Deep Chlorophyll Maxima in the Global Ocean: Occurrences, Drivers and Characteristics.
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ABSTRACT: Stratified oceanic systems are characterized by the presence of a so-called Deep Chlorophyll a Maximum (DCM) not detectable by ocean color satellites. A DCM can either be a phytoplankton (carbon) biomass maximum (Deep Biomass Maximum, DBM), or the consequence of photoacclimation processes (Deep photoAcclimation Maximum, DAM) resulting in the increase of chlorophyll a per phytoplankton carbon. Even though these DCM (further qualified as either DBMs or DAMs) have long been studied, no global-scale assessment has yet been undertaken and large knowledge gaps still remain in relation to the environmental drivers responsible for their formation and maintenance. In order to investigate their spatial and temporal variability in the open ocean, we use a global data set acquired by more than 500 Bio
SUBMITTER: Cornec M
PROVIDER: S-EPMC9285500 | biostudies-literature | 2021 Apr
REPOSITORIES: biostudies-literature
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