Fig. 4: Time series of flow cytometry-derived, euphotic zone integrated phytoplankton carbon biomass (g m−2) and phytoplankton growth rates.
From: Adaptive carbon export response to warming in the Sargasso Sea
A Biomass of cyanobacteria Prochlorococcus and Synechococcus; B biomass of picoeukaryotes and nanoeukaryotes; C total phytoplankton carbon biomass derived from the product of bulk POC:Chl slope and integrated Chl, and summed flow cytometry-derived carbon biomass estimates. D Phytoplankton growth rates estimated by dividing integrated in situ primary production by the two estimates of phytoplankton carbon biomass as described in (C).
