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Compiled proxy data records from different source water regions in the Atlant...
Compiled proxy data records from different source water regions in the Atlantic and Pacific ocean. Data span the last 25 ka BP, comprise benthic stable carbon isotopes, (d13Cb),... -
Stable carbon and oxygen isotope data from benthic foraminifera in the northe...
Stable carbon and oxygen isotope data from benthic foraminifera in the northern North Atlantic and Nordic Seas since the Last Glacial Maximum. Data are compiled from the... -
Dynamic storage of glacial CO2 in the Atlantic Ocean revealed by boron [CO32-...
This dataset has no description
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Seawater carbonate chemistry and hydrogen ions and carbonate chemistry in cal...
A generalized physicochemical model of the response of marine organisms' calcifying fluids to CO2-induced ocean acidification is proposed. The model is based upon the hypothesis... -
New benthic foraminifera stable isotopes from IODP Site 303-U1302
New benthic foraminifera stable isotope data from Site IODP U1302. The data range from core top to the LGM (~ 22 ka BP at 3.73 metres composite depth). Benthic foraminifera from... -
Seawater carbonate chemistry and skeletal isotopic composition and calcifying...
The Tara Pacifc expedition (2016–2018) provided an opportunity to investigate calcifcation patterns in extant corals throughout thePacifc Ocean. Cores from colonies of the... -
Seawater carbonate chemistry and changes in the sources of carbon for calcifi...
It is thought that the active physiological regulation of the chemistry of a parent fluid is an important process in the biomineralization of scleractinian corals. Biological... -
Seawater carbonate chemistry and acid–base balance in the hæmolymph of Europe...
Ocean acidification (OA) and the associated changes in seawater carbonate chemistry pose a threat to calcifying organisms. This is particularly serious for shelled molluscs, in... -
Seawater carbonate chemistry and acid-base physiology, skeleton properties, a...
Antarctic surface waters are expected to be the first to experience severe ocean acidification (OA) with carbonate undersaturation and large decreases in pH forecasted before... -
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 calcification rate, calcifying fluid pH, cal...
Natural variability in pH in the diffusive boundary layer (DBL), the discrete layer of seawater between bulk seawater and the outer surface of organisms, could be an important... -
Seawater carbonate chemistry and calcification conditions and calcification r...
Ocean acidification is expected to negatively impact calcifying organisms, yet we lack understanding of their acclimation potential in the natural environment. Here we measured... -
Seawater carbonate chemistry and internal carbonate chemistry regulation and ...
Corals exert a strong biological control over their calcification processes, but there is a lack of knowledge on their capability of long-term acclimatization to ocean... -
Seawater carbonate chemistry and calcifying fluid carbonate chemistry, calcif...
Ocean acidification (OA) is a pressing threat to reef-building corals, but it remains poorly understood how coral calcification is inhibited by OA and whether corals could... -
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 and Mytilus edulis biological processes during e...
CO2 emissions are leading to an acidification of the oceans. Predicting marine community vulnerability towards acidification is difficult, as adaptation processes cannot be... -
Compiled proxy data records from different source water regions in the Atlant...
We compiled data from five different proxies for the reconstruction of deep water mass composition in the deep Atlantic during the Last Glacial Maximum (23 - 19 ka BP), Heinrich... -
Isotope and elemental data for: Dynamic storage of glacial CO2 in the Atlanti...
The origin and carbon content of the deep water mass that fills the North Atlantic Basin, either Antarctic Bottom Water (AABW) or North Atlantic Deep Water (NADW) is suggested... -
Shell weights above the lysocline over the last ~40 ka measured in sediment c...
In this data set, we present the low carbonate ion condition in the deep sea region of the central Equatorial Indian Ocean (5°N & 77°E) over the last 40ka. The marine... -
Dissolution indices above the lysocline over the last ~40 ka measured in sedi...
We have deciphered the deep sea carbonate-ion content and associated dissolution in the central Equatorial Indian Ocean (5°N & 77°E). The marine sedimentary core was...
