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Monthly proxy and growth parameter from a core of Porites australiensis from ...
This dataset has no description
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Monthly proxy and growth parameter from a core of Porites australiensis from ...
This dataset has no description
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Monthly proxy and growth parameter from a core of Porites australiensis from ...
This dataset has no description
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Isotope and elemental data for: Dynamic storage of glacial CO2 in the Atlanti...
The origin and carbon content of the deep water mass that fills the North Atlantic Basin, either Antarctic Bottom Water (AABW) or North Atlantic Deep Water (NADW) is suggested... -
Monthly and annually proxy and growth parameter from a core of Porites austra...
Identifying the long-term effects of ocean acidification (OA) and global warming on coral calcification has proven elusive yet has major implications for the continuing... -
Changes in planktic foraminiferal shell chemistry and size normalized weight ...
Three high resolution multicore records have been collected at three sites in the western Mediterranean with a MC400-Multicorer system during the MedSeA cruise (Mediterranean... -
Experimental adsorption parameters of boron isotopes on clay minerals
Adsorption and isotopic fractionation of boron on clastic sediment is one process responsible for the heavy boron isotopic composition of the modern ocean. However, the... -
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 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... -
δ13C and δ18O isotopes of Globigerina bulloides 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... -
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... -
Cenozoic CO2 from marine proxies
Atmospheric CO2 has been reconstructed over the last 66 million years from two marine proxies: the boron isotope composition of foraminifera and the carbon isotope composition... -
Sensitivity of boron adsorption on clays to changes in seawater chemistry
The adsorption of boron on detrital particles like clay or metal oxides is thought to be a major mechanism driving changes in the boron isotopic composition of seawater on... -
B isotope ratios of hydrothermal fluids and volcanic rocks from the Manus Bas...
The dataset contains boron (B) concentrations and isotope ratios of hydrothermal vent fluids and volcanic rocks from different vent fields within the Manus Basin, Papua New... -
Dynamic storage of glacial CO2 in the Atlantic Ocean revealed by boron [CO32-...
This dataset has no description
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(Table 1) Boron concentrations and isotope ratios together with previously re...
a: Previously reported by: Tivey et al., 2006; Craddock et al., 2010; Reeves et al., 2011 ; Seewald et al (2015) for fluids from Manus Basin collected in 2006; Bach et al., 2011... -
(Table 3) SiO2, TiO2 and B concentrations and isotope ratios of fresh and alt...
*: Fresh volcanic rocks from the Manus Basin were previously reported by Beier et al. (2015), and fresh volcanic rocks from Nifonea volcano by Lima et al. (2017), uncertainties... -
Alkenone determination from sediment 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...
