Surface ocean biogeochemistry and photochemistry regulate ocean–atmosphere fluxes of
trace gases critical for Earth's atmospheric chemistry and climate. The oceanic processes …

Diatoms account for up to 40% of marine primary production, and require silicic acid to grow
and build their opal shell. On the physiological and ecological level, diatoms are thought to …

Mesocosms are real-world environmental science tools for bridging the gap between
laboratory-scale experiments and actual habitat studies on ecosystem complexities. These …

Despite the distinct benefits of plastics, the environmental impacts stemming from their
production and accumulation in the environment have become a global concern. Therefore …

Ocean acidification, the change in seawater carbonate chemistry due to the uptake of
anthropogenic CO2, affects the physiology of marine organisms in multiple ways. Diverse …

A substantial body of research now exists demonstrating sensitivities of marine organisms to
ocean acidification (OA) in laboratory settings. However, corresponding in situ observations …

Climate‐change‐induced alterations of oceanic conditions will lead to the ecological niches
of some marine phytoplankton species disappearing, at least regionally. How will such …

The oceans absorb~ 25% of the annual anthropogenic CO2 emissions. This causes a shift
in the marine carbonate chemistry termed ocean acidification (OA). OA is expected to …

In vitro incubations using natural marine communities can provide insight into community
structure and function in ways that are challenging through field observations alone. We …

Mesocosm experiments have been fundamental to investigate the effects of elevated CO2
and ocean acidification (OA) on planktic communities. However, few of these experiments …