TY - JOUR
T1 - Palaeoenvironmental and chronological context of hominin occupations of the Armenian Highlands during MIS 3
T2 - Evidence from Ararat-1 cave
AU - Sherriff, Jennifer E.
AU - Petrosyan, Artur
AU - Rogall, Dominik
AU - Nora, David
AU - Frahm, Ellery
AU - Lauer, Tobias
AU - Karambaglidis, Theodoros
AU - Knul, Monika V.
AU - Vettese, Delphine
AU - Arakelyan, Dmitri
AU - Gur-Arieh, Shira
AU - Vidal-Matutano, Paloma
AU - Morales, Jacob
AU - Fewlass, Helen
AU - Blockley, Simon P.E.
AU - Timms, Rhys
AU - Adigyozalyan, Ani
AU - Haydosyan, Hayk
AU - Glauberman, Phil
AU - Gasparyan, Boris
AU - Malinsky-Buller, Ariel
N1 - Funding Information:
This research was funded by The Gerda Henkel Stiftung grant ( n. AZ 10_V_17 and n. AZ 23/F/19 ), the Fritz- Thyssen Foundation grant awarded for the project “Pleistocene Hunter-Gatherer Lifeways and Population Dynamics in the Ararat (paleo-lake) Depression, Armenia”, and The European Research Council grant N 948015 : “Investigating Pleistocene population dynamics in the Southern Caucasus” (awarded to AMB). Further support was provided by Gfoeller Renaissance Foundation (USA) and “Areni-1 Cave” Consortium ( “Areni-1 Cave” Scientific-Research Foundation (Armenia) and the Institute of Archaeology and Ethnography of the National Academy of Sciences of the Republic of Armenia , the Gfoeller Renaissance Foundation , the Leakey Foundation and the Leverhulme Trust-funded Palaeolithic Archaeology, Geochronology, and Environments of the Southern Caucasus (PAGES) project ( RPG-2016-102 ). We kindly thank the following individuals: Hovik Partevyan and the Partevyan Family, Suren Kesejyan, Pavel Avetisyan, Director of the Institute of Archaeology and Ethnography of the National Academy of Sciences of the Republic of Armenia, Paul Lincoln and George Biddulph.
Funding Information:
This research was funded by The Gerda Henkel Stiftung grant (n. AZ 10_V_17 and n. AZ 23/F/19), the Fritz- Thyssen Foundation grant awarded for the project “Pleistocene Hunter-Gatherer Lifeways and Population Dynamics in the Ararat (paleo-lake) Depression, Armenia”, and The European Research Council grant N 948015: “Investigating Pleistocene population dynamics in the Southern Caucasus” (awarded to AMB). Further support was provided by Gfoeller Renaissance Foundation (USA) and “Areni-1 Cave” Consortium (“Areni-1 Cave” Scientific-Research Foundation (Armenia) and the Institute of Archaeology and Ethnography of the National Academy of Sciences of the Republic of Armenia, the Gfoeller Renaissance Foundation, the Leakey Foundation and the Leverhulme Trust-funded Palaeolithic Archaeology, Geochronology, and Environments of the Southern Caucasus (PAGES) project (RPG-2016-102). We kindly thank the following individuals: Hovik Partevyan and the Partevyan Family, Suren Kesejyan, Pavel Avetisyan, Director of the Institute of Archaeology and Ethnography of the National Academy of Sciences of the Republic of Armenia, Paul Lincoln and George Biddulph.
Publisher Copyright:
© 2023 The Authors
PY - 2024/1
Y1 - 2024/1
N2 - Archaeological and palaeoenvironmental evidence from the Armenian Highlands and wider southern Caucasus region emphasises the significance of Marine Oxygen Isotope Stage 3 (c. 57–29 ka) as a crucial period for understanding hominin behaviours amidst environmental fluctuations. Ararat-1 cave, situated in the Ararat Depression, Republic of Armenia, presents potential for resolving emerging key debates regarding hominin land use adaptations during this interval, due to its well-preserved lithic artefacts and faunal assemblages. We present the first results of combined sedimentological, geochronological (luminescence and radiocarbon), archaeological and palaeoecological (macrofauna, microfauna and microcharcoal) study of the Ararat-1 sequence. We demonstrate sediment accumulation occurred between 52 and 35 ka and was caused by a combination of aeolian activity, cave rockfall and water action. Whilst the upper strata of the Ararat-1 sequence experienced post-depositional disturbance due to faunal and anthropogenic processes, the lower strata remain relatively undisturbed. We suggest that during a stable period within MIS 3, Ararat-1 was inhabited by Middle Palaeolithic hominins amidst a mosaic of semi-arid shrub, grassland, and temperate woodland ecosystems. These hominins utilised local and distant toolstone raw materials, indicating their ability to adapt to diverse ecological and elevation gradients. Through comparison of Ararat-1 with other sequences in the region, we highlight the spatial variability of MIS 3 environments and its on hominin land use adaptations. This demonstrates the importance of the Armenian Highlands for understanding regional MP settlement dynamics during a critical period of hominin dispersals and evolution.
AB - Archaeological and palaeoenvironmental evidence from the Armenian Highlands and wider southern Caucasus region emphasises the significance of Marine Oxygen Isotope Stage 3 (c. 57–29 ka) as a crucial period for understanding hominin behaviours amidst environmental fluctuations. Ararat-1 cave, situated in the Ararat Depression, Republic of Armenia, presents potential for resolving emerging key debates regarding hominin land use adaptations during this interval, due to its well-preserved lithic artefacts and faunal assemblages. We present the first results of combined sedimentological, geochronological (luminescence and radiocarbon), archaeological and palaeoecological (macrofauna, microfauna and microcharcoal) study of the Ararat-1 sequence. We demonstrate sediment accumulation occurred between 52 and 35 ka and was caused by a combination of aeolian activity, cave rockfall and water action. Whilst the upper strata of the Ararat-1 sequence experienced post-depositional disturbance due to faunal and anthropogenic processes, the lower strata remain relatively undisturbed. We suggest that during a stable period within MIS 3, Ararat-1 was inhabited by Middle Palaeolithic hominins amidst a mosaic of semi-arid shrub, grassland, and temperate woodland ecosystems. These hominins utilised local and distant toolstone raw materials, indicating their ability to adapt to diverse ecological and elevation gradients. Through comparison of Ararat-1 with other sequences in the region, we highlight the spatial variability of MIS 3 environments and its on hominin land use adaptations. This demonstrates the importance of the Armenian Highlands for understanding regional MP settlement dynamics during a critical period of hominin dispersals and evolution.
KW - Armenia
KW - Faunal analysis
KW - Geoarchaeology
KW - Geochronology
KW - Middle Palaeolithic
KW - MIS 3
UR - http://www.scopus.com/inward/record.url?scp=85176246037&partnerID=8YFLogxK
U2 - 10.1016/j.qsa.2023.100122
DO - 10.1016/j.qsa.2023.100122
M3 - Article
AN - SCOPUS:85176246037
SN - 2666-0334
VL - 13
JO - Quaternary Science Advances
JF - Quaternary Science Advances
M1 - 100122
ER -