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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... -
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... -
Boron isotope raw data for core MedSeA-S7-c2
Boron isotope (δ11B) raw data analyzed in G. ruber albus in MedSeA-S7-c2 -
Biomarker and SST reconstruction of sediment core MedSeA-S7-c2
Alkenone raw data in core MedSeA-S7-c2 (Strait of Sicily) -
Age model of sediment core MedSeA-S7-c2
Age controls for core MedSeA-S7-c2 (Strait of Sicily). Age model is derived through 210PB and 137Cs profiles. Ages for each sample depth are estimated by CF:CS model. -
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... -
Dynamic storage of glacial CO2 in the Atlantic Ocean revealed by boron [CO32-...
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... -
Boron isotope data on uranium-thorium dated Desmophyllum dianthus deep sea co...
The cause of changes in atmospheric carbon dioxide (CO₂) during the recent ice ages is yet to be fully explained. Most mechanisms for glacial–interglacial CO₂ change have... -
A database of the elemental and isotopic composition of water and carbonates ...
The dataset presented here encompasses the results of the geochemical analyses of water and recent carbonate samples collected in the El Peinado basin located in the Southern... -
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... -
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... -
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... -
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... -
(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...
