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HOLOCENE ENVIRONMENTAL CHANGE RECORDED IN LAGOONAL SEDIMENT PROXIES AT HUACA PRIETA, NORTH COASTAL PERU

This study attempts to define the early to mid-Holocene paleoenvironment at Huaca Prieta, an archaeological site on the north coast of Peru, through a combination of sedimentological, paleoecological, and stable isotope analyses. This research is part of a larger collaborative study drawing on many disciplines, and the interpretations of the results presented here are solely from a geological perspective. Multiple studies point to a severely diminished or even absent El Niño in the region during the mid-Holocene, but the Chicama River valley is a relatively unstudied location. Sediment coring from the upper 6 m reveals laminated to thinly bedded carbonates, organic sediments, and fine-grained clays deposited within larger intervals of sands and silts. These finer-grained sediments evidence a coastal lagoon 3 km in length which existed approximately 7300-6200 cal ybp. Stratigraphic analysis of the upper 6 m of sediments reveals a marked decrease in siliciclastic material delivered to the floodplain during this time, with potential implications for the mid-Holocene El Niño frequency debate and human-environment linkages during this time.

Identiferoai:union.ndltd.org:VANDERBILT/oai:VANDERBILTETD:etd-07132011-113921
Date11 August 2011
CreatorsBeavins Tracy, Rachel Anne
ContributorsLarisa DeSantis, Steven Goodbred
PublisherVANDERBILT
Source SetsVanderbilt University Theses
LanguageEnglish
Detected LanguageEnglish
Typetext
Formatapplication/pdf
Sourcehttp://etd.library.vanderbilt.edu/available/etd-07132011-113921/
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