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Seawater carbonate chemistry and Montipora capitata and Porites compressa phy...
Following natural thermal stress in two consecutive years (2014 and 2015), we evaluated the effects of feeding and simulated ocean acidification on the physiological recovery of... -
Seawater carbonate chemistry and oxygen and pH gradients in coral boundary layer
Here, we investigated these effects on the reef-building corals Acropora cytherea, Pocillopora verrucosa, and Porites cylindrica. We preconditioned corals to a control (pH 8.0)... -
Seawater carbonate chemistry and the net photosynthesis, gross photosynthesis...
The absorbtion of human-emitted CO2 by the oceans (elevated PCO2) is projected to alter the physiological performance of coral reef organisms by perturbing seawater chemistry... -
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 the bioerosion rates of two reef-dwelling Ca...
Ocean acidification (OA) is expected to modify the structure and function of coral reef ecosystems by reducing calcification, increasing bioerosion, and altering the physiology... -
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 the larval and juvenile development of the M...
The ability of coral populations to recover from disturbance depends on larval dispersion and recruitment. While ocean warming and acidification effects on adult corals are well... -
Seawater carbonate chemistry and tissue necrosis, photosynthetic efficiency a...
Responses of corals to seawater acidification have been extensively studied. Sensitivity varies widely between species, highlighting the need to avoid extrapolation from one to... -
Seawater carbonate chemistry and growth rates for coral fragments from the sp...
Coral reefs are susceptible to climate change, anthropogenic influence, and environmental stressors. However, corals in Kāneʻohe Bay, Hawaiʻi have repeatedly shown resilience... -
Seawater carbonate chemistry and coral offspring ecological performance
The persistence of reef building corals is threatened by human-induced environmental change. Maintaining coral reefs into the future requires not only the survival of adults,... -
Seawater carbonate chemistry and colony growth and skeletal mass of bryozoans
Phenotypic plasticity has the potential to allow organisms to respond rapidly to global environmental change, but the range and effectiveness of these responses are poorly... -
Seawater carbonate chemistry and coral calcification rates
Estimates of heritability inform evolutionary potential and the likely outcome of many management actions, but such estimates remain scarce for marine organisms. Here, we report... -
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 tissue biomass composition, calcification of...
Ocean acidification (OA) is predicted to reduce reef coral calcification rates and threaten the long-term growth of coral reefs under climate change. Reduced coral growth at... -
Combined ocean acidification and low temperature stressors cause coral mortality
Oceans are predicted to become more acidic and experience more temperature variability-both hot and cold-as climate changes. Ocean acidification negatively impacts reef-building... -
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... -
Understanding cold bias: Variable response of skeletal Sr/Ca to seawater pCO2...
Coral skeletal Sr/Ca is a palaeothermometer commonly used to produce high resolution seasonal sea surface temperature (SST) records and to investigate the amplitude and... -
Colony-specific investigations reveal highly variable responses among individ...
As anthropogenic climate change is an ongoing concern, scientific investigations on its impacts on coral reefs are increasing. Although impacts of combined ocean acidification... -
Coral energy reserves and calcification in a high-CO2 world at two temperatures
Rising atmospheric CO2 concentrations threaten coral reefs globally by causing ocean acidification (OA) and warming. Yet, the combined effects of elevated pCO2 and temperature...