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Hysteresis between coral reef calcification and the seawater aragonite satura...
Some predictions of how ocean acidification (OA) will affect coral reefs assume a linear functional relationship between the ambient seawater aragonite saturation state (Omega... -
Influence of sediment acidification and water flow on sediment acceptance and...
Although ocean acidification is expected to reduce carbonate saturation and yield negative impacts on open-ocean calcifying organisms in the near future, acidification in... -
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... -
Diverse coral communities in naturally acidified waters of a Western Pacific ...
Anthropogenic carbon dioxide emissions are acidifying the oceans, reducing the concentration of carbonate ions ([CO32-) that calcifying organisms need to build and cement coral... -
Seawater carbonate chemistry and sea urchin larval size in a laboratory exper...
Ocean acidification results from an increase in the concentrations of atmospheric carbon dioxide (CO2) impacts on marine calcifying species, which is predicted to become more... -
Ocean acidification has no effect on thermal bleaching in the coral Seriatopo...
The objective of this study was to test whether elevated pCO2 predicted for the year 2100 (85.1 Pa) affects bleaching in the coral Seriatopora caliendrum (Ehrenberg 1834) either... -
Impacts of food availability and pCO2 on planulation, juvenile survival, and ...
Ocean acidification, the assimilation of atmospheric CO2 by the oceans that decreases the pH and CaCO3 saturation state (Omega) of seawater, is projected to have severe adverse... -
Effect of increased pCO2 level on early shell development in great scallop (P...
As a result of high anthropogenic CO2 emissions, the concentration of CO2 in the oceans has increased, causing a decrease in pH, known as ocean acidification (OA). Numerous... -
Permeable coral reef sediment dissolution driven by elevated pCO2 and pore wa...
Ocean acidification (OA) is expected to drive the transition of coral reef ecosystems from net calcium carbonate (CaCO3) precipitating to net dissolving within the next century.... -
Sea urchin response to rising pCO2 shows ocean acidification may fundamentall...
Ocean acidification caused by an increase in pCO2 is expected to drastically affect marine ecosystem composition, yet there is much uncertainty about the mechanisms through... -
Calcification of the Arctic coralline red algae Lithothamnion glaciale in res...
Rising atmospheric CO2 concentrations could cause a calcium carbonate subsaturation of Arctic surface waters in the next 20 yr, making these waters corrosive for calcareous... -
Colimitation of the unicellular photosynthetic diazotroph Crocosphaera watson...
We describe interactive effects of total phosphorus (total P = 0.1-4.0 µmol/L; added as H2NaPO4), irradiance (40 and 150 µmol quanta/m**2/s), and the partial pressure of carbon... -
Carbonate chemistry, community metabolism, PAR, temperature and salinity of O...
There are few in situ studies showing how net community calcification (Gnet) of coral reefs is related to carbonate chemistry, and the studies to date have demonstrated... -
Acclimatization of the crustose coralline alga Porolithon onkodes to variable...
Ocean acidification (OA) has important implications for the persistence of coral reef ecosystems, due to potentially negative effects on biomineralization. Many coral reefs are... -
The photo-physiological response of a model cnidarian-dinoflagellate symbiosi...
We measured the relationship between CO2-induced seawater acidification, photo-physiological performance and intracellular pH (pHi) in a model cnidarian-dinoflagellate symbiosis... -
Combined effects of CO2 and light on large and small isolates of the unicellu...
We examined the combined effects of light and pCO2 on growth, CO2-fixation and N2-fixation rates by strains of the unicellular marine N2-fixing cyanobacterium Crocosphaera... -
CO2 and vitamin B12 interactions determine bioactive trace metal requirements...
Phytoplankton growth can be limited by numerous inorganic nutrients and organic growth factors. Using the subarctic diatom Attheya sp. in culture studies, we examined how the... -
Short- and long-term conditioning of a temperate marine diatom community to a...
Ocean acidification and greenhouse warming will interactively influence competitive success of key phytoplankton groups such as diatoms, but how long-term responses to global... -
Sensitivity to ocean acidification parallels natural pCO2 gradients experienc...
The Arctic Ocean is a bellwether for ocean acidification, yet few direct Arctic studies have been carried out and limited observations exist, especially in winter. We present... -
Bioturbation determines the response of benthic ammonia-oxidizing microorgani...
Ocean acidification (OA), caused by the dissolution of increasing concentrations of atmospheric carbon dioxide (CO2) in seawater, is projected to cause significant changes to...