As with the experimental data, the researchers grouped the 96 species into six functional groups, then assigned each group a range
of responses to ocean acidification, based on the ranges observed in the experiments.
The GOA - ON Requirements and Governance Plan provides both broad concepts and key critical details on how to meet our high level goals of: 1) to improve our understanding of global ocean acidification conditions; 2) to improve our understanding of
ecosystem response to ocean acidification; 3) and to acquire and exchange the data and knowledge necessary to optimize the modeling of ocean acidification and its impacts.
The research, published in Nature Communications, examined preserved fossil remains of coccolithophores from a period of climate warming and ocean acidification that occurred around 56 million years ago — the Paleocene Eocene Thermal Maximum (PETM)-- and provides a much - needed long - term perspective of
coccolithophore response to ocean acidification.
To date, studies of aragonitic, scleractinian
CWC responses to ocean acidification have frequently examined short - term acclimation, with effects on coral bio-mineralization, growth, and skeletal strength only becoming evident in experiments run for periods of a year or more (e.g., Tittensor et al., 2010).
Biofilms rapidly reorganize in response to environmental disturbance and are likely to be both indicators and drivers of community level change
in response to ocean acidification.
Intriguingly though, there was very little evidence for
any response to ocean acidification, other than perhaps a slight thinning of C. pelagicus coccoliths..
Their responses to ocean acidification have mostly been studied in short - term experiments.
To investigate the extent to which nature or nurture determines marine animals»
responses to Ocean Acidification (OA) we carried out in - situ transplants using tolerant and sensitive worms living around a natural CO2 vent.