Zabel, Matthias (2002): Phosphate of sediment core GeoB1720-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.87925
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: -28.995000 * Longitude: 13.840000
Date/Time Start: 1992-01-16T00:00:00 * Date/Time End: 1992-01-16T00:00:00
Minimum DEPTH, sediment/rock: 0.250 m * Maximum DEPTH, sediment/rock: 9.150 m
Event(s):
GeoB1720-1 * Latitude: -28.995000 * Longitude: 13.840000 * Date/Time: 1992-01-16T00:00:00 * Elevation: -2006.0 m * Recovery: 9.35 m * Location: Namibia continental slope * Campaign: M20/2 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: Geochemie, Karbonatschl., H2S
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:
37 data points
Data
| 1 Depth sed [m] | 2 [PO4]3- [µmol/l] |
|---|---|
| 0.250 | 7.30 |
| 0.500 | 8.66 |
| 0.750 | 9.90 |
| 1.000 | 10.01 |
| 1.250 | 9.65 |
| 1.500 | 10.39 |
| 1.750 | 9.40 |
| 2.000 | 11.33 |
| 2.250 | 12.58 |
| 2.500 | 13.43 |
| 2.750 | 13.85 |
| 3.000 | 15.52 |
| 3.250 | 16.57 |
| 3.500 | 17.83 |
| 3.750 | 18.04 |
| 4.000 | 18.46 |
| 4.250 | 18.46 |
| 4.500 | 19.91 |
| 4.750 | 18.35 |
| 5.000 | 20.31 |
| 5.250 | 20.31 |
| 5.500 | 20.31 |
| 5.750 | 19.52 |
| 6.000 | 19.52 |
| 6.250 | 21.48 |
| 6.500 | 22.73 |
| 6.750 | 22.65 |
| 7.000 | 21.87 |
| 7.250 | 23.43 |
| 7.500 | 26.75 |
| 7.750 | 27.16 |
| 8.000 | 26.75 |
| 8.250 | 27.16 |
| 8.500 | 27.58 |
| 8.750 | 29.25 |
| 9.000 | 29.25 |
| 9.150 | 28.00 |