Carbon export buffering and CO2 drawdown by flexible phytoplankton C:N:P under glacial conditions
Modern observations indicate that variations in marine phytoplankton stoichiometry correlate with the boundaries of major surface waters. For example, phytoplankton in the oligotrophic subtropical gyres typically have much higher C:N:P ratios (i.e., higher C:P and higher N:P ratios) than those in eu...
| Príomhchruthaitheoirí: | , , |
|---|---|
| Formáid: | Journal article |
| Teanga: | English |
| Foilsithe / Cruthaithe: |
Wiley
2020
|