The combination of thermal stress and ocean acidification (OA) can more negatively affect
coral calcification than an individual stressors, but the mechanism behind this interaction is …

Early evidence suggests that DNA methylation can mediate phenotypic responses of marine
calcifying species to ocean acidification (OA). Few studies, however, have explicitly studied …

A dynamic energy budget (DEB) model integrating pCO 2 was used to describe ocean
acidification (OA) effects on Atlantic surfclam, Spisula solidissima, bioenergetics. Effects of …

Reef-dwelling calcifiers face numerous environmental stresses associated with anthropogenic
carbon dioxide emissions, including ocean acidification and warming. Photosymbiont-…

Corals are globally important calcifiers that exhibit complex responses to anthropogenic
warming and acidification. Although coral calcification is supported by high seawater pH, …

Anthropogenic CO 2 ‐emission is causing ocean warming and acidification. Understanding
how basic physiological processes of marine organisms respond to these stressors is …

Increasing anthropogenic carbon dioxide is predicted to cause declines in ocean pH and
calcium carbonate saturation state over the coming centuries, making it potentially harder for …

Host‐associated microbial communities are fundamental to host physiology, yet it is unclear
how these communities will respond to environmental disturbances. Here, we disentangle …

It is thought that the active physiological regulation of the chemistry of a parent fluid is an
important process in the biomineralization of scleractinian corals. Biological regulation of …

The Northwest Atlantic Shelf (NAS) region has experienced accelerated warming, heatwaves,
and is susceptible to ocean acidification, yet also suffers from a paucity of carbonate …