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A compilation of published pyrite sulfur isotopic compositions from the past ...
This dataset contains a compilation of the sulfur isotopic composition of pyrite from outcrop and sediment cores over the past 165 million years. The compilation includes 3754... -
Sediment and pore water data of five cores from the continental slope off Uru...
Assessing frequency and extent of mass movement at continental margins is crucial to evaluate risks for offshore constructions and coastal areas. A multidisciplinary approach... -
Sulfate and methane concentrations measured in pore water of sediment core Ge...
Several previous studies have shown that submarine mass-movements can profoundly impact the shape of pore water profiles. Therefore, pore water geochemistry and diffusion models... -
Geochemistry of sediment cores GeoB13820-1 and GeoB13863-1 from the western S...
Here, we present results from sediments collected in the Argentine Basin, a non-steady state depositional marine system characterized by abundant oxidized iron within... -
Stable O and C isotopes of Globorotalia inflata in sediment cores GeoB6209-2,...
Measurements were performed on groups of 3 shells in core GeoB13862-1 and on groups of 3-10 shells in the core top samples using a Thermo MAT 253plus coupled to a Kiel IV device... -
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). -
Counts of Globorotalia inflata genotypes in core GeoB13862-1
Numbers are raw counts done on aliquots containing at least 300 shells. Size fraction 300-1000 μm.Ages from 10.1002/2014PA002677. -
Accelerator mass spectrometry radiocarbon dates and calibrated ages of sedime...
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X-ray flourescence FeK of sediment core GeoB13861-1
X-ray fluorescence (XRF) scans of the sediment cores were performed at 1 cm intervals. We applied generator settings of 10kV, a current of 0.2 mA directly at the split core... -
Total carbon, total oragnic carbon and carbonate contents of sediment core Ge...
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Terrigenous sortable silt of sediment core GeoB13861-1
Sortable silt (10 - 63 µm) arithmetical mean size (SSmean in µm) and percentage (SS%) values can be tightly linked to hydrodynamic processes and can be used as a relative... -
Clay mineral determination of sediment core GeoB13861-1
Device: PANalytical EMPYREAN; CuK[Alpha] radiation (40 kV, 40 mA)Method: Each sample was analyzed between 2.5° and 29° 2 Theta, with a step size of 0.013° in the air-dried state... -
(Figure 4b) Non-linear mapping of surface sediment samples along the continen...
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(Figure 4a) Cluster memberships of surface sediment samples along the contine...
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(Figure 6) Parameters for ratios of rock magnetic and major elements from sur...
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(Figure 6) Rock magnetic and major element ratios presented versus median gra...
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(Figure 3) Grain-size distributions of the terrigenous sediment fraction from...
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(Table 2) Accelerator mass spectrometry radiocarbon dates and calibrated ages...
*: 14C ages being first published in this study.a: Chiessi et al. (2008); Razik et al. (2013), Chiessi et al. (in press).b: Voigt et al. (2013).c: Lantzsch et al. (2014).#:... -
Stable oxygen isotope data of Globorotalia inflata for sediment core GeoB13862-1
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(Figure 3 and Figure 7) X-ray fluorescence scanning of sediment core GeoB13862-1
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