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Impact of atmospheric pCO2, seawater temperature, and calcification rate on t...
The tropical echinoid Echinometra viridis was reared in controlled laboratory experiments at temperatures of approximately 20°C and 30°C to mimic winter and summer temperatures... -
Coral pH regulation of the calcifying fluid is modulated by seawater dissolve...
Reef coral calcification depends on regulation of pH in the internal calcifying fluid in which the coral skeleton forms. However, little is known about calcifying fluid pH... -
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... -
Seawater carbonate chemistry and Calcium carbonate (CaCO3) sediment dissolution
Ocean acidification (OA), attributed to the sequestration of atmospheric carbon dioxide (CO2) into the surface ocean, and coastal eutrophication, attributed in part to land-use... -
Seawater carbonate chemistry and calcification of juvenile Pocillopora damico...
This study tested the interactive effects of increased seawater temperature and CO2 partial pressure (pCO2) on the photochemistry, bleaching, and early growth of the reef coral... -
Seawater carbonate chemistry and maximum quantum yield, net calcification rat...
Crustose coralline algae (CCA) are among the most sensitive marine taxa to the pH changes predicted with ocean acidification (OA). However, many CCA exist in habitats where diel... -
Seawater carbonate chemistry and calcification of Halimeda cuneata, photosynt...
The ultimate effect that ocean acidification (OA) and warming will have on the physiology of calcifying algae is still largely uncertain. Responses depend on the complex... -
Seawater carbonate chemistry and calcification rate of 10 investigated specie...
The response of marine-calcifying organisms to ocean acidification (OA) is highly variable, although the mechanisms behind this variability are not well understood. Here, we use... -
Seawater carbonate chemistry and growth and feeding of deep-sea coral Lopheli...
The global decrease in seawater pH known as ocean acidification has important ecological consequences and is an imminent threat for numerous marine organisms. Even though the... -
Seawater carbonate chemistry and calcification in the temperate coral Turbina...
High-latitude coral reefs provide natural laboratories for investigating the mechanisms and limits of coral calcification. While the calcification processes of tropical corals... -
Seawater carbonate chemistry and coral calcification
Experiments with coral fragments (i.e. nubbins) have shown that net calcification is depressed by elevated PCO2. Evaluating the implications of this finding requires scaling of... -
Seawater carbonate chemistry and carbonate load of seagrass leaves
Seagrass meadows play a significant role in the formation of carbonate sediments, serving as a substrate for carbonate-producing epiphyte communities. The magnitude of the... -
Seawater carbonate chemistry and primary production, respiration, calcificati...
Rising levels of anthropogenic carbon dioxide (CO2) in the atmosphere over the past several decades has resulted in a changing climate and is projected to further fuel global... -
Seawater carbonate chemistry and gross photosynthesis, respiration, calcifica...
Rhodolith beds built by free-living coralline algae are important ecosystems for marine biodiversity and carbonate production. Yet, our mechanistic understanding regarding... -
Seawater carbonate chemistry and phytoplankton growth and mortality
In coastal marine ecosystems coralline algae often create biogenic reefs. These calcareous algal reefs affect their associated invertebrate communities via diurnal oscillations... -
Seawater carbonate chemistry and calcification and respiration of Chlamys far...
Marine acidification will be an important environmental problem in the near future as a result of persistent emissions of CO2 and dissolution into seawater. In this study, we... -
Acclimatization to high-variance habitats does not enhance physiological tole...
Corals are acclimatized to populate dynamic habitats that neighbour coral reefs. Habitats such as seagrass beds exhibit broad diel changes in temperature and pH that routinely... -
Seawater carbonate chemistry and calcification rates of tropical zooxanthella...
Corals are globally important calcifiers that exhibit complex responses to anthropogenic warming and acidification. Although coral calcification is supported by high seawater... -
Calcification response of marine bivalves to changed carbonate chemistry: Fig...
This dataset has no description
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Seawater carbon chemistry and calcification rate of Palau corals
In Palau, calcification rates of two reef-building coral genera (Porites and Favia) are maintained across a strong natural gradient in aragonite saturation state (Omega ar)...
