Zabel, Matthias (2002): Phosphate of sediment core GeoB1702-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.87845
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: -6.565000 * Longitude: 10.318333
Date/Time Start: 1992-01-02T00:00:00 * Date/Time End: 1992-01-02T00:00:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 11.80 m
Event(s):
GeoB1702-4 * Latitude: -6.565000 * Longitude: 10.318333 * Date/Time: 1992-01-02T00:00:00 * Elevation: -3083.0 m * Recovery: 12.07 m * Location: Kongo sediment fan * 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:
60 data points
Data
| 1 Depth sed [m] | 2 [PO4]3- [µmol/l] |
|---|---|
| 0.10 | 3.69 |
| 0.30 | 8.21 |
| 0.50 | 8.42 |
| 0.70 | 14.86 |
| 0.90 | 18.42 |
| 1.05 | 22.87 |
| 1.25 | 22.23 |
| 1.45 | 24.14 |
| 1.60 | 24.77 |
| 1.80 | 26.04 |
| 2.00 | 26.03 |
| 2.20 | 26.63 |
| 2.40 | 28.45 |
| 2.60 | 29.05 |
| 2.80 | 29.66 |
| 3.00 | 32.08 |
| 3.20 | 30.26 |
| 3.40 | 33.29 |
| 3.60 | 32.68 |
| 3.80 | 35.10 |
| 4.00 | 35.10 |
| 4.20 | 36.31 |
| 4.40 | 40.55 |
| 4.60 | 37.52 |
| 4.80 | 39.95 |
| 5.00 | 41.92 |
| 5.20 | 40.65 |
| 5.40 | 44.48 |
| 5.60 | 43.19 |
| 5.80 | 47.00 |
| 6.00 | 45.73 |
| 6.20 | 47.00 |
| 6.40 | 50.81 |
| 6.60 | 50.81 |
| 6.80 | 49.54 |
| 7.00 | 50.81 |
| 7.20 | 50.81 |
| 7.40 | 54.47 |
| 7.60 | 53.26 |
| 7.80 | 54.47 |
| 8.00 | 54.47 |
| 8.20 | 56.89 |
| 8.40 | 64.15 |
| 8.60 | 56.89 |
| 8.80 | 54.47 |
| 9.00 | 60.52 |
| 9.20 | 64.15 |
| 9.40 | 62.94 |
| 9.60 | 69.00 |
| 9.80 | 70.21 |
| 10.00 | 66.58 |
| 10.20 | 76.26 |
| 10.40 | 81.10 |
| 10.60 | 83.52 |
| 10.80 | 82.31 |
| 11.00 | 81.10 |
| 11.20 | 84.73 |
| 11.40 | 92.00 |
| 11.60 | 101.62 |
| 11.80 | 97.32 |