Dataset - B2FIND

Inter‐individual variation and global change: coelomic fluid

Treatment:C Control conditionOA Ocean acidification scenarioOW Ocean warming scenarioOAW Ocean acidification and warming scenarioEOW Extreme ocean warming scenarioEOAW...

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 net calcification rates of cold-water corall...

Ocean acidification and warming are expected to disproportionately affect high-latitude calcifying species, such as crustose coralline algae. Clathromorphum nereostratum and...

Silicon isotopes in Arctic and sub-Arctic glacial meltwaters

This data product contains dissolved and amorphous particulate silicon concentrations and isotopic compositions, and ancillary data (discharge, conductivity, suspended...

(Table 1) Seawater chemistry calculated over the experiment period at the exp...

This dataset has no description

Table 1. pH, Temperature, conductivity and hydrochemistry of samples

Carbon dioxide deep geological storage, especially in deep saline aquifers, is one of the preferred technological options to mitigate the effects of greenhouse gases emissions....

Seawater carbonate chemistry and conditions of Mytilus edulis extracellular b...

Mytilus edulis were cultured for 3 months under six different seawater pCO2 levels ranging from 380 to 4000 µatm. Specimen were taken from Kiel Fjord (Western Baltic Sea,...

Seawater carbonate chemistry, gross photosynthesis and metabolically induced ...

Ocean acidification (OA) is a reduction in oceanic pH due to increased absorption of anthropogenically produced CO2. This change alters the seawater concentrations of inorganic...

Seawater carbonate chemistry and protein sports of barnicle Balanus amphitrit...

The majority of benthic marine invertebrates have a complex life cycle, during which the pelagic larvae select a suitable substrate, attach to it, and then metamorphose into...

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 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, 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...