Tipping elements are components of the Earth system which may respond nonlinearly to
anthropogenic climate change by transitioning toward substantially different long‐term …

Ocean acidification (OA) arises as a consequence of excessive carbon dioxide (CO2) inputs
into the ocean, a situation further exacerbated by anthropogenic gas emissions. Predictions …

Exposure to high‐frequency temperature variability often but not always enhances coral
heat tolerance, raising the question of whether this depends on the type of variability regime …

Ocean acidification (OA) has resulted in global-scale changes in ocean chemistry, which
can disturb marine organisms and ecosystems. Despite its extensively populated coastline …

Sediment runoff from disturbed coastal catchments is a major threat to marine ecosystems.
Understanding where sediments are produced and where they are delivered enables …

Management of coral predators, corallivores, is recommended to improve coral cover on
tropical coral reefs under projected increasing levels of accumulated thermal stress, but …

Most tropical corals live in symbiosis with Symbiodiniaceae algae whose photosynthetic
production of oxygen (O 2) may lead to excess O 2 in the diffusive boundary layer (DBL) …

Integrated pest management (IPM) leverages our understanding of ecological interactions to
mitigate the impact of pest species on economically and/or ecologically important assets. It …

Global warming and ocean acidification represent major threats to coral reefs, the
combination of these stressors may have concomitant impacts on coral holobionts. However …

By the century's end, many tropical seas will reach temperatures exceeding most coral
species' thermal tolerance on an annual basis. The persistence of corals in these regions …