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href="https://www.academia.edu/124955045/El_estudio_antracol%C3%B3gico_de_la_aldea_medieval_de_Aistra">El estudio antracológico de la aldea medieval de Aistra</a></div><div class="wp-workCard_item"><span>Archaeopress Publishing Ltd eBooks</span><span>, Jun 1, 2023</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="124955045"><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="124955045"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { 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So far, the inner bark (phloem) of the lime tree (genus Tilia) could be detected most frequently. Microscopic examination of anatomical features can determine the taxon, requiring manipulation of samples and archaeological objects. In this study, micro-computed tomography (µCT) was reviewed as a method for determining the woody taxon and obtaining additional information from the inner bark. To this end, modern bark samples from different tree organs of lime were first analysed using both µCT and transmitted light microscopy. Both methods were able to detect all characteristic anatomical features in the phloem and identify the genus. With analysis based on µCT data, further anatomical information can be obtained. For example, the shape of the phloem rays in the bast strips can provide information on the position within the bark and on the original ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1dc3f4e5a44c1e72ad827cb5994402bd" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":119084693,"asset_id":124955041,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/119084693/download_file?st=MTczMjgxNDYyNyw4LjIyMi4yMDguMTQ2&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="124955041"><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="124955041"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124955041; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124955041]").text(description); $(".js-view-count[data-work-id=124955041]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124955041; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124955041']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124955041, 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: "1dc3f4e5a44c1e72ad827cb5994402bd" } } $('.js-work-strip[data-work-id=124955041]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124955041,"title":"Micro-computed tomography for the identification and characterization of archaeological lime bark","translated_title":"","metadata":{"abstract":"In the Neolithic pile-dwelling settlements of southwestern Germany, bark played a prominent role in the production of technical textiles. 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Archaeological excavation revealed a trench, a palisade and an occupation layer. The function of the wall and trench system remains unknown but there are several possibilities: It could have been used for protection, as a type of symbolic separation or to demarcate a cult site. The enclosure was constructed around the year zero. Charcoal samples were taken in a spatially detailed manner during excavation, as well as a new pollen core from a small spring mire directly next to the site. Anthracological analysis showed that Quercus (oak) was the main type of wood used in the construction of this enclosure. Thirteen additional wood taxa were identified, of which the next best represented is Corylus (hazel) and surprisingly a significant amount of Ilex (holly) was found. The samples did not contain Fagus (beech) or Carpinus (hornbeam), which are both common in the area today. According to pollen data, Fagus had begun to establish in the local woodland during the time of the enclosure, but did not gain importance before the migration period. By diameter analysis of the charcoals the size of the used wood (branch or trunk) was reconstructed. In addition, mean annual tree ring widths of the used wood e especially Quercus e show that the wood comes from young stems and/or branches of older trees and probably not from coppiced wood. The study shows that even small-scale archaeological excavations can yield important new data on wood utilization with a high spatial precision, which contributes to the reconstruction of local woodland composition.","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"Quaternary International","grobid_abstract_attachment_id":119084715},"translated_abstract":null,"internal_url":"https://www.academia.edu/124955033/Iron_Age_wood_usage_at_an_enclosure_in_northern_Germany","translated_internal_url":"","created_at":"2024-10-22T12:12:27.074-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":43308588,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":119084715,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/119084715/thumbnails/1.jpg","file_name":"j.quaint.2017.02.01420241022-1-e1fe8b.pdf","download_url":"https://www.academia.edu/attachments/119084715/download_file?st=MTczMjgxNDYyOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Iron_Age_wood_usage_at_an_enclosure_in_n.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/119084715/j.quaint.2017.02.01420241022-1-e1fe8b-libre.pdf?1729626797=\u0026response-content-disposition=attachment%3B+filename%3DIron_Age_wood_usage_at_an_enclosure_in_n.pdf\u0026Expires=1732818228\u0026Signature=cTD~clM8UsoB-oOjLL31LXNpASC3UglNej8UQqu3VDvNhDaorfeT~Bdnw7Oi-tiDK-Yvj6eM8sjJavuQ6Nv4-47KCFXDx51ihtrkZ6dYA4lwGWnUCNM-WYACzmwHUKhXm2XH8zXMcOY7jQ-1sJFWTKQQmd7fJIXxQ37qCuZmSlKpvohpbD7wIGlGh009zC~A0XAk2hKpaXzLFw-urzUfIuhY2lF~cnxmFZN8dS9~EXMq0~uZ3bioUatsjcfW0XtAP8Hy5OkxMiZ~HK6PWBehgwlBPSXcKVXRdwZ5of1RGEAtr1ElNRsM1EIryBRvo1~q-WI9H6Er~rCfvvCeq~891g__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Iron_Age_wood_usage_at_an_enclosure_in_northern_Germany","translated_slug":"","page_count":9,"language":"en","content_type":"Work","owner":{"id":43308588,"first_name":"Oliver","middle_initials":null,"last_name":"Nelle","page_name":"OliverNelle","domain_name":"independent","created_at":"2016-02-16T00:09:13.229-08:00","display_name":"Oliver Nelle","url":"https://independent.academia.edu/OliverNelle"},"attachments":[{"id":119084715,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/119084715/thumbnails/1.jpg","file_name":"j.quaint.2017.02.01420241022-1-e1fe8b.pdf","download_url":"https://www.academia.edu/attachments/119084715/download_file?st=MTczMjgxNDYyOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Iron_Age_wood_usage_at_an_enclosure_in_n.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/119084715/j.quaint.2017.02.01420241022-1-e1fe8b-libre.pdf?1729626797=\u0026response-content-disposition=attachment%3B+filename%3DIron_Age_wood_usage_at_an_enclosure_in_n.pdf\u0026Expires=1732818228\u0026Signature=cTD~clM8UsoB-oOjLL31LXNpASC3UglNej8UQqu3VDvNhDaorfeT~Bdnw7Oi-tiDK-Yvj6eM8sjJavuQ6Nv4-47KCFXDx51ihtrkZ6dYA4lwGWnUCNM-WYACzmwHUKhXm2XH8zXMcOY7jQ-1sJFWTKQQmd7fJIXxQ37qCuZmSlKpvohpbD7wIGlGh009zC~A0XAk2hKpaXzLFw-urzUfIuhY2lF~cnxmFZN8dS9~EXMq0~uZ3bioUatsjcfW0XtAP8Hy5OkxMiZ~HK6PWBehgwlBPSXcKVXRdwZ5of1RGEAtr1ElNRsM1EIryBRvo1~q-WI9H6Er~rCfvvCeq~891g__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"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":35587,"name":"Quaternary","url":"https://www.academia.edu/Documents/in/Quaternary"},{"id":261641,"name":"Fraxinus","url":"https://www.academia.edu/Documents/in/Fraxinus"},{"id":295952,"name":"Enclosure","url":"https://www.academia.edu/Documents/in/Enclosure"},{"id":655141,"name":"Beech","url":"https://www.academia.edu/Documents/in/Beech"},{"id":703023,"name":"Coppicing","url":"https://www.academia.edu/Documents/in/Coppicing"}],"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="124955032"><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/124955032/Holocene_landscape_dynamics_at_the_tell_Arslantepe_Malatya_Turkey_Soil_erosion_buried_soils_and_settlement_layers_slope_and_river_activity_in_a_middle_Euphrates_catchment"><img alt="Research paper thumbnail of Holocene landscape dynamics at the tell Arslantepe, Malatya, Turkey – Soil erosion, buried soils and settlement layers, slope and river activity in a middle Euphrates catchment" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/124955032/Holocene_landscape_dynamics_at_the_tell_Arslantepe_Malatya_Turkey_Soil_erosion_buried_soils_and_settlement_layers_slope_and_river_activity_in_a_middle_Euphrates_catchment">Holocene landscape dynamics at the tell Arslantepe, Malatya, Turkey – Soil erosion, buried soils and settlement layers, slope and river activity in a middle Euphrates catchment</a></div><div class="wp-workCard_item"><span>The Holocene</span><span>, 2014</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Alluvial and colluvial sequences were studied around the prehistoric tell Arslantepe in 11 exposu...</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">Alluvial and colluvial sequences were studied around the prehistoric tell Arslantepe in 11 exposures and additional auger cores. The chronology is based on 11 optically stimulated luminescence (OSL) ages, four radiocarbon ages, and the embedded artifacts. Sediments contained wood charcoals, providing information on former vegetation. Fluvial activity is documented during Late Glacial times (15.4 ± 2.5, 12.8 ± 3.1 kyr) and frequently after Roman times. Slope and soil erosion occurred in the early (10.6 ± 1.4, 8.2 ± 0.7 kyr) and mid–late Holocene (6.7 ± 0.9, 5.4 ± 0.7–4.7 ± 0.7, 2.6 ± 0.2–2.5 ± 0.2, 1.9 ± 0.2–1.8 ± 0.2 kyr, and during the last 1000 years). The early Holocene erosion phases pre-date the so far established onset of settlement at the tell. This either indicates an earlier onset of agricultural land use than assumed or climatic influence on erosion, such as the 10.3 and 8.2 kyr climate events known from Western Europe. The erosion phases at around 5.0 and 2.6 kyr could re...</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="124955032"><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="124955032"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124955032; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124955032]").text(description); $(".js-view-count[data-work-id=124955032]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124955032; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124955032']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124955032, 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" } } $('.js-work-strip[data-work-id=124955032]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124955032,"title":"Holocene landscape dynamics at the tell Arslantepe, Malatya, Turkey – Soil erosion, buried soils and settlement layers, slope and river activity in a middle Euphrates catchment","translated_title":"","metadata":{"abstract":"Alluvial and colluvial sequences were studied around the prehistoric tell Arslantepe in 11 exposures and additional auger cores. The chronology is based on 11 optically stimulated luminescence (OSL) ages, four radiocarbon ages, and the embedded artifacts. Sediments contained wood charcoals, providing information on former vegetation. Fluvial activity is documented during Late Glacial times (15.4 ± 2.5, 12.8 ± 3.1 kyr) and frequently after Roman times. Slope and soil erosion occurred in the early (10.6 ± 1.4, 8.2 ± 0.7 kyr) and mid–late Holocene (6.7 ± 0.9, 5.4 ± 0.7–4.7 ± 0.7, 2.6 ± 0.2–2.5 ± 0.2, 1.9 ± 0.2–1.8 ± 0.2 kyr, and during the last 1000 years). The early Holocene erosion phases pre-date the so far established onset of settlement at the tell. This either indicates an earlier onset of agricultural land use than assumed or climatic influence on erosion, such as the 10.3 and 8.2 kyr climate events known from Western Europe. The erosion phases at around 5.0 and 2.6 kyr could re...","publisher":"SAGE Publications","publication_date":{"day":null,"month":null,"year":2014,"errors":{}},"publication_name":"The Holocene"},"translated_abstract":"Alluvial and colluvial sequences were studied around the prehistoric tell Arslantepe in 11 exposures and additional auger cores. The chronology is based on 11 optically stimulated luminescence (OSL) ages, four radiocarbon ages, and the embedded artifacts. Sediments contained wood charcoals, providing information on former vegetation. Fluvial activity is documented during Late Glacial times (15.4 ± 2.5, 12.8 ± 3.1 kyr) and frequently after Roman times. Slope and soil erosion occurred in the early (10.6 ± 1.4, 8.2 ± 0.7 kyr) and mid–late Holocene (6.7 ± 0.9, 5.4 ± 0.7–4.7 ± 0.7, 2.6 ± 0.2–2.5 ± 0.2, 1.9 ± 0.2–1.8 ± 0.2 kyr, and during the last 1000 years). The early Holocene erosion phases pre-date the so far established onset of settlement at the tell. This either indicates an earlier onset of agricultural land use than assumed or climatic influence on erosion, such as the 10.3 and 8.2 kyr climate events known from Western Europe. The erosion phases at around 5.0 and 2.6 kyr could re...","internal_url":"https://www.academia.edu/124955032/Holocene_landscape_dynamics_at_the_tell_Arslantepe_Malatya_Turkey_Soil_erosion_buried_soils_and_settlement_layers_slope_and_river_activity_in_a_middle_Euphrates_catchment","translated_internal_url":"","created_at":"2024-10-22T12:12:26.727-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":43308588,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Holocene_landscape_dynamics_at_the_tell_Arslantepe_Malatya_Turkey_Soil_erosion_buried_soils_and_settlement_layers_slope_and_river_activity_in_a_middle_Euphrates_catchment","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":43308588,"first_name":"Oliver","middle_initials":null,"last_name":"Nelle","page_name":"OliverNelle","domain_name":"independent","created_at":"2016-02-16T00:09:13.229-08:00","display_name":"Oliver Nelle","url":"https://independent.academia.edu/OliverNelle"},"attachments":[],"research_interests":[{"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":408,"name":"Geomorphology","url":"https://www.academia.edu/Documents/in/Geomorphology"},{"id":3790,"name":"Anatolian Archaeology","url":"https://www.academia.edu/Documents/in/Anatolian_Archaeology"},{"id":7232,"name":"Landscape History","url":"https://www.academia.edu/Documents/in/Landscape_History-1"},{"id":42436,"name":"Pedogenesis","url":"https://www.academia.edu/Documents/in/Pedogenesis"},{"id":72548,"name":"Soil Erosion","url":"https://www.academia.edu/Documents/in/Soil_Erosion"},{"id":78965,"name":"Holocene","url":"https://www.academia.edu/Documents/in/Holocene"},{"id":84446,"name":"Erosion","url":"https://www.academia.edu/Documents/in/Erosion"},{"id":93937,"name":"Radiocarbon Dating","url":"https://www.academia.edu/Documents/in/Radiocarbon_Dating"},{"id":159040,"name":"Anthracology","url":"https://www.academia.edu/Documents/in/Anthracology"},{"id":387211,"name":"Fluvial","url":"https://www.academia.edu/Documents/in/Fluvial"},{"id":629014,"name":"Palaeopedology","url":"https://www.academia.edu/Documents/in/Palaeopedology"},{"id":2259473,"name":"Colluvium","url":"https://www.academia.edu/Documents/in/Colluvium"}],"urls":[{"id":45283155,"url":"http://journals.sagepub.com/doi/pdf/10.1177/0959683614540949"}]}, dispatcherData: dispatcherData }); 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It is concluded that tree-ring width measurements along only two orthogonal radial rays are not always accurate enough and therefore averaging along the whole tree-ring profile is recommended.","publication_name":"Dendrochronologia","grobid_abstract_attachment_id":119084699},"translated_abstract":null,"internal_url":"https://www.academia.edu/124954985/Curvilinear_tree_ring_measurements_in_archaeological_wood_samples_from_X_ray_computed_tomography","translated_internal_url":"","created_at":"2024-10-22T12:11:39.861-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":43308588,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":119084699,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/119084699/thumbnails/1.jpg","file_name":"1-s2.0-S1125786522000820-main.pdf","download_url":"https://www.academia.edu/attachments/119084699/download_file?st=MTczMjgxNDYyOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Curvilinear_tree_ring_measurements_in_ar.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/119084699/1-s2.0-S1125786522000820-main-libre.pdf?1729626813=\u0026response-content-disposition=attachment%3B+filename%3DCurvilinear_tree_ring_measurements_in_ar.pdf\u0026Expires=1732818228\u0026Signature=cdRu4dA0vmhKKJv0PcPwJk5ljYYMMapOPBFG8bFifDH1G939QKZCfr8dd~4SeAu8ASAChtZAh2Fo57Vrl3lRc-eFF4lJx7cIe5hD4iyq7A5CnCuOrPwA7SzQpZvWeUmme2sXO2mBd7hPYA4YLC7Qx7wBT7vPpMbfo6peSQ4TUDpN2htD9w7m5B2QOKEkQlOP4h9aBpgZzlih3aij0~GvIUbfPrhQCJSxhf4vh6xFGW9tmbOw19ZL015Dr6m8Hz-tNZ5fnJaZ2AqkZFkMltuGJ-4GB6lsfGSq0LrtLx~dgkSC0X0jN6EYv40OLMJpgjPLTfKupAS1zWvNZiSxhjRhbA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Curvilinear_tree_ring_measurements_in_archaeological_wood_samples_from_X_ray_computed_tomography","translated_slug":"","page_count":6,"language":"en","content_type":"Work","owner":{"id":43308588,"first_name":"Oliver","middle_initials":null,"last_name":"Nelle","page_name":"OliverNelle","domain_name":"independent","created_at":"2016-02-16T00:09:13.229-08:00","display_name":"Oliver Nelle","url":"https://independent.academia.edu/OliverNelle"},"attachments":[{"id":119084699,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/119084699/thumbnails/1.jpg","file_name":"1-s2.0-S1125786522000820-main.pdf","download_url":"https://www.academia.edu/attachments/119084699/download_file?st=MTczMjgxNDYyOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Curvilinear_tree_ring_measurements_in_ar.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/119084699/1-s2.0-S1125786522000820-main-libre.pdf?1729626813=\u0026response-content-disposition=attachment%3B+filename%3DCurvilinear_tree_ring_measurements_in_ar.pdf\u0026Expires=1732818228\u0026Signature=cdRu4dA0vmhKKJv0PcPwJk5ljYYMMapOPBFG8bFifDH1G939QKZCfr8dd~4SeAu8ASAChtZAh2Fo57Vrl3lRc-eFF4lJx7cIe5hD4iyq7A5CnCuOrPwA7SzQpZvWeUmme2sXO2mBd7hPYA4YLC7Qx7wBT7vPpMbfo6peSQ4TUDpN2htD9w7m5B2QOKEkQlOP4h9aBpgZzlih3aij0~GvIUbfPrhQCJSxhf4vh6xFGW9tmbOw19ZL015Dr6m8Hz-tNZ5fnJaZ2AqkZFkMltuGJ-4GB6lsfGSq0LrtLx~dgkSC0X0jN6EYv40OLMJpgjPLTfKupAS1zWvNZiSxhjRhbA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":1648,"name":"Computed Tomography","url":"https://www.academia.edu/Documents/in/Computed_Tomography"},{"id":5541,"name":"Plant Biology","url":"https://www.academia.edu/Documents/in/Plant_Biology"},{"id":9117,"name":"Dendrochronology","url":"https://www.academia.edu/Documents/in/Dendrochronology"},{"id":36022,"name":"Tomography","url":"https://www.academia.edu/Documents/in/Tomography"},{"id":54418,"name":"Geometry","url":"https://www.academia.edu/Documents/in/Geometry"},{"id":1052234,"name":"Curvilinear Coordinates","url":"https://www.academia.edu/Documents/in/Curvilinear_Coordinates"}],"urls":[{"id":45283114,"url":"https://api.elsevier.com/content/article/PII:S1125786522000820?httpAccept=text/xml"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="97922885"><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/97922885/Environmental_development_and_local_human_impact_in_the_Jeetzel_valley_N_Germany_since_10_ka_BP_as_detected_by_geoarchaeological_analyses_in_a_coupled_aeolian_and_lacustrine_sediment_archive_at_Soven"><img alt="Research paper thumbnail of Environmental development and local human impact in the Jeetzel valley (N Germany) since 10 ka BP as detected by geoarchaeological analyses in a coupled aeolian and lacustrine sediment archive at Soven" class="work-thumbnail" src="https://attachments.academia-assets.com/99414417/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/97922885/Environmental_development_and_local_human_impact_in_the_Jeetzel_valley_N_Germany_since_10_ka_BP_as_detected_by_geoarchaeological_analyses_in_a_coupled_aeolian_and_lacustrine_sediment_archive_at_Soven">Environmental development and local human impact in the Jeetzel valley (N Germany) since 10 ka BP as detected by geoarchaeological analyses in a coupled aeolian and lacustrine sediment archive at Soven</a></div><div class="wp-workCard_item"><span>EG Quaternary Science Journal</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Abstract. Wahrend die archaologischen Quellen eine intensive mesolithische Besiedlung der in den ...</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. Wahrend die archaologischen Quellen eine intensive mesolithische Besiedlung der in den Flussniederungen gelegenen Dunen anzeigen, gibt es bislang erst wenige Erkenntnisse zur Mensch-Umwelt-Interaktion in Form von Landnutzungsstrategien und ihres potentiellen Einflusses auf die Landschaft. Die Kombination geoarchaologischer, chronologischer, geochemischer und palaookologischer Methoden und ihre Anwendung sowohl auf den Bereich der mesolithischen Fundstelle auf einer Dunenkuppe als auch die Verlandungssedimente eines benachbarten Altarmes erlaubte eine detaillierte Rekonstruktion der Landschaftsgeschichte bei Soven in der Jeetzel-Niederung (Norddeutschland) seit etwas 10,5 ka cal BP. Ausgehend von diesen Ergebnissen wurden vier Zeitphasen identifiziert, die mit lokalem menschlichen Umwelteinfluss wahrend des Mesolithikums, des Neolithikums und der Eisenzeit in Verbindung stehen konnten und vor dem Hintergrund der Landnutzungsgeschichte diskutiert werden. Obwohl eine mesolith...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1b1213b8f6b6eacf4a1a4ad635fdd184" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":99414417,"asset_id":97922885,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/99414417/download_file?st=MTczMjgxNDYyOCw4LjIyMi4yMDguMTQ2&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="97922885"><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="97922885"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 97922885; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=97922885]").text(description); $(".js-view-count[data-work-id=97922885]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 97922885; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='97922885']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 97922885, 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: "1b1213b8f6b6eacf4a1a4ad635fdd184" } } $('.js-work-strip[data-work-id=97922885]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":97922885,"title":"Environmental development and local human impact in the Jeetzel valley (N Germany) since 10 ka BP as detected by geoarchaeological analyses in a coupled aeolian and lacustrine sediment archive at Soven","translated_title":"","metadata":{"abstract":"Abstract. Wahrend die archaologischen Quellen eine intensive mesolithische Besiedlung der in den Flussniederungen gelegenen Dunen anzeigen, gibt es bislang erst wenige Erkenntnisse zur Mensch-Umwelt-Interaktion in Form von Landnutzungsstrategien und ihres potentiellen Einflusses auf die Landschaft. Die Kombination geoarchaologischer, chronologischer, geochemischer und palaookologischer Methoden und ihre Anwendung sowohl auf den Bereich der mesolithischen Fundstelle auf einer Dunenkuppe als auch die Verlandungssedimente eines benachbarten Altarmes erlaubte eine detaillierte Rekonstruktion der Landschaftsgeschichte bei Soven in der Jeetzel-Niederung (Norddeutschland) seit etwas 10,5 ka cal BP. Ausgehend von diesen Ergebnissen wurden vier Zeitphasen identifiziert, die mit lokalem menschlichen Umwelteinfluss wahrend des Mesolithikums, des Neolithikums und der Eisenzeit in Verbindung stehen konnten und vor dem Hintergrund der Landnutzungsgeschichte diskutiert werden. Obwohl eine mesolith...","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"EG Quaternary Science Journal"},"translated_abstract":"Abstract. Wahrend die archaologischen Quellen eine intensive mesolithische Besiedlung der in den Flussniederungen gelegenen Dunen anzeigen, gibt es bislang erst wenige Erkenntnisse zur Mensch-Umwelt-Interaktion in Form von Landnutzungsstrategien und ihres potentiellen Einflusses auf die Landschaft. Die Kombination geoarchaologischer, chronologischer, geochemischer und palaookologischer Methoden und ihre Anwendung sowohl auf den Bereich der mesolithischen Fundstelle auf einer Dunenkuppe als auch die Verlandungssedimente eines benachbarten Altarmes erlaubte eine detaillierte Rekonstruktion der Landschaftsgeschichte bei Soven in der Jeetzel-Niederung (Norddeutschland) seit etwas 10,5 ka cal BP. Ausgehend von diesen Ergebnissen wurden vier Zeitphasen identifiziert, die mit lokalem menschlichen Umwelteinfluss wahrend des Mesolithikums, des Neolithikums und der Eisenzeit in Verbindung stehen konnten und vor dem Hintergrund der Landnutzungsgeschichte diskutiert werden. Obwohl eine 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Vom Jahrring über den Kalender zu Baudatum und Dorfplan" class="work-thumbnail" src="https://attachments.academia-assets.com/99414415/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/97922884/Dendrochronologie_Vom_Jahrring_%C3%BCber_den_Kalender_zu_Baudatum_und_Dorfplan">Dendrochronologie. Vom Jahrring über den Kalender zu Baudatum und Dorfplan</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Die Jahresringe eines Holzes zeigen, wann und wie der Baum gewachsen ist. Bei Wärme und ausreiche...</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">Die Jahresringe eines Holzes zeigen, wann und wie der Baum gewachsen ist. Bei Wärme und ausreichend Wasser wachsen Bäume besser als bei Trockenheit und Kälte. Entsprechend können sie in der Wuchsperiode mehr oder weniger in den Zuwachs des Stammes investieren. Ein Jahrring wird vom Frühjahr bis zum Herbst im Holzkörper angelegt, wobei man zwischen Frühholz und Spätholz unterscheiden kann (Abb. 1). Dabei gehen Holzzellen aus einer dünnen Zellschicht, dem Kambium, hervor, die direkt unter der Rinde den Stamm und die Äste umläuft. Der Ring wird entsprechend breiter, je besser die Wachstumsbedingungen sind. So entsteht eine Abfolge von unterschiedlich breiten Ringen: Diese Jahrringmuster sind bei vielen Bäumen besonders derselben Art in einer Region sehr ähnlich. Neben der Witterung reagiert ein Baum auf Veränderungen der Lichtverhältnisse. Wird er von Nachbarbäumen beschattet, wächst er schlechter. Fallen Nachbarbäume zum Beispiel durch die Axt eines Siedlers, bekommt er mehr Licht und...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9d934fda5c4927b1eee0394d70b8dc2c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":99414415,"asset_id":97922884,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/99414415/download_file?st=MTczMjgxNDYyOCw4LjIyMi4yMDguMTQ2&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="97922884"><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="97922884"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 97922884; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=97922884]").text(description); $(".js-view-count[data-work-id=97922884]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 97922884; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='97922884']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 97922884, 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: "9d934fda5c4927b1eee0394d70b8dc2c" } } $('.js-work-strip[data-work-id=97922884]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":97922884,"title":"Dendrochronologie. 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Die Öfen konnten durch die hohe Konzentration des Kohlenstoffes in der Holzkohle effizienter betrieben werden, und die Holzkohle diente als Reduktionsmittel für das oxidiert im Erz vorliegende Eisen. Heute wird diese chemische Funktion in der Eisenherstellung von Steinkohle bzw. Koks erfüllt. Gewinnung und Verarbeitung von Eisen ist seit der Eisenzeit ohne die Verwendung von in Meilern verkohlten Bäumen nicht 165 1 Zwei Meilerpodien in einer Weide bei Bernau, Schwarzwald.","publication_date":{"day":null,"month":null,"year":2020,"errors":{}},"grobid_abstract_attachment_id":99414439},"translated_abstract":null,"internal_url":"https://www.academia.edu/97922881/Hunderte_K%C3%B6hler_Tausende_Meiler_Relikte_der_Holzkohleproduktion_in_der_Kulturlandschaft","translated_internal_url":"","created_at":"2023-03-04T10:12:03.585-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":43308588,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":99414439,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/99414439/thumbnails/1.jpg","file_name":"68061.pdf","download_url":"https://www.academia.edu/attachments/99414439/download_file?st=MTczMjgxNDYyOSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Hunderte_Kohler_Tausende_Meiler_Relikte.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/99414439/68061-libre.pdf?1677962410=\u0026response-content-disposition=attachment%3B+filename%3DHunderte_Kohler_Tausende_Meiler_Relikte.pdf\u0026Expires=1732818229\u0026Signature=RfcwVbnBCWDzyw9Bl3nmry2eZs3fMKVKPSz3m2b7GTxYNaqp9S8944JbPBdgBhRD~uSQtqNbEnDYur4~6c3Nq2njIca8xlGV0nGuG~b~myYX1O8bwpxx8ZE4I0PByCzYR7VjY-3zSii-H1zmiExhPO5D4ODFqCAmahiYclqjeCbeQufTDJwDbcgJqa2YbJZ9Dby~nUd25MX0y~fXoWHwWK7I7TfpeigGGuiJBWOkPqOvGXql5Sykvd2FQrgzdhrprRT-hlBLe38IGTs4bpbNYvwwbzdSKpKXFa~6Yg-XNGpb3eStx-RA88bFtdMAgR8LhUtnG3XikaMbyFKx8-X7ug__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Hunderte_Köhler_Tausende_Meiler_Relikte_der_Holzkohleproduktion_in_der_Kulturlandschaft","translated_slug":"","page_count":7,"language":"de","content_type":"Work","owner":{"id":43308588,"first_name":"Oliver","middle_initials":null,"last_name":"Nelle","page_name":"OliverNelle","domain_name":"independent","created_at":"2016-02-16T00:09:13.229-08:00","display_name":"Oliver Nelle","url":"https://independent.academia.edu/OliverNelle"},"attachments":[{"id":99414439,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/99414439/thumbnails/1.jpg","file_name":"68061.pdf","download_url":"https://www.academia.edu/attachments/99414439/download_file?st=MTczMjgxNDYyOSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Hunderte_Kohler_Tausende_Meiler_Relikte.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/99414439/68061-libre.pdf?1677962410=\u0026response-content-disposition=attachment%3B+filename%3DHunderte_Kohler_Tausende_Meiler_Relikte.pdf\u0026Expires=1732818229\u0026Signature=RfcwVbnBCWDzyw9Bl3nmry2eZs3fMKVKPSz3m2b7GTxYNaqp9S8944JbPBdgBhRD~uSQtqNbEnDYur4~6c3Nq2njIca8xlGV0nGuG~b~myYX1O8bwpxx8ZE4I0PByCzYR7VjY-3zSii-H1zmiExhPO5D4ODFqCAmahiYclqjeCbeQufTDJwDbcgJqa2YbJZ9Dby~nUd25MX0y~fXoWHwWK7I7TfpeigGGuiJBWOkPqOvGXql5Sykvd2FQrgzdhrprRT-hlBLe38IGTs4bpbNYvwwbzdSKpKXFa~6Yg-XNGpb3eStx-RA88bFtdMAgR8LhUtnG3XikaMbyFKx8-X7ug__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="97922880"><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/97922880/Vegetation_history_of_the_Maharlou_Lake_basin_SW_Iran_with_special_reference_to_the_Achaemenid_period_550_330_bc_"><img alt="Research paper thumbnail of Vegetation history of the Maharlou Lake basin (SW Iran) with special reference to the Achaemenid period (550–330 bc)" class="work-thumbnail" src="https://attachments.academia-assets.com/99414414/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/97922880/Vegetation_history_of_the_Maharlou_Lake_basin_SW_Iran_with_special_reference_to_the_Achaemenid_period_550_330_bc_">Vegetation history of the Maharlou Lake basin (SW Iran) with special reference to the Achaemenid period (550–330 bc)</a></div><div class="wp-workCard_item"><span>Vegetation History and Archaeobotany</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This study presents the results of a palynological investigation on a sediment core from the seas...</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 presents the results of a palynological investigation on a sediment core from the seasonal and saline Lake Maharlou in the Zagros Mountains in southwest Iran. We emphasised studying the role of man in modifying the vegetation of the area and the dominant agricultural practices during the Imperial Persia period (2,500–1,299 calbp; 550bc-ad651), particularly the Achaemenid Empire (2,500–2,280 calbp; 550–330bc). Scattered pistachio-almond scrub combined withQuercus brantiiwas the main vegetation type of the basin during the period studied. The present study depicts a significant increase in agriculture, suggesting urban development during the Late Antiquity and early Islamic Iranian dynasties. The inferred chronology of arboricultural activities is compatible with historical evidence showing that Fars Province witnessed economic and agricultural flourishing during these periods. The presence of the ‘Persian gardens’ is supported by the co-increase of cypress tree pollen freq...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="4c8225616ab2c10d3523997fb5a85a76" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":99414414,"asset_id":97922880,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/99414414/download_file?st=MTczMjgxNDYyOSw4LjIyMi4yMDguMTQ2&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="97922880"><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="97922880"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 97922880; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=97922880]").text(description); $(".js-view-count[data-work-id=97922880]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 97922880; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='97922880']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 97922880, 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: "4c8225616ab2c10d3523997fb5a85a76" } } $('.js-work-strip[data-work-id=97922880]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":97922880,"title":"Vegetation history of the Maharlou Lake basin (SW Iran) with special reference to the Achaemenid period (550–330 bc)","translated_title":"","metadata":{"abstract":"This study presents the results of a palynological investigation on a sediment core from the seasonal and saline Lake Maharlou in the Zagros Mountains in southwest Iran. We emphasised studying the role of man in modifying the vegetation of the area and the dominant agricultural practices during the Imperial Persia period (2,500–1,299 calbp; 550bc-ad651), particularly the Achaemenid Empire (2,500–2,280 calbp; 550–330bc). Scattered pistachio-almond scrub combined withQuercus brantiiwas the main vegetation type of the basin during the period studied. The present study depicts a significant increase in agriculture, suggesting urban development during the Late Antiquity and early Islamic Iranian dynasties. The inferred chronology of arboricultural activities is compatible with historical evidence showing that Fars Province witnessed economic and agricultural flourishing during these periods. 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The present study depicts a significant increase in agriculture, suggesting urban development during the Late Antiquity and early Islamic Iranian dynasties. The inferred chronology of arboricultural activities is compatible with historical evidence showing that Fars Province witnessed economic and agricultural flourishing during these periods. 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So far, the inner bark (phloem) of the lime tree (genus Tilia) could be detected most frequently. Microscopic examination of anatomical features can determine the taxon, requiring manipulation of samples and archaeological objects. In this study, micro-computed tomography (µCT) was reviewed as a method for determining the woody taxon and obtaining additional information from the inner bark. To this end, modern bark samples from different tree organs of lime were first analysed using both µCT and transmitted light microscopy. Both methods were able to detect all characteristic anatomical features in the phloem and identify the genus. With analysis based on µCT data, further anatomical information can be obtained. For example, the shape of the phloem rays in the bast strips can provide information on the position within the bark and on the original ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1dc3f4e5a44c1e72ad827cb5994402bd" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":119084693,"asset_id":124955041,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/119084693/download_file?st=MTczMjgxNDYyOSw4LjIyMi4yMDguMTQ2&st=MTczMjgxNDYyNyw4LjIyMi4yMDguMTQ2&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="124955041"><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="124955041"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124955041; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124955041]").text(description); $(".js-view-count[data-work-id=124955041]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124955041; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124955041']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124955041, 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: "1dc3f4e5a44c1e72ad827cb5994402bd" } } $('.js-work-strip[data-work-id=124955041]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124955041,"title":"Micro-computed tomography for the identification and characterization of archaeological lime bark","translated_title":"","metadata":{"abstract":"In the Neolithic pile-dwelling settlements of southwestern Germany, bark played a prominent role in the production of technical textiles. 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For example, the shape of the phloem rays in the bast strips can provide information on the position within the bark and on the original ...","publisher":"Springer Science and Business Media LLC","publication_name":"Scientific Reports"},"translated_abstract":"In the Neolithic pile-dwelling settlements of southwestern Germany, bark played a prominent role in the production of technical textiles. So far, the inner bark (phloem) of the lime tree (genus Tilia) could be detected most frequently. Microscopic examination of anatomical features can determine the taxon, requiring manipulation of samples and archaeological objects. In this study, micro-computed tomography (µCT) was reviewed as a method for determining the woody taxon and obtaining additional information from the inner bark. To this end, modern bark samples from different tree organs of lime were first analysed using both µCT and transmitted light microscopy. Both methods were able to detect all characteristic anatomical features in the phloem and identify the genus. With analysis based on µCT data, further anatomical information can be obtained. 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Archaeological excavation revealed a trench, a palisade and an occupation layer. The function of the wall and trench system remains unknown but there are several possibilities: It could have been used for protection, as a type of symbolic separation or to demarcate a cult site. The enclosure was constructed around the year zero. Charcoal samples were taken in a spatially detailed manner during excavation, as well as a new pollen core from a small spring mire directly next to the site. Anthracological analysis showed that Quercus (oak) was the main type of wood used in the construction of this enclosure. Thirteen additional wood taxa were identified, of which the next best represented is Corylus (hazel) and surprisingly a significant amount of Ilex (holly) was found. The samples did not contain Fagus (beech) or Carpinus (hornbeam), which are both common in the area today. According to pollen data, Fagus had begun to establish in the local woodland during the time of the enclosure, but did not gain importance before the migration period. By diameter analysis of the charcoals the size of the used wood (branch or trunk) was reconstructed. In addition, mean annual tree ring widths of the used wood e especially Quercus e show that the wood comes from young stems and/or branches of older trees and probably not from coppiced wood. The study shows that even small-scale archaeological excavations can yield important new data on wood utilization with a high spatial precision, which contributes to the reconstruction of local woodland composition.","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"Quaternary International","grobid_abstract_attachment_id":119084715},"translated_abstract":null,"internal_url":"https://www.academia.edu/124955033/Iron_Age_wood_usage_at_an_enclosure_in_northern_Germany","translated_internal_url":"","created_at":"2024-10-22T12:12:27.074-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":43308588,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":119084715,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/119084715/thumbnails/1.jpg","file_name":"j.quaint.2017.02.01420241022-1-e1fe8b.pdf","download_url":"https://www.academia.edu/attachments/119084715/download_file?st=MTczMjgxNDYyOSw4LjIyMi4yMDguMTQ2&st=MTczMjgxNDYyOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Iron_Age_wood_usage_at_an_enclosure_in_n.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/119084715/j.quaint.2017.02.01420241022-1-e1fe8b-libre.pdf?1729626797=\u0026response-content-disposition=attachment%3B+filename%3DIron_Age_wood_usage_at_an_enclosure_in_n.pdf\u0026Expires=1732818228\u0026Signature=cTD~clM8UsoB-oOjLL31LXNpASC3UglNej8UQqu3VDvNhDaorfeT~Bdnw7Oi-tiDK-Yvj6eM8sjJavuQ6Nv4-47KCFXDx51ihtrkZ6dYA4lwGWnUCNM-WYACzmwHUKhXm2XH8zXMcOY7jQ-1sJFWTKQQmd7fJIXxQ37qCuZmSlKpvohpbD7wIGlGh009zC~A0XAk2hKpaXzLFw-urzUfIuhY2lF~cnxmFZN8dS9~EXMq0~uZ3bioUatsjcfW0XtAP8Hy5OkxMiZ~HK6PWBehgwlBPSXcKVXRdwZ5of1RGEAtr1ElNRsM1EIryBRvo1~q-WI9H6Er~rCfvvCeq~891g__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Iron_Age_wood_usage_at_an_enclosure_in_northern_Germany","translated_slug":"","page_count":9,"language":"en","content_type":"Work","owner":{"id":43308588,"first_name":"Oliver","middle_initials":null,"last_name":"Nelle","page_name":"OliverNelle","domain_name":"independent","created_at":"2016-02-16T00:09:13.229-08:00","display_name":"Oliver Nelle","url":"https://independent.academia.edu/OliverNelle"},"attachments":[{"id":119084715,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/119084715/thumbnails/1.jpg","file_name":"j.quaint.2017.02.01420241022-1-e1fe8b.pdf","download_url":"https://www.academia.edu/attachments/119084715/download_file?st=MTczMjgxNDYyOSw4LjIyMi4yMDguMTQ2&st=MTczMjgxNDYyOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Iron_Age_wood_usage_at_an_enclosure_in_n.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/119084715/j.quaint.2017.02.01420241022-1-e1fe8b-libre.pdf?1729626797=\u0026response-content-disposition=attachment%3B+filename%3DIron_Age_wood_usage_at_an_enclosure_in_n.pdf\u0026Expires=1732818228\u0026Signature=cTD~clM8UsoB-oOjLL31LXNpASC3UglNej8UQqu3VDvNhDaorfeT~Bdnw7Oi-tiDK-Yvj6eM8sjJavuQ6Nv4-47KCFXDx51ihtrkZ6dYA4lwGWnUCNM-WYACzmwHUKhXm2XH8zXMcOY7jQ-1sJFWTKQQmd7fJIXxQ37qCuZmSlKpvohpbD7wIGlGh009zC~A0XAk2hKpaXzLFw-urzUfIuhY2lF~cnxmFZN8dS9~EXMq0~uZ3bioUatsjcfW0XtAP8Hy5OkxMiZ~HK6PWBehgwlBPSXcKVXRdwZ5of1RGEAtr1ElNRsM1EIryBRvo1~q-WI9H6Er~rCfvvCeq~891g__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"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":35587,"name":"Quaternary","url":"https://www.academia.edu/Documents/in/Quaternary"},{"id":261641,"name":"Fraxinus","url":"https://www.academia.edu/Documents/in/Fraxinus"},{"id":295952,"name":"Enclosure","url":"https://www.academia.edu/Documents/in/Enclosure"},{"id":655141,"name":"Beech","url":"https://www.academia.edu/Documents/in/Beech"},{"id":703023,"name":"Coppicing","url":"https://www.academia.edu/Documents/in/Coppicing"}],"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="124955032"><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/124955032/Holocene_landscape_dynamics_at_the_tell_Arslantepe_Malatya_Turkey_Soil_erosion_buried_soils_and_settlement_layers_slope_and_river_activity_in_a_middle_Euphrates_catchment"><img alt="Research paper thumbnail of Holocene landscape dynamics at the tell Arslantepe, Malatya, Turkey – Soil erosion, buried soils and settlement layers, slope and river activity in a middle Euphrates catchment" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/124955032/Holocene_landscape_dynamics_at_the_tell_Arslantepe_Malatya_Turkey_Soil_erosion_buried_soils_and_settlement_layers_slope_and_river_activity_in_a_middle_Euphrates_catchment">Holocene landscape dynamics at the tell Arslantepe, Malatya, Turkey – Soil erosion, buried soils and settlement layers, slope and river activity in a middle Euphrates catchment</a></div><div class="wp-workCard_item"><span>The Holocene</span><span>, 2014</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Alluvial and colluvial sequences were studied around the prehistoric tell Arslantepe in 11 exposu...</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">Alluvial and colluvial sequences were studied around the prehistoric tell Arslantepe in 11 exposures and additional auger cores. The chronology is based on 11 optically stimulated luminescence (OSL) ages, four radiocarbon ages, and the embedded artifacts. Sediments contained wood charcoals, providing information on former vegetation. Fluvial activity is documented during Late Glacial times (15.4 ± 2.5, 12.8 ± 3.1 kyr) and frequently after Roman times. Slope and soil erosion occurred in the early (10.6 ± 1.4, 8.2 ± 0.7 kyr) and mid–late Holocene (6.7 ± 0.9, 5.4 ± 0.7–4.7 ± 0.7, 2.6 ± 0.2–2.5 ± 0.2, 1.9 ± 0.2–1.8 ± 0.2 kyr, and during the last 1000 years). The early Holocene erosion phases pre-date the so far established onset of settlement at the tell. This either indicates an earlier onset of agricultural land use than assumed or climatic influence on erosion, such as the 10.3 and 8.2 kyr climate events known from Western Europe. The erosion phases at around 5.0 and 2.6 kyr could re...</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="124955032"><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="124955032"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 124955032; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=124955032]").text(description); $(".js-view-count[data-work-id=124955032]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 124955032; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='124955032']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 124955032, 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" } } $('.js-work-strip[data-work-id=124955032]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":124955032,"title":"Holocene landscape dynamics at the tell Arslantepe, Malatya, Turkey – Soil erosion, buried soils and settlement layers, slope and river activity in a middle Euphrates catchment","translated_title":"","metadata":{"abstract":"Alluvial and colluvial sequences were studied around the prehistoric tell Arslantepe in 11 exposures and additional auger cores. The chronology is based on 11 optically stimulated luminescence (OSL) ages, four radiocarbon ages, and the embedded artifacts. Sediments contained wood charcoals, providing information on former vegetation. Fluvial activity is documented during Late Glacial times (15.4 ± 2.5, 12.8 ± 3.1 kyr) and frequently after Roman times. Slope and soil erosion occurred in the early (10.6 ± 1.4, 8.2 ± 0.7 kyr) and mid–late Holocene (6.7 ± 0.9, 5.4 ± 0.7–4.7 ± 0.7, 2.6 ± 0.2–2.5 ± 0.2, 1.9 ± 0.2–1.8 ± 0.2 kyr, and during the last 1000 years). The early Holocene erosion phases pre-date the so far established onset of settlement at the tell. This either indicates an earlier onset of agricultural land use than assumed or climatic influence on erosion, such as the 10.3 and 8.2 kyr climate events known from Western Europe. The erosion phases at around 5.0 and 2.6 kyr could re...","publisher":"SAGE Publications","publication_date":{"day":null,"month":null,"year":2014,"errors":{}},"publication_name":"The Holocene"},"translated_abstract":"Alluvial and colluvial sequences were studied around the prehistoric tell Arslantepe in 11 exposures and additional auger cores. The chronology is based on 11 optically stimulated luminescence (OSL) ages, four radiocarbon ages, and the embedded artifacts. Sediments contained wood charcoals, providing information on former vegetation. Fluvial activity is documented during Late Glacial times (15.4 ± 2.5, 12.8 ± 3.1 kyr) and frequently after Roman times. Slope and soil erosion occurred in the early (10.6 ± 1.4, 8.2 ± 0.7 kyr) and mid–late Holocene (6.7 ± 0.9, 5.4 ± 0.7–4.7 ± 0.7, 2.6 ± 0.2–2.5 ± 0.2, 1.9 ± 0.2–1.8 ± 0.2 kyr, and during the last 1000 years). The early Holocene erosion phases pre-date the so far established onset of settlement at the tell. This either indicates an earlier onset of agricultural land use than assumed or climatic influence on erosion, such as the 10.3 and 8.2 kyr climate events known from Western Europe. The erosion phases at around 5.0 and 2.6 kyr could re...","internal_url":"https://www.academia.edu/124955032/Holocene_landscape_dynamics_at_the_tell_Arslantepe_Malatya_Turkey_Soil_erosion_buried_soils_and_settlement_layers_slope_and_river_activity_in_a_middle_Euphrates_catchment","translated_internal_url":"","created_at":"2024-10-22T12:12:26.727-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":43308588,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Holocene_landscape_dynamics_at_the_tell_Arslantepe_Malatya_Turkey_Soil_erosion_buried_soils_and_settlement_layers_slope_and_river_activity_in_a_middle_Euphrates_catchment","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":43308588,"first_name":"Oliver","middle_initials":null,"last_name":"Nelle","page_name":"OliverNelle","domain_name":"independent","created_at":"2016-02-16T00:09:13.229-08:00","display_name":"Oliver Nelle","url":"https://independent.academia.edu/OliverNelle"},"attachments":[],"research_interests":[{"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":408,"name":"Geomorphology","url":"https://www.academia.edu/Documents/in/Geomorphology"},{"id":3790,"name":"Anatolian Archaeology","url":"https://www.academia.edu/Documents/in/Anatolian_Archaeology"},{"id":7232,"name":"Landscape History","url":"https://www.academia.edu/Documents/in/Landscape_History-1"},{"id":42436,"name":"Pedogenesis","url":"https://www.academia.edu/Documents/in/Pedogenesis"},{"id":72548,"name":"Soil Erosion","url":"https://www.academia.edu/Documents/in/Soil_Erosion"},{"id":78965,"name":"Holocene","url":"https://www.academia.edu/Documents/in/Holocene"},{"id":84446,"name":"Erosion","url":"https://www.academia.edu/Documents/in/Erosion"},{"id":93937,"name":"Radiocarbon Dating","url":"https://www.academia.edu/Documents/in/Radiocarbon_Dating"},{"id":159040,"name":"Anthracology","url":"https://www.academia.edu/Documents/in/Anthracology"},{"id":387211,"name":"Fluvial","url":"https://www.academia.edu/Documents/in/Fluvial"},{"id":629014,"name":"Palaeopedology","url":"https://www.academia.edu/Documents/in/Palaeopedology"},{"id":2259473,"name":"Colluvium","url":"https://www.academia.edu/Documents/in/Colluvium"}],"urls":[{"id":45283155,"url":"http://journals.sagepub.com/doi/pdf/10.1177/0959683614540949"}]}, dispatcherData: dispatcherData }); 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Measurements of the curvilinear-tree-ring widths are performed using two approaches: firstly, measuring manually the distance between two points on two consecutive tree-rings along two orthogonal radii and, secondly, using a recently proposed computational approach which averages all calculated pairwise radial distances between two consecutive tree-rings along the whole treering profile. The results show that the irregularity of the tree-ring shape is an important factor to be considered in performing curvilinear-tree-ring measurements. For irregular shaped tree-rings, deviations up to 1.15 mm were observed between the output of both measurement's approaches. It is concluded that tree-ring width measurements along only two orthogonal radial rays are not always accurate enough and therefore averaging along the whole tree-ring profile is recommended.","publication_name":"Dendrochronologia","grobid_abstract_attachment_id":119084699},"translated_abstract":null,"internal_url":"https://www.academia.edu/124954985/Curvilinear_tree_ring_measurements_in_archaeological_wood_samples_from_X_ray_computed_tomography","translated_internal_url":"","created_at":"2024-10-22T12:11:39.861-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":43308588,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":119084699,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/119084699/thumbnails/1.jpg","file_name":"1-s2.0-S1125786522000820-main.pdf","download_url":"https://www.academia.edu/attachments/119084699/download_file?st=MTczMjgxNDYyOSw4LjIyMi4yMDguMTQ2&st=MTczMjgxNDYyOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Curvilinear_tree_ring_measurements_in_ar.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/119084699/1-s2.0-S1125786522000820-main-libre.pdf?1729626813=\u0026response-content-disposition=attachment%3B+filename%3DCurvilinear_tree_ring_measurements_in_ar.pdf\u0026Expires=1732818228\u0026Signature=cdRu4dA0vmhKKJv0PcPwJk5ljYYMMapOPBFG8bFifDH1G939QKZCfr8dd~4SeAu8ASAChtZAh2Fo57Vrl3lRc-eFF4lJx7cIe5hD4iyq7A5CnCuOrPwA7SzQpZvWeUmme2sXO2mBd7hPYA4YLC7Qx7wBT7vPpMbfo6peSQ4TUDpN2htD9w7m5B2QOKEkQlOP4h9aBpgZzlih3aij0~GvIUbfPrhQCJSxhf4vh6xFGW9tmbOw19ZL015Dr6m8Hz-tNZ5fnJaZ2AqkZFkMltuGJ-4GB6lsfGSq0LrtLx~dgkSC0X0jN6EYv40OLMJpgjPLTfKupAS1zWvNZiSxhjRhbA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Curvilinear_tree_ring_measurements_in_archaeological_wood_samples_from_X_ray_computed_tomography","translated_slug":"","page_count":6,"language":"en","content_type":"Work","owner":{"id":43308588,"first_name":"Oliver","middle_initials":null,"last_name":"Nelle","page_name":"OliverNelle","domain_name":"independent","created_at":"2016-02-16T00:09:13.229-08:00","display_name":"Oliver Nelle","url":"https://independent.academia.edu/OliverNelle"},"attachments":[{"id":119084699,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/119084699/thumbnails/1.jpg","file_name":"1-s2.0-S1125786522000820-main.pdf","download_url":"https://www.academia.edu/attachments/119084699/download_file?st=MTczMjgxNDYyOSw4LjIyMi4yMDguMTQ2&st=MTczMjgxNDYyOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Curvilinear_tree_ring_measurements_in_ar.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/119084699/1-s2.0-S1125786522000820-main-libre.pdf?1729626813=\u0026response-content-disposition=attachment%3B+filename%3DCurvilinear_tree_ring_measurements_in_ar.pdf\u0026Expires=1732818228\u0026Signature=cdRu4dA0vmhKKJv0PcPwJk5ljYYMMapOPBFG8bFifDH1G939QKZCfr8dd~4SeAu8ASAChtZAh2Fo57Vrl3lRc-eFF4lJx7cIe5hD4iyq7A5CnCuOrPwA7SzQpZvWeUmme2sXO2mBd7hPYA4YLC7Qx7wBT7vPpMbfo6peSQ4TUDpN2htD9w7m5B2QOKEkQlOP4h9aBpgZzlih3aij0~GvIUbfPrhQCJSxhf4vh6xFGW9tmbOw19ZL015Dr6m8Hz-tNZ5fnJaZ2AqkZFkMltuGJ-4GB6lsfGSq0LrtLx~dgkSC0X0jN6EYv40OLMJpgjPLTfKupAS1zWvNZiSxhjRhbA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":1648,"name":"Computed Tomography","url":"https://www.academia.edu/Documents/in/Computed_Tomography"},{"id":5541,"name":"Plant Biology","url":"https://www.academia.edu/Documents/in/Plant_Biology"},{"id":9117,"name":"Dendrochronology","url":"https://www.academia.edu/Documents/in/Dendrochronology"},{"id":36022,"name":"Tomography","url":"https://www.academia.edu/Documents/in/Tomography"},{"id":54418,"name":"Geometry","url":"https://www.academia.edu/Documents/in/Geometry"},{"id":1052234,"name":"Curvilinear Coordinates","url":"https://www.academia.edu/Documents/in/Curvilinear_Coordinates"}],"urls":[{"id":45283114,"url":"https://api.elsevier.com/content/article/PII:S1125786522000820?httpAccept=text/xml"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="97922885"><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/97922885/Environmental_development_and_local_human_impact_in_the_Jeetzel_valley_N_Germany_since_10_ka_BP_as_detected_by_geoarchaeological_analyses_in_a_coupled_aeolian_and_lacustrine_sediment_archive_at_Soven"><img alt="Research paper thumbnail of Environmental development and local human impact in the Jeetzel valley (N Germany) since 10 ka BP as detected by geoarchaeological analyses in a coupled aeolian and lacustrine sediment archive at Soven" class="work-thumbnail" src="https://attachments.academia-assets.com/99414417/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/97922885/Environmental_development_and_local_human_impact_in_the_Jeetzel_valley_N_Germany_since_10_ka_BP_as_detected_by_geoarchaeological_analyses_in_a_coupled_aeolian_and_lacustrine_sediment_archive_at_Soven">Environmental development and local human impact in the Jeetzel valley (N Germany) since 10 ka BP as detected by geoarchaeological analyses in a coupled aeolian and lacustrine sediment archive at Soven</a></div><div class="wp-workCard_item"><span>EG Quaternary Science Journal</span><span>, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Abstract. Wahrend die archaologischen Quellen eine intensive mesolithische Besiedlung der in den ...</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. Wahrend die archaologischen Quellen eine intensive mesolithische Besiedlung der in den Flussniederungen gelegenen Dunen anzeigen, gibt es bislang erst wenige Erkenntnisse zur Mensch-Umwelt-Interaktion in Form von Landnutzungsstrategien und ihres potentiellen Einflusses auf die Landschaft. Die Kombination geoarchaologischer, chronologischer, geochemischer und palaookologischer Methoden und ihre Anwendung sowohl auf den Bereich der mesolithischen Fundstelle auf einer Dunenkuppe als auch die Verlandungssedimente eines benachbarten Altarmes erlaubte eine detaillierte Rekonstruktion der Landschaftsgeschichte bei Soven in der Jeetzel-Niederung (Norddeutschland) seit etwas 10,5 ka cal BP. Ausgehend von diesen Ergebnissen wurden vier Zeitphasen identifiziert, die mit lokalem menschlichen Umwelteinfluss wahrend des Mesolithikums, des Neolithikums und der Eisenzeit in Verbindung stehen konnten und vor dem Hintergrund der Landnutzungsgeschichte diskutiert werden. Obwohl eine mesolith...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="1b1213b8f6b6eacf4a1a4ad635fdd184" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":99414417,"asset_id":97922885,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/99414417/download_file?st=MTczMjgxNDYyOSw4LjIyMi4yMDguMTQ2&st=MTczMjgxNDYyOCw4LjIyMi4yMDguMTQ2&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="97922885"><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="97922885"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 97922885; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=97922885]").text(description); $(".js-view-count[data-work-id=97922885]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 97922885; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='97922885']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 97922885, 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: "1b1213b8f6b6eacf4a1a4ad635fdd184" } } $('.js-work-strip[data-work-id=97922885]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":97922885,"title":"Environmental development and local human impact in the Jeetzel valley (N Germany) since 10 ka BP as detected by geoarchaeological analyses in a coupled aeolian and lacustrine sediment archive at Soven","translated_title":"","metadata":{"abstract":"Abstract. Wahrend die archaologischen Quellen eine intensive mesolithische Besiedlung der in den Flussniederungen gelegenen Dunen anzeigen, gibt es bislang erst wenige Erkenntnisse zur Mensch-Umwelt-Interaktion in Form von Landnutzungsstrategien und ihres potentiellen Einflusses auf die Landschaft. Die Kombination geoarchaologischer, chronologischer, geochemischer und palaookologischer Methoden und ihre Anwendung sowohl auf den Bereich der mesolithischen Fundstelle auf einer Dunenkuppe als auch die Verlandungssedimente eines benachbarten Altarmes erlaubte eine detaillierte Rekonstruktion der Landschaftsgeschichte bei Soven in der Jeetzel-Niederung (Norddeutschland) seit etwas 10,5 ka cal BP. Ausgehend von diesen Ergebnissen wurden vier Zeitphasen identifiziert, die mit lokalem menschlichen Umwelteinfluss wahrend des Mesolithikums, des Neolithikums und der Eisenzeit in Verbindung stehen konnten und vor dem Hintergrund der Landnutzungsgeschichte diskutiert werden. Obwohl eine mesolith...","publication_date":{"day":null,"month":null,"year":2015,"errors":{}},"publication_name":"EG Quaternary Science Journal"},"translated_abstract":"Abstract. Wahrend die archaologischen Quellen eine intensive mesolithische Besiedlung der in den Flussniederungen gelegenen Dunen anzeigen, gibt es bislang erst wenige Erkenntnisse zur Mensch-Umwelt-Interaktion in Form von Landnutzungsstrategien und ihres potentiellen Einflusses auf die Landschaft. Die Kombination geoarchaologischer, chronologischer, geochemischer und palaookologischer Methoden und ihre Anwendung sowohl auf den Bereich der mesolithischen Fundstelle auf einer Dunenkuppe als auch die Verlandungssedimente eines benachbarten Altarmes erlaubte eine detaillierte Rekonstruktion der Landschaftsgeschichte bei Soven in der Jeetzel-Niederung (Norddeutschland) seit etwas 10,5 ka cal BP. Ausgehend von diesen Ergebnissen wurden vier Zeitphasen identifiziert, die mit lokalem menschlichen Umwelteinfluss wahrend des Mesolithikums, des Neolithikums und der Eisenzeit in Verbindung stehen konnten und vor dem Hintergrund der Landnutzungsgeschichte diskutiert werden. 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Vom Jahrring über den Kalender zu Baudatum und Dorfplan" class="work-thumbnail" src="https://attachments.academia-assets.com/99414415/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/97922884/Dendrochronologie_Vom_Jahrring_%C3%BCber_den_Kalender_zu_Baudatum_und_Dorfplan">Dendrochronologie. Vom Jahrring über den Kalender zu Baudatum und Dorfplan</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Die Jahresringe eines Holzes zeigen, wann und wie der Baum gewachsen ist. Bei Wärme und ausreiche...</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">Die Jahresringe eines Holzes zeigen, wann und wie der Baum gewachsen ist. Bei Wärme und ausreichend Wasser wachsen Bäume besser als bei Trockenheit und Kälte. Entsprechend können sie in der Wuchsperiode mehr oder weniger in den Zuwachs des Stammes investieren. Ein Jahrring wird vom Frühjahr bis zum Herbst im Holzkörper angelegt, wobei man zwischen Frühholz und Spätholz unterscheiden kann (Abb. 1). Dabei gehen Holzzellen aus einer dünnen Zellschicht, dem Kambium, hervor, die direkt unter der Rinde den Stamm und die Äste umläuft. Der Ring wird entsprechend breiter, je besser die Wachstumsbedingungen sind. So entsteht eine Abfolge von unterschiedlich breiten Ringen: Diese Jahrringmuster sind bei vielen Bäumen besonders derselben Art in einer Region sehr ähnlich. Neben der Witterung reagiert ein Baum auf Veränderungen der Lichtverhältnisse. Wird er von Nachbarbäumen beschattet, wächst er schlechter. Fallen Nachbarbäume zum Beispiel durch die Axt eines Siedlers, bekommt er mehr Licht und...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9d934fda5c4927b1eee0394d70b8dc2c" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":99414415,"asset_id":97922884,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/99414415/download_file?st=MTczMjgxNDYyOSw4LjIyMi4yMDguMTQ2&st=MTczMjgxNDYyOCw4LjIyMi4yMDguMTQ2&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="97922884"><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="97922884"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 97922884; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=97922884]").text(description); $(".js-view-count[data-work-id=97922884]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 97922884; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='97922884']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 97922884, 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: "9d934fda5c4927b1eee0394d70b8dc2c" } } $('.js-work-strip[data-work-id=97922884]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":97922884,"title":"Dendrochronologie. 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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="97922880"><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/97922880/Vegetation_history_of_the_Maharlou_Lake_basin_SW_Iran_with_special_reference_to_the_Achaemenid_period_550_330_bc_"><img alt="Research paper thumbnail of Vegetation history of the Maharlou Lake basin (SW Iran) with special reference to the Achaemenid period (550–330 bc)" class="work-thumbnail" src="https://attachments.academia-assets.com/99414414/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/97922880/Vegetation_history_of_the_Maharlou_Lake_basin_SW_Iran_with_special_reference_to_the_Achaemenid_period_550_330_bc_">Vegetation history of the Maharlou Lake basin (SW Iran) with special reference to the Achaemenid period (550–330 bc)</a></div><div class="wp-workCard_item"><span>Vegetation History and Archaeobotany</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">This study presents the results of a palynological investigation on a sediment core from the seas...</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 presents the results of a palynological investigation on a sediment core from the seasonal and saline Lake Maharlou in the Zagros Mountains in southwest Iran. We emphasised studying the role of man in modifying the vegetation of the area and the dominant agricultural practices during the Imperial Persia period (2,500–1,299 calbp; 550bc-ad651), particularly the Achaemenid Empire (2,500–2,280 calbp; 550–330bc). Scattered pistachio-almond scrub combined withQuercus brantiiwas the main vegetation type of the basin during the period studied. The present study depicts a significant increase in agriculture, suggesting urban development during the Late Antiquity and early Islamic Iranian dynasties. The inferred chronology of arboricultural activities is compatible with historical evidence showing that Fars Province witnessed economic and agricultural flourishing during these periods. The presence of the ‘Persian gardens’ is supported by the co-increase of cypress tree pollen freq...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="4c8225616ab2c10d3523997fb5a85a76" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":99414414,"asset_id":97922880,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/99414414/download_file?st=MTczMjgxNDYyOSw4LjIyMi4yMDguMTQ2&st=MTczMjgxNDYyOSw4LjIyMi4yMDguMTQ2&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="97922880"><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="97922880"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 97922880; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=97922880]").text(description); $(".js-view-count[data-work-id=97922880]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 97922880; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='97922880']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 97922880, 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: "4c8225616ab2c10d3523997fb5a85a76" } } $('.js-work-strip[data-work-id=97922880]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":97922880,"title":"Vegetation history of the Maharlou Lake basin (SW Iran) with special reference to the Achaemenid period (550–330 bc)","translated_title":"","metadata":{"abstract":"This study presents the results of a palynological investigation on a sediment core from the seasonal and saline Lake Maharlou in the Zagros Mountains in southwest Iran. 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