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Sand content of sediment core SO202/1_37-2
Sediment samples were freeze-dried and washed through a 63-µm sieve. -
CaCO3 content and carbonate accumulation rates of sediment core SO264_66-2
The CaCO3 content was calculated from TC and TOC which were measured by a CNS-analyzer (Elementar vario EL III) and a carbon/sulfur analyzer (Eltra CS-800). -
CaCO3 content and carbonate accumulation rates of sediment core SO264_55-1
The CaCO3 content was calculated from TC and TOC which were measured by a CNS-analyzer (Elementar vario EL III) and a carbon/sulfur analyzer (Eltra CS-800). -
CaCO3 content and carbonate accumulation rates of sediment core SO264_15-2
The CaCO3 content was calculated from TC and TOC which were measured by a CNS-analyzer (Elementar vario EL III) and a carbon/sulfur analyzer (Eltra CS-800). -
CaCO3 content and carbonate accumulation rates of sediment core SO202/1_37-2
The CaCO3 content was calculated from TC and TOC which were measured by a CNS-analyzer (Elementar vario EL III) and a carbon/sulfur analyzer (Eltra CS-800). -
Sedimentation and accumulation rate of sediment core SO202/1_37-2
This dataset has no description
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Sedimentation and accumulation rate of sediment core SO264_55-1
This dataset has no description
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Stable oxagen isotope ratios of benthic foraminifera of sediment core SO264_55-1
Benthic oxygen isotopes were measured on a Thermo Finnigan MAT 253 isotope ratio mass-spectrometer coupled to an automated KIEL IV CARBO preparation device. -
Stable oxagen isotope ratios of benthic foraminifera of sediment core SO202/1...
Benthic oxygen isotopes were measured on a Thermo Finnigan MAT 253 isotope ratio mass-spectrometer coupled to an automated KIEL IV CARBO preparation device. -
Lipid biomarkers and productivity proxies of sediment core AMD16-117Q
Version 2, 2022-03-10: Previous version doi:10.1594/PANGAEA.939224 contains errors due to data processing. -
Lipid biomarkers and productivity proxies of sediment core AMD16-117Q
This dataset has no description
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Statistical analysis of bulk nitrogen isotopes from IODP Site 323-U1342
Here, we present the results of a statistical analysis published in Knudson et al., (2021, Science Advances), which investigates nitrogen isotopes from Integrated Ocean Drilling... -
XRF down-core scanning data, benthic oxygen isotope, sand fraction and geoche...
A meridional transect of deep sea sediment cores from the subarctic Northwest Pacific were retrieved from the Emperor Seamount Chain and Hess Rise during cruises SO202 in 2009... -
Elemental ratios (Ba/Al and Al/Ca) from IODP Site 350-U1437
Selected elemental ratios (Ba/Al and Al/Ca*1000) calculated from individual element abundances in counts per second (cps) as measured via X-ray fluorescence (XRF)-scanning of... -
Fractional abundances of biomarkers from IODP Hole 350-U1437B
The dataset comprises fractional abundances of individual isoprenoid and branched glycerol dialkyl glycerol tetraethers (GDGTs) and C37 alkenones of samples from the past 1 Ma... -
Concentrations of plant wax lipids from IODP Hole 350-U1437B
Concentrations of plant wax lipids (long-chain n-alkanes, n-alcohols, and nonacosan-10-ol), the carbon preference index of n-alkanes, the branched and isoprenoid tetraether... -
Sea surface temperature reconstruction from IODP Hole 350-U1437B
Sea surface temperature data based on the tetraether index based on glycerol dialkyl glycerol tetraethers consisting of 86 carbon atoms (TEX86) and unsaturated ketone index... -
Drake passage cold-water coral ages during NBP cruises NBP11-03 and NBP08-05
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... -
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... -
Biomarker and XRF scanning data from IODP Site 350-U1437B: a study of paleoce...
Sediment core U1437B was drilled during International Ocean Discovery Program Expedition 350 in 2014. The aim of this study was to infer information on the paleoclimatic and...