▪ Abstract The coastal zone is where land, ocean, and atmosphere interact. It exhibits a wide
diversity of geomorphological types and ecosystems, each one displaying great variability in …

Coral reefs in shallow-water environments (< 30 m) are in decline due to local and global
anthropogenic stresses. This has led to renewed interest in the 'deep reef refugia'hypothesis …

The severity of marine heatwaves (MHWs) that are increasingly impacting ocean
ecosystems, including vulnerable coral reefs, has primarily been assessed using remotely …

The new edition of this widely respected text provides comprehensive and up-to-date
coverage of the effects of biological–physical interactions in the oceans from the microscopic …

Greenhouse gas emissions are warming the ocean with profound consequences at all
levels of organization, from organismal rates to ecosystem processes. The proximate driver …

Long-term monitoring shows that the poleward range edges of intertidal biota have shifted
by as much as 50 km per decade, faster than most recorded shifts of terrestrial species …

Mesophotic coral reefs, reefs at depths of 30 m to 150 m, are receiving renewed interest from
coral reef scientists and managers because they are linked physically and biologically to …

Coral reefs are degrading worldwide at an alarming rate. Nutrient over-enrichment is
considered a major cause of this decline because degraded coral reefs generally exhibit a …

Corridors are commonly used to connect fragments of wildlife habitat, yet the identification of
conservation corridors typically neglects processes of habitat selection and movement for …

Coral reefs are among the most species-rich, productive and economically valuable
ecosystems on Earth but increasingly frequent pantropical coral bleaching events are …