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(Table S4) B/Ca ratios in co-occurring Eocene benthic foraminifera
Size fraction of benthic foraminifera = 150-250 µm. # = [Ca] too low; sample rejected. -
(Table S3) B/Ca ratios Cibicidoides wuellerstorfi from Holocene sediments
Size fraction of benthic foraminifera = 150-250 µm. -
(Table S2) B/Ca ratios Oridorsalis umbonatus from Holocene sediments
Size fraction of benthic foraminifera = 150-250 µm. -
(Table S1) B/Ca ratios and stable isotope record of Nuttallides umbonifera fr...
Size fraction of benthic foraminifera = 150-250 µm. -
(Table 3) B/Ca and d11B measurements of Globigerinoides sacculifer at ODP sit...
size fraction 300-355 µm -
(Table 3) B/Ca and d11B measurements of Globigerinoides ruber white at ODP si...
size fraction 300-355 µm, ss -
(Table 2) Boron concentration and isotope ratio measurements of Globigerinoid...
Age determined from composite depth and the orbitally tuned age models of Schmidt et al., (2006, doi:10.1029/2005GC000957) and Haug and Tiedemann (1998, doi:10.1038/31447) and... -
(Table 2) Boron concentration and isotope ratio measurements of Globigerinoid...
Age determined from composite depth and the orbitally tuned age models of Schmidt et al., (2006, doi:10.1029/2005GC000957) and Haug and Tiedemann (1998, doi:10.1038/31447) and... -
Bottom-water carbonate ion concentrations, oxygen and carbon isotopes, and pt...
This dataset includes foraminiferal trace element ratios, stable isotopes, and pteropod abundance estimates from marine sediment core PS1243, located in the central Norwegian... -
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... -
(Table 3) δ¹⁸O, B/Ca and Mg/Ca ratios in Globorotalia inflata from sediment c...
AGE after I.N. Mc Cave, personal communication, 2006. -
(Table 2) B/Ca and Mg/Ca ratios in planktonic foraminifera from ODP Hole 108-...
AGE vs. Vostock Gas Age Scale from Hönisch and Hemming (2005). Model 1 uses the deconvolution of foraminiferal d18O and Mg/Ca to yield local salinity, while model 2 uses the... -
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 resistance to ocean acidification in coral r...
Ocean acidification (OA) is a major threat to coral reefs, which are built by calcareous species. However, long-term assessments of the impacts of OA are scarce, limiting the... -
Seawater carbonate chemistry and tropical coral calcification
Ocean acidification typically reduces calcification in tropical marine corals but the mechanism for this process is not understood. We use skeletal boron geochemistry (B/Ca and... -
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 B/Ca, calcification rate of Emiliania huxley...
Coccolithophorid algae are microscopic but prolific calcifiers in modern and ancient oceans. When the pH of seawater is modified, as may occur in the future due to ocean... -
Seawater carbonate chemistry and test density, trace elements ratios of Pener...
Large Benthic Foraminifera are a crucial component of coral-reef ecosystems, which are currently threatened by ocean acidification. We conducted culture experiments to evaluate... -
Late Pleistocene δ¹¹B based carbon dioxide levels from ODP Site 154-926
Earth's climate cooled markedly during the Late Miocene from 12 to 5 million years ago, with far-reaching consequences for global ecosystems. However, the driving forces of...
