to disrupt climatic conditions for significant periods of time at a generational level (Harris 2008). Where data is fine grained enough, volcanic activity also seems to impact on human population dispersals, through push and pull factors, and drive changes in the behavioural record (e.g. Groucutt 2020). However, at the broad evolutionary scale, volcanic eruptions do not seem to lead to a significant turnover of hominin species (at least in regard to the resolution of the data currently available). Therefore, we suggest that future work should seek to bring these two perspectives of scale together to better understand super volcanoes in terms of the complex interplay of changing local conditions and their impacts on the broader global picture of human evolution.&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;References:&lt;/p&gt;&lt;p&gt;Ambrose, S.H., 1998. Late Pleistocene human population bottlenecks, volcanic winter, and differentiation of modern humans. Journal of Human Evolution. 34, 623&amp;#8211;651.&lt;/p&gt;&lt;p&gt;Clarkson, C. et al. 2020. Human occupation of northern India spans the Toba super-eruption ~74,000 years ago. Nature Communications 11: 961.&lt;/p&gt;&lt;p&gt;Firth C.R. and Cole J. 2015: A review of super-volcano eruptions and their impact on hominin evolution. INQUA XIX Congress: Japan, July.&lt;/p&gt;&lt;p&gt;Groucutt, H. 2020. Volcanism and human prehistory in Arabia. Journal of Volcanology and Geothermal Research 402: 107003.&lt;/p&gt;&lt;p&gt;Harris, B. 2008. The potential impact of super-volcanic eruptions on the Earth&amp;#8217;s atmosphere. Weather 63 (8): 221 &amp;#8211; 225.&lt;/p&gt;&lt;p&gt;Petraglia, M.D., et al., &amp;#160;2007. Middle Paleolithic assemblages from the Indian subcontinent before and after the Toba super-eruption. Science 317, 114&amp;#8211;116.&lt;/p&gt;&lt;p&gt;Petraglia, M.D., Korisettar, R., Pal, J.N., 2012. The Toba volcanic super-eruption of 74,000 years ago: climate change, environments, and evolving humans. Quaternary International. 258, 1&amp;#8211;4.&lt;/p&gt;</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="67984985"><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="67984985"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984985; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984985]").text(description); $(".js-view-count[data-work-id=67984985]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984985; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984985']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984985, 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" } } $('.js-work-strip[data-work-id=67984985]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984985,"title":"Super-volcanic eruptions and impacts on hominin evolution","translated_title":"","metadata":{"abstract":"\u0026lt;p\u0026gt;The impact of super volcanic eruptions (Volcanic Explosivity Index 7-8+) on human evolution is a topic that has invited much debate and controversy (Ambrose 1998, Petraglia et al. 2007, 2012; Clarkson et al., 2020), and has typically focused on the impacts on human populations within the last 100-200kya (e.g. Groucutt 2020). What is less well understood is whether there is any clear evidence to show how super-volcanic eruptions, and their subsequent impacts on paleo-environments and climates, may have influenced hominin evolution over the last c. 5mya. Previous studies using first and last hominin appearance dates have suggested that orbitally-induced climatic cycles (eccentricity, obliquity and precession) may play a role in hominin speciation events, but that only obliquity shows any significant relationship with extinction events (Grove 2012a). Firth and Cole (2015) subsequently suggested that selected super-eruptions may have acted as critical enhancers to particular orbital forcing events.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;\u0026amp;#160;\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;This paper revisits the Firth and Cole (2015) study and presents a comparison of super volcanic eruptions against first and last hominin appearance dates; orbitally induced climatic cycles; global temperature (measured using the LR04 Benthic Stack \u0026amp;#8211; Lisiecki and Raymo 2005); and broad technological behavioural changes in order to assess to what extent such eruptions may have impacted, either directly or indirectly, on human evolution at different temporal and geographic scales. Such large eruptive events certainly do seem to disrupt climatic conditions for significant periods of time at a generational level (Harris 2008). Where data is fine grained enough, volcanic activity also seems to impact on human population dispersals, through push and pull factors, and drive changes in the behavioural record (e.g. Groucutt 2020). However, at the broad evolutionary scale, volcanic eruptions do not seem to lead to a significant turnover of hominin species (at least in regard to the resolution of the data currently available). Therefore, we suggest that future work should seek to bring these two perspectives of scale together to better understand super volcanoes in terms of the complex interplay of changing local conditions and their impacts on the broader global picture of human evolution.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;\u0026amp;#160;\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;\u0026amp;#160;\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;References:\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Ambrose, S.H., 1998. Late Pleistocene human population bottlenecks, volcanic winter, and differentiation of modern humans. Journal of Human Evolution. 34, 623\u0026amp;#8211;651.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Clarkson, C. et al. 2020. Human occupation of northern India spans the Toba super-eruption ~74,000 years ago. Nature Communications 11: 961.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Firth C.R. and Cole J. 2015: A review of super-volcano eruptions and their impact on hominin evolution. INQUA XIX Congress: Japan, July.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Groucutt, H. 2020. Volcanism and human prehistory in Arabia. Journal of Volcanology and Geothermal Research 402: 107003.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Harris, B. 2008. The potential impact of super-volcanic eruptions on the Earth\u0026amp;#8217;s atmosphere. Weather 63 (8): 221 \u0026amp;#8211; 225.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Petraglia, M.D., et al., \u0026amp;#160;2007. Middle Paleolithic assemblages from the Indian subcontinent before and after the Toba super-eruption. Science 317, 114\u0026amp;#8211;116.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Petraglia, M.D., Korisettar, R., Pal, J.N., 2012. The Toba volcanic super-eruption of 74,000 years ago: climate change, environments, and evolving humans. Quaternary International. 258, 1\u0026amp;#8211;4.\u0026lt;/p\u0026gt;","publication_date":{"day":null,"month":null,"year":2021,"errors":{}}},"translated_abstract":"\u0026lt;p\u0026gt;The impact of super volcanic eruptions (Volcanic Explosivity Index 7-8+) on human evolution is a topic that has invited much debate and controversy (Ambrose 1998, Petraglia et al. 2007, 2012; Clarkson et al., 2020), and has typically focused on the impacts on human populations within the last 100-200kya (e.g. Groucutt 2020). What is less well understood is whether there is any clear evidence to show how super-volcanic eruptions, and their subsequent impacts on paleo-environments and climates, may have influenced hominin evolution over the last c. 5mya. Previous studies using first and last hominin appearance dates have suggested that orbitally-induced climatic cycles (eccentricity, obliquity and precession) may play a role in hominin speciation events, but that only obliquity shows any significant relationship with extinction events (Grove 2012a). Firth and Cole (2015) subsequently suggested that selected super-eruptions may have acted as critical enhancers to particular orbital forcing events.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;\u0026amp;#160;\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;This paper revisits the Firth and Cole (2015) study and presents a comparison of super volcanic eruptions against first and last hominin appearance dates; orbitally induced climatic cycles; global temperature (measured using the LR04 Benthic Stack \u0026amp;#8211; Lisiecki and Raymo 2005); and broad technological behavioural changes in order to assess to what extent such eruptions may have impacted, either directly or indirectly, on human evolution at different temporal and geographic scales. Such large eruptive events certainly do seem to disrupt climatic conditions for significant periods of time at a generational level (Harris 2008). Where data is fine grained enough, volcanic activity also seems to impact on human population dispersals, through push and pull factors, and drive changes in the behavioural record (e.g. Groucutt 2020). However, at the broad evolutionary scale, volcanic eruptions do not seem to lead to a significant turnover of hominin species (at least in regard to the resolution of the data currently available). Therefore, we suggest that future work should seek to bring these two perspectives of scale together to better understand super volcanoes in terms of the complex interplay of changing local conditions and their impacts on the broader global picture of human evolution.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;\u0026amp;#160;\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;\u0026amp;#160;\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;References:\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Ambrose, S.H., 1998. Late Pleistocene human population bottlenecks, volcanic winter, and differentiation of modern humans. Journal of Human Evolution. 34, 623\u0026amp;#8211;651.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Clarkson, C. et al. 2020. Human occupation of northern India spans the Toba super-eruption ~74,000 years ago. Nature Communications 11: 961.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Firth C.R. and Cole J. 2015: A review of super-volcano eruptions and their impact on hominin evolution. INQUA XIX Congress: Japan, July.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Groucutt, H. 2020. Volcanism and human prehistory in Arabia. Journal of Volcanology and Geothermal Research 402: 107003.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Harris, B. 2008. The potential impact of super-volcanic eruptions on the Earth\u0026amp;#8217;s atmosphere. Weather 63 (8): 221 \u0026amp;#8211; 225.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Petraglia, M.D., et al., \u0026amp;#160;2007. Middle Paleolithic assemblages from the Indian subcontinent before and after the Toba super-eruption. Science 317, 114\u0026amp;#8211;116.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Petraglia, M.D., Korisettar, R., Pal, J.N., 2012. The Toba volcanic super-eruption of 74,000 years ago: climate change, environments, and evolving humans. 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This reflects the nature of the archaeological material itself, the histories of research in different parts of the region and, with regard to the Palaeolithic period, the differential preservation of Pleistocene landforms and deposits throughout the region. One of the key features of the Palaeolithic archaeology is the presence of a significant cave-based resource in south Devon and northern Somerset, which is unquestionably of national significance (see for example, Campbell and Sampson 1971; Tratman et al. 1971; Bishop 1975; Harrison 1977; Straw 1995; 1996; Andrews et al. 1999).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="24f36b8ba42df6e24be2b3d08b0bb5ae" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":78626901,"asset_id":67984979,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/78626901/download_file?st=MTczMjUyMDg4OSw4LjIyMi4yMDguMTQ2&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="67984979"><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="67984979"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984979; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984979]").text(description); $(".js-view-count[data-work-id=67984979]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984979; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984979']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984979, 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: "24f36b8ba42df6e24be2b3d08b0bb5ae" } } $('.js-work-strip[data-work-id=67984979]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984979,"title":"Palaeolithic and Mesolithic","translated_title":"","metadata":{"abstract":"The South West contains a diverse variety of Palaeolithic and Mesolithic archaeology of differing degrees of significance. 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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="67984976"><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/67984976/Chapter_4_The_Lower_Middle_Palaeolithic_Research_Agenda"><img alt="Research paper thumbnail of Chapter 4 The Lower / Middle Palaeolithic : Research Agenda" class="work-thumbnail" src="https://attachments.academia-assets.com/78626894/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/67984976/Chapter_4_The_Lower_Middle_Palaeolithic_Research_Agenda">Chapter 4 The Lower / Middle Palaeolithic : Research Agenda</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">It was recognised in the 1980s that the present structure of archaeological curation and investig...</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">It was recognised in the 1980s that the present structure of archaeological curation and investigation in advance of development requires a framework of academic and research priorities against which to consider the significance of sites and to guide their investigation. The seminal English Heritage publication Exploring our Past (1991) identified three main themes – physical evolution, cultural development and global colonisation. English Heritage has subsequently taken the lead, in conjunction with the Prehistoric Society, in keeping core strategic research themes under review, with updated themes and research priorities issued in 1999 and 2008 (English Heritage/ Prehistoric Society 1999, 2008). A condensed list of national research themes is given (Table 4.1), collated from these sources, and taking account of actual ongoing research across Britain. This has led to the inclusion of an element of material cultural study, which is unaccountably omitted from the proposed national fr...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="5bb00264f1a27f846e4111ee5d3b3837" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":78626894,"asset_id":67984976,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/78626894/download_file?st=MTczMjUyMDg4OSw4LjIyMi4yMDguMTQ2&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="67984976"><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="67984976"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984976; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984976]").text(description); $(".js-view-count[data-work-id=67984976]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984976; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984976']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984976, 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: "5bb00264f1a27f846e4111ee5d3b3837" } } $('.js-work-strip[data-work-id=67984976]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984976,"title":"Chapter 4 The Lower / Middle Palaeolithic : Research Agenda","translated_title":"","metadata":{"abstract":"It was recognised in the 1980s that the present structure of archaeological curation and investigation in advance of development requires a framework of academic and research priorities against which to consider the significance of sites and to guide their investigation. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="3092435" id="papers"><div class="js-work-strip profile--work_container" data-work-id="80169597"><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/80169597/Beyond_arrows_on_a_map_The_dynamics_of_Homo_sapiens_dispersal_and_occupation_of_Arabia_during_Marine_Isotope_Stage_5"><img alt="Research paper thumbnail of Beyond arrows on a map: The dynamics of Homo sapiens dispersal and occupation of Arabia during Marine Isotope Stage 5" 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/80169597/Beyond_arrows_on_a_map_The_dynamics_of_Homo_sapiens_dispersal_and_occupation_of_Arabia_during_Marine_Isotope_Stage_5">Beyond arrows on a map: The dynamics of Homo sapiens dispersal and occupation of Arabia during Marine Isotope Stage 5</a></div><div class="wp-workCard_item"><span>Journal of Anthropological Archaeology</span><span>, 2021</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Abstract Arabia occupies a crucial central position between Africa and Eurasia. The northward exp...</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">Abstract Arabia occupies a crucial central position between Africa and Eurasia. The northward expansion of the monsoonal rain-belt and the formation of grasslands during Marine Isotope Stage (MIS) 5 provided favourable conditions for Homo sapiens to occupy and traverse now arid areas of Arabia. While “Green Arabia” may have been a crucial stepping-stone on the way to H. sapiens global settlement, the occupation of Arabia is an important area of study in itself and could offer vital perspectives on human-environment interactions. In particular, Green Arabia can offer a unique insight into processes of human dispersal, occupation and extirpation in an environmentally fluctuating landscape. Here we synthesise archaeological, palaeoclimate and ethnographic data to develop a holistic model for the occupation of Green Arabia and offer targets for future research. We suggest that, on broad timescales, the resource availability and carrying capacity of Green Arabia facilitated rapid population expansion and occupation across Arabia. On human time-scales, dispersal was probably a slow process due to the requirements of metapopulation structures, likely consisting of many “micro-dispersals” spanning numerous generations. Transitions to more arid conditions were probably echoed by local hominin extirpations, dispersals into surrounding regions and retraction to resource-retaining core areas.</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="80169597"><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="80169597"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 80169597; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=80169597]").text(description); $(".js-view-count[data-work-id=80169597]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 80169597; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='80169597']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 80169597, 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" } } $('.js-work-strip[data-work-id=80169597]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":80169597,"title":"Beyond arrows on a map: The dynamics of Homo sapiens dispersal and occupation of Arabia during Marine Isotope Stage 5","translated_title":"","metadata":{"abstract":"Abstract Arabia occupies a crucial central position between Africa and Eurasia. 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Peak populations are suggested for Marine Isotope Stages (MISs) 13 and 11, and population decline is indicated after MIS 10. 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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="67984991"><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/67984991/Flake_tools_and_handaxes_at_High_Lodge_patterns_in_size_and_shape"><img alt="Research paper thumbnail of Flake tools and handaxes at High Lodge: patterns in size and shape?" class="work-thumbnail" src="https://attachments.academia-assets.com/78626979/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/67984991/Flake_tools_and_handaxes_at_High_Lodge_patterns_in_size_and_shape">Flake tools and handaxes at High Lodge: patterns in size and shape?</a></div><div class="wp-workCard_item"><span>Lithics: The Journal of the Lithic Studies Society</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper explores possible size and shape patterning in Lower Palaeolithic flake tools and hand...</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">This paper explores possible size and shape patterning in Lower Palaeolithic flake tools and handaxes, using the published (Ashton & Cook 1992) primary metrics of the High Lodge Old Collections as a case study. Comparison of coefficient of variation (C.V.) values suggests that while raw artefact metrics and shape proxy values inevitably differ by artefact type, the degree of variability by type is frequently comparable for scrapers, notches and denticulates, flaked flakes, and handaxes. The data from this preliminary investigation therefore suggests that long-standing descriptions of Acheulean flake tools as ad hoc and unstandardised might merit further and fuller re-investigation. Full reference: Hosfield, R.T. 2013. Flake tools and handaxes at High Lodge: patterns in size and shape? Lithics: the Journal of the Lithic Studies Society 34: 23–33 Keywords: Typology, flake tools, Lower Palaeolithic, morphometrics</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="5d1e75c15687fdf9a90573d8ea391171" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":78626979,"asset_id":67984991,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/78626979/download_file?st=MTczMjUyMDg4OSw4LjIyMi4yMDguMTQ2&st=MTczMjUyMDg4OSw4LjIyMi4yMDguMTQ2&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="67984991"><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="67984991"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984991; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984991]").text(description); $(".js-view-count[data-work-id=67984991]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984991; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984991']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984991, 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: "5d1e75c15687fdf9a90573d8ea391171" } } $('.js-work-strip[data-work-id=67984991]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984991,"title":"Flake tools and handaxes at High Lodge: patterns in size and shape?","translated_title":"","metadata":{"abstract":"This paper explores possible size and shape patterning in Lower Palaeolithic flake tools and handaxes, using the published (Ashton \u0026 Cook 1992) primary metrics of the High Lodge Old Collections as a case study. 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Lithics: the Journal of the Lithic Studies Society 34: 23–33 Keywords: Typology, flake tools, Lower Palaeolithic, morphometrics","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"Lithics: The Journal of the Lithic Studies Society"},"translated_abstract":"This paper explores possible size and shape patterning in Lower Palaeolithic flake tools and handaxes, using the published (Ashton \u0026 Cook 1992) primary metrics of the High Lodge Old Collections as a case study. Comparison of coefficient of variation (C.V.) values suggests that while raw artefact metrics and shape proxy values inevitably differ by artefact type, the degree of variability by type is frequently comparable for scrapers, notches and denticulates, flaked flakes, and handaxes. The data from this preliminary investigation therefore suggests that long-standing descriptions of Acheulean flake tools as ad hoc and unstandardised might merit further and fuller re-investigation. Full reference: Hosfield, R.T. 2013. Flake tools and handaxes at High Lodge: patterns in size and shape? 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The meeting brought together the increasingly numerous Palaeolithic archaeologists and Pleistocene geologists working in the region to shae and discuss their preliminary results. The papers cover both Pleistocene geological and Palaeolithic archaeological themes and range in scope from regional syntheses and issues to more detailed studies of individual sites. The volume represents both an introduction to the Palaeolithic archaeology and Pleistocene geology of the Solent River and an up-to-date view of current research, as well as signposting directions for future work. Introduction. F.F. Wenban-Smith The Pleistocene geology of the Solent River system. J.K. Dix The Pleistocene evolution and Palaeolithic occupation of the Solent River. D.R Bridgland The meeting of the waters...</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="67984989"><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="67984989"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984989; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984989]").text(description); $(".js-view-count[data-work-id=67984989]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984989; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984989']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984989, 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" } } $('.js-work-strip[data-work-id=67984989]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984989,"title":"Paleolithic archaeology of the Solent River","translated_title":"","metadata":{"abstract":"The ancestral Solent River region has been known since the late 19th century as a prolific area for Palaeolithic artefacts and Pleistocene deposits but had, until the 1990s, been generally neglected for research. 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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="67984987"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/67984987/The_Lower_Palaeolithic_site_of_Broom"><img alt="Research paper thumbnail of The Lower Palaeolithic site of Broom" 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" rel="nofollow" href="https://www.academia.edu/67984987/The_Lower_Palaeolithic_site_of_Broom">The Lower Palaeolithic site of Broom</a></div><div class="wp-workCard_item"><span>Lithics: The Journal of the Lithic Studies Society</span><span>, 2016</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This report presents the results of three seasons’ fieldwork and an initial optical dating progra...</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">This report presents the results of three seasons’ fieldwork and an initial optical dating programme at the Lower Palaeolithic site of Broom (ST 328025 and ST 326020). The site is located in the River Axe valley on the Devon/Dorset border (Hosfield & Terry 2000) and has yielded the largest Acheulean artefact assemblage in southwest Britain. Up to 1800 artefacts, predominantly handaxes, were recovered during the commercial excavation of the Broom gravel pits from the late 19 th century onwards (Green 1988). Chert artefacts are dominant in the extant assemblages, reflecting the Foxmould Chert Beds of Upper Greensand that are incised by the modem River Axe upstream of Broom (Shakesby & Stephens 1984).</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="67984987"><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="67984987"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984987; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984987]").text(description); $(".js-view-count[data-work-id=67984987]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984987; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984987']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984987, 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" } } $('.js-work-strip[data-work-id=67984987]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984987,"title":"The Lower Palaeolithic site of Broom","translated_title":"","metadata":{"abstract":"This report presents the results of three seasons’ fieldwork and an initial optical dating programme at the Lower Palaeolithic site of Broom (ST 328025 and ST 326020). 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Chert artefacts are dominant in the extant assemblages, reflecting the Foxmould Chert Beds of Upper Greensand that are incised by the modem River Axe upstream of Broom (Shakesby \u0026 Stephens 1984).","internal_url":"https://www.academia.edu/67984987/The_Lower_Palaeolithic_site_of_Broom","translated_internal_url":"","created_at":"2022-01-13T10:18:15.935-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":32525063,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"The_Lower_Palaeolithic_site_of_Broom","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":32525063,"first_name":"Robert","middle_initials":null,"last_name":"Hosfield","page_name":"RobertHosfield","domain_name":"independent","created_at":"2015-06-25T02:31:29.760-07:00","display_name":"Robert Hosfield","url":"https://independent.academia.edu/RobertHosfield"},"attachments":[],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="67984986"><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/67984986/Beyond_the_caves_the_palaeolithic_rivers_of_South_West_Britain"><img alt="Research paper thumbnail of Beyond the caves: the palaeolithic rivers of South-West Britain" 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/67984986/Beyond_the_caves_the_palaeolithic_rivers_of_South_West_Britain">Beyond the caves: the palaeolithic rivers of South-West Britain</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This paper introduces a new English Heritage (Aggregates Levy Sustainability Fund) project The Pa...</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">This paper introduces a new English Heritage (Aggregates Levy Sustainability Fund) project The Palaeolithic Rivers of South-West Britain (project no. 3847), and summarises the results of a first phase resource assessment. The goal of this ongoing project is to develop a new synthesis of the Lower and Middle Palaeolithic occupation of the south-west region, focusing upon river terrace-based archaeology and its implications for hominin landscape use. The resource assessment has reached two preliminary conclusions. Firstly that the region’s earliest Palaeolithic archaeological record is significantly richer than previously believed, and secondly that although find locations have been added in several areas which previously had very few or no finds (e.g.West Cornwall) the overall bias of finds to the south coast is maintained. The project has also revealed that the river terrace resource of South-West England offers potential for geochronological dating, landscape reconstruction, and im...</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="67984986"><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="67984986"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984986; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984986]").text(description); $(".js-view-count[data-work-id=67984986]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984986; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984986']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984986, 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" } } $('.js-work-strip[data-work-id=67984986]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984986,"title":"Beyond the caves: the palaeolithic rivers of South-West Britain","translated_title":"","metadata":{"abstract":"This paper introduces a new English Heritage (Aggregates Levy Sustainability Fund) project The Palaeolithic Rivers of South-West Britain (project no. 3847), and summarises the results of a first phase resource assessment. 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The project has also revealed that the river terrace resource of South-West England offers potential for geochronological dating, landscape reconstruction, and im...","publication_date":{"day":null,"month":null,"year":2006,"errors":{}}},"translated_abstract":"This paper introduces a new English Heritage (Aggregates Levy Sustainability Fund) project The Palaeolithic Rivers of South-West Britain (project no. 3847), and summarises the results of a first phase resource assessment. The goal of this ongoing project is to develop a new synthesis of the Lower and Middle Palaeolithic occupation of the south-west region, focusing upon river terrace-based archaeology and its implications for hominin landscape use. The resource assessment has reached two preliminary conclusions. Firstly that the region’s earliest Palaeolithic archaeological record is significantly richer than previously believed, and secondly that although find locations have been added in several areas which previously had very few or no finds (e.g.West Cornwall) the overall bias of finds to the south coast is maintained. The project has also revealed that the river terrace resource of South-West England offers potential for geochronological dating, landscape reconstruction, and im...","internal_url":"https://www.academia.edu/67984986/Beyond_the_caves_the_palaeolithic_rivers_of_South_West_Britain","translated_internal_url":"","created_at":"2022-01-13T10:18:15.783-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":32525063,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Beyond_the_caves_the_palaeolithic_rivers_of_South_West_Britain","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":32525063,"first_name":"Robert","middle_initials":null,"last_name":"Hosfield","page_name":"RobertHosfield","domain_name":"independent","created_at":"2015-06-25T02:31:29.760-07:00","display_name":"Robert Hosfield","url":"https://independent.academia.edu/RobertHosfield"},"attachments":[],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"}],"urls":[{"id":16361831,"url":"http://ussher.org.uk/journal/00s/2006/Hosfield06-rivers.pdf"}]}, 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="67984985"><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/67984985/Super_volcanic_eruptions_and_impacts_on_hominin_evolution"><img alt="Research paper thumbnail of Super-volcanic eruptions and impacts on hominin evolution" 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/67984985/Super_volcanic_eruptions_and_impacts_on_hominin_evolution">Super-volcanic eruptions and impacts on hominin evolution</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">&lt;p&gt;The impact of super volcanic eruptions (Volcanic Explosivity Index 7-8+) on human evolut...</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">&lt;p&gt;The impact of super volcanic eruptions (Volcanic Explosivity Index 7-8+) on human evolution is a topic that has invited much debate and controversy (Ambrose 1998, Petraglia et al. 2007, 2012; Clarkson et al., 2020), and has typically focused on the impacts on human populations within the last 100-200kya (e.g. Groucutt 2020). What is less well understood is whether there is any clear evidence to show how super-volcanic eruptions, and their subsequent impacts on paleo-environments and climates, may have influenced hominin evolution over the last c. 5mya. Previous studies using first and last hominin appearance dates have suggested that orbitally-induced climatic cycles (eccentricity, obliquity and precession) may play a role in hominin speciation events, but that only obliquity shows any significant relationship with extinction events (Grove 2012a). Firth and Cole (2015) subsequently suggested that selected super-eruptions may have acted as critical enhancers to particular orbital forcing events.&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;This paper revisits the Firth and Cole (2015) study and presents a comparison of super volcanic eruptions against first and last hominin appearance dates; orbitally induced climatic cycles; global temperature (measured using the LR04 Benthic Stack &amp;#8211; Lisiecki and Raymo 2005); and broad technological behavioural changes in order to assess to what extent such eruptions may have impacted, either directly or indirectly, on human evolution at different temporal and geographic scales. Such large eruptive events certainly do seem to disrupt climatic conditions for significant periods of time at a generational level (Harris 2008). Where data is fine grained enough, volcanic activity also seems to impact on human population dispersals, through push and pull factors, and drive changes in the behavioural record (e.g. Groucutt 2020). However, at the broad evolutionary scale, volcanic eruptions do not seem to lead to a significant turnover of hominin species (at least in regard to the resolution of the data currently available). Therefore, we suggest that future work should seek to bring these two perspectives of scale together to better understand super volcanoes in terms of the complex interplay of changing local conditions and their impacts on the broader global picture of human evolution.&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;References:&lt;/p&gt;&lt;p&gt;Ambrose, S.H., 1998. Late Pleistocene human population bottlenecks, volcanic winter, and differentiation of modern humans. Journal of Human Evolution. 34, 623&amp;#8211;651.&lt;/p&gt;&lt;p&gt;Clarkson, C. et al. 2020. Human occupation of northern India spans the Toba super-eruption ~74,000 years ago. Nature Communications 11: 961.&lt;/p&gt;&lt;p&gt;Firth C.R. and Cole J. 2015: A review of super-volcano eruptions and their impact on hominin evolution. INQUA XIX Congress: Japan, July.&lt;/p&gt;&lt;p&gt;Groucutt, H. 2020. Volcanism and human prehistory in Arabia. Journal of Volcanology and Geothermal Research 402: 107003.&lt;/p&gt;&lt;p&gt;Harris, B. 2008. The potential impact of super-volcanic eruptions on the Earth&amp;#8217;s atmosphere. Weather 63 (8): 221 &amp;#8211; 225.&lt;/p&gt;&lt;p&gt;Petraglia, M.D., et al., &amp;#160;2007. Middle Paleolithic assemblages from the Indian subcontinent before and after the Toba super-eruption. Science 317, 114&amp;#8211;116.&lt;/p&gt;&lt;p&gt;Petraglia, M.D., Korisettar, R., Pal, J.N., 2012. The Toba volcanic super-eruption of 74,000 years ago: climate change, environments, and evolving humans. Quaternary International. 258, 1&amp;#8211;4.&lt;/p&gt;</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="67984985"><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="67984985"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984985; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984985]").text(description); $(".js-view-count[data-work-id=67984985]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984985; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984985']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984985, 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" } } $('.js-work-strip[data-work-id=67984985]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984985,"title":"Super-volcanic eruptions and impacts on hominin evolution","translated_title":"","metadata":{"abstract":"\u0026lt;p\u0026gt;The impact of super volcanic eruptions (Volcanic Explosivity Index 7-8+) on human evolution is a topic that has invited much debate and controversy (Ambrose 1998, Petraglia et al. 2007, 2012; Clarkson et al., 2020), and has typically focused on the impacts on human populations within the last 100-200kya (e.g. Groucutt 2020). What is less well understood is whether there is any clear evidence to show how super-volcanic eruptions, and their subsequent impacts on paleo-environments and climates, may have influenced hominin evolution over the last c. 5mya. Previous studies using first and last hominin appearance dates have suggested that orbitally-induced climatic cycles (eccentricity, obliquity and precession) may play a role in hominin speciation events, but that only obliquity shows any significant relationship with extinction events (Grove 2012a). Firth and Cole (2015) subsequently suggested that selected super-eruptions may have acted as critical enhancers to particular orbital forcing events.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;\u0026amp;#160;\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;This paper revisits the Firth and Cole (2015) study and presents a comparison of super volcanic eruptions against first and last hominin appearance dates; orbitally induced climatic cycles; global temperature (measured using the LR04 Benthic Stack \u0026amp;#8211; Lisiecki and Raymo 2005); and broad technological behavioural changes in order to assess to what extent such eruptions may have impacted, either directly or indirectly, on human evolution at different temporal and geographic scales. Such large eruptive events certainly do seem to disrupt climatic conditions for significant periods of time at a generational level (Harris 2008). Where data is fine grained enough, volcanic activity also seems to impact on human population dispersals, through push and pull factors, and drive changes in the behavioural record (e.g. Groucutt 2020). However, at the broad evolutionary scale, volcanic eruptions do not seem to lead to a significant turnover of hominin species (at least in regard to the resolution of the data currently available). Therefore, we suggest that future work should seek to bring these two perspectives of scale together to better understand super volcanoes in terms of the complex interplay of changing local conditions and their impacts on the broader global picture of human evolution.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;\u0026amp;#160;\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;\u0026amp;#160;\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;References:\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Ambrose, S.H., 1998. Late Pleistocene human population bottlenecks, volcanic winter, and differentiation of modern humans. Journal of Human Evolution. 34, 623\u0026amp;#8211;651.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Clarkson, C. et al. 2020. Human occupation of northern India spans the Toba super-eruption ~74,000 years ago. Nature Communications 11: 961.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Firth C.R. and Cole J. 2015: A review of super-volcano eruptions and their impact on hominin evolution. INQUA XIX Congress: Japan, July.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Groucutt, H. 2020. Volcanism and human prehistory in Arabia. Journal of Volcanology and Geothermal Research 402: 107003.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Harris, B. 2008. The potential impact of super-volcanic eruptions on the Earth\u0026amp;#8217;s atmosphere. Weather 63 (8): 221 \u0026amp;#8211; 225.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Petraglia, M.D., et al., \u0026amp;#160;2007. Middle Paleolithic assemblages from the Indian subcontinent before and after the Toba super-eruption. Science 317, 114\u0026amp;#8211;116.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Petraglia, M.D., Korisettar, R., Pal, J.N., 2012. The Toba volcanic super-eruption of 74,000 years ago: climate change, environments, and evolving humans. Quaternary International. 258, 1\u0026amp;#8211;4.\u0026lt;/p\u0026gt;","publication_date":{"day":null,"month":null,"year":2021,"errors":{}}},"translated_abstract":"\u0026lt;p\u0026gt;The impact of super volcanic eruptions (Volcanic Explosivity Index 7-8+) on human evolution is a topic that has invited much debate and controversy (Ambrose 1998, Petraglia et al. 2007, 2012; Clarkson et al., 2020), and has typically focused on the impacts on human populations within the last 100-200kya (e.g. Groucutt 2020). What is less well understood is whether there is any clear evidence to show how super-volcanic eruptions, and their subsequent impacts on paleo-environments and climates, may have influenced hominin evolution over the last c. 5mya. Previous studies using first and last hominin appearance dates have suggested that orbitally-induced climatic cycles (eccentricity, obliquity and precession) may play a role in hominin speciation events, but that only obliquity shows any significant relationship with extinction events (Grove 2012a). 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Where data is fine grained enough, volcanic activity also seems to impact on human population dispersals, through push and pull factors, and drive changes in the behavioural record (e.g. Groucutt 2020). However, at the broad evolutionary scale, volcanic eruptions do not seem to lead to a significant turnover of hominin species (at least in regard to the resolution of the data currently available). Therefore, we suggest that future work should seek to bring these two perspectives of scale together to better understand super volcanoes in terms of the complex interplay of changing local conditions and their impacts on the broader global picture of human evolution.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;\u0026amp;#160;\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;\u0026amp;#160;\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;References:\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Ambrose, S.H., 1998. Late Pleistocene human population bottlenecks, volcanic winter, and differentiation of modern humans. Journal of Human Evolution. 34, 623\u0026amp;#8211;651.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Clarkson, C. et al. 2020. Human occupation of northern India spans the Toba super-eruption ~74,000 years ago. Nature Communications 11: 961.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Firth C.R. and Cole J. 2015: A review of super-volcano eruptions and their impact on hominin evolution. INQUA XIX Congress: Japan, July.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Groucutt, H. 2020. Volcanism and human prehistory in Arabia. Journal of Volcanology and Geothermal Research 402: 107003.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Harris, B. 2008. The potential impact of super-volcanic eruptions on the Earth\u0026amp;#8217;s atmosphere. Weather 63 (8): 221 \u0026amp;#8211; 225.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Petraglia, M.D., et al., \u0026amp;#160;2007. Middle Paleolithic assemblages from the Indian subcontinent before and after the Toba super-eruption. Science 317, 114\u0026amp;#8211;116.\u0026lt;/p\u0026gt;\u0026lt;p\u0026gt;Petraglia, M.D., Korisettar, R., Pal, J.N., 2012. The Toba volcanic super-eruption of 74,000 years ago: climate change, environments, and evolving humans. 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This reflects the nature of the archaeological material itself, the histories of research in different parts of the region and, with regard to the Palaeolithic period, the differential preservation of Pleistocene landforms and deposits throughout the region. One of the key features of the Palaeolithic archaeology is the presence of a significant cave-based resource in south Devon and northern Somerset, which is unquestionably of national significance (see for example, Campbell and Sampson 1971; Tratman et al. 1971; Bishop 1975; Harrison 1977; Straw 1995; 1996; Andrews et al. 1999).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="24f36b8ba42df6e24be2b3d08b0bb5ae" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":78626901,"asset_id":67984979,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/78626901/download_file?st=MTczMjUyMDg4OSw4LjIyMi4yMDguMTQ2&st=MTczMjUyMDg4OSw4LjIyMi4yMDguMTQ2&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="67984979"><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="67984979"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984979; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984979]").text(description); $(".js-view-count[data-work-id=67984979]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984979; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984979']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984979, 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: "24f36b8ba42df6e24be2b3d08b0bb5ae" } } $('.js-work-strip[data-work-id=67984979]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984979,"title":"Palaeolithic and Mesolithic","translated_title":"","metadata":{"abstract":"The South West contains a diverse variety of Palaeolithic and Mesolithic archaeology of differing degrees of significance. 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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="67984976"><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/67984976/Chapter_4_The_Lower_Middle_Palaeolithic_Research_Agenda"><img alt="Research paper thumbnail of Chapter 4 The Lower / Middle Palaeolithic : Research Agenda" class="work-thumbnail" src="https://attachments.academia-assets.com/78626894/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/67984976/Chapter_4_The_Lower_Middle_Palaeolithic_Research_Agenda">Chapter 4 The Lower / Middle Palaeolithic : Research Agenda</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">It was recognised in the 1980s that the present structure of archaeological curation and investig...</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">It was recognised in the 1980s that the present structure of archaeological curation and investigation in advance of development requires a framework of academic and research priorities against which to consider the significance of sites and to guide their investigation. The seminal English Heritage publication Exploring our Past (1991) identified three main themes – physical evolution, cultural development and global colonisation. English Heritage has subsequently taken the lead, in conjunction with the Prehistoric Society, in keeping core strategic research themes under review, with updated themes and research priorities issued in 1999 and 2008 (English Heritage/ Prehistoric Society 1999, 2008). A condensed list of national research themes is given (Table 4.1), collated from these sources, and taking account of actual ongoing research across Britain. This has led to the inclusion of an element of material cultural study, which is unaccountably omitted from the proposed national fr...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="5bb00264f1a27f846e4111ee5d3b3837" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":78626894,"asset_id":67984976,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/78626894/download_file?st=MTczMjUyMDg4OSw4LjIyMi4yMDguMTQ2&st=MTczMjUyMDg4OSw4LjIyMi4yMDguMTQ2&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="67984976"><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="67984976"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 67984976; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=67984976]").text(description); $(".js-view-count[data-work-id=67984976]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 67984976; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='67984976']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 67984976, 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: "5bb00264f1a27f846e4111ee5d3b3837" } } $('.js-work-strip[data-work-id=67984976]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":67984976,"title":"Chapter 4 The Lower / Middle Palaeolithic : Research Agenda","translated_title":"","metadata":{"abstract":"It was recognised in the 1980s that the present structure of archaeological curation and investigation in advance of development requires a framework of academic and research priorities against which to consider the significance of sites and to guide their investigation. 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