As a first-order approximation, we can assume that the diel signal of POC can be attributed exclusively to changes in phytoplankton carbon, with microheterotroph and detrital pools independent of time. Then, the phytoplankton carbon pool size will be determined by: dP/dt=(prg) P (1) ...
CITATION STYLE
Geider, R. J. (1992). Respiration: Taxation Without Representation? In Primary Productivity and Biogeochemical Cycles in the Sea (pp. 333–360). Springer US. https://doi.org/10.1007/978-1-4899-0762-2_19
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