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Zhang, Yancheng; Chiessi, Cristiano Mazur; Mulitza, Stefan; Zabel, Matthias; Trindade, Ricardo F; Hollanda, Maria Helena B M; Dantas, Elton L; Govin, Aline; Tiedemann, Ralf; Wefer, Gerold (2015): (Table S2, Figure 3a) Sr-Nd isotopic compositions of sediment cores drilled during MSM20/3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.854052, In supplement to: Zhang, Y et al. (2015): Origin of increased terrigenous supply to the NE South American continental margin during Heinrich Stadial 1 and the Younger Dryas. Earth and Planetary Science Letters, 432, 493-500, https://doi.org/10.1016/j.epsl.2015.09.054

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Coverage:
Median Latitude: 3.215345 * Median Longitude: -48.707917 * South-bound Latitude: -2.035167 * West-bound Longitude: -52.116500 * North-bound Latitude: 6.656333 * East-bound Longitude: -41.718500
Date/Time Start: 2012-02-22T18:07:00 * Date/Time End: 2012-03-08T16:07:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 7.80 m
Event(s):
GeoB16203-1 (054-1) * Latitude: -2.035167 * Longitude: -41.718500 * Date/Time: 2012-02-22T18:07:00 * Elevation: -1591.0 m * Location: Continental Slope Northeast Brazil * Campaign: MSM20/3 (AMADEUS) * Basis: Maria S. Merian * Method/Device: Gravity corer (Kiel type) (SL) * Comment: Geology, 858 cm, ~10 sediment lost from top
GeoB16204-2 (055-2) * Latitude: -1.995833 * Longitude: -42.338500 * Date/Time: 2012-02-23T00:50:00 * Elevation: -1211.0 m * Recovery: 2.77 m * Location: Continental Slope Northeast Brazil * Campaign: MSM20/3 (AMADEUS) * Basis: Maria S. Merian * Method/Device: Gravity corer (Kiel type) (SL) * Comment: Geology, 277 cm
GeoB16205-4 (056-4) * Latitude: -1.351833 * Longitude: -43.096667 * Date/Time: 2012-02-23T23:32:00 * Elevation: -1955.0 m * Recovery: 6.2 m * Location: Continental Slope Northeast Brazil * Campaign: MSM20/3 (AMADEUS) * Basis: Maria S. Merian * Method/Device: Gravity corer (Kiel type) (SL) * Comment: Geology, 620 cm
Comment:
SPS + Numbers: measured at CPGeo, University of São Paulo; Numbers: measured at the Laboratory of Geochronology, University of Brasília.
The ages are calibrated by the available 14C-AMS dates (i.e. core GeoB16206-1 and GeoB16224-1), while others (i.e., late Holocene, Mid-Holocene ) are roughly estimated by 14C-constrained age model of sediment cores nearby and/or water depth at which the sediment core was raised.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventZhang, Yancheng
2DEPTH, sediment/rockDepth sedmZhang, YanchengGeocode
3Laboratory code/labelLab labelZhang, Yancheng
4NeodymiumNdmg/kgZhang, Yanchengppm
5Neodymium-143/Neodymium-144 ratio143Nd/144NdZhang, Yancheng
6Neodymium-143/Neodymium-144 ratio, error143Nd/144Nd e±Zhang, Yancheng2 Sigma (×10**-6)
7ε-Neodymiumε-NdZhang, YanchengCalculated
8Age, datedAge datedkaZhang, YanchengAge, 14C AMS
9Age, commentCommZhang, Yancheng
Size:
240 data points

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