Fu, Yanzhe (2010): (Fig. 5a) Sulfate (SO4**2-) and iron (Fe**2+) contents in pore water of IODP Hole 308-U1319A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.733341, 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
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Coverage:
Latitude: 27.266252 * Longitude: -94.403180
Minimum DEPTH, sediment/rock: 1.45 m * Maximum DEPTH, sediment/rock: 142.75 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):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
94 data points
Data
| 1 Depth sed [m] | 2 [SO4]2- [mmol/l] | 3 Fe [µmol/l] |
|---|---|---|
| 1.45 | 26.1 | 6.0 |
| 2.95 | 22.6 | 15.2 |
| 4.27 | 21.2 | 13.2 |
| 5.95 | 13.8 | 104.6 |
| 7.37 | 13.6 | 11.4 |
| 8.95 | 8.5 | 17.4 |
| 11.87 | 2.9 | 64.7 |
| 13.45 | 0.5 | 13.6 |
| 15.45 | 0.8 | 18.4 |
| 16.88 | 1.1 | 27.0 |
| 18.45 | 0.4 | 15.3 |
| 19.95 | 0.6 | 19.5 |
| 21.38 | 0.4 | 17.0 |
| 22.95 | 0.4 | 10.8 |
| 23.74 | 0.6 | 7.2 |
| 24.95 | 0.6 | 0.1 |
| 27.95 | 0.6 | 1.1 |
| 29.37 | 0.6 | 0.0 |
| 30.95 | 0.3 | 19.8 |
| 32.45 | 0.3 | 16.1 |
| 33.08 | 0.4 | 2.0 |
| 34.45 | 1.8 | 3.0 |
| 35.95 | 1.4 | 1.3 |
| 37.37 | 1.6 | 25.0 |
| 38.95 | 0.7 | 10.2 |
| 40.45 | 0.7 | 14.5 |
| 41.95 | 0.6 | 34.3 |
| 42.68 | 0.5 | 4.8 |
| 43.95 | 1.0 | 32.5 |
| 45.45 | 0.7 | 22.5 |
| 46.87 | 1.1 | 21.2 |
| 48.45 | 0.6 | 3.9 |
| 49.95 | 0.6 | 47.7 |
| 52.03 | 0.6 | 2.7 |
| 53.45 | 0.9 | 3.1 |
| 54.95 | 1.0 | 2.0 |
| 56.37 | 0.8 | 0.0 |
| 65.87 | 0.8 | 0.3 |
| 76.87 | 0.7 | 4.3 |
| 84.87 | 1.3 | 60.7 |
| 93.07 | 1.4 | 3.7 |
| 102.07 | 1.1 | 0.0 |
| 109.72 | 1.4 | 9.3 |
| 117.46 | 1.7 | 0.0 |
| 123.55 | 2.9 | 17.1 |
| 133.07 | 2.1 | 0.0 |
| 142.75 | 2.5 | 0.0 |