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Yearly averaged Ba/Ca and Mg/Ca LA-ICP-MS data from the forereef (FR-12) and ...
This dataset has no description
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Monthly averaged Ba/Ca LA-ICP-MS data from the forereef (FR-12) and backreef ...
This dataset has no description
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Repeated top core transects for 0.5 mm average binned LA-ICP-MS Ba/Ca alongsi...
This dataset has no description
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Monthly averaged Ba/Ca solution data from the forereef (FR-12) and backreef (...
This dataset has no description
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Coral species abundance on nearshore lagoonal reefs on the Belize Mesoamerica...
This dataset has no description
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Seawater carbonate chemistry and calcification rate of reef-building coral Si...
Anthropogenic increases in atmospheric CO2 over this century are predicted to cause global average surface ocean pH to decline by 0.1–0.3 pH units and sea surface temperature to... -
Seawater carbonate chemistry and physiological parameters of Caribbean coral
Global change driven by anthropogenic carbon emissions is altering ecosystems at unprecedented rates, especially coral reefs, whose symbiosis with algal symbionts is... -
Seawater carbonate chemistry and changes in the sources of carbon for calcifi...
It is thought that the active physiological regulation of the chemistry of a parent fluid is an important process in the biomineralization of scleractinian corals. Biological... -
Seawater carbonate chemistry and physiology of reef-building corals (Siderast...
Global change, including rising temperatures and acidification, threatens corals globally. Although bleaching events reveal fine-scale patterns of resilience, traits enabling... -
Seawater carbonate chemistry and survival, calcification rate of 4 species of...
We conducted a 93-day experiment investigating the independent and combined effects of acidification (280−3300 µatm pCO2) and warming (28°C and 31°C) on calcification and linear... -
Seawater carbonate chemistry and calcification, survival, concentrations of S...
Coral calcification is expected to decline as atmospheric carbon dioxide concentration increases. We assessed the potential of Porites astreoides, Siderastrea siderea and... -
Species-specific responses to climate change and community composition determ...
Anthropogenic climate change compromises reef growth as a result of increasing temperatures and ocean acidification. Scleractinian corals vary in their sensitivity to these... -
Next-century ocean acidification and warming both reduce calcification rate, ...
Atmospheric pCO2 is predicted to rise from 400 to 900 ppm by year 2100, causing seawater temperature to increase by 1-4 °C and pH to decrease by 0.1-0.3. Sixty-day experiments...
