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A summary of consistently dated Atlantic sediment cores over the last 40 thou...
Rapid changes in ocean circulation and climate have been observed in marine-sediment and ice cores over the last glacial period and deglaciation, highlighting the non-linear... -
Stable isotopes of sediment core GeoB6201-5
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Planktonic foraminifera census counts from the western South Atlantic, supple...
Planktonic foraminifera census data have been widely used to reconstruct changes in ocean ecosystems as well as ocean chemistry and circulation through calibration functions.... -
Biogenic opal and diatoms in surface sediments of the South Western Atlantic,...
Based on 66 surface sediment samples collected in the SW Atlantic Ocean between 27 and 50°S, this study presents an overview of the spatial distribution of biogenic opal and... -
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... -
11 landmark coordinates of Globorotalia inflata oriented in the laterall view...
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12 landmark coordinates of Globorotalia inflata oriented in the umbilical view
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16 landmark coordinates of Globorotalia inflata oriented in the lateral view
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(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 GeoB6211...
Composite record GeoB6211 was produced merging the gravity core GeoB6211-2 and the companion multicore GeoB6211-1 [Schulz et al., 2001]. Parts of the 14C ages to produce the age... -
(Table 3) Accelerator mass spectrometry (AMS) radiocarbon dates and calibrate...
a: Radiocarbon laboratory: KIA = Leibniz Laboratory in Kiel (Germany); NOSAMS = National Ocean Sciences Accelerator Mass Spectrometry Facility, Woods Hole Oceanographic... -
(Table 2) Neodymium isotopic data
The age of the samples is calculated based on: (1) detailed age models of Cores GeoB6211-2 and GeoB6308-3 (Fig. 7); and (2) linear age models of Cores GeoB13814-3, GeoB13817-2,... -
(Table 2) Radiocarbon dates and calibrated ages from cores GeoB2107-5 and Geo...
KIA: Leibniz-Laboratory for Radiometric Dating and Stable Isotope Research, Kiel, GermanyPoz: Poznan Radiocarbon Laboratory, Poznan, Poland -
(Figure 3c, 3d, 3e and 3f) Globigerinoides ruber, Globorotalia truncatulinoid...
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Calculated oxygen and silicon benthic fluxes in sediments of the South Atlantic
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