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 …

The environmental conditions in the ocean have long been considered relatively more
stable through time compared to the conditions on land. Advances in sensing technologies …

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 …

Climate change refugia in the terrestrial biosphere are areas where species are protected
from global environmental change and arise from natural heterogeneity in landscapes and …

Climate warming is occurring at a rate not experienced by life on Earth for 10 s of millions of
years, and it is unknown whether the coral‐dinoflagellate (Symbiodinium spp.) symbiosis …

Environmental heterogeneity gives rise to phenotypic variation through a combination of
phenotypic plasticity and fixed genetic effects. For reef-building corals, understanding the …

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

Coral reefs are deteriorating under climate change as oceans continue to warm and acidify
and thermal anomalies grow in frequency and intensity. In vitro experiments are widely used …

Coral reefs are facing intensifying stressors, largely due to global increases in seawater
temperature and decreases in pH. However, there is extensive environmental variability …

Eastern boundary current systems (EBCSs) experience dynamic fluctuations in seawater pH
due to coastal upwelling and primary production. The lack of high‐resolution pH …