Seasonal variation in alkenones, bulk suspended POM, plankton and temperature in Monterey Bay, California: implications for carbon cycling and climate assessment
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作者:
Bac, MG
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机构:Indiana Univ, Dept Geol Sci, Biogeochem Labs, Bloomington, IN 47405 USA
Bac, MG
Buck, KR
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机构:Indiana Univ, Dept Geol Sci, Biogeochem Labs, Bloomington, IN 47405 USA
Buck, KR
Chavez, FP
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机构:Indiana Univ, Dept Geol Sci, Biogeochem Labs, Bloomington, IN 47405 USA
Chavez, FP
Brassell, SC
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Indiana Univ, Dept Geol Sci, Biogeochem Labs, Bloomington, IN 47405 USAIndiana Univ, Dept Geol Sci, Biogeochem Labs, Bloomington, IN 47405 USA
Brassell, SC
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机构:
[1] Indiana Univ, Dept Geol Sci, Biogeochem Labs, Bloomington, IN 47405 USA
[2] Monterey Bay Aquarium Res Inst, Moss Landing, CA 95039 USA
[3] Stanford Univ, Geol & Environm Sci Dept, Stanford, CA 94305 USA
The utility of alkenone abundance and U-37(K') ratios as proxies for haptophyte productivity and temperature variations, respectively, was examined in an upwelling setting by comparison of alkenones with other environmental variables including carbon concentrations, plankton populations, productivity, and temperature. Suspended particulate organic material (SPOM) was collected from surface waters (1-5 m) in Monterey Bay, California during the 1992 El Nino. Haptophyte algae comprise a small but significant fraction of the plankton assemblage (0.5-30%). In this upwelling environment either the haptophytes contain low cellular abundances of alkenones (0.4-5% C-org) and/or alkenone producers are weakly represented among their populations. The U-37(K')-temperature relationship for SPOM exhibits a better correlation (r(2) = 0.870; n = 8) during periods of active upwelling and in the winter than throughout the entire annual cycle (r(2) = 0.308; n = 18). The alkenone-based temperatures also suggest, as observed elsewhere, that these compounds originated in colder waters at depth and were subsequently transferred to surface waters. (C) 2003 Elsevier Science Ltd. All rights reserved.