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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 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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(Figure 7B) Biogenic opal of sediment core GeoB13862-1
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(Figure 5) Bulk geochemistry of sediment core GeoB13862-1
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(Figure 5) Bulk grain size distribution of sediment core GeoB13862-1
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(Table 2) Accelerator mass spectrometry (AMS) radiocarbon dates and calibrate...
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11 landmark coordinates of Globorotalia inflata oriented in the laterall view...
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