Oceanic dissolved inorganic carbon (TC) is the largest pool of carbon that substantially
interacts with the atmosphere on human timescales. Oceanic TC is increasing through …

Ocean acidification describes the progressive, global reduction in seawater pH that is
currently underway because of the accelerating oceanic uptake of atmospheric CO2 …

Oceanic uptake of anthropogenic CO2 leads to decreased pH, carbonate ion concentration,
and saturation state with respect to CaCO3 minerals, causing increased dissolution of these …

Ocean acidification affects a wide diversity of marine organisms and is of particular concern
for vulnerable larval stages critical to population replenishment and connectivity. Whereas it …

The Atlantic and Arctic Oceans are critical components of the global carbon cycle. Here we
quantify the net sea–air CO 2 flux, for the first time, across different methodologies for …

With the accumulation of anthropogenic carbon dioxide (CO 2), a proceeding decline in
seawater pH has been induced that is referred to as ocean acidification. The ocean's …

Increasing anthropogenic CO 2 emissions to the atmosphere are causing a rise in p CO 2
concentrations in the ocean surface and lowering pH. To predict the effects of these …

The number and quality of ocean pH measurements have increased substantially over the
past few decades such that trends, variability, and spatial patterns of change are now being …

The Iceland Sea is one part of the Nordic Seas. Cold Arctic Water prevails there and the
deep-water is an important source of North Atlantic Deep Water. We have evaluated time …

Modern reef-building corals sustain a wide range of ecosystem services because of their
ability to build calcium carbonate reef systems. The influence of environmental variables on …