Linkages between dynamic phytoplankton C:N:P and the ocean carbon cycle under climate change
Modelers of global ocean biogeochemistry are beginning to represent a phenomenon that biologists have long observed in laboratory and field settings: that the elemental stoichiometry of phytoplankton is quite flexible. Today, it is well recognized that the C:N:P ratio in phytoplankton and particulat...
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Fformat: | Journal article |
Iaith: | English |
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Oceanography Society
2020
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