Climate projections suggest–with substantial certainty–that global warming> 1.5° C will
occur by mid-century (2050). Population is also projected to increase, amplifying the …

Morphological evolution from a unicellular to multicellular state provides greater
opportunities for organisms to attain larger and more complex living forms. As the most …

Biodiversity of phytoplankton is important for ecosystem stability and marine
biogeochemistry. However, the large-scale patterns of diversity are not well understood and …

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 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 …

Organisms are projected to face unprecedented rates of change in future ocean conditions
due to anthropogenic climate‐change. At present, marine life encounters a wide range of …

Climate change will alter concurrently many environmental factors that exert control over
oceanic phytoplankton. Recent laboratory culture work, shipboard experiments, and field …

Photoinhibition is an inevitable consequence of oxygenic photosynthesis. However, the
concept of a 'photoinhibition‐proof'plant in which photosystem II (PSII) is immune to …

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 …

Carbon dioxide concentrating mechanisms (also known as inorganic carbon concentrating
mechanisms; both abbreviated as CCMs) presumably evolved under conditions of low CO 2 …