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Stable isotope record of foraminifera from the Southern Ocean
Sediment cores from the southern continental margin of Australia are near the formation region of Antarctic Intermediate Water (AAIW) and Subantarctic Mode Water and record the... -
Biogenic opal, carbonat concentrations and stable oxygen isotope ratios of fo...
We present records of biogenic opal percentage and burial rate in 12 piston cores from the Atlantic and Indian sectors of the Southern Ocean. These records provide a detailed,... -
Estimates of annual mean surface temperatures in the late Quaternary of the t...
At least two modes of glacial-interglacial climate change have existed within the tropical Atlantic Ocean during the last 20,000 years. The first mode (defined by cold glacial... -
UK'37 and UK'37-derived SST of sediment cores GeoB22230-1 from R/V SONNE expe...
UK'37 and -derived SST estimates of sediment core SO256_30-1 (GeoB22230-1). Sample preparation and measurements were done at the German Federal Institute for Geosciences and... -
Planktic foraminiferal oxygen isotopes, Mg/Ca and Mg/Ca-derived SST estimates...
Planktic foraminiferal oxygen isotopes, Mg/Ca and Mg/Ca-derived SST estimates of sediment core SO256_30-1 (GeoB22230-1). Oxygen isotope analyses were carried out by the isotope... -
UK'37 and UK'37-derived SST of sediment cores GeoB22229-1 from R/V SONNE expe...
UK'37 and -derived SST estimates of sediment core SO256_29-1 (GeoB22229-1). Sample preparation and measurements were done at the German Federal Institute for Geosciences and... -
Planktic foraminiferal oxygen isotopes, Mg/Ca and Mg/Ca-derived SST estimates...
Planktic foraminiferal oxygen isotopes, Mg/Ca and Mg/Ca-derived SST estimates of sediment core SO256_29-1 (GeoB22229-1). Oxygen isotope analyses were carried out by the isotope... -
Age control points of sediment cores GeoB22229-1 and GeoB22230-1 from R/V SON...
Tie points used to create the age-depth models of sediment core SO256_29-1 (GeoB22229-1) and SO256_30-1 (GeoB22230-1). The tie points are based on the alignment of the G. ruber... -
AMS 14C ages and calibrated calendar ages of sediment core GeoB22229-1 from R...
AMS-14C ages and calibrated calendar ages, reported as median probability ages. AMS 14C dating was performed at the Analytical Center for Environmental Science, Atmosphere and... -
Sub-decadal diatom oxygen isotope record of the last 220 years (2015-1790CE) ...
The dataset includes diatom oxygen isotope data for 39 samples from short core EN18232-1, Lake Khamra, and corresponding key geochemical characteristics of the purified lake... -
A global compilation of diatom silica oxygen isotope records from lake sedime...
Oxygen isotopes in biogenic silica (δ18O BSi) from lake sediments allow for quantitative reconstruction of past hydroclimate and proxy–model comparison in terrestrial... -
A global compilation of diatom silica oxygen isotope records from lake sedime...
Oxygen isotopes in biogenic silica (δ18O BSi) from lake sediments allow for quantitative reconstruction of past hydroclimate and proxy–model comparison in terrestrial... -
Bulk mineral assemblage of surface sediment samples from Svalbard fjord systems
This dataset has no description
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Bulk mineral assemblage of sediment core HH17-1106-GC
This dataset has no description
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Bulk mineral assemblage of sediment core HH17-1100-GC
This dataset has no description
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Bulk mineral assemblage of sediment core HH17-1094-GC
This dataset has no description
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Bulk mineral assemblage of sediment core HH17-1085-GC
This dataset has no description
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Relative intensity and age depostion range in the north of the South China Se...
Relative intensity (RPI) was constructed using the equation:RPI=NRM((20-60)mT)/SIRM (20-60)mTwhere SIRM were imparted with DC fields of 1000 mT, then demagnetized using 20,... -
Bulk chemistry measurements and XRF spectra of sediments from the high latitu...
This dataset has no description
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Age model analyses from sediment core GeoB13862-1
Age models are based on 14C AMS ages. For sediment core GeoB13862-1 we used the ages originally published in Voigt et al. (2013, doi:10.1016/j.margeo.2013.05.002).