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

Marine phytoplankton have many obvious characters, such as rapid cell division rates and
large population sizes, that give them the capacity to evolve in response to global change on …

Ocean ecosystems have responded and will continue to respond to climate changes of
different rates, magnitudes, and durations (virtually certain). Human societies depend on …

Anthropogenic CO 2 is accumulating in the atmosphere and trap** reflected infrared
radiation, resulting in warming of both terrestrial and ocean ecosystems. At the same time …

Coccolithophores are important calcifying phytoplankton predicted to be impacted by
changes in ocean carbonate chemistry caused by the absorption of anthropogenic CO 2 …

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 …

Under global change, populations have four possible responses:'migrate, acclimate, adapt
or die'(Gienapp et al. 2008 Climate change and evolution: disentangling environmental and …

All phytoplankton and higher plants perform photosynthesis, where carbon dioxide is
incorporated into biomass during cell growth. Ocean acidification (OA) has the potential to …

Increasing atmospheric CO2 concentrations are expected to impact pelagic ecosystem
functioning in the near future by driving ocean warming and acidification. While numerous …

Coccolithophores are the most abundant calcifying phytoplankton in the ocean. These tiny
primary producers have an important role in the global carbon cycle, substantially …