Abstract The Global Ocean Data Analysis Project (GLODAP) is a synthesis effort providing
regular compilations of surface to bottom ocean biogeochemical data, with an emphasis on …

Uncertainties in projections of marine biogeochemistry from Earth system models (ESMs)
are associated to a large degree with the imperfect representation of the marine plankton …

Temperature is a master parameter in the marine carbon cycle, exerting a critical control on
the rate of biological transformation of a variety of solid and dissolved reactants and …

Planktic foraminifera are major marine calcifiers in the modern ocean, regulating the marine
inorganic carbon pump, and generating marine fossil archives of past climate change. The …

The coupled biogeochemical cycles of iron and sulfur are central to the long-term
biogeochemical evolution of Earth's oceans. For instance, before the development of a …

We extend the ecological component (ECOGEM) of the carbon-centric Grid-Enabled
Integrated Earth system model (cGEnIE) to include a diatom functional group. ECOGEM …

Marine biota and biogeophysical mechanisms, such as phytoplankton light absorption, have
attracted increasing attention in recent climate studies. Under global warming, the influence …

We analyse 400 perturbed-parameter simulations for two configurations of an optimality-
based plankton–ecosystem model (OPEM), implemented in the University of Victoria Earth …

The Earth's oceans are one of the largest sinks in the Earth system for anthropogenic CO 2
emissions, acting as a negative feedback on climate change. Earth system models predict …

We investigate the ways in which marine biologically mediated heating increases the
surface atmospheric temperature. While the effects of phytoplankton light absorption on the …