Dählmann, Anke (2001): Geochemistry on sediment core PS47/086-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.61399
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Dählmann, Anke (2001): Geochemische Untersuchungen an hydrothermal beeinflußten Sedimenten der Bransfield Straße (Antarktis) (Geochemical investigation on hydrothermally influenced sediments of Bransfield Strait (Antarctica)). Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 392, 157 pp, https://doi.org/10.2312/BzPM_0392_2001
Project(s):
Coverage:
Latitude: -62.274333 * Longitude: -57.550500
Date/Time Start: 1997-12-18T13:48:00 * Date/Time End: 1997-12-18T15:40:00
Minimum DEPTH, sediment/rock: 0.060 m * Maximum DEPTH, sediment/rock: 8.550 m
Event(s):
PS47/086-2 (SL86) * Latitude: -62.274333 * Longitude: -57.550500 * Date/Time Start: 1997-12-18T13:48:00 * Date/Time End: 1997-12-18T15:40:00 * Elevation: -2009.0 m * Recovery: 8.67 m * Location: South Atlantic Ocean * Campaign: ANT-XV/2 (PS47) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sulfur, total | TS | % | Dählmann, Anke | Element analyser CNS, Carlo Erba NA1500 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
35 data points
Data
1 Depth sed [m] | 2 TS [%] |
---|---|
0.060 | 0.18 |
0.200 | 0.15 |
0.400 | 0.12 |
0.560 | 0.31 |
0.800 | 0.33 |
1.000 | 0.32 |
1.250 | 0.35 |
1.500 | 0.34 |
1.750 | 0.34 |
2.250 | 0.34 |
2.500 | 0.34 |
2.750 | 0.34 |
3.000 | 0.32 |
3.250 | 0.32 |
3.500 | 0.31 |
3.750 | 0.30 |
4.070 | 0.37 |
4.280 | 0.38 |
4.550 | 0.53 |
4.800 | 0.13 |
5.050 | 0.40 |
5.300 | 0.47 |
5.680 | 0.13 |
5.900 | 0.16 |
6.120 | 0.35 |
6.350 | 0.17 |
6.640 | 0.16 |
6.800 | 0.46 |
7.030 | 0.47 |
7.300 | 0.30 |
7.600 | 0.23 |
7.850 | 0.25 |
8.100 | 0.27 |
8.300 | 0.29 |
8.550 | 0.30 |