Palaeoenvironmental and chronological context of hominin occupations of the Armenian Highlands during MIS 3: Evidence from Ararat-1 cave

  1. Jennifer E. Sherriff
  2. Artur Petrosyan
  3. Dominik Rogall
  4. David Nora
  5. Ellery Frahm
  6. Tobias Lauer
  7. Theodoros Karambaglidis
  8. Monika V. Knul
  9. Delphine Vettese
  10. Dmitri Arakelyan
  11. Shira Gur-Arieh
  12. Paloma Vidal-Matutano 1
  13. Jacob Morales
  14. Helen Fewlass
  15. Simon P.E. Blockley
  16. Rhys Timms
  17. Ani Adigyozalyan
  18. Hayk Haydosyan
  19. Phil Glauberman
  20. Boris Gasparyan
  21. Ariel Malinsky-Buller
  1. 1 Universidad de La Laguna
    info

    Universidad de La Laguna

    San Cristobal de La Laguna, España

    ROR https://ror.org/01r9z8p25

Revista:
Quaternary Science Advances

ISSN: 2666-0334

Año de publicación: 2024

Volumen: 13

Páginas: 100122

Tipo: Artículo

DOI: 10.1016/J.QSA.2023.100122 GOOGLE SCHOLAR lock_openAcceso abierto editor

Otras publicaciones en: Quaternary Science Advances

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Resumen

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.