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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Project(s):
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):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | Zhang, Yancheng | |||
2 | DEPTH, sediment/rock | Depth sed | m | Zhang, Yancheng | Geocode | |
3 | Laboratory code/label | Lab label | Zhang, Yancheng | |||
4 | Neodymium | Nd | mg/kg | Zhang, Yancheng | ppm | |
5 | Neodymium-143/Neodymium-144 ratio | 143Nd/144Nd | Zhang, Yancheng | |||
6 | Neodymium-143/Neodymium-144 ratio, error | 143Nd/144Nd e | ± | Zhang, Yancheng | 2 Sigma (×10**-6) | |
7 | ε-Neodymium | ε-Nd | Zhang, Yancheng | Calculated | ||
8 | Age, dated | Age dated | ka | Zhang, Yancheng | Age, 14C AMS | |
9 | Age, comment | Comm | Zhang, Yancheng |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
240 data points
Data
1 Event | 2 Depth sed [m] | 3 Lab label | 4 Nd [mg/kg] | 5 143Nd/144Nd | 6 143Nd/144Nd e [±] | 7 ε-Nd | 8 Age dated [ka] | 9 Comm |
---|---|---|---|---|---|---|---|---|
GeoB16206-1 | 0.10 | 5 | 13.811 | 0.511742 | 4 | -17.47 | 1.2 | |
GeoB16206-1 | 0.90 | 6 | 8.2 | |||||
GeoB16206-1 | 1.80 | 7 | 32.474 | 0.511783 | 17 | -16.69 | 9.9 | |
GeoB16206-1 | 2.50 | 8 | 61.563 | 0.511757 | 14 | -17.19 | 11.3 | |
GeoB16206-1 | 2.90 | 9 | 44.070 | 0.511715 | 17 | -18.01 | 11.9 | |
GeoB16206-1 | 3.30 | 10 | 56.521 | 0.511744 | 14 | -17.44 | 12.6 | |
GeoB16206-1 | 3.66 | 11 | 32.153 | 0.511746 | 15 | -17.40 | 13.3 | |
GeoB16206-1 | 3.80 | 12 | 13.8 | |||||
GeoB16206-1 | 3.96 | 13 | 31.125 | 0.511742 | 10 | -17.48 | 14.4 | |
GeoB16206-1 | 4.50 | 14 | 51.044 | 0.511694 | 13 | -18.42 | 15.1 | |
GeoB16206-1 | 5.36 | 15 | 58.363 | 0.511720 | 11 | -17.91 | 16.3 | |
GeoB16206-1 | 6.20 | 16 | 49.164 | 0.511766 | 7 | -17.00 | 17.8 | |
GeoB16206-1 | 6.70 | 17 | 33.090 | 0.511783 | 14 | -16.67 | 19.6 | |
GeoB16206-1 | 7.15 | SPS7981 | 0.511760 | 8 | -17.12 | 24.6 | ||
GeoB16206-1 | 7.22 | SPS7982 | 0.511775 | 8 | -16.84 | 25.0 | ||
GeoB16206-1 | 7.27 | SPS7983 | 0.511774 | 8 | -16.85 | 25.3 | ||
GeoB16206-1 | 7.36 | 18 | 52.981 | 0.511788 | 17 | -16.58 | 25.8 | |
GeoB16206-1 | 7.80 | 19 | 35.725 | 0.511785 | 19 | -16.64 | 28.3 | |
GeoB16224-1 | 0.10 | SPS7966 | 0.512042 | 9 | -11.62 | 5.3 | ||
GeoB16224-1 | 0.40 | SPS7967 | 0.512065 | 11 | -11.18 | 6.0 | ||
GeoB16224-1 | 0.70 | SPS8071 | 0.512052 | 8 | -11.44 | 12.9 | ||
GeoB16224-1 | 1.00 | SPS7969 | 0.512034 | 7 | -11.78 | 14.1 | ||
GeoB16224-1 | 1.30 | SPS7970 | 0.512039 | 11 | -11.68 | 15.7 | ||
GeoB16224-1 | 1.60 | SPS7971 | 0.512011 | 8 | -12.22 | 17.0 | ||
GeoB16224-1 | 1.90 | SPS7972 | 0.512042 | 8 | -11.63 | 18.2 | ||
GeoB16224-1 | 2.20 | SPS7973 | 0.512050 | 7 | -11.47 | 19.7 | ||
GeoB16224-1 | 2.50 | SPS7974 | 0.512062 | 8 | -11.23 | 21.2 | ||
GeoB16224-1 | 2.80 | SPS7975 | 0.512052 | 8 | -11.44 | 22.4 | ||
GeoB16224-1 | 3.10 | SPS7976 | 0.512042 | 10 | -11.62 | 23.7 | ||
GeoB16224-1 | 3.40 | SPS7977 | 0.512044 | 8 | -11.59 | 25.2 | ||
GeoB16224-1 | 3.70 | SPS7978 | 0.512068 | 7 | -11.11 | 26.5 | ||
GeoB16224-1 | 4.00 | SPS7979 | 0.512062 | 8 | -11.23 | 27.7 | ||
GeoB16224-1 | 4.30 | SPS7980 | 0.512034 | 9 | -11.78 | 29.6 | ||
GeoB16203-1 | 0.10 | 2 | 8.816 | 0.511796 | 17 | -16.42 | 1.5 | |
GeoB16204-2 | 0.10 | 3 | 8.308 | 0.511743 | 22 | -17.46 | Late Holocene | |
GeoB16205-4 | 0.10 | 4 | 13.317 | 0.511782 | 15 | -16.69 | 1.5 | |
GeoB16211-3 | 0.10 | 20 | 18.763 | 0.512173 | 18 | -9.07 | Late Holocene | |
GeoB16212-3 | 0.10 | 21 | 33.504 | 0.512066 | 11 | -11.15 | Late Holocene | |
GeoB16216-3 | 0.10 | 22 | 24.580 | 0.512053 | 14 | -11.41 | Mid-Holocene | |
GeoB16217-2 | 0.10 | 23 | 32.237 | 0.512073 | 17 | -11.02 | Mid-Holocene | |
GeoB16218-4 | 0.10 | 24 | 39.680 | 0.512094 | 18 | -10.61 | Late Holocene | |
GeoB16219-2 | 0.10 | 25 | 35.613 | 0.512179 | 19 | -8.96 | Late Holocene | |
GeoB16220-1 | 0.10 | 26 | Late Holocene | |||||
GeoB16222-1 | 0.10 | 27 | 19.566 | 0.512111 | 20 | -10.28 | Mid-Holocene | |
GeoB16223-2 | 0.10 | 28 | 34.182 | 0.512072 | 12 | -11.04 | Mid-Holocene |