Geological Society of America

T111 The Context of Our Origins: Geological Studies of Old World Fossil Primate and Hominin Sites

Monday, 26 September 2016
8:00 AM - 12:00 PM
Room 401

CLIMATE IMPACT ON HUMAN BEHAVIOR IN THE UPPER PALEOLITHIC OF THE ARMENIAN HIGHLANDS

Paper number: T111-14
Program: Technical Sessions
Time: 11:10 AM – 11:25 AM

Authors

Alex Brittingham Presenting Author
Univeristy of Connecticut, Storrs, CT
Michael T. Hren
University of Connecticut, Storrs, CT
Andrew W. Kandel
“The Role of Culture in Early Expansions of Humans” at the University of Tübingen, Tübingen
Ellery Frahm
University of Minnesota, Minneapolis, MN
Boris Gasparyan
National Academy of Sciences of Armenia, Yerevan
Gideon Hartman
Univeristy of Connecticut, Storrs, CT

Abstract

During the Late Pleistocene, modern humans expanded out of Africa and inhabited Eurasia for the first time. To better understand the context of this process in the Armenian Highlands and determine how climate affected the behavior of these early modern humans, we collected sediments from the Upper Paleolithic archaeological cave site Aghitu-3. This is the first stratified Upper Paleolithic cave in Armenia, which includes two main occupational phases. Sediments within the cave are well dated, and span from 40 ka cal BP to 24 ka cal BP. We analyzed hydrogen isotope (δD) values of higher plant-derived biomarkers (n-alkanes) to assess changes in local hydrology associated with human occupation at the site. δD values from n-alkanes at Aghitu-3 are more positive during the early occupation phase, indicating a general warming trend beginning around 36 ka cal BP and reaching a peak around 31 ka cal BP. Following this, there is a general negative trend in δD values during the late occupation phase from 31 ka cal BP to 24 ka cal BP, leading up to the Last Glacial Maximum. Stone tool technology remains relatively unchanged over time; however, occupation density is much higher during the colder phase of occupation. Sourced obsidian indicates that during the warmer occupation phase, lithic raw material was exclusively regional, limited to Syunik sources a maximum of 40 km away from the site. During the colder phase of occupation more exotic sources are present at Aghitu-3, including obsidian coming from up to 300 km away in northwest Armenia and eastern Turkey, showing either an increase in group mobility or exchange of artifacts.

Geological Society of America Abstracts with Programs. Vol. 48, No. 7

doi: 10.1130/abs/2016AM-282528

© Copyright 2016 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.