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Development of the California Current during the past 12,000 yr based on diatoms and silicoflagellates

Palaeogeography, Palaeoclimatology, Palaeoecology
By:  and 
https://doi.org/10.1016/j.palaeo.2006.12.009

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Abstract

Detailed diatom and silicoflagellates records in three cores from the offshore region of southern Oregon to central California reveal the evolution of the northern part of the California Current during the past 12,000 yr. The early Holocene, prior to ∼ 9 ka, was characterized by relatively warm sea surface temperatures (SST), owing to enhanced northerly flow of the subtropical waters comparable to the modern Davidson Current. Progressive strengthening of the North Pacific High lead to intensification of the southward flow of the California Current at ∼ 8 ka, resulting in increased coastal upwelling and relatively cooler SST which persisted until ∼ 5 ka. Reduced southward flow of the California Current between ∼ 4.8 ka and 3.6 ka may have been responsible for a period of decreased upwelling. Modern seasonal oceanographic cycles, as evidenced by increased spring–early summer coastal upwelling and warming of early fall SST evolved between 3.5 and 3.2 ka. Widespread occurrence of paleoceanographic and paleoclimatic change between ∼ 3.5–3.0 ka along the eastern margins of the North Pacific was likely a response to increasing ENSO variability in the tropical Pacific.

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Publication type Article
Publication Subtype Journal Article
Title Development of the California Current during the past 12,000 yr based on diatoms and silicoflagellates
Series title Palaeogeography, Palaeoclimatology, Palaeoecology
DOI 10.1016/j.palaeo.2006.12.009
Volume 248
Issue 3-4
Year Published 2007
Language English
Publisher Elsevier
Contributing office(s) Volcano Science Center
Description 26 p.
First page 313
Last page 338
Country United States
State California, Oregon
Online Only (Y/N) N
Additional Online Files (Y/N) N
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