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Dating Human Occupation on Diatom-Phytolith-Rich Sediment: Case Studies of Mustang Spring and Lubbock Lake, Texas, USA

Published online by Cambridge University Press:  18 July 2016

Christine Hatté ,
Gregory Hodgins ,
Vance T Holliday  and
A J Timothy Jull
Christine Hatté*
Affiliation:
Laboratoire des Sciences du Climat et de l'Environnement, UMR CEA-CNRS-UVSQ 1572, Domaine du CNRS, bâtiment 12, F-91198 Gif-sur-Yvette Cedex, France
Gregory Hodgins
Affiliation:
NSF-Arizona AMS Laboratory, Physics Building, University of Arizona, Tucson, Arizona 85721, USA
Vance T Holliday
Affiliation:
Department of Anthropology, University of Arizona, Tucson, Arizona 85721, USA Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA
A J Timothy Jull
Affiliation:
NSF-Arizona AMS Laboratory, Physics Building, University of Arizona, Tucson, Arizona 85721, USA Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA
*
Corresponding author. Email: [email protected].
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Abstract

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The Great Plains of North America have a rich archaeological record that spans the period from Late Glacial to Historic times, a period that also witnessed significant changes in climate and ecology. Chronometric dating of archaeological sites in many areas of the Great Plains, however, is often problematic, largely because charcoal and wood—the preferred materials for radiocarbon dating—are scarce in this grassland environment with few trees. Two reference archaeological sites are studied here: Mustang Spring and Lubbock Lake, Texas, USA. We carry out a geochronological approach based on a cross-study of carbon-derived data: combustion yield, δ13C, 14C age differences between high temperature and low temperature released carbon, and the 14C age itself. A study that incorporates multiple approaches is required to solve issues induced by the sedimentological context, which is rich in both freshwater diatoms and phytoliths from quite different origins. Analysis of carbon-derived data allows us to draw a succession model of dry and wet episodes and to associate it with a chronological framework. In this way, we can assert that, for the Mustang Spring site, several human occupations existed from ∼11 kyr BP to ∼8.7 kyr BP along the 110-cm-long series with an interruption of ∼150 yr that is associated with a palustrine environment between the Plainview and Firstview occupations.

Type
Archaeology
Information
Radiocarbon , Volume 52 , Issue 1 , 2010 , pp. 13 - 24
Copyright
Copyright © 2010 by the Arizona Board of Regents on behalf of the University of Arizona 

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