Moore, T S; Murray, Richard W; Kurtz, A C; Schrag, Daniel P (2004): (Table 1) Stable carbon isotope composition of dissolved inorganic carbon from ODP Site 175-1082 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.714832, In supplement to: Moore, TS et al. (2004): Anaerobic methane oxidation and the formation of dolomite. Earth and Planetary Science Letters, 229(1-2), 141-154, https://doi.org/10.1016/j.epsl.2004.10.015
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -21.094194 * Longitude: 11.820556
Date/Time Start: 1997-09-13T00:00:00 * Date/Time End: 1997-09-13T00:00:00
Minimum DEPTH, sediment/rock: 1.40 m * Maximum DEPTH, sediment/rock: 489.05 m
Event(s):
175-1082 * Latitude: -21.094194 * Longitude: 11.820556 * Date/Time: 1997-09-13T00:00:00 * Elevation: -1280.6 m * Penetration: 929.6 m * Recovery: 853 m * Location: Benguela Current, South Atlantic Ocean * Campaign: Leg175 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 102 cores; 929.6 m cored; 0 m drilled; 91.8% recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | δ13C, dissolved inorganic carbon | δ13C DIC | ‰ PDB | Moore, T S | Isotope ratio mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
50 data points
Data
| 1 Depth sed [m] | 2 δ13C DIC [‰ PDB] |
|---|---|
| 1.40 | -2.23 |
| 2.90 | -4.02 |
| 4.40 | -7.27 |
| 7.53 | -13.06 |
| 9.20 | -14.47 |
| 10.70 | -16.24 |
| 12.10 | -16.18 |
| 13.50 | -18.07 |
| 14.90 | -17.85 |
| 16.25 | -19.03 |
| 18.55 | -20.46 |
| 19.95 | -19.91 |
| 21.35 | -19.17 |
| 22.75 | -13.43 |
| 25.55 | -9.42 |
| 28.05 | -5.63 |
| 29.45 | -3.60 |
| 30.85 | -5.43 |
| 32.25 | -2.35 |
| 33.65 | -1.50 |
| 35.05 | 1.96 |
| 37.55 | 1.17 |
| 38.95 | 1.96 |
| 40.35 | 2.34 |
| 41.75 | 2.67 |
| 43.15 | 3.39 |
| 44.55 | 4.04 |
| 47.05 | 4.94 |
| 48.45 | 8.12 |
| 49.85 | 6.51 |
| 51.35 | 7.60 |
| 52.75 | 6.16 |
| 59.65 | 8.57 |
| 78.45 | 10.59 |
| 88.39 | 10.91 |
| 97.50 | 12.22 |
| 107.04 | 13.01 |
| 131.07 | 13.88 |
| 160.10 | 13.28 |
| 189.77 | 13.04 |
| 219.61 | 12.56 |
| 248.75 | 12.35 |
| 277.65 | 11.78 |
| 306.49 | 11.41 |
| 334.04 | 11.20 |
| 365.04 | 10.32 |
| 392.34 | 9.89 |
| 420.55 | 8.74 |
| 461.61 | 6.72 |
| 489.05 | 5.95 |