Zabel, Matthias (2002): Phosphate of sediment core GeoB1711-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.87920
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Zabel, Matthias; Dahmke, Andreas; Schulz, Horst D (1998): Regional distribution of diffusive phosphate and silicate fluxes through the sediment–water interface: the eastern South Atlantic. Deep Sea Research Part I: Oceanographic Research Papers, 45(2-3), 277-300, https://doi.org/10.1016/S0967-0637(97)00073-3
Project(s):
Coverage:
Latitude: -23.321667 * Longitude: 12.378333
Date/Time Start: 1992-01-11T00:00:00 * Date/Time End: 1992-01-11T00:00:00
Minimum DEPTH, sediment/rock: 0.250 m * Maximum DEPTH, sediment/rock: 11.000 m
Event(s):
GeoB1711-3 * Latitude: -23.321667 * Longitude: 12.378333 * Date/Time: 1992-01-11T00:00:00 * Elevation: -1963.0 m * Recovery: 11.11 m * Location: Namibia continental slope * Campaign: M20/2 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: Geochemie
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Phosphate | [PO4]3- | µmol/l | Zabel, Matthias | Continuous Flow Analysis (CFA) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
44 data points
Data
| 1 Depth sed [m] | 2 [PO4]3- [µmol/l] |
|---|---|
| 0.250 | 6.53 |
| 0.550 | 6.21 |
| 0.800 | 5.79 |
| 1.000 | 5.48 |
| 1.250 | 5.90 |
| 1.500 | 7.16 |
| 1.750 | 8.21 |
| 2.000 | 9.69 |
| 2.250 | 12.11 |
| 2.500 | 18.32 |
| 2.750 | 19.37 |
| 3.000 | 22.85 |
| 3.250 | 25.90 |
| 3.500 | 28.43 |
| 3.750 | 32.01 |
| 4.000 | 34.54 |
| 4.250 | 38.75 |
| 4.500 | 40.43 |
| 4.750 | 39.59 |
| 5.000 | 39.59 |
| 5.250 | 45.67 |
| 5.500 | 48.63 |
| 5.750 | 48.63 |
| 6.000 | 53.28 |
| 6.250 | 52.86 |
| 6.500 | 52.02 |
| 6.750 | 57.09 |
| 7.000 | 60.05 |
| 7.250 | 61.31 |
| 7.500 | 59.76 |
| 7.750 | 61.81 |
| 8.000 | 66.85 |
| 8.250 | 68.65 |
| 8.500 | 83.50 |
| 8.750 | 81.60 |
| 9.000 | 72.34 |
| 9.250 | 84.45 |
| 9.500 | 81.82 |
| 9.750 | 96.87 |
| 10.000 | 97.82 |
| 10.250 | 85.08 |
| 10.500 | 89.50 |
| 10.750 | 94.13 |
| 11.000 | 88.66 |