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 …

Abstract Changes in CaCO3 dissolution due to ocean acidification are potentially more
important than changes in calcification to the future accretion and survival of coral reef …

Ocean acidification due to anthropogenic CO 2 emissions is a dominant driver of long-term
changes in pH in the open ocean, raising concern for the future of calcifying organisms …

Ocean acidification (OA) is generally assumed to negatively impact calcification rates of
marine organisms. At a local scale however, biological activity of macrophytes may generate …

Abstract The Red Sea is a unique body of water, hosting some of the most productive and
diverse coral reefs. Human populations along coasts of the Red Sea were initially sparse …

Coastal upwelling zones may be at enhanced risk from ocean acidification as upwelling
brings low aragonite saturation state (ΩAr) waters to the surface that are further suppressed …

The combination of ocean warming and acidification as a result of increasing atmospheric
carbon dioxide (CO2) is considered to be a significant threat to calcifying organisms and …

Ocean acidification is projected to shift coral reefs from a state of net accretion to one of net
dissolution this century. Presently, our ability to predict global-scale changes to coral reef …

Much of our past research on ocean acidification has focussed on direct responses to pCO2
increase at the (sub-) organism level, but does not produce findings that can be projected …

Warming of sea surface temperatures and alteration of ocean chemistry associated with
anthropogenic increases in atmospheric carbon dioxide will have profound consequences …