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christine chataigner - Academia.edu

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js-section-heading" data-section="Papers" id="Papers"><h3 class="profile--tab_heading_container">Papers by christine chataigner</h3></div><div class="js-work-strip profile--work_container" data-work-id="127736902"><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/127736902/The_South_Caucasus_from_the_Upper_Palaeolithic_to_the_Neolithic_Intersection_of_the_genetic_and_archaeological_data"><img alt="Research paper thumbnail of The South Caucasus from the Upper Palaeolithic to the Neolithic: Intersection of the genetic and archaeological data" class="work-thumbnail" src="https://attachments.academia-assets.com/121424545/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/127736902/The_South_Caucasus_from_the_Upper_Palaeolithic_to_the_Neolithic_Intersection_of_the_genetic_and_archaeological_data">The South Caucasus from the Upper Palaeolithic to the Neolithic: Intersection of the genetic and archaeological data</a></div><div class="wp-workCard_item"><span>Journal of Quaternary Science Reviews</span><span>, 2024</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The genomic characterisation of human remains and the study of archaeological assemblages are com...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The genomic characterisation of human remains and the study of archaeological assemblages are complementary keys to understanding the evolution of ancient human groups. This article proposes a dialogue between these two approaches for the South Caucasus between the Upper Palaeolithic and the Neolithic periods. In the Upper Palaeolithic before the Last Glacial Maximum (ca. 40.-23. ka cal BP), genetic and archaeological data demonstrate the originality of the populations of the South Caucasus (Caucasus_UP genome) compared with their neighbours in SE Europe and SW Asia and also show the existence of links between these different regions. For the post-LGM phase (ca. 20.9-11.7 ka cal BP), archaeological data suggest a certain continuity with the previous period during the cold phase of the Oldest Dryas, followed by a marked rapprochement with the Zarzian culture in the Zagros starting with the warming of the Bølling-Allerød. Genetic analyses, which are available only for the latter phase, reveal a new genome (Caucasus Hunter-Gatherer or CHG), that is very close to that of the ancestors of the Neolithic populations of the Zagros. For the Early Holocene (ca. 11.7-8.2 ka cal BP or 9700-6200 cal BCE), the CHG genome, which still characterises the populations of the South Caucasus, is difficult to distinguish in modelling from that of the Zagros (Iran_N). However, archaeological data suggest that the spread of the Iran_N/CHG gene pool from Iran to Upper Mesopotamia and Central Anatolia was due to populations from the northwest Zagros, and not to those from the South Caucasus, who had only occasional contacts with the Fertile Crescent. At the beginning of the Middle Holocene (ca. 8.2-7.2 ka cal BP or 6200-5200 cal BCE), the appearance in the South Caucasus of animals and plants presenting a high level of domestication, as well as the introduction of new techniques (pressure knapping with a lever, pottery), are clearly due to the arrival of populations from the Fertile Crescent, as confirmed by genetic analyses. These analyses also show that there was not a replacement of local Mesolithic communities by Neolithic farmers, which the archaeological evidence confirms.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="8288c2f4b6e48832023210ad37917259" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:121424545,&quot;asset_id&quot;:127736902,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/121424545/download_file?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="127736902"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127736902"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127736902; 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$(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="127669939"><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/127669939/The_South_Caucasus_from_the_Upper_Palaeolithic_to_the_Neolithic_Intersection_of_the_genetic_and_archaeological_data"><img alt="Research paper thumbnail of The South Caucasus from the Upper Palaeolithic to the Neolithic: Intersection of the genetic and archaeological data" class="work-thumbnail" src="https://attachments.academia-assets.com/121369375/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/127669939/The_South_Caucasus_from_the_Upper_Palaeolithic_to_the_Neolithic_Intersection_of_the_genetic_and_archaeological_data">The South Caucasus from the Upper Palaeolithic to the Neolithic: Intersection of the genetic and archaeological data</a></div><div class="wp-workCard_item"><span>Journal of Quaternary Science Reviews</span><span>, 2024</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The genomic characterisation of human remains and the study of archaeological assemblages are com...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The genomic characterisation of human remains and the study of archaeological assemblages are complementary keys to understanding the evolution of ancient human groups. This article proposes a dialogue between these two approaches for the South Caucasus between the Upper Palaeolithic and the Neolithic periods. In the Upper Palaeolithic before the Last Glacial Maximum (ca. 40.-23. ka cal BP), genetic and archaeological data demonstrate the originality of the populations of the South Caucasus (Caucasus_UP genome) compared with their neighbours in SE Europe and SW Asia and also show the existence of links between these different regions. For the post-LGM phase (ca. 20.9-11.7 ka cal BP), archaeological data suggest a certain continuity with the previous period during the cold phase of the Oldest Dryas, followed by a marked rapprochement with the Zarzian culture in the Zagros starting with the warming of the Bølling-Allerød. Genetic analyses, which are available only for the latter phase, reveal a new genome (Caucasus Hunter-Gatherer or CHG), that is very close to that of the ancestors of the Neolithic populations of the Zagros. For the Early Holocene (ca. 11.7-8.2 ka cal BP or 9700-6200 cal BCE), the CHG genome, which still characterises the populations of the South Caucasus, is difficult to distinguish in modelling from that of the Zagros (Iran_N). However, archaeological data suggest that the spread of the Iran_N/CHG gene pool from Iran to Upper Mesopotamia and Central Anatolia was due to populations from the northwest Zagros, and not to those from the South Caucasus, who had only occasional contacts with the Fertile Crescent. At the beginning of the Middle Holocene (ca. 8.2-7.2 ka cal BP or 6200-5200 cal BCE), the appearance in the South Caucasus of animals and plants presenting a high level of domestication, as well as the introduction of new techniques (pressure knapping with a lever, pottery), are clearly due to the arrival of populations from the Fertile Crescent, as confirmed by genetic analyses. These analyses also show that there was not a replacement of local Mesolithic communities by Neolithic farmers, which the archaeological evidence confirms.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e1248b4c4f10f104b8817eb4ec9421ee" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:121369375,&quot;asset_id&quot;:127669939,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/121369375/download_file?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="127669939"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127669939"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127669939; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="126611827"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/126611827/Environments_and_Societies_in_the_Southern_Caucasus_during_the_Holocene"><img alt="Research paper thumbnail of Environments and Societies in the Southern Caucasus during the Holocene" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/126611827/Environments_and_Societies_in_the_Southern_Caucasus_during_the_Holocene">Environments and Societies in the Southern Caucasus during the Holocene</a></div><div class="wp-workCard_item"><span>Quaternary International</span><span>, Feb 1, 2016</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="126611827"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="126611827"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 126611827; 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=126611827]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":126611827,"title":"Environments and Societies in the Southern Caucasus during the Holocene","internal_url":"https://www.academia.edu/126611827/Environments_and_Societies_in_the_Southern_Caucasus_during_the_Holocene","owner_id":58602709,"coauthors_can_edit":true,"owner":{"id":58602709,"first_name":"christine","middle_initials":null,"last_name":"chataigner","page_name":"cchataigner","domain_name":"independent","created_at":"2017-01-06T05:38:55.820-08:00","display_name":"christine chataigner","url":"https://independent.academia.edu/cchataigner"},"attachments":[]}, 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="126244296"><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/126244296/NEW_DATA_ON_THE_EXPLOITATION_OF_OBSIDIAN_IN_THE_SOUTHERN_CAUCASUS_ARMENIA_GEORGIA_AND_EASTERN_TURKEY_PART_2_OBSIDIAN_PROCUREMENT_FROM_THE_UPPER_PALAEOLITHIC_TO_THE_LATE_BRONZE_AGE"><img alt="Research paper thumbnail of NEW DATA ON THE EXPLOITATION OF OBSIDIAN IN THE SOUTHERN CAUCASUS (ARMENIA, GEORGIA) AND EASTERN TURKEY, PART 2: OBSIDIAN PROCUREMENT FROM THE UPPER PALAEOLITHIC TO THE LATE BRONZE AGE" 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/126244296/NEW_DATA_ON_THE_EXPLOITATION_OF_OBSIDIAN_IN_THE_SOUTHERN_CAUCASUS_ARMENIA_GEORGIA_AND_EASTERN_TURKEY_PART_2_OBSIDIAN_PROCUREMENT_FROM_THE_UPPER_PALAEOLITHIC_TO_THE_LATE_BRONZE_AGE">NEW DATA ON THE EXPLOITATION OF OBSIDIAN IN THE SOUTHERN CAUCASUS (ARMENIA, GEORGIA) AND EASTERN TURKEY, PART 2: OBSIDIAN PROCUREMENT FROM THE UPPER PALAEOLITHIC TO THE LATE BRONZE AGE</a></div><div class="wp-workCard_item"><span>Archaeometry</span><span>, 2014</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Within the framework of the French archaeological mission &#39;Caucasus&#39;, in a previous paper we have...</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">Within the framework of the French archaeological mission &#39;Caucasus&#39;, in a previous paper we have presented new geochemical analyses on geological obsidians from the southern Caucasus (Armenia, Georgia) and eastern Turkey. We present here the second part of this research, which deals with provenance studies of archaeological obsidians from Armenia. These new data enhance our knowledge of obsidian exploitation over a period of more than 14 000 years, from the Upper Palaeolithic to the Late Bronze Age. The proposed methodology shows that source attribution can be easily made by plotting element contents and element ratios on three simple binary diagrams. The same diagrams were used for source discrimination. As the southern Caucasus is a mountainous region for which the factor of distance as the crow flies cannot be applied, we have explored the capacity of the Geographic Information System to evaluate the nature and patterns of travel costs between the sources of obsidian and the archaeological sites. The role of the secondary obsidian deposits, which enabled the populations to acquire raw material at a considerable distance from the outcrops, is also considered.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="207ea6855204e7b676dda131ba8daa0d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:120150945,&quot;asset_id&quot;:126244296,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/120150945/download_file?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="126244296"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="126244296"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 126244296; 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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="126244116"><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/126244116/NEW_DATA_ON_THE_EXPLOITATION_OF_OBSIDIAN_IN_THE_SOUTHERN_CAUCASUS_ARMENIA_GEORGIA_AND_EASTERN_TURKEY_PART_1_SOURCE_CHARACTERIZATION"><img alt="Research paper thumbnail of NEW DATA ON THE EXPLOITATION OF OBSIDIAN IN THE SOUTHERN CAUCASUS (ARMENIA, GEORGIA) AND EASTERN TURKEY, PART 1: SOURCE CHARACTERIZATION" 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/126244116/NEW_DATA_ON_THE_EXPLOITATION_OF_OBSIDIAN_IN_THE_SOUTHERN_CAUCASUS_ARMENIA_GEORGIA_AND_EASTERN_TURKEY_PART_1_SOURCE_CHARACTERIZATION">NEW DATA ON THE EXPLOITATION OF OBSIDIAN IN THE SOUTHERN CAUCASUS (ARMENIA, GEORGIA) AND EASTERN TURKEY, PART 1: SOURCE CHARACTERIZATION</a></div><div class="wp-workCard_item"><span>Archaeometry</span><span>, 2014</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A large analytical programme involving both obsidian source characterization and obsidian artefac...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">A large analytical programme involving both obsidian source characterization and obsidian artefact sourcing was initiated recently within the framework of the French archaeological mission &#39;Caucasus&#39;. The results will be presented in two parts: the first part, this paper, deals with the presentation and characterization of obsidian outcrops in the southern Caucasus, while the second presents some results obtained from a selection of artefacts originating from different Armenian sites dated to between the Upper Palaeolithic and the Late Bronze Age. The same analytical method, LA-ICP-MS (laser ablation inductively coupled plasma mass spectrometry), has been used to characterize all the studied samples (both geological and archaeological). This method is more and more widely used to determine the elemental composition of obsidian artefacts, as it causes minimal damage to the studied objects. We present in this first part new geochemical analyses on geological obsidians originating from the southern Caucasus (Armenia, Georgia) and eastern Turkey. These data enhance our knowledge of the obsidian sources in these regions. A simple methodology, based on the use of three diagrams, is proposed to easily differentiate the deposits and to study the early exploitation of this material in the southern Caucasus.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="6b8f474017705bb6b2ef162b54bb7cb1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:120150663,&quot;asset_id&quot;:126244116,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/120150663/download_file?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="126244116"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="126244116"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 126244116; 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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="125538363"><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/125538363/Diachronic_variability_in_obsidian_procurement_patterns_and_the_role_of_the_cave_sheepfold_of_Getahovit_2_NE_Armenia_during_the_Chalcolithic_period"><img alt="Research paper thumbnail of Diachronic variability in obsidian procurement patterns and the role of the cave-sheepfold of Getahovit-2 (NE Armenia) during the Chalcolithic period" class="work-thumbnail" src="https://attachments.academia-assets.com/119561300/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/125538363/Diachronic_variability_in_obsidian_procurement_patterns_and_the_role_of_the_cave_sheepfold_of_Getahovit_2_NE_Armenia_during_the_Chalcolithic_period">Diachronic variability in obsidian procurement patterns and the role of the cave-sheepfold of Getahovit-2 (NE Armenia) during the Chalcolithic period</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/cchataigner">christine chataigner</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://sci.academia.edu/RomanHovsepyan">Roman Hovsepyan</a></span></div><div class="wp-workCard_item"><span>Quaternary International</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The cave of Getahovit-2 is situated in north-eastern Armenia, in the foothills of the Lesser Cauc...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The cave of Getahovit-2 is situated in north-eastern Armenia, in the foothills of the Lesser Caucasus which dominate the valley of the Kura. The excavations (2011–2017), carried out by the Armenian-French mission ‘Caucasus’, have revealed several phases of occupation – Upper Palaeolithic (ca 22,000 cal BC), Chalcolithic (ca. 4700-4050 cal BC), and early Middle Ages (ca. 900–1200 cal AD). Although the cave is near outcroppings of flint (lower valley of the Aghstev river), the artifacts found there are mainly in obsidian, whatever the period of occupation. During the Chalcolithic period (levels IV-III), the cave served as a shelter for herds, as seen in the succession of coprolite deposits, that were regularly burned to clean the floor of the cave. The origin of the populations that sheltered their herds in this cave is difficult to determine. LA-ICP-MS analyses have been carried out to study the provenance of the obsidian artifacts found in level III. Corroborated by the techno-typological study of the artifacts, they have enabled the differentiation of two assemblages: the first, coming from deposits situated on Armenian territory (Geghasar, Gutansar, Arteni, Tsaghkunyats) and consisting of blanks knapped by percussion (flakes above all), and the second coming from deposits situated in Georgia (Chikiani) or Turkey (region of Sarıkamış) and consisting of pressure-flaked blades. In the lower part of level III (ca 4700-4400 cal BC), the provenance of the obsidian (mainly Gutansar) suggests links with the south, the Ararat plain. For the upper part of level III (ca. 4400-4050 cal BC), it is the outcrops situated farther north (Tsaghkunyats) that were the origin of almost 60% of the pieces analysed. Based on environmental, cultural and ethnographic data, we discuss the role of the cave of Getahovit-2 and the mobility of the human groups who occupied it in the 5th millennium BC.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="439c6ccd11e02701a820d86841cf4fc5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:119561300,&quot;asset_id&quot;:125538363,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/119561300/download_file?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="125538363"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="125538363"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 125538363; 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</script> <div class="js-work-strip profile--work_container" data-work-id="111841332"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/111841332/A_GIS_for_the_analysis_of_obsidian_circulation_in_the_northern_near_east_during_prehistory"><img alt="Research paper thumbnail of A GIS for the analysis of obsidian circulation in the northern near east during prehistory" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/111841332/A_GIS_for_the_analysis_of_obsidian_circulation_in_the_northern_near_east_during_prehistory">A GIS for the analysis of obsidian circulation in the northern near east during prehistory</a></div><div class="wp-workCard_item"><span>HAL (Le Centre pour la Communication Scientifique Directe)</span><span>, Nov 1, 2004</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="111841332"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="111841332"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111841332; 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The results will be presented in two parts: the first part, this paper, deals with the presentation and characterization of obsidian outcrops in the southern Caucasus, while the second presents some results obtained from a selection of artefacts originating from different Armenian sites dated to between the Upper Palaeolithic and the Late Bronze Age. The same analytical method, LA-ICP-MS (laser ablation inductively coupled plasma mass spectrometry), has been used to characterize all the studied samples (both geological and archaeological). This method is more and more widely used to determine the elemental composition of obsidian artefacts, as it causes minimal damage to the studied objects. We present in this first part new geochemical analyses on geological obsidians originating from the southern Caucasus (Armenia, Georgia) and eastern Turkey. These data enhance our knowledge of the obsidian sources in these regions. A simple methodology, based on the use of three diagrams, is proposed to easily differentiate the deposits and to study the early exploitation of this material in the southern Caucasus.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="28ef40802b7df08a0617bbccc494df50" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:109256569,&quot;asset_id&quot;:111841331,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/109256569/download_file?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="111841331"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="111841331"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111841331; 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We present here the second part of this research, which deals with provenance studies of archaeological obsidians from Armenia. These new data enhance our knowledge of obsidian exploitation over a period of more than 14 000 years, from the Upper Palaeolithic to the Late Bronze Age. The proposed methodology shows that source attribution can be easily made by plotting element contents and element ratios on three simple binary diagrams. The same diagrams were used for source discrimination. As the southern Caucasus is a mountainous region for which the factor of distance as the crow flies cannot be applied, we have explored the capacity of the Geographic Information System to evaluate the nature and patterns of travel costs between the sources of obsidian and the archaeological sites. The role of the secondary obsidian deposits, which enabled the populations to acquire raw material at a considerable distance from the outcrops, is also considered.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="33a5ffdb7558f57d24844da4d777fec9" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:109256567,&quot;asset_id&quot;:111841329,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/109256567/download_file?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="111841329"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="111841329"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111841329; 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</script> <div class="js-work-strip profile--work_container" data-work-id="111841327"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/111841327/Pal%C3%A9olithique_moyen_de_la_haute_vall%C3%A9e_du_Kasakh_Arm%C3%A9nie_peuplement_de_montagne_et_exploitation_dobsidienne"><img alt="Research paper thumbnail of Paléolithique moyen de la haute vallée du Kasakh (Arménie) : peuplement de montagne et exploitation d&#39;obsidienne" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/111841327/Pal%C3%A9olithique_moyen_de_la_haute_vall%C3%A9e_du_Kasakh_Arm%C3%A9nie_peuplement_de_montagne_et_exploitation_dobsidienne">Paléolithique moyen de la haute vallée du Kasakh (Arménie) : peuplement de montagne et exploitation d&#39;obsidienne</a></div><div class="wp-workCard_item"><span>HAL (Le Centre pour la Communication Scientifique Directe)</span><span>, 2013</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">International audienc</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="111841327"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="111841327"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111841327; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="12729178" id="papers"><div class="js-work-strip profile--work_container" data-work-id="127736902"><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/127736902/The_South_Caucasus_from_the_Upper_Palaeolithic_to_the_Neolithic_Intersection_of_the_genetic_and_archaeological_data"><img alt="Research paper thumbnail of The South Caucasus from the Upper Palaeolithic to the Neolithic: Intersection of the genetic and archaeological data" class="work-thumbnail" src="https://attachments.academia-assets.com/121424545/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/127736902/The_South_Caucasus_from_the_Upper_Palaeolithic_to_the_Neolithic_Intersection_of_the_genetic_and_archaeological_data">The South Caucasus from the Upper Palaeolithic to the Neolithic: Intersection of the genetic and archaeological data</a></div><div class="wp-workCard_item"><span>Journal of Quaternary Science Reviews</span><span>, 2024</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The genomic characterisation of human remains and the study of archaeological assemblages are com...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The genomic characterisation of human remains and the study of archaeological assemblages are complementary keys to understanding the evolution of ancient human groups. This article proposes a dialogue between these two approaches for the South Caucasus between the Upper Palaeolithic and the Neolithic periods. In the Upper Palaeolithic before the Last Glacial Maximum (ca. 40.-23. ka cal BP), genetic and archaeological data demonstrate the originality of the populations of the South Caucasus (Caucasus_UP genome) compared with their neighbours in SE Europe and SW Asia and also show the existence of links between these different regions. For the post-LGM phase (ca. 20.9-11.7 ka cal BP), archaeological data suggest a certain continuity with the previous period during the cold phase of the Oldest Dryas, followed by a marked rapprochement with the Zarzian culture in the Zagros starting with the warming of the Bølling-Allerød. Genetic analyses, which are available only for the latter phase, reveal a new genome (Caucasus Hunter-Gatherer or CHG), that is very close to that of the ancestors of the Neolithic populations of the Zagros. For the Early Holocene (ca. 11.7-8.2 ka cal BP or 9700-6200 cal BCE), the CHG genome, which still characterises the populations of the South Caucasus, is difficult to distinguish in modelling from that of the Zagros (Iran_N). However, archaeological data suggest that the spread of the Iran_N/CHG gene pool from Iran to Upper Mesopotamia and Central Anatolia was due to populations from the northwest Zagros, and not to those from the South Caucasus, who had only occasional contacts with the Fertile Crescent. At the beginning of the Middle Holocene (ca. 8.2-7.2 ka cal BP or 6200-5200 cal BCE), the appearance in the South Caucasus of animals and plants presenting a high level of domestication, as well as the introduction of new techniques (pressure knapping with a lever, pottery), are clearly due to the arrival of populations from the Fertile Crescent, as confirmed by genetic analyses. These analyses also show that there was not a replacement of local Mesolithic communities by Neolithic farmers, which the archaeological evidence confirms.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="8288c2f4b6e48832023210ad37917259" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:121424545,&quot;asset_id&quot;:127736902,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/121424545/download_file?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="127736902"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127736902"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127736902; 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This article proposes a dialogue between these two approaches for the South Caucasus between the Upper Palaeolithic and the Neolithic periods. In the Upper Palaeolithic before the Last Glacial Maximum (ca. 40.-23. ka cal BP), genetic and archaeological data demonstrate the originality of the populations of the South Caucasus (Caucasus_UP genome) compared with their neighbours in SE Europe and SW Asia and also show the existence of links between these different regions. For the post-LGM phase (ca. 20.9-11.7 ka cal BP), archaeological data suggest a certain continuity with the previous period during the cold phase of the Oldest Dryas, followed by a marked rapprochement with the Zarzian culture in the Zagros starting with the warming of the Bølling-Allerød. Genetic analyses, which are available only for the latter phase, reveal a new genome (Caucasus Hunter-Gatherer or CHG), that is very close to that of the ancestors of the Neolithic populations of the Zagros. For the Early Holocene (ca. 11.7-8.2 ka cal BP or 9700-6200 cal BCE), the CHG genome, which still characterises the populations of the South Caucasus, is difficult to distinguish in modelling from that of the Zagros (Iran_N). However, archaeological data suggest that the spread of the Iran_N/CHG gene pool from Iran to Upper Mesopotamia and Central Anatolia was due to populations from the northwest Zagros, and not to those from the South Caucasus, who had only occasional contacts with the Fertile Crescent. At the beginning of the Middle Holocene (ca. 8.2-7.2 ka cal BP or 6200-5200 cal BCE), the appearance in the South Caucasus of animals and plants presenting a high level of domestication, as well as the introduction of new techniques (pressure knapping with a lever, pottery), are clearly due to the arrival of populations from the Fertile Crescent, as confirmed by genetic analyses. These analyses also show that there was not a replacement of local Mesolithic communities by Neolithic farmers, which the archaeological evidence confirms.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e1248b4c4f10f104b8817eb4ec9421ee" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:121369375,&quot;asset_id&quot;:127669939,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/121369375/download_file?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="127669939"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="127669939"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 127669939; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="126611827"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/126611827/Environments_and_Societies_in_the_Southern_Caucasus_during_the_Holocene"><img alt="Research paper thumbnail of Environments and Societies in the Southern Caucasus during the Holocene" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/126611827/Environments_and_Societies_in_the_Southern_Caucasus_during_the_Holocene">Environments and Societies in the Southern Caucasus during the Holocene</a></div><div class="wp-workCard_item"><span>Quaternary International</span><span>, Feb 1, 2016</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="126611827"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="126611827"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 126611827; 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We present here the second part of this research, which deals with provenance studies of archaeological obsidians from Armenia. These new data enhance our knowledge of obsidian exploitation over a period of more than 14 000 years, from the Upper Palaeolithic to the Late Bronze Age. The proposed methodology shows that source attribution can be easily made by plotting element contents and element ratios on three simple binary diagrams. The same diagrams were used for source discrimination. As the southern Caucasus is a mountainous region for which the factor of distance as the crow flies cannot be applied, we have explored the capacity of the Geographic Information System to evaluate the nature and patterns of travel costs between the sources of obsidian and the archaeological sites. The role of the secondary obsidian deposits, which enabled the populations to acquire raw material at a considerable distance from the outcrops, is also considered.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="207ea6855204e7b676dda131ba8daa0d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:120150945,&quot;asset_id&quot;:126244296,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/120150945/download_file?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="126244296"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="126244296"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 126244296; 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$(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="126244116"><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/126244116/NEW_DATA_ON_THE_EXPLOITATION_OF_OBSIDIAN_IN_THE_SOUTHERN_CAUCASUS_ARMENIA_GEORGIA_AND_EASTERN_TURKEY_PART_1_SOURCE_CHARACTERIZATION"><img alt="Research paper thumbnail of NEW DATA ON THE EXPLOITATION OF OBSIDIAN IN THE SOUTHERN CAUCASUS (ARMENIA, GEORGIA) AND EASTERN TURKEY, PART 1: SOURCE CHARACTERIZATION" 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/126244116/NEW_DATA_ON_THE_EXPLOITATION_OF_OBSIDIAN_IN_THE_SOUTHERN_CAUCASUS_ARMENIA_GEORGIA_AND_EASTERN_TURKEY_PART_1_SOURCE_CHARACTERIZATION">NEW DATA ON THE EXPLOITATION OF OBSIDIAN IN THE SOUTHERN CAUCASUS (ARMENIA, GEORGIA) AND EASTERN TURKEY, PART 1: SOURCE CHARACTERIZATION</a></div><div class="wp-workCard_item"><span>Archaeometry</span><span>, 2014</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A large analytical programme involving both obsidian source characterization and obsidian artefac...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">A large analytical programme involving both obsidian source characterization and obsidian artefact sourcing was initiated recently within the framework of the French archaeological mission &#39;Caucasus&#39;. The results will be presented in two parts: the first part, this paper, deals with the presentation and characterization of obsidian outcrops in the southern Caucasus, while the second presents some results obtained from a selection of artefacts originating from different Armenian sites dated to between the Upper Palaeolithic and the Late Bronze Age. The same analytical method, LA-ICP-MS (laser ablation inductively coupled plasma mass spectrometry), has been used to characterize all the studied samples (both geological and archaeological). This method is more and more widely used to determine the elemental composition of obsidian artefacts, as it causes minimal damage to the studied objects. We present in this first part new geochemical analyses on geological obsidians originating from the southern Caucasus (Armenia, Georgia) and eastern Turkey. These data enhance our knowledge of the obsidian sources in these regions. A simple methodology, based on the use of three diagrams, is proposed to easily differentiate the deposits and to study the early exploitation of this material in the southern Caucasus.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="6b8f474017705bb6b2ef162b54bb7cb1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:120150663,&quot;asset_id&quot;:126244116,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/120150663/download_file?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="126244116"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="126244116"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 126244116; 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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="125538363"><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/125538363/Diachronic_variability_in_obsidian_procurement_patterns_and_the_role_of_the_cave_sheepfold_of_Getahovit_2_NE_Armenia_during_the_Chalcolithic_period"><img alt="Research paper thumbnail of Diachronic variability in obsidian procurement patterns and the role of the cave-sheepfold of Getahovit-2 (NE Armenia) during the Chalcolithic period" class="work-thumbnail" src="https://attachments.academia-assets.com/119561300/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/125538363/Diachronic_variability_in_obsidian_procurement_patterns_and_the_role_of_the_cave_sheepfold_of_Getahovit_2_NE_Armenia_during_the_Chalcolithic_period">Diachronic variability in obsidian procurement patterns and the role of the cave-sheepfold of Getahovit-2 (NE Armenia) during the Chalcolithic period</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/cchataigner">christine chataigner</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://sci.academia.edu/RomanHovsepyan">Roman Hovsepyan</a></span></div><div class="wp-workCard_item"><span>Quaternary International</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The cave of Getahovit-2 is situated in north-eastern Armenia, in the foothills of the Lesser Cauc...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The cave of Getahovit-2 is situated in north-eastern Armenia, in the foothills of the Lesser Caucasus which dominate the valley of the Kura. The excavations (2011–2017), carried out by the Armenian-French mission ‘Caucasus’, have revealed several phases of occupation – Upper Palaeolithic (ca 22,000 cal BC), Chalcolithic (ca. 4700-4050 cal BC), and early Middle Ages (ca. 900–1200 cal AD). Although the cave is near outcroppings of flint (lower valley of the Aghstev river), the artifacts found there are mainly in obsidian, whatever the period of occupation. During the Chalcolithic period (levels IV-III), the cave served as a shelter for herds, as seen in the succession of coprolite deposits, that were regularly burned to clean the floor of the cave. The origin of the populations that sheltered their herds in this cave is difficult to determine. LA-ICP-MS analyses have been carried out to study the provenance of the obsidian artifacts found in level III. Corroborated by the techno-typological study of the artifacts, they have enabled the differentiation of two assemblages: the first, coming from deposits situated on Armenian territory (Geghasar, Gutansar, Arteni, Tsaghkunyats) and consisting of blanks knapped by percussion (flakes above all), and the second coming from deposits situated in Georgia (Chikiani) or Turkey (region of Sarıkamış) and consisting of pressure-flaked blades. In the lower part of level III (ca 4700-4400 cal BC), the provenance of the obsidian (mainly Gutansar) suggests links with the south, the Ararat plain. For the upper part of level III (ca. 4400-4050 cal BC), it is the outcrops situated farther north (Tsaghkunyats) that were the origin of almost 60% of the pieces analysed. Based on environmental, cultural and ethnographic data, we discuss the role of the cave of Getahovit-2 and the mobility of the human groups who occupied it in the 5th millennium BC.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="439c6ccd11e02701a820d86841cf4fc5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:119561300,&quot;asset_id&quot;:125538363,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/119561300/download_file?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="125538363"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="125538363"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 125538363; 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</script> <div class="js-work-strip profile--work_container" data-work-id="111841332"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/111841332/A_GIS_for_the_analysis_of_obsidian_circulation_in_the_northern_near_east_during_prehistory"><img alt="Research paper thumbnail of A GIS for the analysis of obsidian circulation in the northern near east during prehistory" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/111841332/A_GIS_for_the_analysis_of_obsidian_circulation_in_the_northern_near_east_during_prehistory">A GIS for the analysis of obsidian circulation in the northern near east during prehistory</a></div><div class="wp-workCard_item"><span>HAL (Le Centre pour la Communication Scientifique Directe)</span><span>, Nov 1, 2004</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="111841332"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="111841332"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111841332; 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The results will be presented in two parts: the first part, this paper, deals with the presentation and characterization of obsidian outcrops in the southern Caucasus, while the second presents some results obtained from a selection of artefacts originating from different Armenian sites dated to between the Upper Palaeolithic and the Late Bronze Age. The same analytical method, LA-ICP-MS (laser ablation inductively coupled plasma mass spectrometry), has been used to characterize all the studied samples (both geological and archaeological). This method is more and more widely used to determine the elemental composition of obsidian artefacts, as it causes minimal damage to the studied objects. We present in this first part new geochemical analyses on geological obsidians originating from the southern Caucasus (Armenia, Georgia) and eastern Turkey. These data enhance our knowledge of the obsidian sources in these regions. A simple methodology, based on the use of three diagrams, is proposed to easily differentiate the deposits and to study the early exploitation of this material in the southern Caucasus.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="28ef40802b7df08a0617bbccc494df50" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:109256569,&quot;asset_id&quot;:111841331,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/109256569/download_file?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="111841331"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="111841331"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111841331; 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window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=111841330]").text(description); $(".js-view-count[data-work-id=111841330]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 111841330; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='111841330']"); 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></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.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); 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We present here the second part of this research, which deals with provenance studies of archaeological obsidians from Armenia. These new data enhance our knowledge of obsidian exploitation over a period of more than 14 000 years, from the Upper Palaeolithic to the Late Bronze Age. The proposed methodology shows that source attribution can be easily made by plotting element contents and element ratios on three simple binary diagrams. The same diagrams were used for source discrimination. As the southern Caucasus is a mountainous region for which the factor of distance as the crow flies cannot be applied, we have explored the capacity of the Geographic Information System to evaluate the nature and patterns of travel costs between the sources of obsidian and the archaeological sites. 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</script> <div class="js-work-strip profile--work_container" data-work-id="111841327"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/111841327/Pal%C3%A9olithique_moyen_de_la_haute_vall%C3%A9e_du_Kasakh_Arm%C3%A9nie_peuplement_de_montagne_et_exploitation_dobsidienne"><img alt="Research paper thumbnail of Paléolithique moyen de la haute vallée du Kasakh (Arménie) : peuplement de montagne et exploitation d&#39;obsidienne" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/111841327/Pal%C3%A9olithique_moyen_de_la_haute_vall%C3%A9e_du_Kasakh_Arm%C3%A9nie_peuplement_de_montagne_et_exploitation_dobsidienne">Paléolithique moyen de la haute vallée du Kasakh (Arménie) : peuplement de montagne et exploitation d&#39;obsidienne</a></div><div class="wp-workCard_item"><span>HAL (Le Centre pour la Communication Scientifique Directe)</span><span>, 2013</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">International audienc</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="111841327"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="111841327"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 111841327; 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