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Late Holocene Sea Temperatures along the Central California Coast

Published online by Cambridge University Press:  20 January 2017

Terry L. Jones  and
Douglas J. Kennett
Terry L. Jones
Affiliation:
Department of Social Sciences, California Polytechnic State University, San Luis Obispo, California, 93407
Douglas J. Kennett
Affiliation:
Department of Anthropology, California State University, Long Beach, California, 90840
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Abstract

Mussel shells from central California coastal archaeological sites record changes in sea surface temperatures in the past 2000 years. Water temperatures, inferred from oxygen isotopes in the shells, were about 1°C cooler than present and stable between 2000 and 700 yr ago. Between about 700 and 500 yr ago, seasonal variation was greater than present, with extremes above and below historic levels. Water temperatures were 2–3°C cooler than today 500–300 yr ago. The interval of variable sea temperatures 700–500 yr ago partially coincided with an interval of drought throughout central California. A coincident disruption in human settlement along the coast suggests movements of people related to declining water sources. Quantities of fish bone in central coast middens dating to this same period are high relative to other periods, and the remains of northern anchovies, a species sensitive to changing oceanographic conditions, are also abundant. The continued use of local fisheries suggests that changes in settlement and diet were influenced more by drought than by a decrease in marine productivity, as fish provided a staple during an interval of low terrestrial productivity.

Keywords

California coastsea temperaturesdroughtEl Niñooxygen isotopesprehistoryfish
Type
Original Articles
Information
Quaternary Research , Volume 51 , Issue 1 , January 1999 , pp. 74 - 82
Copyright
University of Washington

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