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δ11B of well-preserved brachiopod fossils coupled with geochemical modeling
We present the δ11B of well-preserved brachiopod fossils coupled with geochemical modeling to examine how seawater boron responded to abrupt and dynamic climate changes in the... -
(Table 2) B/Ca, d11B, Mg/Ca and δ¹⁸O record for ODP Hole 130-806B samples
We present the first continuous records from 0 to 5 Ma (in 0.333 m.y. integrated time steps) of paired boron/calcium (B/Ca) ratios and boron isotopes (d11B) in the planktonic... -
(Table 1) Boron concentration and d11B ratios of ODP Hole 130-803D
The pH of the surface ocean is a sensitive function of its alkalinity and total inorganic carbon concentration, properties which also control the partial pressure of atmospheric... -
(Table 1) Boron-isotope measurements of foraminifera of ODP Hole 143-865C
The carbon dioxide content of the atmosphere [measured as the partial pressure of CO2 (pCO2)] affects the content of the surface ocean, which in turn affects seawater pH. The... -
(Table 1) Boron-isotope measurements of planktonic and benthic foraminifera o...
Measurement of boron isotope compositions in species of planktonic foraminifera that calcified their tests at different depths in the water column are used to reconstruct the pH... -
(Table 1) Boron-isotope measurements of shallow-dwelling planktonic foraminif...
Knowledge of the evolution of atmospheric carbon dioxide concentrations throughout the Earth's history is important for a reconstruction of the links between climate and... -
(Table 1) Boron analyses from ODP Sites 186-1150 and 186-1151
Interstitial pore waters from Ocean Drilling Program (ODP) Sites 1150 and 1151, both penetrating ca. 1200 m of sub-seafloor sediment from the upper Japan Trench forearc, were... -
(Table 1) Boron concentration and d11B values of interstitial water from IODP...
The Integrated Ocean Drilling Program Expedition 308 (IODP308) drilled normal-pressured sediments from the Brazos-Trinity Basin IV and over-pressured sediments from the Ursa... -
(Table 1) B content, d11B, δ¹⁸O, degree of alteration, and lithology of basal...
Boron contents and boron isotopic compositions were determined for the uppermost 1.3 km section of typical 6.2 Ma oceanic crust from DSDP/ODP Hole 504B, Costa Rica Rift,... -
Seawater carbonate chemistry and resistance of corals and coralline algae to ...
Ocean acidification is a threat to the continued accretion of coral reefs, though some undergo daily fluctuations in pH exceeding declines predicted by 2100. We test whether... -
U-Th, 14C and d11B results for Holocene North Atlantic deep sea corals (Lophe...
Sediment Core MD01-2454G SW Rockall BANK 747m water depth on Logatechev Mounds (Core was taken during Marion Dufresne Cruise Geosciences 2001 at 55°31'N and 15°39'W)ENAM corals... -
Annually-resolved coral-based d11B-pH reconstruction for the past 323 years f...
Increasing atmospheric CO2 from man-made climate change is reducing surface ocean pH. Due to limited instrumental measurements and historical pH records in the world's oceans,... -
Boron isotopes, pH and pCO2 calculation for one Fiji coral specimen Porites (...
delta11B results and deduced pH, pCO2 and omega values obtained for a tropical coral specimen Porites collected in 1998 at Yasawa (16°48'S- 177°27'E) on the western side of the...
