Phenotypic plasticity, both within and across generations, is an important mechanism that
organisms use to cope with rapid climate change. While an increasing number of studies …

Global climate change and localized anthropogenic stressors are driving rapid declines in
coral reef health. In vitro experiments have been fundamental in providing insight into how …

Ocean acidification refers to the lowering of the ocean's pH due to the uptake of
anthropogenic CO2 from the atmosphere. Coral reef calcification is expected to decrease as …

Approximately one-quarter of the anthropogenic carbon dioxide released into the
atmosphere each year is absorbed by the global oceans, causing measurable declines in …

Coral reefs and the services they provide are seriously threatened by ocean acidification
and climate change impacts like coral bleaching. Here, we present updated global …

Worldwide, coral reef ecosystems are experiencing increasing pressure from a variety of
anthropogenic perturbations including ocean warming and acidification, increased …

Coral calcification is dependent on the mutualistic partnership between endosymbiotic
zooxanthellae and the coral host. Here, using newly developed geochemical proxies (δ11B …

Coral reefs are threatened by global and local stressors. Yet, reefs appear to respond
differently to different environmental stressors. Using a global dataset of coral reef …

For reef framework to persist, calcium carbonate production by corals and other calcifiers
needs to outpace loss due to physical, chemical, and biological erosion. This balance is …

Ocean acidification is projected to lower the Ωar of reefal waters by 0.3–0.4 units by the end
of century, making it more difficult for calcifying organisms to secrete calcium carbonate …