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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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(Table 1) Chemical and isotope compositions of interstitial water in sediment...
This dataset has no description
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Foraminifera boron isotope, sea surface temperature, salinity, pH and pCO2 da...
Data presented here are trace-elements and boron isotope composition of planktic foraminifera G. ruber (250-355 μm) along with reconstructed surface ocean temperature, salinity,... -
Endmember B and Li concentration and isotope ratios of high temperature black...
Calculated pure hydrothermal end-member Li and B isotope compositions in high-temperature fluids from Brothers volcano, Kermadec Arc, Western Pacific collected during SO-253... -
Boron, lithium and isotope compositions in acid-sulfate and black smoker flui...
Lithium, boron and magnesium isotope compositions in high-temperature and acid-sulfate fluids from Brothers and Macauley volcano, Kermadec Arc, Western Pacific collected during... -
Benthic boron isotope data and associated pH determinations, from paper on Ce...
Boron isotope data on benthic foraminifera, spanning 1 to 59 Ma, and used to reconstruct deep ocean pH change over the Cenozoic. Data are from ODP sites spanning water depths... -
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... -
Boron isotope, trace elements and pH data (1990-2013) of the Porites lutea co...
Atmospheric CO2 rise in post-industrial era has resulted in decline in surface ocean pH, commonly known as “ocean acidification (OA)”, which has become a threat to marine... -
δ11B isotopes, CO2 release and pH analysis from sedeiment core TAN1106/28
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... -
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... -
Drake passage cold-water coral Ba/Ca and boron isotopes during NBP cruises NB...
The Antarctic Cold Reversal (ACR; 14.7 to 13 ka) phase of the last deglaciation saw a pause in the rise of atmospheric pCO2 and Antarctic temperature, contrasted with warming in... -
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... -
Boron, oxygen and carbon isotopes, and trace element ratios in planktic foram...
This dataset contains measurements of δ11B, δ13C and δ18O, as well as the elemental ratios Magnesium/Calcium, Aluminium/Calcium, Strontium/Calcium from planktic foraminifera... -
(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... -
(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 1) Boron, carbon, magnesium and calcium isotope data, post-Marinoan Ne...
A marked ocean acidification event and elevated atmospheric carbon dioxide concentrations following the extreme environmental conditions of the younger Cryogenian glaciation... -
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) 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...