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

Trace metals are required for numerous processes in phytoplankton and can influence the
growth and structure of natural phytoplankton communities. The metal contents of …

The Southern Ocean plays a critical role in regulating global climate as a major sink for
atmospheric carbon dioxide (CO2), and in global ocean biogeochemistry by supplying …

The reliable and efficient production of microalgae in large-scale commercial culture,
whether in open ponds or in closed photobioreactors, requires a good understanding of the …

Predicting the ecological causes and consequences of global climate change requires a
variety of approaches, including the use of experiments, models, and surveys. Among …

Stoichiometric relations in plants, with emphasis on C: N: P, are reviewed. Both theoretically
and empirically it is found for whole plants as well as for different tissues that nitrogen …

Inorganic carbon concentrating mechanisms (CCMs) catalyse the accumulation of CO2
around rubisco in all cyanobacteria, most algae and aquatic plants and in C4 and …

The major nutrients nitrate and phosphate have one of the strongest correlations in the sea,
with a slope similar to the average nitrogen (N) to phosphorus (P) content of plankton …

Predicting the effects of multiple global change stressors on microbial communities remains
a challenge because of the complex interactions among those factors. Here, we explore the …

Continental margins are disproportionally important for global primary production, fisheries
and CO2 uptake. However, across the Northeast Atlantic shelves, there has been an …