Not exact matches
Rising
ocean temperatures will
alter the productivity and composition of marine phytoplankton
communities, thereby affecting global biogeochemical cycles.
These results imply that acidified seawater impacts larval physiology, suggesting that suppressed metabolism and metamorphosis may
alter the dispersal potential of larvae and subsequently reduce the resilience of coral
communities in the near future as the
ocean pH decreases.
Recognition has grown in the scientific
community that droughts, heat - waves and other catastrophic weather and climate events are not random in occurrence, nor are they caused only by variations in remote
ocean temperatures
altering large - scale atmospheric circulation.
The warmer
ocean surface temperatures impact corals and
alter coral reef
communities by prompting coral bleaching events and
altering ocean chemistry.
Predicted levels of future
ocean acidification and temperature rise could
alter community structure and biodiversity in marine benthic
communities
While biotic interactions play a fundamental role in defining change to species distribution and
communities structure [22 — 24], the degree to which
ocean acidification and climate change may
alter the way in which species interact with one another is not fully understood.