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Sherwood</h1><div class="affiliations-container fake-truncate js-profile-affiliations"><div><a class="u-tcGrayDarker" href="https://utk.academia.edu/">University of Tennessee Knoxville</a>, <a class="u-tcGrayDarker" href="https://utk.academia.edu/Departments/Anthropology/Documents">Anthropology</a>, <span class="u-tcGrayDarker">Adjunct</span></div><div><a class="u-tcGrayDarker" href="https://sewanee.academia.edu/">Sewanee: The University of the South</a>, <a class="u-tcGrayDarker" href="https://sewanee.academia.edu/Departments/Earth_and_Environmental_Systems/Documents">Earth and Environmental Systems</a>, <span class="u-tcGrayDarker">Research Professor</span></div></div></div></div><div class="sidebar-cta-container"><button class="ds2-5-button hidden profile-cta-button grow js-profile-follow-button" data-broccoli-component="user-info.follow-button" data-click-track="profile-user-info-follow-button" data-follow-user-fname="Sarah C." data-follow-user-id="6042077" 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Sherwood</h3></div><div class="js-work-strip profile--work_container" data-work-id="124555517"><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/124555517/Phase_II_Archeological_Investigation_of_the_Borrow_Pit_2_Site_Chesterfield_County_Virginia"><img alt="Research paper thumbnail of Phase II Archeological Investigation of the Borrow Pit 2 Site, Chesterfield County, Virginia" 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/124555517/Phase_II_Archeological_Investigation_of_the_Borrow_Pit_2_Site_Chesterfield_County_Virginia">Phase II Archeological Investigation of the Borrow Pit 2 Site, Chesterfield County, Virginia</a></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="124555517"><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="124555517"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124555517; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124555517]").text(description); $(".js-view-count[data-work-id=124555517]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124555517; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124555517']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124555517, 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" } } $('.js-work-strip[data-work-id=124555517]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124555517,"title":"Phase II Archeological Investigation of the Borrow Pit 2 Site, Chesterfield County, Virginia","translated_title":"","metadata":{"publication_date":{"day":null,"month":null,"year":1985,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/124555517/Phase_II_Archeological_Investigation_of_the_Borrow_Pit_2_Site_Chesterfield_County_Virginia","translated_internal_url":"","created_at":"2024-10-08T20:24:33.893-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6042077,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Phase_II_Archeological_Investigation_of_the_Borrow_Pit_2_Site_Chesterfield_County_Virginia","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":6042077,"first_name":"Sarah C.","middle_initials":null,"last_name":"Sherwood","page_name":"SarahSherwood","domain_name":"sewanee","created_at":"2013-10-09T08:07:57.348-07:00","display_name":"Sarah C. 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Edited by: Burkhard Vogt, Annette Kühlem, Andreas Mieth, Hans-Rudolf Bork</span><span>, 2019</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Rano Raraku is a collapsed structure on the flank of an erosional remnant of a former volcano. Wo...</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">Rano Raraku is a collapsed structure on the flank of an erosional remnant of a former volcano. Wood samples confirm the former presence of palm forests and other forests in the basin, including at least one species of a large tree that was utilized to build canoes. Very fine wood coal found in the excavated levels represents clearing of the vegetation and colluvium movement. There were twenty one samples collected from two sub-profiles from 15 cm to a depth of 225cm and 245 to 430 cm of depth respectively; these phytoliths contain banana leaves (Musa) and paper mulberry leaf filaments (Broussonetia papyrifera). This supports the idea that the crops and arboriculture were transferred from Polynesia.<br /><br />All this evidence suggests that the quarries were established and developed after the initiation of agriculture and the clearing of the forests which produced sterile slopes. The erosion of the slopes was responsible for burying the statues in a vertical position at a speed of ~1 cm per year at a level of 4.5 m in the chambers of the quarries that act like local depot centers. Evidence from human bones and the mention of a burial ceremonial (mortuaries) from Routledge 1919, point to the burial activities that were carried out. However, there was no supporting evidence behind Moai 156. The analysis of the bones is still ongoing, and is not described here.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d69caf42defaee6fb7262580261b1c23" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":109330327,"asset_id":111945782,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/109330327/download_file?st=MTczMjg3NTA0Nyw4LjIyMi4yMDguMTQ2&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="111945782"><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="111945782"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111945782; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=111945782]").text(description); $(".js-view-count[data-work-id=111945782]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 111945782; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='111945782']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 111945782, 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: "d69caf42defaee6fb7262580261b1c23" } } $('.js-work-strip[data-work-id=111945782]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":111945782,"title":"Rano Raraku Statue Quarry: Preliminary Interpretations of Human Activites Suggested by Recent Excavations, Geological Mapping and Coring, Soils Micromorphological Analyses and Related Scientific Tests","translated_title":"","metadata":{"abstract":"Rano Raraku is a collapsed structure on the flank of an erosional remnant of a former volcano. 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There were twenty one samples collected from two sub-profiles from 15 cm to a depth of 225cm and 245 to 430 cm of depth respectively; these phytoliths contain banana leaves (Musa) and paper mulberry leaf filaments (Broussonetia papyrifera). This supports the idea that the crops and arboriculture were transferred from Polynesia.\n\nAll this evidence suggests that the quarries were established and developed after the initiation of agriculture and the clearing of the forests which produced sterile slopes. The erosion of the slopes was responsible for burying the statues in a vertical position at a speed of ~1 cm per year at a level of 4.5 m in the chambers of the quarries that act like local depot centers. Evidence from human bones and the mention of a burial ceremonial (mortuaries) from Routledge 1919, point to the burial activities that were carried out. However, there was no supporting evidence behind Moai 156. The analysis of the bones is still ongoing, and is not described here. 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The objective of this study is to gather quantitative data through the chemical and physical analysis of soils collected within a valley transect to gain insights into landscape processes and soil fertility that may have played a role in the early development of plant domestication and the location of garden plots in relation to rock shelter sites in the upper Cumberland Plateau region of eastern Kentucky. Soils on upland benches formed in limestones have soil fertility values that are comparable to fertile floodplain soils. Upslope outcrops of calcareous bedrock are contributing basic cations to these bench soils. Additionally, in comparison to other landscape positions these upland soils have high levels of organic carbon, available P and greater C:N ratios. Soil morphology, radiocarbon dates, and archaeological evidence indicate that many of the numerous earthflows and debris flows within the region are Early to Middle Holocene in age. These slides were likely generated by Mid-Holocene climatic shifts in which the frequency and intensity of summer precipitation increased across the southeastern United States. These slope failures may have contributed to the development of plant domestication by creating forest canopy gaps and disturbed soils in which weedy plants thrived.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2c21d4e3dfff3103f42f3573123f76f9" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":109330055,"asset_id":111945385,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/109330055/download_file?st=MTczMjg3NTA0Nyw4LjIyMi4yMDguMTQ2&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="111945385"><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="111945385"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111945385; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=111945385]").text(description); $(".js-view-count[data-work-id=111945385]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 111945385; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='111945385']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 111945385, 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: "2c21d4e3dfff3103f42f3573123f76f9" } } $('.js-work-strip[data-work-id=111945385]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":111945385,"title":"Soil fertility and slope processes in the Western Cumberland Escarpment of Kentucky: influences on the development of horticulture in the Eastern Woodlands","translated_title":"","metadata":{"doi":"10.1016/j.jas.2007.11.023","abstract":"The archaeological record of dry rockshelters in the Red River Valley of eastern Kentucky contains botanical remains of several weedy annual seed-bearing plants that point to the independent development of agriculture during the Late Archaic and Early Woodland Period. The objective of this study is to gather quantitative data through the chemical and physical analysis of soils collected within a valley transect to gain insights into landscape processes and soil fertility that may have played a role in the early development of plant domestication and the location of garden plots in relation to rock shelter sites in the upper Cumberland Plateau region of eastern Kentucky. Soils on upland benches formed in limestones have soil fertility values that are comparable to fertile floodplain soils. Upslope outcrops of calcareous bedrock are contributing basic cations to these bench soils. Additionally, in comparison to other landscape positions these upland soils have high levels of organic carbon, available P and greater C:N ratios. Soil morphology, radiocarbon dates, and archaeological evidence indicate that many of the numerous earthflows and debris flows within the region are Early to Middle Holocene in age. These slides were likely generated by Mid-Holocene climatic shifts in which the frequency and intensity of summer precipitation increased across the southeastern United States. These slope failures may have contributed to the development of plant domestication by creating forest canopy gaps and disturbed soils in which weedy plants thrived.","publication_date":{"day":null,"month":null,"year":2008,"errors":{}},"publication_name":"Journal of Archaeological Science"},"translated_abstract":"The archaeological record of dry rockshelters in the Red River Valley of eastern Kentucky contains botanical remains of several weedy annual seed-bearing plants that point to the independent development of agriculture during the Late Archaic and Early Woodland Period. The objective of this study is to gather quantitative data through the chemical and physical analysis of soils collected within a valley transect to gain insights into landscape processes and soil fertility that may have played a role in the early development of plant domestication and the location of garden plots in relation to rock shelter sites in the upper Cumberland Plateau region of eastern Kentucky. Soils on upland benches formed in limestones have soil fertility values that are comparable to fertile floodplain soils. Upslope outcrops of calcareous bedrock are contributing basic cations to these bench soils. Additionally, in comparison to other landscape positions these upland soils have high levels of organic carbon, available P and greater C:N ratios. Soil morphology, radiocarbon dates, and archaeological evidence indicate that many of the numerous earthflows and debris flows within the region are Early to Middle Holocene in age. These slides were likely generated by Mid-Holocene climatic shifts in which the frequency and intensity of summer precipitation increased across the southeastern United States. These slope failures may have contributed to the development of plant domestication by creating forest canopy gaps and disturbed soils in which weedy plants thrived.","internal_url":"https://www.academia.edu/111945385/Soil_fertility_and_slope_processes_in_the_Western_Cumberland_Escarpment_of_Kentucky_influences_on_the_development_of_horticulture_in_the_Eastern_Woodlands","translated_internal_url":"","created_at":"2023-12-20T15:05:20.832-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6042077,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":40761388,"work_id":111945385,"tagging_user_id":6042077,"tagged_user_id":null,"co_author_invite_id":3144308,"email":"j***d@sricrm.com","display_order":1,"name":"J. 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Sherwood","url":"https://sewanee.academia.edu/SarahSherwood"},"attachments":[{"id":109330055,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/109330055/thumbnails/1.jpg","file_name":"Windingstad_et_al_2008.pdf","download_url":"https://www.academia.edu/attachments/109330055/download_file?st=MTczMjg3NTA0Nyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Soil_fertility_and_slope_processes_in_th.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/109330055/Windingstad_et_al_2008-libre.pdf?1703116279=\u0026response-content-disposition=attachment%3B+filename%3DSoil_fertility_and_slope_processes_in_th.pdf\u0026Expires=1732878647\u0026Signature=hHiiyrON~Zfr33FmsSuucw4WyYr7oIeja5mZQbk45wwxTE7WxkDzwa~ujG25FtZyeJg6xkebdqlD2tJ2xZlgXkrVqwT2b5AmgftjZd5wD8n7nQ6p~vqtvn7MVxqHjRtuLJLkiNmoinUr4Ltf~w8xGHBBX9J~vr9Eh~7ICuCfahECoFUTfWqegUfnsZhwAtmZmNpWB9xCJh7N2YAFxkRpDIt4-RGqDLde6JQlL~birYK4QbXnbVlI1y8S~vjkWgDQZofHAv5FhM~xtxvhb0Q2CdLiI5qRs4fZ8Pwizn-3Tye2gS5Lf3~fbR-xEIZKkLldfkhGOc2Ivmu-jFQv4SFLFw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":18088,"name":"Southeastern Archaeology (Archaeology in North America)","url":"https://www.academia.edu/Documents/in/Southeastern_Archaeology_Archaeology_in_North_America_"}],"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="82248597"><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/82248597/Legacies_of_Past_Land_Use_on_the_Southern_Cumberland_Plateau"><img alt="Research paper thumbnail of Legacies of Past Land Use on the Southern Cumberland Plateau" class="work-thumbnail" src="https://attachments.academia-assets.com/109331351/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/82248597/Legacies_of_Past_Land_Use_on_the_Southern_Cumberland_Plateau">Legacies of Past Land Use on the Southern Cumberland Plateau</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://sewanee.academia.edu/SarahSherwood">Sarah C. Sherwood</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/kevinHiers">kevin Hiers</a></span></div><div class="wp-workCard_item"><span>Natural Areas Journal</span><span>, 2019</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT: Prior land use and soil legacies related to land use continue to play a significant rol...</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: Prior land use and soil legacies related to land use continue to play a significant role in ecosystem structure and functioning in the eastern deciduous forest. On the surface of the southern Cumberland Plateau in Tennessee, abandoned agricultural and home sites are characterized by unusual assemblages of tree species and ground cover, as well as light artifact scatters. To better understand the legacies of past land use on soil properties and forest composition in this region, we intensively sampled three home sites that were abandoned more than 70 y ago and compared them to adjacent forest controls. The home sites had significantly higher concentrations (soil A horizons) for eight of the fourteen elements studied. After examining our plots in ordination space by soil variables, we found that surface soil calcium and phosphorus concentrations were negatively associated to control plots and were the best indicators of intensive human disturbance. Sourwood (Oxydendrum arboreum) had the highest importance value in the control forest, and the 23rd highest importance value at the home sites. There were 34 different species encountered at the home sites, including many species usually found at lower elevations in limestone-derived soils (e.g., Celtis occidentalis, Juglans nigra, Viburnum rufidulum, Fraxinus spp.). We recovered historic artifacts and charcoal from surface soils at all three sites, and prehistoric artifacts were found at two sites. Abandoned home sites are common throughout the eastern deciduous forest and evidence from this study indicates that land use legacies continue to influence forest dynamics several decades after anthropogenic inputs ceased.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2379a651b41610e2b9678b60eb6a8763" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":109331351,"asset_id":82248597,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/109331351/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&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="82248597"><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="82248597"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 82248597; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=82248597]").text(description); $(".js-view-count[data-work-id=82248597]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 82248597; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='82248597']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 82248597, 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: "2379a651b41610e2b9678b60eb6a8763" } } $('.js-work-strip[data-work-id=82248597]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":82248597,"title":"Legacies of Past Land Use on the Southern Cumberland Plateau","translated_title":"","metadata":{"doi":"10.3375/043.039.0212","issue":"2","volume":"39","abstract":"ABSTRACT: Prior land use and soil legacies related to land use continue to play a significant role in ecosystem structure and functioning in the eastern deciduous forest. On the surface of the southern Cumberland Plateau in Tennessee, abandoned agricultural and home sites are characterized by unusual assemblages of tree species and ground cover, as well as light artifact scatters. To better understand the legacies of past land use on soil properties and forest composition in this region, we intensively sampled three home sites that were abandoned more than 70 y ago and compared them to adjacent forest controls. The home sites had significantly higher concentrations (soil A horizons) for eight of the fourteen elements studied. After examining our plots in ordination space by soil variables, we found that surface soil calcium and phosphorus concentrations were negatively associated to control plots and were the best indicators of intensive human disturbance. Sourwood (Oxydendrum arboreum) had the highest importance value in the control forest, and the 23rd highest importance value at the home sites. There were 34 different species encountered at the home sites, including many species usually found at lower elevations in limestone-derived soils (e.g., Celtis occidentalis, Juglans nigra, Viburnum rufidulum, Fraxinus spp.). We recovered historic artifacts and charcoal from surface soils at all three sites, and prehistoric artifacts were found at two sites. Abandoned home sites are common throughout the eastern deciduous forest and evidence from this study indicates that land use legacies continue to influence forest dynamics several decades after anthropogenic inputs ceased.","publisher":"Natural Areas Journal","ai_title_tag":"Influence of Past Land Use on Southern Cumberland Plateau Ecosystem","page_numbers":"264 - 174","publication_date":{"day":null,"month":null,"year":2019,"errors":{}},"publication_name":"Natural Areas Journal"},"translated_abstract":"ABSTRACT: Prior land use and soil legacies related to land use continue to play a significant role in ecosystem structure and functioning in the eastern deciduous forest. On the surface of the southern Cumberland Plateau in Tennessee, abandoned agricultural and home sites are characterized by unusual assemblages of tree species and ground cover, as well as light artifact scatters. To better understand the legacies of past land use on soil properties and forest composition in this region, we intensively sampled three home sites that were abandoned more than 70 y ago and compared them to adjacent forest controls. The home sites had significantly higher concentrations (soil A horizons) for eight of the fourteen elements studied. After examining our plots in ordination space by soil variables, we found that surface soil calcium and phosphorus concentrations were negatively associated to control plots and were the best indicators of intensive human disturbance. Sourwood (Oxydendrum arboreum) had the highest importance value in the control forest, and the 23rd highest importance value at the home sites. There were 34 different species encountered at the home sites, including many species usually found at lower elevations in limestone-derived soils (e.g., Celtis occidentalis, Juglans nigra, Viburnum rufidulum, Fraxinus spp.). We recovered historic artifacts and charcoal from surface soils at all three sites, and prehistoric artifacts were found at two sites. Abandoned home sites are common throughout the eastern deciduous forest and evidence from this study indicates that land use legacies continue to influence forest dynamics several decades after anthropogenic inputs ceased.","internal_url":"https://www.academia.edu/82248597/Legacies_of_Past_Land_Use_on_the_Southern_Cumberland_Plateau","translated_internal_url":"","created_at":"2022-06-27T10:24:44.021-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6042077,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":40761484,"work_id":82248597,"tagging_user_id":6042077,"tagged_user_id":28562947,"co_author_invite_id":null,"email":"k***h@fcs.utah.edu","display_order":-1,"name":"Ken Smith","title":"Legacies of Past Land Use on the Southern Cumberland Plateau"},{"id":40761482,"work_id":82248597,"tagging_user_id":6042077,"tagged_user_id":216294126,"co_author_invite_id":null,"email":"s***i@talltimbers.org","display_order":1,"name":"Scott Pokswinski","title":"Legacies of Past Land Use on the Southern Cumberland Plateau"},{"id":40761483,"work_id":82248597,"tagging_user_id":6042077,"tagged_user_id":297901215,"co_author_invite_id":7999196,"email":"j***s@ag.tamu.edu","display_order":2,"name":"kevin Hiers","title":"Legacies of Past Land Use on the Southern Cumberland Plateau"}],"downloadable_attachments":[{"id":109331351,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/109331351/thumbnails/1.jpg","file_name":"smith_et_al_2019.pdf","download_url":"https://www.academia.edu/attachments/109331351/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Legacies_of_Past_Land_Use_on_the_Souther.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/109331351/smith_et_al_2019-libre.pdf?1703120205=\u0026response-content-disposition=attachment%3B+filename%3DLegacies_of_Past_Land_Use_on_the_Souther.pdf\u0026Expires=1732878648\u0026Signature=DTLQQuY~OHn4SATYiyb5f7MUwXjPpNX1WnYu6DBrpCKSgQ4wZidCuCN1gBFpSdUEGJ2x4LvTUfh0PAVkNmarcUOfm-sxuiMY3dIcNmpcWJPBPtwaaIqaCGNvOFz6HvLkiNoygK84Jgb9FaMB4FwJrhDYhSJkKNVNyu1nVo~~UrV0pqX8Wt03QFw~AVm6FJOz4~ANAZBZ7TqbnG2tlpUB3tIWxUs3LmYsILkpGLw3kjx~cFCsJ-PIIZ6BtCL7s8svhBvQEyspipBmpQjyTKrCULGGbmch~66VAm8pKN3cWobh4TXu03E9U0vpP8wy23-YThJ0i5hSyI43utJpeFQZhg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Legacies_of_Past_Land_Use_on_the_Southern_Cumberland_Plateau","translated_slug":"","page_count":12,"language":"en","content_type":"Work","owner":{"id":6042077,"first_name":"Sarah C.","middle_initials":null,"last_name":"Sherwood","page_name":"SarahSherwood","domain_name":"sewanee","created_at":"2013-10-09T08:07:57.348-07:00","display_name":"Sarah C. 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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="81727680"><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/81727680/A_Preliminary_Report_on_the_Archaeology_of_a_New_Mississippian_Cave_Art_Site_In_East_Tennessee"><img alt="Research paper thumbnail of A Preliminary Report on the Archaeology of a New Mississippian Cave Art Site In East Tennessee" class="work-thumbnail" src="https://attachments.academia-assets.com/109331481/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/81727680/A_Preliminary_Report_on_the_Archaeology_of_a_New_Mississippian_Cave_Art_Site_In_East_Tennessee">A Preliminary Report on the Archaeology of a New Mississippian Cave Art Site In East Tennessee</a></div><div class="wp-workCard_item"><span>Southeastern Archaeology</span><span>, 1997</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="46ebf76ce875c49c5e9fc72f8f2e95e2" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":109331481,"asset_id":81727680,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/109331481/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&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="81727680"><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="81727680"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 81727680; 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The cøae uestibule contains intact sedimentary deposits preseraing prehistoric archaeolo gical lay ers in undisturb ed stratigr øphic p o sition ; øt least two hearth features are present. Artifacts from the aestibule indicnte occupation from Løte Woodland through Late Mississippiøn times. A radiocørbon døte from inside the caae (260 t 50yrs B.P.) confirms use during the Løte Mississþpian. The glyph ørt aøries in form and subject matter. There is spatial patterning at seaeral scales: glyphs are grouped into panels, and sets of panels form concentrations within the cøae. Content aaries at both of these spatial scales. 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Midcontinental journal of archaeology</span><span>, 2001</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Cave deposits are complex sequences derived from multiple sources and numerous processes which of...</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">Cave deposits are complex sequences derived from multiple sources and numerous processes which often operate simultaneously. These sequences are largely the result of unique microenvironments that vary between subterranean passages (beyond the reaches of natural light and ambient conditions) and subaerial entrances (natural light and ambient temperature and moisture conditions). In subterranean passages, where sedimentation rates are extremely low, endogenous processes are the primary sediment source, and archaeologists must identify artifact palimpsests on ancient surfaces. In cave entrances where sedimentation rates are high and artifact preservation can be exceptional, both endogenous and exogenous processes must be considered. In both depositional environments human activity can generate significant amounts of sediment. With an emphasis on the karstic Eastern Woodlands, we suggest a geoarchaeological framework that focuses on the description and classification of the sediments. ...</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="72139443"><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="72139443"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 72139443; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=72139443]").text(description); $(".js-view-count[data-work-id=72139443]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 72139443; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='72139443']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 72139443, 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" } } $('.js-work-strip[data-work-id=72139443]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":72139443,"title":"A geoarchaeological framework for the study of karstic cave sites in the Eastern Woodlands","translated_title":"","metadata":{"abstract":"Cave deposits are complex sequences derived from multiple sources and numerous processes which often operate simultaneously. 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Sherwood. In ARCHEOLOGICAL INVESTIGATIONS AT SHILOH INDIAN MOUNDS NATIONAL HISTORIC LANDMARK (40HR7) 1999-2004 VOLUME 2 of 2. Edited by David G. Anderson, John E. Cornelison, Jr. and Sarah C. Sherwood" 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/72140286/A_Geoarchaeological_Study_of_the_Mound_A_Stratigraphy_Chapter_10_by_Sarah_C_Sherwood_In_ARCHEOLOGICAL_INVESTIGATIONS_AT_SHILOH_INDIAN_MOUNDS_NATIONAL_HISTORIC_LANDMARK_40HR7_1999_2004_VOLUME_2_of_2_Edited_by_David_G_Anderson_John_E_Cornelison_Jr_and_Sarah_C_Sherwood">A Geoarchaeological Study of the Mound A Stratigraphy, Chapter 10, by Sarah C. Sherwood. In ARCHEOLOGICAL INVESTIGATIONS AT SHILOH INDIAN MOUNDS NATIONAL HISTORIC LANDMARK (40HR7) 1999-2004 VOLUME 2 of 2. Edited by David G. Anderson, John E. Cornelison, Jr. and Sarah C. Sherwood</a></div><div class="wp-workCard_item"><span>ARCHEOLOGICAL INVESTIGATIONS AT SHILOH INDIAN MOUNDS NATIONAL HISTORIC LANDMARK (40HR7) 1999-2004 VOLUMES 1 and 2</span><span>, 2013</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Full report ARCHEOLOGICAL INVESTIGATIONS AT SHILOH INDIAN MOUNDS NATIONAL HISTORIC LANDMARK (40HR...</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">Full report ARCHEOLOGICAL INVESTIGATIONS AT SHILOH INDIAN MOUNDS NATIONAL HISTORIC LANDMARK (40HR7) 1999-2004, 2 VOLUMES published by the US National Park Service, Southeast Archeological Center, Tallahassee, Florida<br />Available online <br /><a href="http://pidba.org/anderson/cv/2013.Anderson.Shiloh.pdf" rel="nofollow">http://pidba.org/anderson/cv/2013.Anderson.Shiloh.pdf</a></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="72140286"><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="72140286"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 72140286; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=72140286]").text(description); $(".js-view-count[data-work-id=72140286]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 72140286; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='72140286']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 72140286, 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" } } $('.js-work-strip[data-work-id=72140286]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":72140286,"title":"A Geoarchaeological Study of the Mound A Stratigraphy, Chapter 10, by Sarah C. 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Sherwood</h3></div><div class="js-work-strip profile--work_container" data-work-id="16856756"><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/16856756/Book_Review_Archaeological_sediments_and_soils_Analysis_interpretation_and_management"><img alt="Research paper thumbnail of Book Review: Archaeological sediments and soils: Analysis, interpretation and management" class="work-thumbnail" src="https://attachments.academia-assets.com/42382351/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/16856756/Book_Review_Archaeological_sediments_and_soils_Analysis_interpretation_and_management">Book Review: Archaeological sediments and soils: Analysis, interpretation and management</a></div><div class="wp-workCard_item"><span>Geoarchaeology</span><span>, 1998</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="7e6979f9dfca0c61b342a0898c2a3935" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":42382351,"asset_id":16856756,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/42382351/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&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="16856756"><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="16856756"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 16856756; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=16856756]").text(description); $(".js-view-count[data-work-id=16856756]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 16856756; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='16856756']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 16856756, 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: "7e6979f9dfca0c61b342a0898c2a3935" } } $('.js-work-strip[data-work-id=16856756]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":16856756,"title":"Book Review: Archaeological sediments and soils: Analysis, interpretation and management","translated_title":"","metadata":{"grobid_abstract":"There are few books that focus specifically on archaeological sediments and soils and even fewer that clearly make the distinction between the two. 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Sherwood</h3></div><div class="js-work-strip profile--work_container" data-work-id="111946645"><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/111946645/The_Geoarchaeology_of_the_Tennessee_Valley_Methodological_and_Archaeological_Milestones"><img alt="Research paper thumbnail of The Geoarchaeology of the Tennessee Valley: Methodological and Archaeological Milestones" class="work-thumbnail" src="https://attachments.academia-assets.com/109330960/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/111946645/The_Geoarchaeology_of_the_Tennessee_Valley_Methodological_and_Archaeological_Milestones">The Geoarchaeology of the Tennessee Valley: Methodological and Archaeological Milestones</a></div><div class="wp-workCard_item"><span>TVA Archaeology: Seventy-five Years of Prehistoric Site Research</span><span>, 2009</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="385de9c49bb42236fed146a9962cb56d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":109330960,"asset_id":111946645,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/109330960/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&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="111946645"><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="111946645"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111946645; 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Edited by Valentí Rull, Christopher Stevenson</span><span>, 2022</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The geographical remoteness and physical location of Rapa Nui relative to coastal South America h...</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 geographical remoteness and physical location of Rapa Nui relative to coastal South America have long encouraged research speculation about the island’s possible role, if any, in the transfer into Polynesia and subsequent dispersal of sweet potato (Ipomoea batatas; kumara) (Dixon 1932; Stokes 1932; Heyerdahl and Ferdon Jr. 1961; Yen 1974; Green 1988, 2001, 2005; Clarke 2009; Scaglion and Cordero 2011). New evidence is presented in this chapter for the first well-documented, directly dated, pre-European contact find of carbonized sweet potato tuber, which was derived from recent excavations in Rano Raraku, the monolithic statue (moai) quarry (Horrocks 2014; Sherwood et al. 2019).</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="111946378"><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="111946378"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111946378; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=111946378]").text(description); $(".js-view-count[data-work-id=111946378]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 111946378; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='111946378']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 111946378, 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" } } $('.js-work-strip[data-work-id=111946378]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":111946378,"title":"Pre-European Contact Sweet Potato (Ipomoea batatas) at Rapa Nui: Macrobotanical Evidence from Recent Excavations in Rano Raraku Quarry, Rapa Nui","translated_title":"","metadata":{"abstract":"The geographical remoteness and physical location of Rapa Nui relative to coastal South America have long encouraged research speculation about the island’s possible role, if any, in the transfer into Polynesia and subsequent dispersal of sweet potato (Ipomoea batatas; kumara) (Dixon 1932; Stokes 1932; Heyerdahl and Ferdon Jr. 1961; Yen 1974; Green 1988, 2001, 2005; Clarke 2009; Scaglion and Cordero 2011). 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In Earth Sciences and Archaeology. edited by P. Goldberg, V.T. Holliday, and C.R. Ferring. pp. 327-351. Kluwer Academic/Plenum Publishers, New York." class="work-thumbnail" src="https://attachments.academia-assets.com/32298489/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/5079686/2001_Microartifacts_In_Earth_Sciences_and_Archaeology_edited_by_P_Goldberg_V_T_Holliday_and_C_R_Ferring_pp_327_351_Kluwer_Academic_Plenum_Publishers_New_York">2001 Microartifacts. In Earth Sciences and Archaeology. edited by P. Goldberg, V.T. Holliday, and C.R. Ferring. pp. 327-351. Kluwer Academic/Plenum Publishers, New York.</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="84d2691b30b10f37d8645a38a968766d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":32298489,"asset_id":5079686,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/32298489/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&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="5079686"><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="5079686"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 5079686; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=5079686]").text(description); $(".js-view-count[data-work-id=5079686]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 5079686; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='5079686']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 5079686, 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: "84d2691b30b10f37d8645a38a968766d" } } $('.js-work-strip[data-work-id=5079686]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":5079686,"title":"2001\tMicroartifacts. 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Sherwood</a></span></div><div class="wp-workCard_item"><span>Evolutionary Anthropology: Issues, News, and Reviews</span><span>, 2006</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="63d340a05a882a0905970319ac54417a" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39221466,"asset_id":16856754,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39221466/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&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="16856754"><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="16856754"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 16856754; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=16856754]").text(description); $(".js-view-count[data-work-id=16856754]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 16856754; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='16856754']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 16856754, 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: "63d340a05a882a0905970319ac54417a" } } $('.js-work-strip[data-work-id=16856754]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":16856754,"title":"Deciphering human prehistory through the geoarcheological study of cave sediments","translated_title":"","metadata":{"grobid_abstract":"Much of our knowledge about cave sediments and people comes from as-sociation with archeologists and earth scientists over many years and even decades. 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Edited by: Burkhard Vogt, Annette Kühlem, Andreas Mieth, Hans-Rudolf Bork</span><span>, 2019</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Rano Raraku is a collapsed structure on the flank of an erosional remnant of a former volcano. Wo...</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">Rano Raraku is a collapsed structure on the flank of an erosional remnant of a former volcano. Wood samples confirm the former presence of palm forests and other forests in the basin, including at least one species of a large tree that was utilized to build canoes. Very fine wood coal found in the excavated levels represents clearing of the vegetation and colluvium movement. There were twenty one samples collected from two sub-profiles from 15 cm to a depth of 225cm and 245 to 430 cm of depth respectively; these phytoliths contain banana leaves (Musa) and paper mulberry leaf filaments (Broussonetia papyrifera). This supports the idea that the crops and arboriculture were transferred from Polynesia.<br /><br />All this evidence suggests that the quarries were established and developed after the initiation of agriculture and the clearing of the forests which produced sterile slopes. The erosion of the slopes was responsible for burying the statues in a vertical position at a speed of ~1 cm per year at a level of 4.5 m in the chambers of the quarries that act like local depot centers. Evidence from human bones and the mention of a burial ceremonial (mortuaries) from Routledge 1919, point to the burial activities that were carried out. However, there was no supporting evidence behind Moai 156. The analysis of the bones is still ongoing, and is not described here.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d69caf42defaee6fb7262580261b1c23" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":109330327,"asset_id":111945782,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/109330327/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&st=MTczMjg3NTA0Nyw4LjIyMi4yMDguMTQ2&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="111945782"><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="111945782"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111945782; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=111945782]").text(description); $(".js-view-count[data-work-id=111945782]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 111945782; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='111945782']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 111945782, 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: "d69caf42defaee6fb7262580261b1c23" } } $('.js-work-strip[data-work-id=111945782]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":111945782,"title":"Rano Raraku Statue Quarry: Preliminary Interpretations of Human Activites Suggested by Recent Excavations, Geological Mapping and Coring, Soils Micromorphological Analyses and Related Scientific Tests","translated_title":"","metadata":{"abstract":"Rano Raraku is a collapsed structure on the flank of an erosional remnant of a former volcano. Wood samples confirm the former presence of palm forests and other forests in the basin, including at least one species of a large tree that was utilized to build canoes. Very fine wood coal found in the excavated levels represents clearing of the vegetation and colluvium movement. There were twenty one samples collected from two sub-profiles from 15 cm to a depth of 225cm and 245 to 430 cm of depth respectively; these phytoliths contain banana leaves (Musa) and paper mulberry leaf filaments (Broussonetia papyrifera). This supports the idea that the crops and arboriculture were transferred from Polynesia.\n\nAll this evidence suggests that the quarries were established and developed after the initiation of agriculture and the clearing of the forests which produced sterile slopes. The erosion of the slopes was responsible for burying the statues in a vertical position at a speed of ~1 cm per year at a level of 4.5 m in the chambers of the quarries that act like local depot centers. 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","internal_url":"https://www.academia.edu/111945782/Rano_Raraku_Statue_Quarry_Preliminary_Interpretations_of_Human_Activites_Suggested_by_Recent_Excavations_Geological_Mapping_and_Coring_Soils_Micromorphological_Analyses_and_Related_Scientific_Tests","translated_internal_url":"","created_at":"2023-12-20T15:14:53.126-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6042077,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":40761418,"work_id":111945782,"tagging_user_id":6042077,"tagged_user_id":30127095,"co_author_invite_id":null,"email":"j***l@g.ucla.edu","affiliation":"University of California, Los Angeles","display_order":-1,"name":"Jo Anne Van Tilburg","title":"Rano Raraku Statue Quarry: Preliminary Interpretations of Human Activites Suggested by Recent Excavations, Geological Mapping and Coring, Soils Micromorphological Analyses and Related Scientific Tests"},{"id":40761419,"work_id":111945782,"tagging_user_id":6042077,"tagged_user_id":101291,"co_author_invite_id":null,"email":"r***n@norwich.edu","affiliation":"Norwich University","display_order":1,"name":"Richard Dunn","title":"Rano Raraku Statue Quarry: Preliminary Interpretations of Human Activites Suggested by Recent Excavations, Geological Mapping and Coring, Soils Micromorphological Analyses and Related Scientific Tests"}],"downloadable_attachments":[{"id":109330327,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/109330327/thumbnails/1.jpg","file_name":"VanTilburg_et_al_2019.pdf","download_url":"https://www.academia.edu/attachments/109330327/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&st=MTczMjg3NTA0Nyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Rano_Raraku_Statue_Quarry_Preliminary_In.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/109330327/VanTilburg_et_al_2019-libre.pdf?1703116285=\u0026response-content-disposition=attachment%3B+filename%3DRano_Raraku_Statue_Quarry_Preliminary_In.pdf\u0026Expires=1732878647\u0026Signature=X5FdRFVa~kUTdztQGOnmNypckTNsVpfwnPdZpG4hBv9mn3Bom364xfMsTcfB6fCq~a0KHqrGBTRiAxkFcmHe1rAGrvHg9Yp~lNf~6fvjiqmoN7ca1b9lrQ8RaKkx-n05yMoptXFq71LV-0M7sGTf6PEWz-dbBx2wqhfsfGWAEdUgfRyX3Dk9PAYiiLZm3wn6IePKz7S~a2idHbIQ9z-MX0t3RcDt2LYVHSTFhZ4FdtvsGyf1vU4~pSshAcHwG9icd~o2GMm6SPwff263qixznVyvj3h5aZJAMtJLBMHeX5i80G00OgLkJEqyW9RMJmBIpXMfW9~1PFb7d6siSHeFWg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Rano_Raraku_Statue_Quarry_Preliminary_Interpretations_of_Human_Activites_Suggested_by_Recent_Excavations_Geological_Mapping_and_Coring_Soils_Micromorphological_Analyses_and_Related_Scientific_Tests","translated_slug":"","page_count":12,"language":"en","content_type":"Work","owner":{"id":6042077,"first_name":"Sarah C.","middle_initials":null,"last_name":"Sherwood","page_name":"SarahSherwood","domain_name":"sewanee","created_at":"2013-10-09T08:07:57.348-07:00","display_name":"Sarah C. 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The objective of this study is to gather quantitative data through the chemical and physical analysis of soils collected within a valley transect to gain insights into landscape processes and soil fertility that may have played a role in the early development of plant domestication and the location of garden plots in relation to rock shelter sites in the upper Cumberland Plateau region of eastern Kentucky. Soils on upland benches formed in limestones have soil fertility values that are comparable to fertile floodplain soils. Upslope outcrops of calcareous bedrock are contributing basic cations to these bench soils. Additionally, in comparison to other landscape positions these upland soils have high levels of organic carbon, available P and greater C:N ratios. Soil morphology, radiocarbon dates, and archaeological evidence indicate that many of the numerous earthflows and debris flows within the region are Early to Middle Holocene in age. These slides were likely generated by Mid-Holocene climatic shifts in which the frequency and intensity of summer precipitation increased across the southeastern United States. These slope failures may have contributed to the development of plant domestication by creating forest canopy gaps and disturbed soils in which weedy plants thrived.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2c21d4e3dfff3103f42f3573123f76f9" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":109330055,"asset_id":111945385,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/109330055/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&st=MTczMjg3NTA0Nyw4LjIyMi4yMDguMTQ2&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="111945385"><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="111945385"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111945385; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=111945385]").text(description); $(".js-view-count[data-work-id=111945385]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 111945385; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='111945385']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 111945385, 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: "2c21d4e3dfff3103f42f3573123f76f9" } } $('.js-work-strip[data-work-id=111945385]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":111945385,"title":"Soil fertility and slope processes in the Western Cumberland Escarpment of Kentucky: influences on the development of horticulture in the Eastern Woodlands","translated_title":"","metadata":{"doi":"10.1016/j.jas.2007.11.023","abstract":"The archaeological record of dry rockshelters in the Red River Valley of eastern Kentucky contains botanical remains of several weedy annual seed-bearing plants that point to the independent development of agriculture during the Late Archaic and Early Woodland Period. The objective of this study is to gather quantitative data through the chemical and physical analysis of soils collected within a valley transect to gain insights into landscape processes and soil fertility that may have played a role in the early development of plant domestication and the location of garden plots in relation to rock shelter sites in the upper Cumberland Plateau region of eastern Kentucky. Soils on upland benches formed in limestones have soil fertility values that are comparable to fertile floodplain soils. Upslope outcrops of calcareous bedrock are contributing basic cations to these bench soils. Additionally, in comparison to other landscape positions these upland soils have high levels of organic carbon, available P and greater C:N ratios. Soil morphology, radiocarbon dates, and archaeological evidence indicate that many of the numerous earthflows and debris flows within the region are Early to Middle Holocene in age. 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Sherwood</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/kevinHiers">kevin Hiers</a></span></div><div class="wp-workCard_item"><span>Natural Areas Journal</span><span>, 2019</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT: Prior land use and soil legacies related to land use continue to play a significant rol...</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: Prior land use and soil legacies related to land use continue to play a significant role in ecosystem structure and functioning in the eastern deciduous forest. On the surface of the southern Cumberland Plateau in Tennessee, abandoned agricultural and home sites are characterized by unusual assemblages of tree species and ground cover, as well as light artifact scatters. To better understand the legacies of past land use on soil properties and forest composition in this region, we intensively sampled three home sites that were abandoned more than 70 y ago and compared them to adjacent forest controls. The home sites had significantly higher concentrations (soil A horizons) for eight of the fourteen elements studied. After examining our plots in ordination space by soil variables, we found that surface soil calcium and phosphorus concentrations were negatively associated to control plots and were the best indicators of intensive human disturbance. Sourwood (Oxydendrum arboreum) had the highest importance value in the control forest, and the 23rd highest importance value at the home sites. There were 34 different species encountered at the home sites, including many species usually found at lower elevations in limestone-derived soils (e.g., Celtis occidentalis, Juglans nigra, Viburnum rufidulum, Fraxinus spp.). We recovered historic artifacts and charcoal from surface soils at all three sites, and prehistoric artifacts were found at two sites. Abandoned home sites are common throughout the eastern deciduous forest and evidence from this study indicates that land use legacies continue to influence forest dynamics several decades after anthropogenic inputs ceased.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2379a651b41610e2b9678b60eb6a8763" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":109331351,"asset_id":82248597,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/109331351/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&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="82248597"><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="82248597"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 82248597; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=82248597]").text(description); $(".js-view-count[data-work-id=82248597]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 82248597; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='82248597']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 82248597, 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: "2379a651b41610e2b9678b60eb6a8763" } } $('.js-work-strip[data-work-id=82248597]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":82248597,"title":"Legacies of Past Land Use on the Southern Cumberland Plateau","translated_title":"","metadata":{"doi":"10.3375/043.039.0212","issue":"2","volume":"39","abstract":"ABSTRACT: Prior land use and soil legacies related to land use continue to play a significant role in ecosystem structure and functioning in the eastern deciduous forest. 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Midcontinental journal of archaeology</span><span>, 2001</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Cave deposits are complex sequences derived from multiple sources and numerous processes which of...</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">Cave deposits are complex sequences derived from multiple sources and numerous processes which often operate simultaneously. These sequences are largely the result of unique microenvironments that vary between subterranean passages (beyond the reaches of natural light and ambient conditions) and subaerial entrances (natural light and ambient temperature and moisture conditions). In subterranean passages, where sedimentation rates are extremely low, endogenous processes are the primary sediment source, and archaeologists must identify artifact palimpsests on ancient surfaces. In cave entrances where sedimentation rates are high and artifact preservation can be exceptional, both endogenous and exogenous processes must be considered. In both depositional environments human activity can generate significant amounts of sediment. With an emphasis on the karstic Eastern Woodlands, we suggest a geoarchaeological framework that focuses on the description and classification of the sediments. ...</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="72139443"><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="72139443"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 72139443; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=72139443]").text(description); $(".js-view-count[data-work-id=72139443]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 72139443; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='72139443']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 72139443, 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" } } $('.js-work-strip[data-work-id=72139443]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":72139443,"title":"A geoarchaeological framework for the study of karstic cave sites in the Eastern Woodlands","translated_title":"","metadata":{"abstract":"Cave deposits are complex sequences derived from multiple sources and numerous processes which often operate simultaneously. 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Sherwood. In ARCHEOLOGICAL INVESTIGATIONS AT SHILOH INDIAN MOUNDS NATIONAL HISTORIC LANDMARK (40HR7) 1999-2004 VOLUME 2 of 2. Edited by David G. Anderson, John E. Cornelison, Jr. and Sarah C. Sherwood" 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/72140286/A_Geoarchaeological_Study_of_the_Mound_A_Stratigraphy_Chapter_10_by_Sarah_C_Sherwood_In_ARCHEOLOGICAL_INVESTIGATIONS_AT_SHILOH_INDIAN_MOUNDS_NATIONAL_HISTORIC_LANDMARK_40HR7_1999_2004_VOLUME_2_of_2_Edited_by_David_G_Anderson_John_E_Cornelison_Jr_and_Sarah_C_Sherwood">A Geoarchaeological Study of the Mound A Stratigraphy, Chapter 10, by Sarah C. Sherwood. In ARCHEOLOGICAL INVESTIGATIONS AT SHILOH INDIAN MOUNDS NATIONAL HISTORIC LANDMARK (40HR7) 1999-2004 VOLUME 2 of 2. Edited by David G. Anderson, John E. Cornelison, Jr. and Sarah C. Sherwood</a></div><div class="wp-workCard_item"><span>ARCHEOLOGICAL INVESTIGATIONS AT SHILOH INDIAN MOUNDS NATIONAL HISTORIC LANDMARK (40HR7) 1999-2004 VOLUMES 1 and 2</span><span>, 2013</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Full report ARCHEOLOGICAL INVESTIGATIONS AT SHILOH INDIAN MOUNDS NATIONAL HISTORIC LANDMARK (40HR...</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">Full report ARCHEOLOGICAL INVESTIGATIONS AT SHILOH INDIAN MOUNDS NATIONAL HISTORIC LANDMARK (40HR7) 1999-2004, 2 VOLUMES published by the US National Park Service, Southeast Archeological Center, Tallahassee, Florida<br />Available online <br /><a href="http://pidba.org/anderson/cv/2013.Anderson.Shiloh.pdf" rel="nofollow">http://pidba.org/anderson/cv/2013.Anderson.Shiloh.pdf</a></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="72140286"><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="72140286"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 72140286; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=72140286]").text(description); $(".js-view-count[data-work-id=72140286]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 72140286; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='72140286']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 72140286, 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" } } $('.js-work-strip[data-work-id=72140286]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":72140286,"title":"A Geoarchaeological Study of the Mound A Stratigraphy, Chapter 10, by Sarah C. 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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="10611598" id="articlesbookchapters"><div class="js-work-strip profile--work_container" data-work-id="111946645"><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/111946645/The_Geoarchaeology_of_the_Tennessee_Valley_Methodological_and_Archaeological_Milestones"><img alt="Research paper thumbnail of The Geoarchaeology of the Tennessee Valley: Methodological and Archaeological Milestones" class="work-thumbnail" src="https://attachments.academia-assets.com/109330960/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/111946645/The_Geoarchaeology_of_the_Tennessee_Valley_Methodological_and_Archaeological_Milestones">The Geoarchaeology of the Tennessee Valley: Methodological and Archaeological Milestones</a></div><div class="wp-workCard_item"><span>TVA Archaeology: Seventy-five Years of Prehistoric Site Research</span><span>, 2009</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="385de9c49bb42236fed146a9962cb56d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":109330960,"asset_id":111946645,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/109330960/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&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="111946645"><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="111946645"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111946645; 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Edited by Valentí Rull, Christopher Stevenson</span><span>, 2022</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The geographical remoteness and physical location of Rapa Nui relative to coastal South America h...</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 geographical remoteness and physical location of Rapa Nui relative to coastal South America have long encouraged research speculation about the island’s possible role, if any, in the transfer into Polynesia and subsequent dispersal of sweet potato (Ipomoea batatas; kumara) (Dixon 1932; Stokes 1932; Heyerdahl and Ferdon Jr. 1961; Yen 1974; Green 1988, 2001, 2005; Clarke 2009; Scaglion and Cordero 2011). New evidence is presented in this chapter for the first well-documented, directly dated, pre-European contact find of carbonized sweet potato tuber, which was derived from recent excavations in Rano Raraku, the monolithic statue (moai) quarry (Horrocks 2014; Sherwood et al. 2019).</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="111946378"><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="111946378"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111946378; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=111946378]").text(description); $(".js-view-count[data-work-id=111946378]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 111946378; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='111946378']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 111946378, 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" } } $('.js-work-strip[data-work-id=111946378]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":111946378,"title":"Pre-European Contact Sweet Potato (Ipomoea batatas) at Rapa Nui: Macrobotanical Evidence from Recent Excavations in Rano Raraku Quarry, Rapa Nui","translated_title":"","metadata":{"abstract":"The geographical remoteness and physical location of Rapa Nui relative to coastal South America have long encouraged research speculation about the island’s possible role, if any, in the transfer into Polynesia and subsequent dispersal of sweet potato (Ipomoea batatas; kumara) (Dixon 1932; Stokes 1932; Heyerdahl and Ferdon Jr. 1961; Yen 1974; Green 1988, 2001, 2005; Clarke 2009; Scaglion and Cordero 2011). 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In Earth Sciences and Archaeology. edited by P. Goldberg, V.T. Holliday, and C.R. Ferring. pp. 327-351. Kluwer Academic/Plenum Publishers, New York." class="work-thumbnail" src="https://attachments.academia-assets.com/32298489/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/5079686/2001_Microartifacts_In_Earth_Sciences_and_Archaeology_edited_by_P_Goldberg_V_T_Holliday_and_C_R_Ferring_pp_327_351_Kluwer_Academic_Plenum_Publishers_New_York">2001 Microartifacts. In Earth Sciences and Archaeology. edited by P. Goldberg, V.T. Holliday, and C.R. Ferring. pp. 327-351. Kluwer Academic/Plenum Publishers, New York.</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="84d2691b30b10f37d8645a38a968766d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":32298489,"asset_id":5079686,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/32298489/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&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="5079686"><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="5079686"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 5079686; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=5079686]").text(description); $(".js-view-count[data-work-id=5079686]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 5079686; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='5079686']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 5079686, 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: "84d2691b30b10f37d8645a38a968766d" } } $('.js-work-strip[data-work-id=5079686]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":5079686,"title":"2001\tMicroartifacts. 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Sherwood</a></span></div><div class="wp-workCard_item"><span>Evolutionary Anthropology: Issues, News, and Reviews</span><span>, 2006</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="63d340a05a882a0905970319ac54417a" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39221466,"asset_id":16856754,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39221466/download_file?st=MTczMjg3NTA0OCw4LjIyMi4yMDguMTQ2&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="16856754"><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="16856754"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 16856754; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=16856754]").text(description); $(".js-view-count[data-work-id=16856754]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 16856754; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='16856754']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 16856754, 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: "63d340a05a882a0905970319ac54417a" } } $('.js-work-strip[data-work-id=16856754]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":16856754,"title":"Deciphering human prehistory through the geoarcheological study of cave sediments","translated_title":"","metadata":{"grobid_abstract":"Much of our knowledge about cave sediments and people comes from as-sociation with archeologists and earth scientists over many years and even decades. 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Juan Pardo&#39;s network of six forts, extending from the Atlantic coast over the Appalachian Mountains, was the least successful of these presidio systems, lasting only from late 1566 to early 1568. The failure of Pardo&#39;s defensive network has long been attributed to poor planning and an insufficient investment of resources. Yet recent archaeological discoveries at the Berry site in western North Carolina—the location of both the Native American town of Joara and Pardo&#39;s first garrison, Fort San Juan—warrants a reappraisal of this interpretation. While previous archaeological research at Berry concentrated on the domestic compound where Pardo&#39;s soldiers resided, the location of the fort itself remained unknown. 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Edited by S.E. Price and P.J. Carr</span><span>, 2018</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This chapter reconsiders monumental architecture as everyday, both for people in the past and arc...</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 chapter reconsiders monumental architecture as everyday, both for people in the past and archaeologists today. Since the authors see sediments as evidence akin to artifacts, they assert that it is capable of being interpreted in many of the same ways. 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Sherwood</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://brynmawr.academia.edu/CaseyBarrier">Casey Barrier</a></span></div><div class="wp-workCard_item"><span>Journal of Archaeological Science</span><span>, 2019</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This study centers on excavations in the inner region of Rano Raraku, the megalithic statue (moai...</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 study centers on excavations in the inner region of Rano Raraku, the megalithic statue (moai) quarry of Rapa Nui (Easter Island). In Rano Raraku a transformed landscape is reconstructed based upon soil chemistry, micromorphology, and macro and micro-botanical data framed within a stratigraphic and radiocarbon informed Bayesian model that is the first for Rapa Nui. We focus on moai RR-0001-156, one of only three moai in the island-wide corpus known to be embellished with a dense suite of cohesive petroglyph motifs. Our results confirm a cultivated landscape present on the inner south and east slopes of Rano Raraku that included sweet potato and probably bottle gourd along with Polynesian transfers banana, taro, and paper mulberry from the 14th century AD continuing into the early 19th century AD. During this time of sociopolitical transformation and land use change across the island labor-intensive rock gardens were developed to increase productivity as soil fertility declined in the context of deforestation and perhaps drought while the pan-island center of 'Oroŋo (Orongo) emerged at Rano Kau with an intensive ritual focus on fertility. Rano Raraku in sharp contrast had (and still has) extremely fertile soils that are the weathering byproduct of lapilli tuff sediments generated from the quarrying process and localized human activity. This study validates Rano Raraku as the major moai production center, establishes chronological parameters for the unique embellished statue and describes agricultural fertility to hypothesize a rich, multi-use landscape for Rano Raraku inner region that is unparalleled elsewhere on Rapa Nui.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="93c1ef9bd6e6a5c9d382f022c76c2464" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":64281621,"asset_id":43955023,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/64281621/download_file?st=MTczMjg3NTA0OSw4LjIyMi4yMDguMTQ2&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="43955023"><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="43955023"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 43955023; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=43955023]").text(description); $(".js-view-count[data-work-id=43955023]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 43955023; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='43955023']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 43955023, 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: "93c1ef9bd6e6a5c9d382f022c76c2464" } } $('.js-work-strip[data-work-id=43955023]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":43955023,"title":"New excavations in Easter Island's statue quarry: Soil fertility, site formation and chronology","translated_title":"","metadata":{"abstract":"This study centers on excavations in the inner region of Rano Raraku, the megalithic statue (moai) quarry of Rapa Nui (Easter Island). In Rano Raraku a transformed landscape is reconstructed based upon soil chemistry, micromorphology, and macro and micro-botanical data framed within a stratigraphic and radiocarbon informed Bayesian model that is the first for Rapa Nui. We focus on moai RR-0001-156, one of only three moai in the island-wide corpus known to be embellished with a dense suite of cohesive petroglyph motifs. Our results confirm a cultivated landscape present on the inner south and east slopes of Rano Raraku that included sweet potato and probably bottle gourd along with Polynesian transfers banana, taro, and paper mulberry from the 14th century AD continuing into the early 19th century AD. During this time of sociopolitical transformation and land use change across the island labor-intensive rock gardens were developed to increase productivity as soil fertility declined in the context of deforestation and perhaps drought while the pan-island center of 'Oroŋo (Orongo) emerged at Rano Kau with an intensive ritual focus on fertility. Rano Raraku in sharp contrast had (and still has) extremely fertile soils that are the weathering byproduct of lapilli tuff sediments generated from the quarrying process and localized human activity. This study validates Rano Raraku as the major moai production center, establishes chronological parameters for the unique embellished statue and describes agricultural fertility to hypothesize a rich, multi-use landscape for Rano Raraku inner region that is unparalleled elsewhere on Rapa Nui.","publication_date":{"day":null,"month":null,"year":2019,"errors":{}},"publication_name":"Journal of Archaeological Science"},"translated_abstract":"This study centers on excavations in the inner region of Rano Raraku, the megalithic statue (moai) quarry of Rapa Nui (Easter Island). In Rano Raraku a transformed landscape is reconstructed based upon soil chemistry, micromorphology, and macro and micro-botanical data framed within a stratigraphic and radiocarbon informed Bayesian model that is the first for Rapa Nui. We focus on moai RR-0001-156, one of only three moai in the island-wide corpus known to be embellished with a dense suite of cohesive petroglyph motifs. Our results confirm a cultivated landscape present on the inner south and east slopes of Rano Raraku that included sweet potato and probably bottle gourd along with Polynesian transfers banana, taro, and paper mulberry from the 14th century AD continuing into the early 19th century AD. During this time of sociopolitical transformation and land use change across the island labor-intensive rock gardens were developed to increase productivity as soil fertility declined in the context of deforestation and perhaps drought while the pan-island center of 'Oroŋo (Orongo) emerged at Rano Kau with an intensive ritual focus on fertility. Rano Raraku in sharp contrast had (and still has) extremely fertile soils that are the weathering byproduct of lapilli tuff sediments generated from the quarrying process and localized human activity. 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Sherwood","title":"New excavations in Easter Island's statue quarry: Soil fertility, site formation and chronology"},{"id":37345363,"work_id":43955023,"tagging_user_id":1263218,"tagged_user_id":30127095,"co_author_invite_id":null,"email":"j***l@g.ucla.edu","affiliation":"University of California, Los Angeles","display_order":-1,"name":"Jo Anne Van Tilburg","title":"New excavations in Easter Island's statue quarry: Soil fertility, site formation and chronology"},{"id":37345367,"work_id":43955023,"tagging_user_id":1263218,"tagged_user_id":101291,"co_author_invite_id":null,"email":"r***n@norwich.edu","affiliation":"Norwich University","display_order":1,"name":"Richard Dunn","title":"New excavations in Easter Island's statue quarry: Soil fertility, site formation and chronology"}],"downloadable_attachments":[{"id":64281621,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/64281621/thumbnails/1.jpg","file_name":"Sherwood et al. 2019.pdf","download_url":"https://www.academia.edu/attachments/64281621/download_file?st=MTczMjg3NTA0OSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"New_excavations_in_Easter_Islands_statue.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/64281621/Sherwood_et_al._2019-libre.pdf?1598458060=\u0026response-content-disposition=attachment%3B+filename%3DNew_excavations_in_Easter_Islands_statue.pdf\u0026Expires=1732878649\u0026Signature=DHT7wUsplzgi3irT6UuApwBopoSfKVLXXTi8IOVR1QrKZWDFNwxMyp2qiI0FqZWPxwfYWmXGRz1kyP75kAZXtmwpFbhiiHqvs~c3H4k7SWmW6DOG~op-GUPLQd8y22GEt0RXIKUnu~l-HhB29ooVbLWI0zRMBYVuZibd8CfsXI2uKiq3MP07E~I7LsWmZkevMEJ7SZKXr8EGW-hfmgEzGEY8qGM2Mah6yZ9U01I1RM92JGgZu0t3GXUBw5~WjTivOm0T7Z3zs~teDroPqb8cwsQs~m56py8RQqXDnhMCxwy2vu-ktuSUOU39APLkYLck0940ix1sPq5HJbh4MFHZFQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"New_excavations_in_Easter_Islands_statue_quarry_Soil_fertility_site_formation_and_chronology","translated_slug":"","page_count":22,"language":"en","content_type":"Work","owner":{"id":1263218,"first_name":"Casey","middle_initials":null,"last_name":"Barrier","page_name":"CaseyBarrier","domain_name":"brynmawr","created_at":"2012-03-02T23:51:12.313-08:00","display_name":"Casey Barrier","url":"https://brynmawr.academia.edu/CaseyBarrier"},"attachments":[{"id":64281621,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/64281621/thumbnails/1.jpg","file_name":"Sherwood et al. 2019.pdf","download_url":"https://www.academia.edu/attachments/64281621/download_file?st=MTczMjg3NTA0OSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"New_excavations_in_Easter_Islands_statue.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/64281621/Sherwood_et_al._2019-libre.pdf?1598458060=\u0026response-content-disposition=attachment%3B+filename%3DNew_excavations_in_Easter_Islands_statue.pdf\u0026Expires=1732878649\u0026Signature=DHT7wUsplzgi3irT6UuApwBopoSfKVLXXTi8IOVR1QrKZWDFNwxMyp2qiI0FqZWPxwfYWmXGRz1kyP75kAZXtmwpFbhiiHqvs~c3H4k7SWmW6DOG~op-GUPLQd8y22GEt0RXIKUnu~l-HhB29ooVbLWI0zRMBYVuZibd8CfsXI2uKiq3MP07E~I7LsWmZkevMEJ7SZKXr8EGW-hfmgEzGEY8qGM2Mah6yZ9U01I1RM92JGgZu0t3GXUBw5~WjTivOm0T7Z3zs~teDroPqb8cwsQs~m56py8RQqXDnhMCxwy2vu-ktuSUOU39APLkYLck0940ix1sPq5HJbh4MFHZFQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":392,"name":"Archaeology","url":"https://www.academia.edu/Documents/in/Archaeology"},{"id":1706,"name":"Geoarchaeology","url":"https://www.academia.edu/Documents/in/Geoarchaeology"},{"id":112668,"name":"Radiocarbon Dating (Archaeology)","url":"https://www.academia.edu/Documents/in/Radiocarbon_Dating_Archaeology_"}],"urls":[]}, dispatcherData: dispatcherData }); $(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="16236639" id="articles"><div class="js-work-strip profile--work_container" data-work-id="5079533"><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/5079533/2004_Chronology_and_Stratigraphy_at_Dust_Cave_Alabama_S_C_Sherwood_B_Driskell_A_Randall_and_S_C_Meeks_American_Antiquity_69_3_533_554"><img alt="Research paper thumbnail of 2004 Chronology and Stratigraphy at Dust Cave, Alabama. (S.C. Sherwood, B. Driskell, A. Randall, and S.C. Meeks), American Antiquity. 69(3):533-554." class="work-thumbnail" src="https://attachments.academia-assets.com/32298351/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/5079533/2004_Chronology_and_Stratigraphy_at_Dust_Cave_Alabama_S_C_Sherwood_B_Driskell_A_Randall_and_S_C_Meeks_American_Antiquity_69_3_533_554">2004 Chronology and Stratigraphy at Dust Cave, Alabama. (S.C. Sherwood, B. Driskell, A. Randall, and S.C. Meeks), American Antiquity. 69(3):533-554.</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://sewanee.academia.edu/SarahSherwood">Sarah C. Sherwood</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/BoyceDriskell">Boyce Driskell</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://ou.academia.edu/AsaRandall">Asa Randall</a></span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2c3abac761cfb21d9987608816f8b8c4" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":32298351,"asset_id":5079533,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/32298351/download_file?st=MTczMjg3NTA1MCw4LjIyMi4yMDguMTQ2&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="5079533"><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="5079533"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 5079533; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=5079533]").text(description); $(".js-view-count[data-work-id=5079533]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 5079533; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='5079533']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 5079533, 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: "2c3abac761cfb21d9987608816f8b8c4" } } $('.js-work-strip[data-work-id=5079533]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":5079533,"title":"2004\tChronology and Stratigraphy at Dust Cave, Alabama. (S.C. Sherwood, B. Driskell, A. Randall, and S.C. Meeks), American Antiquity. 69(3):533-554.","translated_title":"","metadata":{"grobid_abstract":"Dust Cave (1Lu496) is a habitation site in a karstic vestibule in the middle Tennessee River Valley of Northern Alabama. The cave, periodically occupied over 7,000 years, contains well-preserved bone and botanical materials and exhibits microstratigraphy and intact occupation surfaces. The chronostratigraphic framework for Dust Cave is based on 43 14C dates, temporally diagnostic artifacts, and detailed geoarchaeological analysis. In a broad sense, five cultural components are defined and designated: Quad/Beaver Lake/Dalton (10,650-9200 cal B.C.), Early Side-Notched (10,000-9000 cal B.C.), Kirk Stemmed (8200-5800 cal B.C.), Eva/Morrow Mountain (6400 to 4000 cal B.C.), and Benton (4500-3600 cal B.C.). Microstratigraphic and artifact analyses indicate that the primary differences in the deposits over time relate to intensity of activity and spatial organization with regard to changing conditions in the cave, not to the types of activities. Geomorphic transformations influenced the timing of occupation at Dust Cave, especially the initial occupation. The chronostratigraphy provides a framework for assessing the stratigraphic separation of Dalton and Early Side-Notched materials, the shift in technology from blades to bifacial tools, and the context of detailed flora and fauna evidence. These remains provide unique insights into forager adaptations in the Midsouth from the end of the Pleistocene through the first half of the Holocene.","grobid_abstract_attachment_id":32298351},"translated_abstract":null,"internal_url":"https://www.academia.edu/5079533/2004_Chronology_and_Stratigraphy_at_Dust_Cave_Alabama_S_C_Sherwood_B_Driskell_A_Randall_and_S_C_Meeks_American_Antiquity_69_3_533_554","translated_internal_url":"","created_at":"2013-11-12T13:01:25.156-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6042077,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":5527263,"work_id":5079533,"tagging_user_id":6042077,"tagged_user_id":34700962,"co_author_invite_id":1229397,"email":"b***l@utk.edu","display_order":0,"name":"Boyce Driskell","title":"2004\tChronology and Stratigraphy at Dust Cave, Alabama. (S.C. Sherwood, B. Driskell, A. Randall, and S.C. 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Sherwood</a></span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b7122147057157ec59b5dc962d5e65ef" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":35899014,"asset_id":9710353,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/35899014/download_file?st=MTczMjg3NTA1MCw4LjIyMi4yMDguMTQ2&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="9710353"><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="9710353"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 9710353; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=9710353]").text(description); $(".js-view-count[data-work-id=9710353]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 9710353; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='9710353']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 9710353, 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: "b7122147057157ec59b5dc962d5e65ef" } } $('.js-work-strip[data-work-id=9710353]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":9710353,"title":"The DaVinci's of Dirt","translated_title":"","metadata":{"grobid_abstract":"The complexity of mound construction, as revealed through geoarchaeological analyses, indicates the cultural significance of mounds may be as well reflected in the earthen construction materials and their arrangement, as it is in the artifacts abandoned on their summits. We use geoarchaeological examples from three sites in the Mississippi River basin, Shiloh Mounds, Cahokia, and Poverty Point, to advocate a geoarchaeological approach that considers multiple scales from the regional soils and geomorphology, field observation of lithostratigraphic units, to the micro-scale identification of the mineralogy and soil development in order to decipher the source and processing of the soils and sediments. We focus on the use of five types of construction referred to here as: sod blocks, soil blocks, loaded fills, zoned fills and veneers. Also we address the selection and transportation of soils and sediments used in mound building and what these types of deposits reveal about the methods used to build mounds. These data can be used to evaluate and understand organization of labor, pace of construction, and mound appearance. We hold there is a considerable (although unquantified) difference between earth moving and mound building and that the construction of these important monuments required considerable knowledge, skill, planning, hard work, and attention to symbolic and ritual meaning.","grobid_abstract_attachment_id":35899014},"translated_abstract":null,"internal_url":"https://www.academia.edu/9710353/The_DaVincis_of_Dirt","translated_internal_url":"","created_at":"2014-12-10T08:12:05.825-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":8502910,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":56567,"work_id":9710353,"tagging_user_id":8502910,"tagged_user_id":6042077,"co_author_invite_id":null,"email":"s***d@sewanee.edu","display_order":null,"name":"Sarah C. 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Sherwood</a></span></div><div class="wp-workCard_item"><span>Geoarchaeology</span><span>, 1995</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b04d8d34c33580b465b167f2195cad97" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":109329519,"asset_id":16856755,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/109329519/download_file?st=MTczMjg3NTA1MCw4LjIyMi4yMDguMTQ2&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="16856755"><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="16856755"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 16856755; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=16856755]").text(description); $(".js-view-count[data-work-id=16856755]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 16856755; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='16856755']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 16856755, 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: "b04d8d34c33580b465b167f2195cad97" } } $('.js-work-strip[data-work-id=16856755]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":16856755,"title":"Artifact size and spatial process: Macro- and microartifacts in a Mississippian house","translated_title":"","metadata":{"grobid_abstract":"Despite their evident utility in archaeological analysis, microartifacts (those artifacts smaller than 2 mm) have, as a class, been used only sparingly by archaeologists and then only as if they were larger artifacts. 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Sherwood</a></span></div><div class="wp-workCard_item"><span>Geoarchaeology</span><span>, 1995</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b3baeae90a4673d52ef7f276f4fe8903" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":39221467,"asset_id":16856757,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/39221467/download_file?st=MTczMjg3NTA1MCw4LjIyMi4yMDguMTQ2&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="16856757"><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="16856757"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 16856757; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=16856757]").text(description); $(".js-view-count[data-work-id=16856757]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 16856757; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='16856757']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 16856757, 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: "b3baeae90a4673d52ef7f276f4fe8903" } } $('.js-work-strip[data-work-id=16856757]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":16856757,"title":"Quantifying microartifacts using a personal computer","translated_title":"","metadata":{"grobid_abstract":"Microartifact analysis is a worthwhile endeavor in archaeological research. A recurring problem, however, has been the time invested in sample quantification. In this paper we offer an interactive way to quantify microartifact samples using a computer program called MMCOUNT. 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Sherwood</a></span></div><div class="wp-workCard_item"><span>Antiquity</span><span>, 2013</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c5ccd83260fa364d2b1225809349ac1a" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":109330252,"asset_id":4282663,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/109330252/download_file?st=MTczMjg3NTA1MCw4LjIyMi4yMDguMTQ2&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="4282663"><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="4282663"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 4282663; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=4282663]").text(description); $(".js-view-count[data-work-id=4282663]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 4282663; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='4282663']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 4282663, 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: "c5ccd83260fa364d2b1225809349ac1a" } } $('.js-work-strip[data-work-id=4282663]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4282663,"title":"Sacred landscapes of the south-eastern USA: prehistoric rock and cave art in Tennessee","translated_title":"","metadata":{"volume":"87","more_info":"Jan F. 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Sherwood</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://utfsm.academia.edu/Jos%C3%A9MiguelRam%C3%ADrezAliaga">José Miguel Ramírez-Aliaga</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://norwich.academia.edu/RichardDunn">Richard Dunn</a></span></div><div class="wp-workCard_item"><span>Journal of Archaeological Science</span><span>, 2019</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This study centers on excavations in the inner region of Rano Raraku, the megalithic statue (moai...</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 study centers on excavations in the inner region of Rano Raraku, the megalithic statue (moai) quarry of Rapa Nui (Easter Island). In Rano Raraku a transformed landscape is reconstructed based upon soil chemistry, micromorphology, and macro and micro-botanical data framed within a stratigraphic and radiocarbon informed Bayesian model that is the first for Rapa Nui. We focus on moai RR-0001-156, one of only three moai in the island-wide corpus known to be embellished with a dense suite of cohesive petroglyph motifs. Our results confirm a cultivated landscape present on the inner south and east slopes of Rano Raraku that included sweet potato and probably bottle gourd along with Polynesian transfers banana, taro, and paper mulberry from the 14th century AD continuing into the early 19th century AD. During this time of sociopolitical transformation and land use change across the island labor-intensive rock gardens were developed to increase productivity as soil fertility declined in the context of deforestation and perhaps drought while the pan-island center of 'Oroŋo (Orongo) emerged at Rano Kau with an intensive ritual focus on fertility. Rano Raraku in sharp contrast had (and still has) extremely fertile soils that are the weathering byproduct of lapilli tuff sediments generated from the quarrying process and localized human activity. This study validates Rano Raraku as the major moai production center, establishes chronological parameters for the unique embellished statue and describes agricultural fertility to hypothesize a rich, multi-use landscape for Rano Raraku inner region that is unparalleled elsewhere on Rapa Nui.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="24af22ceb963d050721122ae1a0500af" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":61445115,"asset_id":41207090,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/61445115/download_file?st=MTczMjg3NTA1MCw4LjIyMi4yMDguMTQ2&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="41207090"><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="41207090"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 41207090; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=41207090]").text(description); $(".js-view-count[data-work-id=41207090]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 41207090; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='41207090']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 41207090, 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: "24af22ceb963d050721122ae1a0500af" } } $('.js-work-strip[data-work-id=41207090]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":41207090,"title":"New excavations in Easter Island's statue quarry: Soil fertility, site formation and chronology","translated_title":"","metadata":{"doi":"10.1016/j.jas.2019.104994","abstract":"This study centers on excavations in the inner region of Rano Raraku, the megalithic statue (moai) quarry of Rapa Nui (Easter Island). 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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="51429975"><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/51429975/Look_to_the_earth_the_search_for_ritual_in_the_context_of_mound_construction"><img alt="Research paper thumbnail of Look to the earth: the search for ritual in the context of mound construction" class="work-thumbnail" src="https://attachments.academia-assets.com/109329310/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/51429975/Look_to_the_earth_the_search_for_ritual_in_the_context_of_mound_construction">Look to the earth: the search for ritual in the context of mound construction</a></div><div class="wp-workCard_item"><span>Archaeological and Anthropological Sciences</span><span>, 2016</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="348d8e2edb1f325b963dad43a7129efe" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":109329310,"asset_id":51429975,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/109329310/download_file?st=MTczMjg3NTA1MSw4LjIyMi4yMDguMTQ2&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="51429975"><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="51429975"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 51429975; 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This paper acknowledges mound building as the purposeful selection of soils and sediments for specific color, texture, or engineering properties and the organization of deposits suggesting that the building process reflects both shared knowledge and communicates specific information. We present two examples: Late Archaic period Poverty Point site Mound A, and Mississippian period Shiloh site Mound A, in the exploration of structured deposits to identify ritual in contrast to a more mundane or purely practical origin. We argue the building of these earthen monuments was not only architecturally important as a means to serve a subsequent purpose but that the act of construction itself was a ritual process intended to serve its own religious and social purposes. 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Sherwood</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://osu.academia.edu/KristenGremillion">Kristen Gremillion</a></span></div><div class="wp-workCard_item"><span>Journal of Archaeological Science</span><span>, 2008</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The archaeological record of dry rockshelters in the Red River Valley of eastern Kentucky contain...</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 archaeological record of dry rockshelters in the Red River Valley of eastern Kentucky contains botanical remains of several weedy annual seed-bearing plants that point to the independent development of agriculture during the Late Archaic and Early Woodland Period. The objective of this study is to gather quantitative data through the chemical and physical analysis of soils collected within a valley transect to gain insights into landscape processes and soil fertility that may have played a role in the early development of plant domestication and the location of garden plots <br />in relation to rock shelter sites in the upper Cumberland Plateau region of eastern Kentucky. Soils on upland benches formed in limestones have soil fertility values that are comparable to fertile floodplain soils. Upslope outcrops of calcareous bedrock are contributing basic cations to these bench soils. Additionally, in comparison to other landscape positions these upland soils have high levels of organic carbon, available P and greater C:N ratios. Soil morphology, radiocarbon dates, and archaeological evidence indicate that many of the numerous earthflows and debris flows within the region are Early to Middle Holocene in age. These slides were likely generated by Mid-Holocene climatic shifts in which the frequency and intensity of summer precipitation increased across the southeastern United States. These slope failures may have  contributed to the development of plant domestication by creating forest canopy gaps and disturbed soils in which weedy plants thrived. <br /> 2007 Elsevier Ltd. All rights reserved.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="7ca170578f67e118e02b574a113d91b9" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":81258284,"asset_id":72139439,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/81258284/download_file?st=MTczMjg3NTA1MSw4LjIyMi4yMDguMTQ2&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="72139439"><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="72139439"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 72139439; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=72139439]").text(description); $(".js-view-count[data-work-id=72139439]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 72139439; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='72139439']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 72139439, 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: "7ca170578f67e118e02b574a113d91b9" } } $('.js-work-strip[data-work-id=72139439]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":72139439,"title":"Soil fertility and slope processes in the Western Cumberland Escarpment of Kentucky: influences on the development of horticulture in the Eastern Woodlands","translated_title":"","metadata":{"doi":"10.1016/j.jas.2007.11.023","volume":"35","abstract":"The archaeological record of dry rockshelters in the Red River Valley of eastern Kentucky contains botanical remains of several weedy annual seed-bearing plants that point to the independent development of agriculture during the Late Archaic and Early Woodland Period. The objective of this study is to gather quantitative data through the chemical and physical analysis of soils collected within a valley transect to gain insights into landscape processes and soil fertility that may have played a role in the early development of plant domestication and the location of garden plots\r\nin relation to rock shelter sites in the upper Cumberland Plateau region of eastern Kentucky. Soils on upland benches formed in limestones have soil fertility values that are comparable to fertile floodplain soils. Upslope outcrops of calcareous bedrock are contributing basic cations to these bench soils. Additionally, in comparison to other landscape positions these upland soils have high levels of organic carbon, available P and greater C:N ratios. Soil morphology, radiocarbon dates, and archaeological evidence indicate that many of the numerous earthflows and debris flows within the region are Early to Middle Holocene in age. These slides were likely generated by Mid-Holocene climatic shifts in which the frequency and intensity of summer precipitation increased across the southeastern United States. These slope failures may have contributed to the development of plant domestication by creating forest canopy gaps and disturbed soils in which weedy plants thrived.\r\n\u0002 2007 Elsevier Ltd. All rights reserved.","publisher":"Elsevier","page_numbers":"1717-1731","publication_date":{"day":null,"month":null,"year":2008,"errors":{}},"publication_name":"Journal of Archaeological Science"},"translated_abstract":"The archaeological record of dry rockshelters in the Red River Valley of eastern Kentucky contains botanical remains of several weedy annual seed-bearing plants that point to the independent development of agriculture during the Late Archaic and Early Woodland Period. The objective of this study is to gather quantitative data through the chemical and physical analysis of soils collected within a valley transect to gain insights into landscape processes and soil fertility that may have played a role in the early development of plant domestication and the location of garden plots\r\nin relation to rock shelter sites in the upper Cumberland Plateau region of eastern Kentucky. Soils on upland benches formed in limestones have soil fertility values that are comparable to fertile floodplain soils. Upslope outcrops of calcareous bedrock are contributing basic cations to these bench soils. Additionally, in comparison to other landscape positions these upland soils have high levels of organic carbon, available P and greater C:N ratios. Soil morphology, radiocarbon dates, and archaeological evidence indicate that many of the numerous earthflows and debris flows within the region are Early to Middle Holocene in age. These slides were likely generated by Mid-Holocene climatic shifts in which the frequency and intensity of summer precipitation increased across the southeastern United States. These slope failures may have contributed to the development of plant domestication by creating forest canopy gaps and disturbed soils in which weedy plants thrived.\r\n\u0002 2007 Elsevier Ltd. All rights reserved.","internal_url":"https://www.academia.edu/72139439/Soil_fertility_and_slope_processes_in_the_Western_Cumberland_Escarpment_of_Kentucky_influences_on_the_development_of_horticulture_in_the_Eastern_Woodlands","translated_internal_url":"","created_at":"2022-02-21T14:14:04.284-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6042077,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":37738759,"work_id":72139439,"tagging_user_id":6042077,"tagged_user_id":124014806,"co_author_invite_id":null,"email":"j***d@email.arizona.edu","affiliation":"The University of Arizona","display_order":-1,"name":"Jason Dean Windingstad","title":"Soil fertility and slope processes in the Western Cumberland Escarpment of Kentucky: influences on the development of horticulture in the Eastern Woodlands"},{"id":37738760,"work_id":72139439,"tagging_user_id":6042077,"tagged_user_id":36939,"co_author_invite_id":null,"email":"g***1@osu.edu","affiliation":"Ohio State University","display_order":1,"name":"Kristen Gremillion","title":"Soil fertility and slope processes in the Western Cumberland Escarpment of Kentucky: influences on the development of horticulture in the Eastern Woodlands"}],"downloadable_attachments":[{"id":81258284,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/81258284/thumbnails/1.jpg","file_name":"Windingstad_et_al_2008.pdf","download_url":"https://www.academia.edu/attachments/81258284/download_file?st=MTczMjg3NTA1MSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Soil_fertility_and_slope_processes_in_th.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/81258284/Windingstad_et_al_2008-libre.pdf?1645573625=\u0026response-content-disposition=attachment%3B+filename%3DSoil_fertility_and_slope_processes_in_th.pdf\u0026Expires=1732697424\u0026Signature=Ro-n4uzDh7VlO-fQ4j4J3tsnw2mt6xjeWrMjS7xyRTf-fus70I5cL1~GMb0ztSupBAUOXDC1iMbnHFm2FAN1qxWJaJF0mmL2FQHKXLH-KzOuHsdhnN~6srixMZII9jtsmdjbrMirZZGxuWvh-fQLLwVS00rGjuOLht5EfQa2IQn2~6r~yZ2IV-Q5Q1SLUXoCBIq48LIy6o0rCIaRqTunIcbVNiyuE9LuQxS7WU09m~dw52zC6vvU0kGR24xxEuFArrnSCSuhCHMKR1rI38XKo8IvC6EZ2DQaqVBKz40eG1k~Tgdzx1e75nPXgkxTuAtXma8SWxoZhrwHZRORwNIwaw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Soil_fertility_and_slope_processes_in_the_Western_Cumberland_Escarpment_of_Kentucky_influences_on_the_development_of_horticulture_in_the_Eastern_Woodlands","translated_slug":"","page_count":15,"language":"en","content_type":"Work","owner":{"id":6042077,"first_name":"Sarah C.","middle_initials":null,"last_name":"Sherwood","page_name":"SarahSherwood","domain_name":"sewanee","created_at":"2013-10-09T08:07:57.348-07:00","display_name":"Sarah C. 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The Late Woodland mound (A.D. 590–780) is composed of local soils, and its presence today is a testament to the ancient builders’ knowledge of earthen construction materials and methods. Central to the study of the mound is an integrated geoarchaeological approach that uses stratigraphy and micromorphology to decipher material source and selection, construction techniques, and periodicity, in combination with more traditional artifacts, revealing the activities that created this ultimately monumental space. The mound was built in three rapid stages beginning with a low earthwork demarcating a ritual precinct used during late spring/early summer. Stage II quickly followed with a series of alternating zoned fills, sealing the space that was then subsequently covered by Stage III, a massive hard red surface that marked the location wi...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="74cd4f3ac918bbd24ffdfc7227302aa5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":83106091,"asset_id":75269327,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/83106091/download_file?st=MTczMjg3NTA1MSw4LjIyMi4yMDguMTQ2&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="75269327"><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="75269327"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 75269327; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=75269327]").text(description); $(".js-view-count[data-work-id=75269327]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 75269327; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='75269327']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 75269327, 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: "74cd4f3ac918bbd24ffdfc7227302aa5" } } $('.js-work-strip[data-work-id=75269327]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":75269327,"title":"An Integrated Geoarchaeology of a Late Woodland Sand Mound","translated_title":"","metadata":{"abstract":"The Graveline Mound (22JA503) is a sand platform mound in Jackson County, Mississippi, built on a low, late Pleistocene terrace on the Mississippi Sound. 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However, rarely are the two integrated in a way that offers a robust understanding of the complex historical palimpsests embedded within a social landscape. In this paper we present an integrated aerial and terrestrial remote sensing program at the Johnston Site, part of the larger Pinson Mounds landscape in the American MidSouth. Our work at Johnston was focused on better understanding the history of human landscape use and change so that we can begin to compare the Johnston Site with other large Middle Woodland (200 BC–AD 500) ceremonial centers in the region. Our research allowed us to examine the accuracy of an early map of the Johnston Site made in the early 20th century. However, our integrated remote sensing approach allows us to go well beyond testing the usefulness of the map; it helps identify different uses of the site through time and across space. 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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="92113065"><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/92113065/The_Context_of_Early_Southeastern_Prehistoric_Cave_Art_A_Report_on_the_Archaeology_of_3rd_Unnamed_Cave"><img alt="Research paper thumbnail of The Context of Early Southeastern Prehistoric Cave Art: A Report on the Archaeology of 3rd Unnamed Cave" 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/92113065/The_Context_of_Early_Southeastern_Prehistoric_Cave_Art_A_Report_on_the_Archaeology_of_3rd_Unnamed_Cave">The Context of Early Southeastern Prehistoric Cave Art: A Report on the Archaeology of 3rd Unnamed Cave</a></div><div class="wp-workCard_item"><span>American Antiquity</span><span>, 1998</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In the deep recesses of “3rd Unnamed Cave,” a karst cavern in Tennessee, evidence for an ancient ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">In the deep recesses of “3rd Unnamed Cave,” a karst cavern in Tennessee, evidence for an ancient association between dark zone cave art and chert mining has recently been documented. The art comprises petroglyphs on the ceiling of a chamber more than 1 km from the cave entrance. On the floor below the art, natural sediments were excavated prehistorically to obtain high-quality chert nodules. Radiocarbon age determinations place the mining during the Terminal Archaic period. Studies in lithic technology, geoarchaeology, and petroglyph description are presented.</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="92113065"><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="92113065"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 92113065; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=92113065]").text(description); $(".js-view-count[data-work-id=92113065]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 92113065; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='92113065']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 92113065, 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" } } $('.js-work-strip[data-work-id=92113065]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":92113065,"title":"The Context of Early Southeastern Prehistoric Cave Art: A Report on the Archaeology of 3rd Unnamed Cave","translated_title":"","metadata":{"abstract":"In the deep recesses of “3rd Unnamed Cave,” a karst cavern in Tennessee, evidence for an ancient association between dark zone cave art and chert mining has recently been documented. 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Radiocarbon age determinations place the mining during the Terminal Archaic period. Studies in lithic technology, geoarchaeology, and petroglyph description are presented.","internal_url":"https://www.academia.edu/92113065/The_Context_of_Early_Southeastern_Prehistoric_Cave_Art_A_Report_on_the_Archaeology_of_3rd_Unnamed_Cave","translated_internal_url":"","created_at":"2022-12-03T07:52:58.624-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6042077,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"The_Context_of_Early_Southeastern_Prehistoric_Cave_Art_A_Report_on_the_Archaeology_of_3rd_Unnamed_Cave","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":6042077,"first_name":"Sarah C.","middle_initials":null,"last_name":"Sherwood","page_name":"SarahSherwood","domain_name":"sewanee","created_at":"2013-10-09T08:07:57.348-07:00","display_name":"Sarah C. Sherwood","url":"https://sewanee.academia.edu/SarahSherwood"},"attachments":[],"research_interests":[{"id":128,"name":"History","url":"https://www.academia.edu/Documents/in/History"},{"id":392,"name":"Archaeology","url":"https://www.academia.edu/Documents/in/Archaeology"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":34817,"name":"Prehistory","url":"https://www.academia.edu/Documents/in/Prehistory"},{"id":48310,"name":"Cave","url":"https://www.academia.edu/Documents/in/Cave"},{"id":93937,"name":"Radiocarbon Dating","url":"https://www.academia.edu/Documents/in/Radiocarbon_Dating"},{"id":102456,"name":"American antiquity","url":"https://www.academia.edu/Documents/in/American_antiquity"},{"id":110290,"name":"Karst","url":"https://www.academia.edu/Documents/in/Karst"}],"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="92113068"><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/92113068/Evidence_for_Holocene_Aeolian_Activity_at_the_Close_of_the_Middle_Bronze_Age_in_the_Eastern_Carpathian_Basin_Geoarchaeological_Results_from_the_Mure%C5%9F_River_Valley_Romania"><img alt="Research paper thumbnail of Evidence for Holocene Aeolian Activity at the Close of the Middle Bronze Age in the Eastern Carpathian Basin: Geoarchaeological Results from the Mureş River Valley, Romania" class="work-thumbnail" src="https://attachments.academia-assets.com/95210143/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/92113068/Evidence_for_Holocene_Aeolian_Activity_at_the_Close_of_the_Middle_Bronze_Age_in_the_Eastern_Carpathian_Basin_Geoarchaeological_Results_from_the_Mure%C5%9F_River_Valley_Romania">Evidence for Holocene Aeolian Activity at the Close of the Middle Bronze Age in the Eastern Carpathian Basin: Geoarchaeological Results from the Mureş River Valley, Romania</a></div><div class="wp-workCard_item"><span>Geoarchaeology</span><span>, 2013</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="931e998241999157790870f6d309e06c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":95210143,"asset_id":92113068,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/95210143/download_file?st=MTczMjg3NTA1MSw4LjIyMi4yMDguMTQ2&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="92113068"><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="92113068"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 92113068; 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We explore possible loess deposits in the Mureş River Valley of western Romania, providing a regional signal of increased aridity during the mid-late Holocene. This proposed aridity may be responsible for the abandonment of Middle Bronze Age tell settlements along the major drainages of the eastern Carpathian Basin (Pannonian plain). This hypothesis centers on a proposed aeolian deposit (the \"Pecica deposit\"), a ca. 50-80 cm thick, relatively homogeneous, gray layer blanketing the top of the Bronze Age tell of Pecica-Şanţul Mare. Comparing the morphological, geochemical, and physical characteristics of this specific tell deposit with two representative profiles near the site containing glaciogenic calcareous loess and potential Holocene loess deposits developed in Chernozems, we find significant similarities to support this hypothesis. We then review various forms of proxy data published from elsewhere in Central and Eastern Europe suggesting a warming trend during this period. The temporal placement of the Pecica deposit is bracketed using diagnostic artifacts, radiocarbon dates, and the degree of soil development, suggesting a period of increased aridity likely occurring soon after the 17th century B.C.","publication_date":{"day":null,"month":null,"year":2013,"errors":{}},"publication_name":"Geoarchaeology","grobid_abstract_attachment_id":95210143},"translated_abstract":null,"internal_url":"https://www.academia.edu/92113068/Evidence_for_Holocene_Aeolian_Activity_at_the_Close_of_the_Middle_Bronze_Age_in_the_Eastern_Carpathian_Basin_Geoarchaeological_Results_from_the_Mure%C5%9F_River_Valley_Romania","translated_internal_url":"","created_at":"2022-12-03T07:52:58.922-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":6042077,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":40761378,"work_id":92113068,"tagging_user_id":6042077,"tagged_user_id":124014806,"co_author_invite_id":null,"email":"j***d@email.arizona.edu","affiliation":"The University of Arizona","display_order":1,"name":"Jason Dean Windingstad","title":"Evidence for Holocene Aeolian Activity at the Close of the Middle Bronze Age in the Eastern Carpathian Basin: Geoarchaeological Results from the Mureş River Valley, Romania"}],"downloadable_attachments":[{"id":95210143,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/95210143/thumbnails/1.jpg","file_name":"gea21434.pdf","download_url":"https://www.academia.edu/attachments/95210143/download_file?st=MTczMjg3NTA1MSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Evidence_for_Holocene_Aeolian_Activity_a.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/95210143/gea21434-libre.pdf?1670083710=\u0026response-content-disposition=attachment%3B+filename%3DEvidence_for_Holocene_Aeolian_Activity_a.pdf\u0026Expires=1732878651\u0026Signature=HPmDmrMBostS5dg3Umk9sWZpnLky8Ysd1V2wTOkZWXtv4sSiq1p04amcToX6XQX6k0~STesRoyI6vghwMPAp-Esu6LrnmBIDpjxC1H2vuSRHawxsJwvfhQVjBrXzoYSTW1Rni6Q3YztKzYSrdl5UnXU4T8iokhxYU4BHx6V9O5Gfh8ATH4setRhjy6-oB5cW-R~eQvGcbjr4ZkJnG5WbOoDzBRyYXQqkzdyHuQOXiFfJr81ynKeAHSRP4PLfeJzCZ5Jc~apPdVXVxT2EBemjit~W~JiFdAOQVQe9WpsU1jX0Zmxd9YoT1QCvJ0WzklZX-b59eXOQk7YhDYdhJ2WEFA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Evidence_for_Holocene_Aeolian_Activity_at_the_Close_of_the_Middle_Bronze_Age_in_the_Eastern_Carpathian_Basin_Geoarchaeological_Results_from_the_Mureş_River_Valley_Romania","translated_slug":"","page_count":16,"language":"en","content_type":"Work","owner":{"id":6042077,"first_name":"Sarah C.","middle_initials":null,"last_name":"Sherwood","page_name":"SarahSherwood","domain_name":"sewanee","created_at":"2013-10-09T08:07:57.348-07:00","display_name":"Sarah C. 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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="92113069"><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/92113069/Soapstone_Vessel_Chronology_and_Function_in_the_Southern_Appalachians_of_Eastern_Tennessee_The_Apple_Barn_Site_40BT90_Assemblage"><img alt="Research paper thumbnail of Soapstone Vessel Chronology and Function in the Southern Appalachians of Eastern Tennessee: The Apple Barn Site (40BT90) Assemblage" class="work-thumbnail" src="https://attachments.academia-assets.com/95210144/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/92113069/Soapstone_Vessel_Chronology_and_Function_in_the_Southern_Appalachians_of_Eastern_Tennessee_The_Apple_Barn_Site_40BT90_Assemblage">Soapstone Vessel Chronology and Function in the Southern Appalachians of Eastern Tennessee: The Apple Barn Site (40BT90) Assemblage</a></div><div class="wp-workCard_item"><span>Southeastern Archaeology</span><span>, 2014</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="78c45b4d7efb27adeaa8f7fdeff371e5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":95210144,"asset_id":92113069,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/95210144/download_file?st=MTczMjg3NTA1MSw4LjIyMi4yMDguMTQ2&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="92113069"><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="92113069"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 92113069; 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