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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="56777151" href="https://www.academia.edu/Documents/in/Earth_and_Environmental_Science"><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://independent.academia.edu/HelenLewis21","location":"/HelenLewis21","scheme":"https","host":"independent.academia.edu","port":null,"pathname":"/HelenLewis21","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":["Earth and Environmental Science"]}" data-trace="false" data-dom-id="Pill-react-component-b7fc6001-7f65-4eb8-ab22-9a91a9acef2e"></div> <div 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data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/86561571/Early_occupation_at_Ille_Cave_New_Ibajay_El_Nido_Palawan_Philippines_Report_on_the_2005_excavation_season"><img alt="Research paper thumbnail of Early occupation at Ille Cave, New Ibajay, El Nido, Palawan, Philippines: Report on the 2005 excavation season" class="work-thumbnail" src="https://attachments.academia-assets.com/90985922/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/86561571/Early_occupation_at_Ille_Cave_New_Ibajay_El_Nido_Palawan_Philippines_Report_on_the_2005_excavation_season">Early occupation at Ille Cave, New Ibajay, El Nido, Palawan, Philippines: Report on the 2005 excavation season</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">4 Introduction and previous investigations 5 Aims of the new investigations 6 East Mouth excavati...</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">4 Introduction and previous investigations 5 Aims of the new investigations 6 East Mouth excavations 2005 8 Preliminary observations on the East Mouth cemetery 17 sequence and human remains The cemetery, West Mouth excavations and notes on the early 22</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="68c21b18b364af4f9382720bb46b43bd" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":90985922,"asset_id":86561571,"asset_type":"Work","button_location":"profile"}" 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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="86561570"><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/86561570/Geoarchaeology_at_Snusgar_Orkney_Mainland_2007"><img alt="Research paper thumbnail of Geoarchaeology at Snusgar, Orkney Mainland, 2007" class="work-thumbnail" src="https://attachments.academia-assets.com/90985963/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/86561570/Geoarchaeology_at_Snusgar_Orkney_Mainland_2007">Geoarchaeology at Snusgar, Orkney Mainland, 2007</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A brief visit was carried out for geoarchaeological assessment and continued soil micromorphology...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">A brief visit was carried out for geoarchaeological assessment and continued soil micromorphology sampling of deposits revealed during University of Oxford excavations at Snusgar and the Bay of Skaill, Mainland, Orkney, Scotland. Several additional samples were taken from Trenches 5 and 7 on the South-east mound at Snusgar, and an auger assessment of the upper mound was conducted. Continued excavations of a Norse period structure on the East mound at Snusgar were the focus of this year&#39;s project. There appear to be at least two phases of the structure (a probable house), with evidence of remodelling apparent in the later phase. Near the end of the excavation a further intriguing structural component was revealed: a deep wall with apparent corbelling, underlying the later structures. Soil micromorphology sampling focused primarily on a series of clay layers, apparently laid floors or structural deposits, associated with both this deep wall and with the later structures. In 2006, ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e5dee482af7b3b16c70c3f76f1953be1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":90985963,"asset_id":86561570,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/90985963/download_file?st=MTczMjg4MzczOCw4LjIyMi4yMDguMTQ2&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="86561570"><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="86561570"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 86561570; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=86561570]").text(description); $(".js-view-count[data-work-id=86561570]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 86561570; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='86561570']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 86561570, 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: "e5dee482af7b3b16c70c3f76f1953be1" } } $('.js-work-strip[data-work-id=86561570]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":86561570,"title":"Geoarchaeology at Snusgar, Orkney Mainland, 2007","translated_title":"","metadata":{"abstract":"A brief visit was carried out for geoarchaeological assessment and continued soil micromorphology sampling of deposits revealed during University of Oxford excavations at Snusgar and the Bay of Skaill, Mainland, Orkney, Scotland. Several additional samples were taken from Trenches 5 and 7 on the South-east mound at Snusgar, and an auger assessment of the upper mound was conducted. Continued excavations of a Norse period structure on the East mound at Snusgar were the focus of this year\u0026#39;s project. There appear to be at least two phases of the structure (a probable house), with evidence of remodelling apparent in the later phase. Near the end of the excavation a further intriguing structural component was revealed: a deep wall with apparent corbelling, underlying the later structures. Soil micromorphology sampling focused primarily on a series of clay layers, apparently laid floors or structural deposits, associated with both this deep wall and with the later structures. In 2006, ..."},"translated_abstract":"A brief visit was carried out for geoarchaeological assessment and continued soil micromorphology sampling of deposits revealed during University of Oxford excavations at Snusgar and the Bay of Skaill, Mainland, Orkney, Scotland. Several additional samples were taken from Trenches 5 and 7 on the South-east mound at Snusgar, and an auger assessment of the upper mound was conducted. Continued excavations of a Norse period structure on the East mound at Snusgar were the focus of this year\u0026#39;s project. There appear to be at least two phases of the structure (a probable house), with evidence of remodelling apparent in the later phase. Near the end of the excavation a further intriguing structural component was revealed: a deep wall with apparent corbelling, underlying the later structures. Soil micromorphology sampling focused primarily on a series of clay layers, apparently laid floors or structural deposits, associated with both this deep wall and with the later structures. 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The LGM was probably the most extreme climatic episode of cold and aridity at a global scale that our species has ever experienced, followed by sustained global warming. Within this broad picture, one of the most important developments in palaeoclimatic studies in recent decades has been the recognition of the instability of Late Pleistocene climates and the abrupt nature of climatic shifts, with millennial-, centennial and even shorter-scale shifts being discerned in the North Atlantic MIS 2 records (e.g. Blockley et al. 2006; Clark et al. 2002; Taylor et al. 1993; Fig. 5.1). In the northern hemisphere, there was a major shift to warmer and wetter conditions following the LGM termed the Bølling-Allerød interstadial (c. 14,700-12,800 bp), which was punctuated by at least two significant cold episodes, followed by a return to cold and dry near-glacial conditions, the Younger Dryas (c. 12,800-11,700 bp) before the shift to warmer climates that marked the Holocene. In the southern hemisphere, isotope studies of ice cores in Antarctica suggest a more continuous pattern of uninterrupted deglaciation and warming. It used to be thought that environmental change in the tropical lowlands of Southeast Asia during the Late Pleistocene must have been far less extreme than in northern latitudes, but it is now clear that many profound changes also took place in this region (Flenley 1997; Kershaw et al. 2007). The human populations of northern Borneo certainly had to cope with dramatic changes in the geography and ecology of the landscapes they inhabited in the Late Pleistocene, though as discussed in the next section their precise characteristics in the Niah region remain uncertain. Much important evidence about the climate, geography, and habitats of the region through this period derives from locations far distant from Niah. 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As in many other regions of the world, the term 'Neolithic' in Island Southeast Asia has traditionally been used to define the first agricultural communities, people who used a new material culture that included polished stone tools and pottery, and who based their subsistence primarily on the use of domestic crops and livestock. There are valid concerns about whether it is appropriate to apply to other parts of the world a term originally coined in the second half of the nineteenth century within the classification systems being established then for European prehistory. However, despite alternative local terminologies being proposed (e.g. Bacus 2004; Soejono 1997), the term 'Neolithic' remains a convenient label for the first pottery-using societies in Island Southeast Asia. As in Europe, though, one of the difficulties with the term is that archaeologists often use it with alternative meanings (sometimes within the same sentence, and often implicitly rather than explicitly): to denote a period of time; and/or a set of material culture (notably pottery and polished stone tools); and/or a way of life (agriculture). Although the term as originally proposed implied all three meanings-that everybody in the Neolithic period used Neolithic material culture and practised a 'Neolithic way of life' (i.e. agriculture)-subsequent research in many parts of the world has found examples of farmers living side by side with foragers in the 'Neolithic period'; of farmers not using the full suite of 'Neolithic material culture'; and of foragers using part of it (Barker 2006). 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Here we present the archaeobiological record of Pasimbahan-Magsanib site dating from c. 10,500 yr. BP to the subrecent. The terrestrial vertebrate record provides for a more robust Palawan biostratigraphy and chronicles Late Quaternary changes in mammalian composition and human responses to the changing abundance of large mammal communities. Well-stratified shell layers and middens contain a wide variety of taxa derived from freshwater, estuarine and marine environments that also provide insights on varying subsistence strategies and the local ecology. 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href="https://www.academia.edu/86561564/Terminal_Pleistocene_to_mid_Holocene_occupation_and_an_early_cremation_burial_at_Ille_Cave_Palawan_Philippines">Terminal Pleistocene to mid-Holocene occupation and an early cremation burial at Ille Cave, Palawan, Philippines</a></div><div class="wp-workCard_item"><span>Antiquity</span><span>, 2008</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Excavations at a cave site on the island of Palawan in the Philippines show occupation from c. 11...</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">Excavations at a cave site on the island of Palawan in the Philippines show occupation from c. 11000 BP. A fine assemblage of tools and faunal remains shows the reliance of hunter-foragers switching from deer to pig. In 9500-9000 BP, a human cremation burial in a container was emplaced, the earliest yet known in the region.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b92bd34393af5f4c94155133fa01bfe9" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":90985960,"asset_id":86561564,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/90985960/download_file?st=MTczMjg4MzczOCw4LjIyMi4yMDguMTQ2&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="86561564"><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="86561564"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 86561564; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=86561564]").text(description); $(".js-view-count[data-work-id=86561564]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 86561564; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='86561564']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 86561564, 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: "b92bd34393af5f4c94155133fa01bfe9" } } $('.js-work-strip[data-work-id=86561564]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":86561564,"title":"Terminal Pleistocene to mid-Holocene occupation and an early cremation burial at Ille Cave, Palawan, Philippines","translated_title":"","metadata":{"abstract":"Excavations at a cave site on the island of Palawan in the Philippines show occupation from c. 11000 BP. 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The samples were taken as part of the first author's Ph.D. research, investigating Palaeolithic-Neolithic transitions in the northern Philippine region (Mijares 2005a, 2006), but also form a comparative collection for cultural cave sediments from the southern Philippines and Borneo, which are being investigated by the second author (Lewis 2003, 2007). Both of these projects focus on understanding the prehistory of cave occupation and how changes in this reflect larger-scale movements of people, cultural materials, and ideas in the Island Southeast Asian region, with an aim to relate cave sites to the wider landscape through a variety of approaches, including geoarchaeology and the location and excavation of contemporaneous open-air sites. background to the study Northeastern Luzon is composed of a large basin called the Cagayan Valley, which is circumscribed by the mountains of the Sierra Madre in the east, the Cordillera Central in the west, and the Caraballo range in the south (Fig. 1). The Sierra Madre is an inactive volcanic arc with peaks up to 1800 m, while the active Cordillera Central has peaks up to 3000 m. The Cagayan Valley, which is dissected by the northward flowing Cagayan River, is composed of marine, transitional marine, and non-marine volcaniclastic sediments (Mathisen and Vondra 1983). The cave sites discussed here are found in the Callao limestone formation, which runs along the western foothills of the Sierra Madre. 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Soil Micromorphology","url":"https://www.academia.edu/Documents/in/Archaeological_Soil_Micromorphology"},{"id":33457,"name":"Material Culture","url":"https://www.academia.edu/Documents/in/Material_Culture"},{"id":41906,"name":"Neolithic","url":"https://www.academia.edu/Documents/in/Neolithic"},{"id":48310,"name":"Cave","url":"https://www.academia.edu/Documents/in/Cave"},{"id":78965,"name":"Holocene","url":"https://www.academia.edu/Documents/in/Holocene"},{"id":106896,"name":"Cave and Karst Studies","url":"https://www.academia.edu/Documents/in/Cave_and_Karst_Studies"},{"id":109780,"name":"Archaeology of Caves","url":"https://www.academia.edu/Documents/in/Archaeology_of_Caves"},{"id":109828,"name":"Fauna","url":"https://www.academia.edu/Documents/in/Fauna"},{"id":284069,"name":"Cave Archaeology","url":"https://www.academia.edu/Documents/in/Cave_Archaeology"},{"id":371285,"name":"Local 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href="https://www.academia.edu/86561561/Archaeological_investigations_in_northern_Laos_new_contributions_to_Southeast_Asian_prehistory"><img alt="Research paper thumbnail of Archaeological investigations in northern Laos: new contributions to Southeast Asian prehistory" class="work-thumbnail" src="https://attachments.academia-assets.com/90986043/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/86561561/Archaeological_investigations_in_northern_Laos_new_contributions_to_Southeast_Asian_prehistory">Archaeological investigations in northern Laos: new contributions to Southeast Asian prehistory</a></div><div class="wp-workCard_item"><span>Antiquity</span><span>, Mar 1, 2009</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Middle Mekong Archaeological Project (MMAP) was designed to investigate the prehistoric archa...</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">The Middle Mekong Archaeological Project (MMAP) was designed to investigate the prehistoric archaeology of the Luang Prabang region, which, although centrally located in mainland Southeast Asia, has seen little previous archaeological research (Figure 1; White & Bouasisengpaseuth 2008). The Mekong has long been thought to be an ancient highway for peoples, technologies and cultures, but due to historic political conditions, vast stretches of it remained inaccessible to modern archaeology until the 1990s.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3cd113aa7c32b65301c497786ae0f2ef" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":90986043,"asset_id":86561561,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/90986043/download_file?st=MTczMjg4MzczOCw4LjIyMi4yMDguMTQ2&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="86561561"><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="86561561"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 86561561; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=86561561]").text(description); $(".js-view-count[data-work-id=86561561]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 86561561; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='86561561']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 86561561, 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: "3cd113aa7c32b65301c497786ae0f2ef" } } $('.js-work-strip[data-work-id=86561561]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":86561561,"title":"Archaeological investigations in northern Laos: new contributions to Southeast Asian prehistory","translated_title":"","metadata":{"abstract":"The Middle Mekong Archaeological Project (MMAP) was designed to investigate the prehistoric archaeology of the Luang Prabang region, which, although centrally located in mainland Southeast Asia, has seen little previous archaeological research (Figure 1; White \u0026 Bouasisengpaseuth 2008). The Mekong has long been thought to be an ancient highway for peoples, technologies and cultures, but due to historic political conditions, vast stretches of it remained inaccessible to modern archaeology until the 1990s.","publisher":"antiquity.ac.uk","publication_date":{"day":1,"month":3,"year":2009,"errors":{}},"publication_name":"Antiquity"},"translated_abstract":"The Middle Mekong Archaeological Project (MMAP) was designed to investigate the prehistoric archaeology of the Luang Prabang region, which, although centrally located in mainland Southeast Asia, has seen little previous archaeological research (Figure 1; White \u0026 Bouasisengpaseuth 2008). The Mekong has long been thought to be an ancient highway for peoples, technologies and cultures, but due to historic political conditions, vast stretches of it remained inaccessible to modern archaeology until the 1990s.","internal_url":"https://www.academia.edu/86561561/Archaeological_investigations_in_northern_Laos_new_contributions_to_Southeast_Asian_prehistory","translated_internal_url":"","created_at":"2022-09-12T23:50:05.173-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":56777151,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":90986043,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/90986043/thumbnails/1.jpg","file_name":"Antiquity_20Vol_2083_20Issue_20319_20March_202009.pdf","download_url":"https://www.academia.edu/attachments/90986043/download_file?st=MTczMjg4MzczOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Archaeological_investigations_in_norther.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/90986043/Antiquity_20Vol_2083_20Issue_20319_20March_202009-libre.pdf?1663052745=\u0026response-content-disposition=attachment%3B+filename%3DArchaeological_investigations_in_norther.pdf\u0026Expires=1732887338\u0026Signature=QSpBHtB6fUrxocADK2wRurPbEuBx1EFsaWpD92jDueYnUw1NEfsDn2rpEzCcC18KUJA8~xsnJ0ZHJFeOyl0yQGzJfIRW1gJNpmfsaNoaGoptHJLgxhGKx66~GzSCxkNc9j9WpS69MNjthXYCNb6Qx5VFE-v0gnne7~84TpxPUxnMeO71~525VtmgWPAwyalpMbapoGklt5tQTo4KrK9kDfR9q8cWtsoTTgFoY2t4U3Pd4aL2dW0H-tusQq8cZ8~RL3jMlWJ7f5E5iJGnsAfP-mcskLHDtI8LnOEGNNwk334EI7ZpzzJ548Ma4L-hlHb9lvtA42MKx659zrFADyn71w__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Archaeological_investigations_in_northern_Laos_new_contributions_to_Southeast_Asian_prehistory","translated_slug":"","page_count":6,"language":"en","content_type":"Work","owner":{"id":56777151,"first_name":"Helen","middle_initials":null,"last_name":"Lewis","page_name":"HelenLewis21","domain_name":"independent","created_at":"2016-11-16T18:21:51.056-08:00","display_name":"Helen 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Journal of the University of the Philippines Archaeological Studies Program</span><span>, 2008</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Preliminary Results of Speleothem Dating from Tabon Cave, Palawan, Philippines: Moisture increase...</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">Preliminary Results of Speleothem Dating from Tabon Cave, Palawan, Philippines: Moisture increase at the Last Glacial Maximum Helen Lewis1, Kathleen Johnson2, and Wilf redo Ronquillo3 Abstract Preliminary study of a thick speleothem layer at Tabon Cave, Palawan ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="07f75fbcaa9ed24e71fb88e5064c7838" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":90985946,"asset_id":86561543,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/90985946/download_file?st=MTczMjg4MzczOSw4LjIyMi4yMDguMTQ2&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="86561543"><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="86561543"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 86561543; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=86561543]").text(description); $(".js-view-count[data-work-id=86561543]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 86561543; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='86561543']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 86561543, 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: "07f75fbcaa9ed24e71fb88e5064c7838" } } $('.js-work-strip[data-work-id=86561543]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":86561543,"title":"Preliminary results of speleothem dating from Tabon Cave, Palawan, Philippines: Moisture increase at the last glacial maximum?","translated_title":"","metadata":{"abstract":"Preliminary Results of Speleothem Dating from Tabon Cave, Palawan, Philippines: Moisture increase at the Last Glacial Maximum Helen Lewis1, Kathleen Johnson2, and Wilf redo Ronquillo3 Abstract Preliminary study of a thick speleothem layer at Tabon Cave, Palawan ...","publisher":"ucd-ie.academia.edu","publication_date":{"day":null,"month":null,"year":2008,"errors":{}},"publication_name":"Hukay. 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Several additional samples were taken from Trenches 5 and 7 on the South-east mound at Snusgar, and an auger assessment of the upper mound was conducted. Continued excavations of a Norse period structure on the East mound at Snusgar were the focus of this year&#39;s project. There appear to be at least two phases of the structure (a probable house), with evidence of remodelling apparent in the later phase. Near the end of the excavation a further intriguing structural component was revealed: a deep wall with apparent corbelling, underlying the later structures. Soil micromorphology sampling focused primarily on a series of clay layers, apparently laid floors or structural deposits, associated with both this deep wall and with the later structures. In 2006, ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e5dee482af7b3b16c70c3f76f1953be1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":90985963,"asset_id":86561570,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/90985963/download_file?st=MTczMjg4MzczOSw4LjIyMi4yMDguMTQ2&st=MTczMjg4MzczOCw4LjIyMi4yMDguMTQ2&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="86561570"><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="86561570"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 86561570; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=86561570]").text(description); $(".js-view-count[data-work-id=86561570]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 86561570; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='86561570']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 86561570, 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: "e5dee482af7b3b16c70c3f76f1953be1" } } $('.js-work-strip[data-work-id=86561570]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":86561570,"title":"Geoarchaeology at Snusgar, Orkney Mainland, 2007","translated_title":"","metadata":{"abstract":"A brief visit was carried out for geoarchaeological assessment and continued soil micromorphology sampling of deposits revealed during University of Oxford excavations at Snusgar and the Bay of Skaill, Mainland, Orkney, Scotland. 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The LGM was probably the most extreme climatic episode of cold and aridity at a global scale that our species has ever experienced, followed by sustained global warming. Within this broad picture, one of the most important developments in palaeoclimatic studies in recent decades has been the recognition of the instability of Late Pleistocene climates and the abrupt nature of climatic shifts, with millennial-, centennial and even shorter-scale shifts being discerned in the North Atlantic MIS 2 records (e.g. Blockley et al. 2006; Clark et al. 2002; Taylor et al. 1993; Fig. 5.1). In the northern hemisphere, there was a major shift to warmer and wetter conditions following the LGM termed the Bølling-Allerød interstadial (c. 14,700-12,800 bp), which was punctuated by at least two significant cold episodes, followed by a return to cold and dry near-glacial conditions, the Younger Dryas (c. 12,800-11,700 bp) before the shift to warmer climates that marked the Holocene. In the southern hemisphere, isotope studies of ice cores in Antarctica suggest a more continuous pattern of uninterrupted deglaciation and warming. It used to be thought that environmental change in the tropical lowlands of Southeast Asia during the Late Pleistocene must have been far less extreme than in northern latitudes, but it is now clear that many profound changes also took place in this region (Flenley 1997; Kershaw et al. 2007). The human populations of northern Borneo certainly had to cope with dramatic changes in the geography and ecology of the landscapes they inhabited in the Late Pleistocene, though as discussed in the next section their precise characteristics in the Niah region remain uncertain. Much important evidence about the climate, geography, and habitats of the region through this period derives from locations far distant from Niah. 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As in many other regions of the world, the term 'Neolithic' in Island Southeast Asia has traditionally been used to define the first agricultural communities, people who used a new material culture that included polished stone tools and pottery, and who based their subsistence primarily on the use of domestic crops and livestock. There are valid concerns about whether it is appropriate to apply to other parts of the world a term originally coined in the second half of the nineteenth century within the classification systems being established then for European prehistory. However, despite alternative local terminologies being proposed (e.g. Bacus 2004; Soejono 1997), the term 'Neolithic' remains a convenient label for the first pottery-using societies in Island Southeast Asia. As in Europe, though, one of the difficulties with the term is that archaeologists often use it with alternative meanings (sometimes within the same sentence, and often implicitly rather than explicitly): to denote a period of time; and/or a set of material culture (notably pottery and polished stone tools); and/or a way of life (agriculture). Although the term as originally proposed implied all three meanings-that everybody in the Neolithic period used Neolithic material culture and practised a 'Neolithic way of life' (i.e. agriculture)-subsequent research in many parts of the world has found examples of farmers living side by side with foragers in the 'Neolithic period'; of farmers not using the full suite of 'Neolithic material culture'; and of foragers using part of it (Barker 2006). 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Here we present the archaeobiological record of Pasimbahan-Magsanib site dating from c. 10,500 yr. BP to the subrecent. The terrestrial vertebrate record provides for a more robust Palawan biostratigraphy and chronicles Late Quaternary changes in mammalian composition and human responses to the changing abundance of large mammal communities. Well-stratified shell layers and middens contain a wide variety of taxa derived from freshwater, estuarine and marine environments that also provide insights on varying subsistence strategies and the local ecology. 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href="https://www.academia.edu/86561564/Terminal_Pleistocene_to_mid_Holocene_occupation_and_an_early_cremation_burial_at_Ille_Cave_Palawan_Philippines">Terminal Pleistocene to mid-Holocene occupation and an early cremation burial at Ille Cave, Palawan, Philippines</a></div><div class="wp-workCard_item"><span>Antiquity</span><span>, 2008</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Excavations at a cave site on the island of Palawan in the Philippines show occupation from c. 11...</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">Excavations at a cave site on the island of Palawan in the Philippines show occupation from c. 11000 BP. A fine assemblage of tools and faunal remains shows the reliance of hunter-foragers switching from deer to pig. In 9500-9000 BP, a human cremation burial in a container was emplaced, the earliest yet known in the region.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b92bd34393af5f4c94155133fa01bfe9" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":90985960,"asset_id":86561564,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/90985960/download_file?st=MTczMjg4MzczOSw4LjIyMi4yMDguMTQ2&st=MTczMjg4MzczOCw4LjIyMi4yMDguMTQ2&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="86561564"><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="86561564"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 86561564; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=86561564]").text(description); $(".js-view-count[data-work-id=86561564]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 86561564; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='86561564']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 86561564, 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: "b92bd34393af5f4c94155133fa01bfe9" } } $('.js-work-strip[data-work-id=86561564]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":86561564,"title":"Terminal Pleistocene to mid-Holocene occupation and an early cremation burial at Ille Cave, Palawan, Philippines","translated_title":"","metadata":{"abstract":"Excavations at a cave site on the island of Palawan in the Philippines show occupation from c. 11000 BP. 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The samples were taken as part of the first author's Ph.D. research, investigating Palaeolithic-Neolithic transitions in the northern Philippine region (Mijares 2005a, 2006), but also form a comparative collection for cultural cave sediments from the southern Philippines and Borneo, which are being investigated by the second author (Lewis 2003, 2007). Both of these projects focus on understanding the prehistory of cave occupation and how changes in this reflect larger-scale movements of people, cultural materials, and ideas in the Island Southeast Asian region, with an aim to relate cave sites to the wider landscape through a variety of approaches, including geoarchaeology and the location and excavation of contemporaneous open-air sites. background to the study Northeastern Luzon is composed of a large basin called the Cagayan Valley, which is circumscribed by the mountains of the Sierra Madre in the east, the Cordillera Central in the west, and the Caraballo range in the south (Fig. 1). The Sierra Madre is an inactive volcanic arc with peaks up to 1800 m, while the active Cordillera Central has peaks up to 3000 m. The Cagayan Valley, which is dissected by the northward flowing Cagayan River, is composed of marine, transitional marine, and non-marine volcaniclastic sediments (Mathisen and Vondra 1983). The cave sites discussed here are found in the Callao limestone formation, which runs along the western foothills of the Sierra Madre. 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href="https://www.academia.edu/86561561/Archaeological_investigations_in_northern_Laos_new_contributions_to_Southeast_Asian_prehistory"><img alt="Research paper thumbnail of Archaeological investigations in northern Laos: new contributions to Southeast Asian prehistory" class="work-thumbnail" src="https://attachments.academia-assets.com/90986043/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/86561561/Archaeological_investigations_in_northern_Laos_new_contributions_to_Southeast_Asian_prehistory">Archaeological investigations in northern Laos: new contributions to Southeast Asian prehistory</a></div><div class="wp-workCard_item"><span>Antiquity</span><span>, Mar 1, 2009</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Middle Mekong Archaeological Project (MMAP) was designed to investigate the prehistoric archa...</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">The Middle Mekong Archaeological Project (MMAP) was designed to investigate the prehistoric archaeology of the Luang Prabang region, which, although centrally located in mainland Southeast Asia, has seen little previous archaeological research (Figure 1; White & Bouasisengpaseuth 2008). The Mekong has long been thought to be an ancient highway for peoples, technologies and cultures, but due to historic political conditions, vast stretches of it remained inaccessible to modern archaeology until the 1990s.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3cd113aa7c32b65301c497786ae0f2ef" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":90986043,"asset_id":86561561,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/90986043/download_file?st=MTczMjg4MzczOSw4LjIyMi4yMDguMTQ2&st=MTczMjg4MzczOCw4LjIyMi4yMDguMTQ2&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="86561561"><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="86561561"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 86561561; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=86561561]").text(description); $(".js-view-count[data-work-id=86561561]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 86561561; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='86561561']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 86561561, 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: "3cd113aa7c32b65301c497786ae0f2ef" } } $('.js-work-strip[data-work-id=86561561]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":86561561,"title":"Archaeological investigations in northern Laos: new contributions to Southeast Asian prehistory","translated_title":"","metadata":{"abstract":"The Middle Mekong Archaeological Project (MMAP) was designed to investigate the prehistoric archaeology of the Luang Prabang region, which, although centrally located in mainland Southeast Asia, has seen little previous archaeological research (Figure 1; White \u0026 Bouasisengpaseuth 2008). The Mekong has long been thought to be an ancient highway for peoples, technologies and cultures, but due to historic political conditions, vast stretches of it remained inaccessible to modern archaeology until the 1990s.","publisher":"antiquity.ac.uk","publication_date":{"day":1,"month":3,"year":2009,"errors":{}},"publication_name":"Antiquity"},"translated_abstract":"The Middle Mekong Archaeological Project (MMAP) was designed to investigate the prehistoric archaeology of the Luang Prabang region, which, although centrally located in mainland Southeast Asia, has seen little previous archaeological research (Figure 1; White \u0026 Bouasisengpaseuth 2008). The Mekong has long been thought to be an ancient highway for peoples, technologies and cultures, but due to historic political conditions, vast stretches of it remained inaccessible to modern archaeology until the 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href="https://www.academia.edu/86561543/Preliminary_results_of_speleothem_dating_from_Tabon_Cave_Palawan_Philippines_Moisture_increase_at_the_last_glacial_maximum">Preliminary results of speleothem dating from Tabon Cave, Palawan, Philippines: Moisture increase at the last glacial maximum?</a></div><div class="wp-workCard_item"><span>Hukay. Journal of the University of the Philippines Archaeological Studies Program</span><span>, 2008</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Preliminary Results of Speleothem Dating from Tabon Cave, Palawan, Philippines: Moisture increase...</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">Preliminary Results of Speleothem Dating from Tabon Cave, Palawan, Philippines: Moisture increase at the Last Glacial Maximum Helen Lewis1, Kathleen Johnson2, and Wilf redo Ronquillo3 Abstract Preliminary study of a thick speleothem layer at Tabon Cave, Palawan ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="07f75fbcaa9ed24e71fb88e5064c7838" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":90985946,"asset_id":86561543,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/90985946/download_file?st=MTczMjg4MzczOSw4LjIyMi4yMDguMTQ2&st=MTczMjg4MzczOSw4LjIyMi4yMDguMTQ2&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="86561543"><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="86561543"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 86561543; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=86561543]").text(description); $(".js-view-count[data-work-id=86561543]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 86561543; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='86561543']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 86561543, 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: "07f75fbcaa9ed24e71fb88e5064c7838" } } $('.js-work-strip[data-work-id=86561543]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":86561543,"title":"Preliminary results of speleothem dating from Tabon Cave, Palawan, Philippines: Moisture increase at the last glacial maximum?","translated_title":"","metadata":{"abstract":"Preliminary Results of Speleothem Dating from Tabon Cave, Palawan, Philippines: Moisture increase at the Last Glacial Maximum Helen Lewis1, Kathleen Johnson2, and Wilf redo Ronquillo3 Abstract Preliminary study of a thick speleothem layer at Tabon Cave, Palawan ...","publisher":"ucd-ie.academia.edu","publication_date":{"day":null,"month":null,"year":2008,"errors":{}},"publication_name":"Hukay. 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