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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... -
Planktonic foraminifera census counts from the western South Atlantic
Planktonic foraminifera census data have been widely used to reconstruct changes in ocean ecosystems as well as ocean chemistry and circulation through calibration functions.... -
(Table 1) Elemental composition of benthic foraminifera from South Atlantic c...
The ocean plays a major role in the global carbon cycle, and attempts to reconstruct past changes in the marine carbonate system are increasing. The speciation of dissolved... -
Magnesium/Calcium ratios in benthic foraminifera from surface sediments
We used modern epibenthic foraminifer tests of Cibicidoides mundulus and Planulina wuellerstorfi from South Atlantic core top sediments in order to establish Mg/Ca-temperature... -
Age model analyses from sediment core GeoB6308-1 and GeoB6308-3
Age models are based on 14C AMS ages. For sediment core GeoB6308-1 and GeoB6308-3 we used the ages originally published by Lantzsch et al. (2014,... -
(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 GeoB6308-3
Composite record GeoB6308 was produced merging the gravity core GeoB6308-3 and the companion multicore GeoB6308-1 [Bleil et al., 2001]. The age model for GeoB6308 is based on... -
(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,... -
Sample locations, stratigraphic information and listing of carbon and oxygen ...
We explored the potential to use the stable isotopic compositions of planktonic foraminifera as a proxy for the position of the Brazil-Malvinas Confluence (BMC) in the Argentine... -
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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Table 1. Surface sample locations, G. inflata δ¹⁸O, Mg/Ca, apparent calcifica...
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Modern major element concentrations and ratios measured in Atlantic surface s...
Numerous studies use major element concentrations measured on continental margin sediments to reconstruct terrestrial climate variations. The choice and interpretation of...
