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Carbon and oxygen isotope literature data for foraminifera from ODP Site 197-...
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Pb-Pb and trace element analyses of detrital feldspars from sediment core IN2...
Pb-Pb ratios, ages and trace element data from detrital feldspars in kasten core IN2017_V01-A042-KC14 from the continental slope of central Wilkes Land, East Antarctica and... -
Abundance of Prokaryotes in deep-sea sediments analyzed by CARD-FISH
We fixed 0.5 g aliquots of sediment with a 4% formaldehyde solution for 2-4 h, washed the fixed sediments three times with 1x phosphate-buffered saline (PBS), before storing... -
(Table 3) Protist occurrence in bottom sea ice and surface water samples obta...
X = found, - = not found. -
(Table 9.4.4) Rates of microbial processes in hot and warm hydrothermal solut...
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(Table 7b) Azide, ammonium chloride and thiosulfate influences on carbon-14 d...
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(Table 7a) Azide, sulfide, ammonium chloride and thiosulfate influences on ca...
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(Table 5) Carbon-14 dioxide assimilation rate in bottom sediments from the Br...
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(Table 3) Carbon-14 dioxide assimilation rate in water samples from the Broke...
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(Table 7) Rates of microbiological processes in hot and warm solutions within...
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Mineralogical and geochemical characterisation of iron-sulfur deposits from t...
In this dataset, seven inactive massive sulfide chimneys, collected in the Manus Basin (Bismarck Sea, Papua New Guinea, SW Pacific) during SONNE cruise SO216 in 2011, are... -
Table S1. Past Himalayan erosion from Bengal Fan: Sample information, dating,...
Samples from the Bengal Fan and Lower Meghna River were measured. Each line gives the 10Be measurement result for one aliquot of the sample in a specific granulometric sandy... -
Global soil and peat branched GDGT compilation dataset, supplement to: Dearin...
Accurate temperature records for the deep geological past are a vital component of paleoclimate research. Distributional changes of branched glycerol dialkyl glycerol tetraether... -
Eocene-Oligocene paleomagnetic and foraminiferal stable isotopic and Mg/Ca re...
The Eocene-Oligocene transition (EOT) marked the initiation of large-scale Antarctic glaciation. This fundamental change in Cenozoic climate state is recorded in deep-sea... -
Sterol, n-alcohol and n-alkane composition of living fen plants, supplement t...
In groundwater-fed fen peatlands, the surface biomass decays rapidly and, as a result, highly humified peat is formed. A high degree of humification constrains palaeoecological... -
(Table 1) Chemical and isotopic compositions of rudist aragonite and magnesia...
The classic paleotemperature record based on d18O data from pelagic foraminiferal calcite suggests that equatorial sea-surface temperatures during the Maastrichtian (~12-20°C)... -
(Table 1) Strontium isotope ratios of planktonic foraminifera and ostracoda f...
Stable and radiogenic isotopic and sedimentological data from sub-Antarctic deep sea sediment cores reveal a temporal link between changes in seawater 87Sr/86Sr ratios and major... -
(Table S3) Lead isotopic data for clinopyroxene and groudmass from Wudi, clin...
C, core. R, rim.Reference values for standard BHVO-2G are taken from source (https://crustal.usgs.gov/geochemical_reference_standards/). -
(Table 1) Major and trace elements from the Jorullo volcano in the Michoacan ...
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Radiogenic neodymium composition of surface sediments from the Arctic Ocean
This dataset has no description