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(Tables 1&2) B, d11B, K and δ¹⁸O data for altered oceanic crust at DSDP Site ...
This dataset has no description
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(Tables 1&2) B, d11B, K and δ¹⁸O data for altered oceanic crust at DSDP Site ...
This dataset has no description
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(Table 1) Chemical and isotope compositions of interstitial water in sediment...
This dataset has no description
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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... -
δ11B isotopes, CO2 release and pH analysis from ODP Site 177-1090
Over the last deglaciation there were two transient intervals of pronounced atmospheric CO2 rise; Heinrich Stadial 1 (17.5-15 kyr) and the Younger Dryas (12.9-11.5 kyr). Leading... -
(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... -
Summary of boron isotope and Mg/Ca data
Biological productivity and carbon export in the equatorial Atlantic are thought to have been dramatically higher during the last glacial period than during the Holocene. Here... -
d11B and metal/Ca ratios versus size fractions in the Surface and deep dwelli...
We have assessed the reliability of several foraminifer-hosted proxies of the ocean carbonate system (d11B, B/Ca, and U/Ca) using Holocene samples from the Atlantic and Pacific... -
(Table S1) Globigerinoides sacculifer Boron isotope ratios of ODP Hole 165-999A
everal hypotheses have been put forward to explain the onset of intensive glaciations on Greenland, Scandinavia, and North America during the Pliocene epoch between 3.6 and 2.7... -
(Table 3) Geochemistry of borehole fluids of ODP Hole 137-504B
Circulation of seawater through basaltic basement for several million years after crustal emplacement has been inferred from studies of surface heat flow, and may play a... -
(Table 1) I, Br, B, d11B and Mn concentrations in ODP Site 131-808
This study of the interstitial water concentration-depth distributions of iodide, bromide, boron, d11B, and dissolved organic carbon, as represented by absorbance at 325 nm... -
(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 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) Results of pore water analyses, including boron content and boron i...
Drilling a transect of holes across the Costa Rica forearc during ODP Leg 170 demonstrated the margin wedge to be of continental, non accretionary origin, which is intersected... -
B- and O-isotope and Mg/Ca ratios of planktonic foraminifera and estimates of...
The dominant period of Pleistocene glacial cycles changed during the mid-Pleistocene from 40,000 years to 100,000 years, for as yet unknown reasons. Here we present a... -
Boron isotopic ratios and concentrations of pore fluids and carbonates from O...
We have determined the boron content and isotopic composition of bulk carbonates and associated pore waters from Ocean Drilling Program Site 851. The delta11B of the carbonates... -
(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,... -
Chemical and isotopic compositions of pore and botom waters at Sites ARA06C-J...
Cl- and alkalinity were determined by visual titration with 0.1 M AgNO~3~ and 0.02 M HCl, respectively. NH~4~+ and PO~4~3 were measured spectrophotometrically (UV-2450, Shimazu)...
