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Responses of three tropical seagrass species to CO2 enrichment
Increased atmospheric carbon dioxide leads to ocean acidification and carbon dioxide (CO2) enrichment of seawater. Given the important ecological functions of seagrass meadows,... -
Effects of increasing hydrostatic pressure on sinking diatom aggregates
The effect of increasing hydrostatic pressure on the microbial degradation, the organic matter composition, and the microbiome of 'marine snow' particles was studied in... -
Acidification, not carbonation, is the major regulator of carbon fluxes in th...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2015) was used to compute a complete and consistent set of... -
Seawater carbonate chemistry and processes during experiments with marine mus...
In the context of future scenarios of progressive accumulation of anthropogenic CO2 in marine surface waters, the present study addresses the effects of long-term hypercapnia on... -
Seawater carbonate chemistry and shell growth, survival and respiration of E...
We exposed Eastern oyster larvae (Crassostrea virginica) to a full-factorial experimental design using two temperatures (23°C and 27°C), salinities (17 and 27), and pCO2 levels... -
Seawater pH predicted for the year 2100 affects the metabolic response to fee...
Widespread ocean acidification (OA) is transforming the chemistry of the global ocean, and the Arctic is recognised as a region where the earliest and strongest impacts of OA... -
Performance of the Arctic calanoid copepods Calanus glacialis and C. hyperbor...
The sensitivity of copepods to ocean acidification (OA) and warming may increase with time, however, studies >10 days and on synergistic effects are rare. We therefore... -
Seawater carbonate chemistry and biological processes of oysters Crassostrea ...
Estuarine organisms are exposed to periodic strong fluctuations in seawater pH driven by biological carbon dioxide (CO2) production, which may in the future be further... -
Seawater carbonate chemistry and growth and photosynthesis of a Great Barrier...
This study examined the individual and interactive impacts of global and local stressors by investigating the effects of increased seawater pCO2, elevated nutrient... -
Diatom assemblage in ODP Hole 105-646B
no sediment depth given by the author ! -
Respiration rates of the cold-water coral Dendrophyllia cornigera from a long...
A 9-month aquarium experiment with the cold-water Dendrophyllia cornigera was conducted to investigate the single and combined effects of warming, acidification and... -
Seawater carbonate chemistry and photosynthetic performance and N2 fixation i...
Effects of changed levels of dissolved O2 and CO2 on marine primary producers are of general concern with respect to ecological effects of ongoing ocean deoxygenation and... -
Seawater carbonate chemistry and physiological performance parameters of Carc...
Ocean acidification causes an accumulation of CO2 in marine organisms and leads to shifts in acid-base parameters. Acid-base regulation in gill breathers involves a net increase... -
Svalbard 2010 team (2010): EPOCA Svalbard mesocosm experiment 2010 depth-inte...
Latest data set update: 9 October 2013. In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) was used... -
Effect of temperature on aerobic microbial respiration associated with decayi...
The effect of varying temperature on the kinetics of aerobic microbial respiration (a proxy for oxidative carbon mineralization) associated with copepod carcasses was studied in... -
Seawater carbonate chemistry and carbonate chemistry in the microenvironment ...
Photosynthesis and respiration cause distinct chemical microenvironments within cyanobacterial aggregates. Here, we used microsensors and a diffusion–reaction model to... -
Seawater carbonate chemistry and microbioerosion of coral skeletons
Biological mediation of carbonate dissolution represents a fundamental component of the destructive forces acting on coral reef ecosystems. Whereas ocean acidification can... -
Seawater carbonate chemistry and biological processes during experiments with...
Atmospheric CO2 partial pressure (pCO2) is expected to increase to 700 µatm or more by the end of the present century. Anthropogenic CO2 is absorbed by the oceans, leading to... -
Seawater carbonate chemistry and growth rate of a bloom forming macroalga
Introduction: The coastal macroalgal genus, Ulva, is found worldwide and is considered a nuisance algal genus due to its propensity for forming vast blooms. The response of Ulva... -
Seawater carbonate chemistry and kelp densities and coral coverages at three ...
Ocean warming is altering the biogeographical distribution of marine organisms. In the tropics, rising sea surface temperatures are restructuring coral reef communities with...