2 D3. Advances in Geoarchaeology
Monday, 26 October 2020
1:30 PM - 5:30 PM
Meeting Rooms
QUANTIFYING THE SCALE OF AGE MIXING OF HOLOCENE MOLLUSK ASSEMBLAGES FROM IFRI OUDADANE ARCHEOLOGICAL SITE, MOROCCO, NW AFRICA
Paper number: 2-13
Program: Technical Sessions
Time: 4:00 PM – 4:10 PM
Authors
-
Yurena YanesUniversity of Cincinnati, Cincinnati, OH
-
Jörg LinstädterKommission für Archäologie Außereuropäischer Kulturen (KAAK), Bonn
-
Rainer HuttererZoologisches Forschungsmuseum Alexander Koenig, Bonn
Abstract
The coastal Mediterranean site in Northeast Morocco, Ifri Oudadane embraces a rare relatively continuous Holocene archeological succession with extensive accumulations of harvested marine shells that provide key clues into past subsistence strategies and paleoclimate. Stratigraphic evidence suggests two main cultural periods, Epipaleolithic (pre-food production) and Neolithic (post-food production), which is further subdivided into Early Neolithic A, B, and C. In the current work, numerous harvested shells of the topshell Phorcus turbinatus (Gastropoda:Trocoidea) were radiocarbon dated using the cost effective, novel carbonate-target radiocarbon dating method to assess the chronology and quantify the degree of age mixing for these mollusk assemblages. Results from this study indicate that calcitic and aragonitic layers of the same shell yielded statistically equivalent ages, and therefore, both minerals can be used for radiocarbon dating when pristinely preserved. Uncalibrated radiocarbon results retrieved from the same archeological phases suggest that harvested shells exhibit multi-centennial age mixing (between 300 to 700 14C years) that could not be explained by analytical imprecisions alone. This research is the first to illustrate the multi-centennial scale of time-averaging in Ifri Oudadane mollusk assemblages and suggest the need for individually dating specimens in future paleoclimate investigations.
Geological Society of America Abstracts with Programs. Vol. 52, No. 6
doi: 10.1130/abs/2020AM-355557
© Copyright 2020 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.