Global warming and local eutrophication simultaneously lower oxygen (O2) saturation and
increase biological O2 demands to cause deoxygenation. Tropical shallow waters, and their …

To thrive in nutrient-poor waters, coral reefs must retain and recycle materials efficiently. This
review centers microbial processes in facilitating the persistence and stability of coral reefs …

Water motion is a key determinant of marine macroalgal production, influencing directly or
indirectly physiological rates and community structure. Our understanding of how marine …

When describing coral shape and form the term phenotypic plasticity, ie environment‐
induced changes in morphology, is often used synonymously with intraspecific variation …

Coral reef declines have been recorded for all major tropical ocean basins since the 1980s,
averaging approximately 30-50% reductions in reef cover globally. These losses are a result …

Coral reefs are suffering unprecedented declines worldwide. Most studies focus on stressors
such as rising temperatures, nutrient pollution, overfishing, and ocean acidification as …

There is a need to develop water quality thresholds for dredging near coral reefs that can
relate physical pressures to biological responses and define exposure conditions above …

Recent work has shown that hydrophilic and hydrophobic organic matter (OM) from algae
disrupts the function of the coral holobiont and promotes the invasion of opportunistic …

To elucidate the determinants of intertidal invertebrate body temperatures during aerial
exposure, I developed deterministic models using the environmental inputs of solar …

Coral reefs are in decline worldwide, making it increasingly important to promote coral
recruitment in new or degraded habitat. Coral reef morphology—the structural form of reef …