Marine plankton elemental stoichiometric ratios can deviate from the Redfield ratio (106C:
16N: 1P); here, we examine physiological and biogeochemical mechanisms that lead to the …

To understand and predict the physical, chemical, and biological processes at play in
coastal and nearshore marine areas requires an integrated, interdisciplinary approach. The …

This contribution describes the ocean biogeochemical component of the Geophysical Fluid
Dynamics Laboratory's Earth System Model 4.1 (GFDL‐ESM4. 1), assesses GFDL‐ESM4 …

Enhanced ocean carbon storage during the Pleistocene ice ages lowered atmospheric CO2
concentrations by 80 to 100 ppm relative to interglacial levels. Leading hypotheses to …

Oceanic nutrient cycles are coupled, yet carbon-nitrogen-phosphorus (C: N: P) stoichiometry
in marine ecosystems is variable through space and time, with no clear consensus on the …

A common assumption of a constant nitrogen-to-phosphorus ratio (N: P) of 16: 1 in marine
particulate organic matter (POM) appears to be invalidated by observations of major spatial …

The elemental stoichiometry of marine phytoplankton plays a critical role in global
biogeochemical cycles through its impact on nutrient cycling, secondary production, and …

One of the most important factors that determine the ocean‐atmosphere carbon partitioning
is the sinking of particulate organic matter (POM) from the surface ocean to the deep ocean …

The effect of environmental change in structuring the phytoplankton communities of the
coastal waters of the Eastern English Channel was investigated by applying a trait-based …

The CARIACO (Carbon Retention in a Colored Ocean) Ocean Time-Series Program station,
located at 10.50° N, 64.66° W, observed biogeochemical and ecological processes in the …