Winn, Kyaw (2016): Stable isotope ratios on planktonic and benthic foraminifera in sediment core U306 from the Manihiki Plateau, tropical Southwest Pacific [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.859006
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Winn, Kyaw; Zheng, Lianfu; Stoffers, Peter; Erlenkeuser, Helmut (1992): Stable oxygen/carbon isotopes and paleoproductivity in the South China Sea during the past 110,000 years. In: Jin Xiang- long, Hermann Rudolf Kudrass & Guy Pautot (eds), Marine Geology and Geophysics of the South China Sea. China Ocean Press, Hangzhou, China, 154-166, hdl:10013/epic.46006.d001
Project(s):
Coverage:
Latitude: -12.618000 * Longitude: -162.685000
Minimum DEPTH, sediment/rock: 0.005 m * Maximum DEPTH, sediment/rock: 2.100 m
Event(s):
U306 * Latitude: -12.618000 * Longitude: -162.685000 * Elevation: -2460.0 m * Location: Manihiki Plateau, Pacific Ocean * Method/Device: Gravity corer (GC)
Comment:
Sample at depth 2.1 m is from core catcher.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Winn, Kyaw | Geocode | |
2 | Globigerinoides ruber white, δ18O | G. ruber w δ18O | ‰ PDB | Winn, Kyaw | Isotope ratio mass spectrometry | |
3 | Globigerinoides ruber white, δ13C | G. ruber w δ13C | ‰ PDB | Winn, Kyaw | Isotope ratio mass spectrometry | |
4 | Globigerinoides sacculifer, δ18O | G. sacculifer δ18O | ‰ PDB | Winn, Kyaw | Isotope ratio mass spectrometry | |
5 | Globigerinoides sacculifer, δ13C | G. sacculifer δ13C | ‰ PDB | Winn, Kyaw | Isotope ratio mass spectrometry | |
6 | Cibicides wuellerstorfi, δ18O | C. wuellerstorfi δ18O | ‰ PDB | Winn, Kyaw | Isotope ratio mass spectrometry | |
7 | Cibicides wuellerstorfi, δ13C | C. wuellerstorfi δ13C | ‰ PDB | Winn, Kyaw | Isotope ratio mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
108 data points
Data
1 Depth sed [m] | 2 G. ruber w δ18O [‰ PDB] | 3 G. ruber w δ13C [‰ PDB] | 4 G. sacculifer δ18O [‰ PDB] | 5 G. sacculifer δ13C [‰ PDB] | 6 C. wuellerstorfi δ18O [‰ PDB] | 7 C. wuellerstorfi δ13C [‰ PDB] |
---|---|---|---|---|---|---|
0.005 | -1.60 | 1.83 | -1.16 | 2.10 | 3.45 | 0.13 |
0.060 | -1.45 | 1.79 | -1.41 | 1.89 | 3.72 | 0.22 |
0.200 | -1.23 | 1.81 | -1.34 | 1.68 | 3.76 | 0.16 |
0.300 | -1.14 | 1.81 | -0.97 | 2.07 | 3.62 | 0.25 |
0.400 | -1.48 | 2.03 | -1.24 | 2.28 | 3.44 | 0.29 |
0.600 | -1.26 | 1.55 | -1.17 | 1.80 | 3.58 | 0.01 |
0.800 | -1.38 | 1.53 | -1.09 | 1.86 | 3.62 | -0.04 |
1.000 | -1.40 | 1.64 | -1.21 | 1.93 | 3.35 | 0.11 |
1.150 | -1.22 | 1.66 | -0.75 | 1.82 | 3.53 | 0.02 |
1.200 | -1.17 | 1.67 | -0.90 | 1.91 | 3.50 | 0.07 |
1.250 | -1.22 | 1.91 | -1.08 | 1.86 | 3.40 | -0.04 |
1.300 | -1.35 | 1.79 | -1.13 | 2.03 | 3.51 | -0.02 |
1.400 | -1.30 | 1.65 | -1.21 | 1.88 | 3.66 | -0.07 |
1.500 | -1.01 | 1.77 | -1.04 | 1.83 | 3.58 | 0.05 |
1.600 | -1.33 | 1.88 | -1.03 | 2.13 | 3.51 | 0.06 |
1.800 | -1.46 | 1.77 | -1.00 | 1.92 | 3.54 | 0.20 |
2.000 | -1.31 | 2.17 | -1.12 | 2.40 | 3.27 | 0.46 |
2.100 | -1.53 | 1.73 | -0.85 | 2.00 | 3.36 | 0.43 |