Carbon isotope ratio of marine plankton related to surface water masses

Mathematics – Logic

Scientific paper

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Scientific paper

Carbon isotopic ratios of plankton organic tissue present no linear relationship with seawater temperature, salinity or CO2 partial pressure such as reported for phytoplankton cultures and previous studies of natural plankton δ13C variations. However, the isotopic composition of plankton organic carbon is characteristic of a well-defined surface water mass and changes from one water mass to another, recording hydrologic discontinuities.

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