The prokaryotic and eukaryotic microorganisms that drive the pelagic ocean's
biogeochemical cycles are currently facing an unprecedented set of comprehensive …

The oceans take up over 1 million tons of anthropogenic CO2 per hour, increasing dissolved
p CO2 and decreasing seawater pH in a process called ocean acidification (OA). At the …

The Arctic marine biome, shrinking with increasing temperature and receding sea-ice cover,
is tightly connected to lower latitudes through the North Atlantic. By flowing northward …

Prediction of the impact of global climate change on marine HABs is fraught with difficulties.
However, we can learn important lessons from the fossil record of dinoflagellate cysts; long …

This study examined the literature in ISI Web of Science to identify the effects that the main
drivers of global change have on the nutrient concentrations and C: N: P stoichiometry of …

Global increases in atmospheric CO2 and temperature are associated with changes in
ocean chemistry and circulation, altering light and nutrient regimes. Resulting changes in …

The public health, tourism, fisheries, and ecosystem impacts from harmful algal blooms
(HABs) have all increased over the past few decades. This has led to heightened scientific …

It is increasingly apparent that adequately mitigating anthropogenic climate interference will
require ocean carbon dioxide removal (CDR) strategies. Ocean alkalinity enhancement …

Ocean acidification poses a global threat to biodiversity, yet species might have the capacity
to adapt through evolutionary change. Here we summarize tools available to determine …

The accumulation of inorganic carbon from seawater by eukaryotic marine phytoplankton is
limited by the diffusion of carbon dioxide (CO2) in water and the dehydration kinetics of …