Ocean acidification results in co-varying inorganic carbon system variables. Of these, an
explicit focus on pH and organismal acid–base regulation has failed to distinguish the …

Ocean acidification (OA) is altering the chemistry of the world's oceans at rates unparalleled
in the past roughly 1 million years. Understanding the impacts of this rapid change in …

Understanding mollusk calcification sensitivity to ocean acidification (OA) requires a better
knowledge of calcification mechanisms. Especially in rapidly calcifying larval stages …

Ocean acidification, a reduction in ocean pH due to the uptake of anthropogenic carbon
dioxide (CO2) by surface waters, has recently emerged as a research theme in marine …

Anthropogenic CO2 is reducing the pH and altering the carbonate chemistry of seawater,
with repercussions for marine organisms and ecosystems. Current research suggests that …

Acidified waters are impacting commercial oyster production in the US Pacific Northwest,
and favorable carbonate chemistry conditions are predicted to become less frequent. Within …

Physiological increases in energy expenditure frequently occur in response to
environmental stress. Although energy limitation is often invoked as a basis for decreased …

Increasing anthropogenic carbon dioxide is altering marine carbonate chemistry through a
process called ocean acidification. Many calcium carbonate forming organisms are sensitive …

Calcifying echinoid larvae respond to changes in seawater carbonate chemistry with
reduced growth and developmental delay. To date, no information exists on how ocean …

Ocean acidification (OA) and the biological consequences of altered seawater chemistry
have emerged as a significant environmental threat to healthy marine ecosystems. Because …