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- W2079135598 abstract "Particulate carbonate was concentrated with a flow centrifuge out of the waters from a coccolithophore bloom in the Gulf of Maine for δ18OCaCO3 measurement. The particulate samples were composed of diverse organic materials, but most samples were observed to be dominated by Emiliana huxleyi CaCO3. The oxygen isotopic fractionation associated with these E. huxleyi populations were determined by comparing oxygen isotope ratios in coccoliths with those of anbient waters at the time of collection. The observed isotopic fractionations were large (up to 2.8%), but did not match well with the expected values based on previous laboratory experiments. The temperatures calculated from the isotopic values of surface samples averaged 7.4°C cooler than the waters from which this carbonate was collected. These discrepancies may indicate that the coccoliths were precipatated in cooler water 10–20 m below the surface waters were they were captured, or that the waters had warmed since the coccoliths grew." @default.
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- W2079135598 date "1994-01-01" @default.
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- W2079135598 title "Oxygen isotopic disequilibrium in coccolith carbonate from phytoplankton blooms" @default.
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- W2079135598 doi "https://doi.org/10.1016/0967-0637(94)90034-5" @default.
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