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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 carbon, oxygen and boron isotopes within Och...
Ocean acidification will potentially inhibit calcification by marine organisms; however, the response of the most prolific ocean calcifiers, coccolithophores, to this... -
Seawater carbonate chemistry and coral calcifying fluid pH and calcification
Evaluating the factors responsible for differing species-specific sensitivities to declining seawater pH is central to understanding the mechanisms via which ocean acidification... -
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 boron isotope and trace elements incorporati...
Early-life stages of reef-building corals are vital to coral existence and reef maintenance. It is therefore crucial to study juvenile coral response to future climate change... -
Seawater carbonate chemistry and pH at the site of calcification within the c...
Coralline algae provide important ecosystem services but are susceptible to the impacts of ocean acidification. However, the mechanisms are uncertain, and the magnitude is... -
Decoupled carbonate chemistry controls on the incorporation of boron into Orb...
In order to fully constrain paleo-carbonate systems, proxies for two out of seven parameters, plus temperature and salinity are required. The boron isotopic composition (delta... -
Coral calcifying fluid pH dictates response to ocean acidification
Ocean acidification driven by rising levels of CO2 impairs calcification, threatening coral reef growth. Predicting how corals respond to CO2 requires a better understanding of... -
(Table 1, 2) Foraminifera biometric data, and boron isotopic composition of G...
Sediment samples from the Ontong-Java Plateau in the Pacific and the 90° east ridge in the Indian Ocean were used to investigate whether shell size and early diagenesis affect... -
(Table S1) Boron isotope and trace element data and reconstructed carbonate s...
The middle Miocene Climatic Optimum (17-15 Ma; MCO) is a period of global warmth and relatively high CO2 and is thought to be associated with a significant retreat of the... -
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,... -
Boron isotopes, trace elements and pH calculation for Norwegian deep sea cora...
d11B and trace results obtained for a deep sea coral specimen Madrepora oculata collected from the Norwegian Sea (67°N, 9°E, 340 m) during the RV Polarstern ARK/II/Ia cruise... -
Seawater carbonate chemistry and zooxanthellate coral Cladocora caespitosa bo...
Boron isotopic and elemental systematics are used to define the vital effects for the temperate shallow water Mediterranean coral Cladocora caespitosa. The corals are from a... -
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... -
Diatom boron isotope data from ODP Site 882 over the intensification of North...
Diatom boron and boron isotope data from ODP Site 882 in the subarctic Pacific Ocean over the intensification of Northern Hemisphere glaciation (iNHG) at 2.73 Ma. -
(Table 1) B/Ca and d11B ratios of foraminifera from marine surface sediments
All environmental parameters taken from nearby GLODAP site -
B/Ca, δ¹¹B and calcifying fluid carbonate chemistry reconstruction of Porites...
Samples were collected from two Porites sp. coral cores in the Southwestern Pacific, specifically at Nomuka Iki Island (Tonga). Parameters measured in this study include boron... -
B/Ca, δ¹¹B and calcifying fluid carbonate chemistry reconstruction of Porites...
Samples were collected from two Porites sp. coral cores in the Southwestern Pacific, specifically at Rotuma Island (Fiji). Parameters measured in this study include boron stable... -
Boron and carbon isotope, and B/Ca data for a Siderastrea siderea coral core ...
Massive scleractinian corals provide unique opportunities to reconstruct past climatic and chemical changes in the ocean, where there is no additional information. Regular pH...