Stassen, Peter; Thomas, Ellen; Speijer, Robert P (2012): Stable carbon isotope record of sediment core Wilson_Lake [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.824529, In supplement to: Stassen, P et al. (2012): Integrated stratigraphy of the Paleocene-Eocene thermal maximum in the New Jersey Coastal Plain: Toward understanding the effects of global warming in a shelf environment. Paleoceanography, 27(4), PA4210, https://doi.org/10.1029/2012PA002323
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 39.655800 * Longitude: -75.042000
Minimum DEPTH, sediment/rock: 91.78 m * Maximum DEPTH, sediment/rock: 111.05 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Cibicidoides spp., δ13C | Cibicidoides spp. δ13C | ‰ PDB | Stassen, Peter | Isotope ratio mass spectrometry | C. alleni/succedens, size fraction 125-630 µm |
3 | Anomalinoides acuta, δ13C | A. acuta δ13C | ‰ PDB | Stassen, Peter | Isotope ratio mass spectrometry | size fraction 125-630 µm |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
62 data points
Data
1 Depth sed [m] | 2 Cibicidoides spp. δ13C [‰ PDB] | 3 A. acuta δ13C [‰ PDB] |
---|---|---|
91.78 | -1.45 | |
92.38 | -0.87 | -1.37 |
92.99 | -1.42 | -1.51 |
93.60 | -0.55 | |
93.60 | -1.19 | |
93.60 | -1.12 | |
94.82 | -1.25 | |
96.04 | -0.98 | -2.40 |
96.65 | -2.94 | |
97.26 | -2.80 | |
98.18 | -3.08 | |
98.79 | -3.05 | |
99.40 | -3.82 | |
99.40 | -4.19 | |
100.00 | -3.21 | |
100.61 | -3.29 | |
101.22 | -2.99 | |
101.83 | -3.04 | |
102.44 | -3.29 | |
103.05 | -3.01 | |
103.66 | -3.48 | |
103.66 | -3.45 | |
104.58 | -3.22 | |
105.19 | -2.91 | |
105.80 | -3.09 | |
106.41 | -3.33 | |
107.02 | -3.64 | |
107.09 | -3.45 | |
107.18 | -3.29 | |
107.32 | -3.75 | |
107.32 | -3.77 | |
107.40 | -3.19 | |
107.49 | -3.32 | |
107.62 | -3.28 | |
107.70 | -3.17 | |
107.79 | -3.21 | |
107.93 | -3.39 | |
108.01 | -3.31 | |
108.23 | -3.39 | |
108.40 | -3.23 | |
108.40 | -3.41 | |
108.54 | -3.26 | |
108.62 | -3.17 | |
108.71 | -3.09 | |
108.84 | -3.40 | |
108.92 | -3.22 | |
109.01 | -3.12 | |
109.15 | -2.89 | |
109.45 | -2.98 | -3.14 |
110.06 | 0.20 | |
110.14 | 0.52 | |
110.37 | 0.87 | |
110.37 | 0.70 | |
110.44 | 0.35 | |
110.67 | 0.75 | 0.36 |
110.84 | 0.48 | |
111.05 | 0.91 |