Dataset - B2FIND

(Table S1) Geochemistry for sediment core MD02-2515

A high-resolution, 55-kyr long record of chalcophile and redox-sensitive trace element accumulation (Ag, Cd, Re, Mo) from MD02-2515, western Guaymas Basin, is investigated in...

Seawater carbonate chemistry, Mg/Ca, Sr/Ca, oxygen production and calcificati...

The Sr/Ca of aragonitic coral skeletons is a commonly used palaeothermometer. However skeletal Sr/Ca is typically dominated by weekly-monthly oscillations which do not reflect...

Seawater carbonate chemistry, nutrients, particulate carbon and growth rate o...

The response of Emiliania huxleyi (Lohmann) W. W. Hay et H. Mohler, Calcidiscus leptoporus (G. Murray et V. H. Blackman) J. Schiller, andSyracosphaera pulchra Lohmann to...

Seawater carbonate chemistry, length and survival of Inland silverside, Menid...

Absorption of anthropogenic carbon dioxide by the world's oceans is causing mankind's 'other CO2 problem', ocean acidification. Although this process will challenge marine...

Seawater carbonate chemistry and biological processes of sand dollars Dendras...

Reduction in global ocean pH due to the uptake of increased atmospheric CO2 is expected to negatively affect calcifying organisms, including the planktonic larval stages of many...

(Table 1) Chemical and isotopic composition of pore fluids in cores TGC-1 and...

The role of sediment diagenesis in the marine cycles of Li and B is poorly understood. Because Li and B are easily mobilized during burial and are consumed in authigenic clay...

Seawater carbonate chemistry and biological processes of foraminifera, Globig...

Specimens of two species of planktic foraminifera, Globigerinoides ruber and Globigerinella siphonifera, were grown under controlled laboratory conditions at a range of...

Seawater carbonate chemistry and biological processes of Pandalus borealis du...

Ocean acidification (OA) resulting from anthropogenic emissions of carbon dioxide (CO2) has already lowered and is predicted to further lower surface ocean pH. There is a...

Seawater carbonate chemistry and biological processes of Mytilus edulis durin...

Ocean acidification (OA) resulting from anthropogenic emissions of carbon dioxide (CO2) has already lowered and is predicted to further lower surface ocean pH. There is a...

Seawater carbonate chemistry, primary production, biomass and calcification o...

Production (abundance and biomass) and net calcification rates of the coccolithophorid Pleurochrysis carterae under different partial pressures of CO2 (pCO2) were examined using...

Seawater carbonate chemistry and calcification during experiments with coral ...

The effect of increased CO2 partial pressure (pCO2) on the community metabolism (primary production, respiration, and calcification) of a coral community was investigated over...

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 processed during experiments with...

Uptake of anthropogenic CO2 by the oceans is altering seawater chemistry with potentially serious consequences for coral reef ecosystems due to the reduction of seawater pH and...