Fu, Yanzhe (2010): (Fig. 5a) Total organic carbon in pore water of IODP Hole 308-U1319A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.733343, In supplement to: Fu, Yanzhe; von Dobeneck, Tilo; Franke, Christine; Heslop, David; Kasten, Sabine (2008): Rock magnetic identification and geochemical process models of greigite formation in Quaternary marine sediments from the Gulf of Mexico (IODP Hole U1319A). Earth and Planetary Science Letters, 275(3-4), 233-245, https://doi.org/10.1016/j.epsl.2008.07.034
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Project(s):
Coverage:
Latitude: 27.266252 * Longitude: -94.403180
Minimum DEPTH, sediment/rock: 1.45 m * Maximum DEPTH, sediment/rock: 152.27 m
Event(s):
308-U1319A * Latitude: 27.266252 * Longitude: -94.403180 * Elevation: -1429.6 m * Recovery: 155.29 m * Campaign: Exp308 (Gulf of Mexico Hydrogeology) * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 18 cores; 157.5 m cored; 98.6 % recovered; 0 m drilled; 157.5 m penetrated
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Carbon, organic, total | TOC | % | Fu, Yanzhe |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
49 data points
Data
| 1 Depth sed [m] | 2 TOC [%] |
|---|---|
| 1.45 | 0.63 |
| 2.95 | 0.23 |
| 4.27 | 0.68 |
| 5.95 | 0.81 |
| 8.95 | 0.87 |
| 10.45 | 0.79 |
| 11.87 | 0.61 |
| 13.45 | 1.06 |
| 15.45 | 0.52 |
| 16.88 | 0.54 |
| 18.45 | 0.70 |
| 19.95 | 0.46 |
| 21.38 | 0.61 |
| 22.95 | 0.34 |
| 23.74 | 0.52 |
| 24.95 | 0.71 |
| 26.45 | 0.76 |
| 27.95 | 0.77 |
| 29.37 | 0.49 |
| 30.95 | 0.57 |
| 32.45 | 0.16 |
| 33.08 | 0.82 |
| 34.45 | 1.90 |
| 35.95 | 0.00 |
| 37.37 | 1.27 |
| 38.95 | 1.03 |
| 40.45 | 0.88 |
| 41.95 | 0.88 |
| 42.68 | 0.93 |
| 43.95 | 0.84 |
| 45.45 | 0.88 |
| 46.87 | 0.96 |
| 48.45 | 1.04 |
| 49.95 | 0.94 |
| 52.03 | 0.93 |
| 53.45 | 1.08 |
| 54.95 | 0.87 |
| 56.37 | 0.81 |
| 65.87 | 0.69 |
| 76.87 | 0.80 |
| 84.87 | 0.77 |
| 93.07 | 0.55 |
| 102.07 | 0.55 |
| 109.72 | 0.53 |
| 117.46 | 0.64 |
| 123.55 | 0.55 |
| 133.07 | 0.56 |
| 142.75 | 0.60 |
| 152.27 | 0.67 |