Stein, Ruediger; Fahl, Kirsten (2004): Total organic carbon of sediment core BP00-14/04 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.136943
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Stein, Ruediger; Fahl, Kirsten (2004): The Kara Sea: Distribution, sources, variability and burial of organic carbon. In: Stein, R & Macdonald, R W (Eds.), The Organic Carbon Cycle in the Arctic Ocean, Springer-Verlag, Berlin, 213-237
Project(s):
Siberian River Run-Off (SIRRO)
Coverage:
Latitude: 72.930883 * Longitude: 79.789683
Date/Time Start: 2000-09-09T17:48:00 * Date/Time End: 2000-09-09T17:48:00
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 2.35 m
Event(s):
BP00-14/04 * Latitude: 72.930883 * Longitude: 79.789683 * Date/Time: 2000-09-09T17:48:00 * Elevation: -19.2 m * Recovery: 2.56 m * Location: Kara Sea * Campaign: BP00 * Basis: Akademik Boris Petrov * Method/Device: Gravity corer (GC) * Comment: gravity corer 5 m
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Carbon, organic, total | TOC | % | Stein, Ruediger | Element analyser CHN, LECO |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
47 data points
Data
1 Depth sed [m] | 2 TOC [%] |
---|---|
0.05 | 1.3400 |
0.10 | 1.6770 |
0.15 | 1.4840 |
0.20 | 1.4460 |
0.25 | 1.4780 |
0.30 | 1.6440 |
0.35 | 1.5020 |
0.40 | 1.4420 |
0.45 | 1.4850 |
0.50 | 1.4850 |
0.55 | 1.5340 |
0.60 | 1.4630 |
0.65 | 1.5570 |
0.70 | 1.4480 |
0.75 | 1.3960 |
0.80 | 1.2540 |
0.85 | 1.1010 |
0.90 | 1.4970 |
0.95 | 1.5740 |
1.00 | 1.3930 |
1.05 | 1.1740 |
1.10 | 1.4710 |
1.15 | 1.4080 |
1.20 | 1.4820 |
1.25 | 1.0760 |
1.30 | 1.4500 |
1.35 | 1.1600 |
1.40 | 1.4420 |
1.45 | 1.3550 |
1.50 | 1.2700 |
1.55 | 1.2780 |
1.60 | 1.4570 |
1.65 | 1.1710 |
1.70 | 1.2070 |
1.75 | 1.0360 |
1.80 | 0.9029 |
1.85 | 1.0190 |
1.90 | 1.1010 |
1.95 | 1.2310 |
2.00 | 1.0530 |
2.05 | 0.9364 |
2.10 | 1.1190 |
2.15 | 1.0380 |
2.20 | 1.3060 |
2.25 | 1.3060 |
2.30 | 2.9370 |
2.35 | 1.1150 |