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Seawater carbonate chemistry, pigments and proteins during experiments with p...
In the high-nutrient, low-chlorophyll waters of the Gulf of Alaska, microcosm manipulation experiments were used to assess the effect of CO2 on growth and primary production... -
Seawater carbonate chemistry and biological parameters of Sepia officinalis d...
Low pO2 values have been measured in the perivitelline fluids (PVF) of marine animal eggs on several occasions, especially towards the end of development, when embryonic oxygen... -
Seawater carbonate chemistry and morphometric coordinates and morphology of t...
The world's oceans are slowly becoming more acidic. In the last 150 yr, the pH of the oceans has dropped by ~0.1 units, which is equivalent to a 25% increase in acidity.... -
Seawater carbonate chemistry and biological processes of Sepia officinalis du...
Acidification of ocean surface waters by anthropogenic carbon dioxide (CO2) emissions is a currently developing scenario that warrants a broadening of research foci in the study... -
Seawater carbonate chemistry and biological processes during experiments with...
Ocean acidification (OA) is believed to be a major threat for near-future marine ecosystems, and that the most sensitive organisms will be calcifying organisms and the... -
Seawater carbonate chemistry and biological processes of Mytilus edulis durin...
Marine organisms are exposed to increasingly acidic oceans, as a result of equilibration of surface ocean water with rising atmospheric CO2 concentrations. In this study, we... -
Seawater carbonate chemistry and shell weights of Laternula elliptica, Yoldia...
Antarctic calcified macroorganisms are particularly vulnerable to ocean acidification because many are weakly calcified, the dissolution rates of calcium carbonate are inversely... -
Seawater carbonate chemistry and calcification in the Bahama Bank, 1964-1965
Carbon dioxide is lost from the ocean by calcium carbonate precipitation (-p), photosynthesis (-b) and gas evasion at the sea surface (-g). Among the most active sites are warm... -
Seawater carbonate chemistry and biological processes during experiments with...
Anthropogenic elevation of atmospheric pCO2 is predicted to cause the pH of surface seawater to decline by 0.3-0.4 units by 2100 AD, causing a 50% reduction in seawater [CO3]... -
Seawater carbonate chemistry and biological processes duirng experiments with...
There are serious concerns that ocean acidification will combine with the effects of global warming to cause major shifts in marine ecosystems, but there is a lack of field data... -
Seawater carbonate chemistry and biological processes during experiments with...
The Arctic Ocean and its associated ecosystems face numerous challenges over the coming century. Increasing atmospheric CO2 is causing increasing warming and ice melting as well... -
Seawater carbonate chemistry and biological processes during experiments with...
The persistence of most coastal marine species depends on larvae finding suitable adult habitat at the end of an offshore dispersive stage that can last weeks or months. We... -
Seawater carbonate chemistry and processes during experiments with cyanobacte...
We investigated carbon acquisition by the N2-fixing cyanobacterium Trichodesmium IMS101 in response to CO2 levels of 15.1, 37.5, and 101.3 Pa (equivalent to 150, 370, and 1000... -
Seawater carbonate chemistry and biological processes during experiments with...
The effect of pCO2 on carbon acquisition and intracellular assimilation was investigated in the three bloom-forming diatom species, Eucampia zodiacus (Ehrenberg), Skeletonema... -
Seawater carbonate chemistry and biological processes during experiments with...
Anthropogenic elevation of atmospheric carbon dioxide (pCO2) is making the oceans more acidic, thereby reducing their degree of saturation with respect to calcium carbonate... -
Seawater carbonate chemistry, pigments and biological processes during experi...
Previous studies have shown that increasing atmospheric CO2 concentrations affect calcification in some planktonic and macroalgal calcifiers due to the changed carbonate... -
Seawater carbonate chemistry and biological processes during experiments with...
The response of Emiliania huxleyi (Lohmann), Calcidiscus leptoporus (Murray and Blackman), and Syracosphaera pulchra (Lohmann) to elevated partial pressure of carbon dioxide... -
Seawater carbonate chemistry and shell length of Mediterranean pteropod Cavol...
Larvae of the Mediterranean pteropod Cavolinia inflexa were maintained at controlled pHT values of 8.1, 7.82 and 7.51, equivalent respectively to pCO2 levels of 380, 857 and... -
Seawater carbonate chemistry and calcification during experiments with a cora...
Physiological data and models of coral calcification indicate that corals utilize a combination of seawater bicarbonate and (mainly) respiratory CO2 for calcification, not... -
Seawater carbonate chemistry and processes during experiments with Emiliania ...
The formation of calcareous skeletons by marine planktonic organisms and their subsequent sinking to depth generates a continuous rain of calcium carbonate to the deep ocean and...
