Stein, Ruediger; Fahl, Kirsten (2004): Total organic carbon of sediment core BP00-35/06 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.136955
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: 75.347117 * Longitude: 83.801433
Date/Time Start: 2000-09-18T09:43:00 * Date/Time End: 2000-09-18T09:43:00
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 2.55 m
Event(s):
BP00-35/06 * Latitude: 75.347117 * Longitude: 83.801433 * Date/Time: 2000-09-18T09:43:00 * Elevation: -46.0 m * Recovery: 2.58 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:
51 data points
Data
1 Depth sed [m] | 2 TOC [%] |
---|---|
0.05 | 1.1180 |
0.10 | 0.8541 |
0.15 | 0.9254 |
0.20 | 0.9277 |
0.25 | 1.0030 |
0.30 | 0.9045 |
0.35 | 0.9787 |
0.40 | 0.9177 |
0.45 | 0.9432 |
0.50 | 1.0820 |
0.55 | 1.0410 |
0.60 | 1.0550 |
0.65 | 1.0490 |
0.70 | 0.9482 |
0.75 | 0.9395 |
0.80 | 1.0300 |
0.85 | 1.0720 |
0.90 | 1.0850 |
0.95 | 1.0740 |
1.00 | 1.1700 |
1.05 | 1.1590 |
1.10 | 1.1210 |
1.15 | 1.0600 |
1.20 | 0.9656 |
1.25 | 0.9381 |
1.30 | 0.9992 |
1.35 | 1.0150 |
1.40 | 1.1500 |
1.45 | 1.2210 |
1.50 | 1.2340 |
1.55 | 1.3240 |
1.60 | 1.1300 |
1.65 | 1.1650 |
1.70 | 1.1280 |
1.75 | 1.0730 |
1.80 | 1.2250 |
1.85 | 1.1600 |
1.90 | 1.1720 |
1.95 | 1.0560 |
2.00 | 1.0990 |
2.05 | 1.0770 |
2.10 | 1.1050 |
2.15 | 1.1880 |
2.20 | 1.2820 |
2.25 | 1.2010 |
2.30 | 1.1480 |
2.35 | 1.2950 |
2.40 | 1.2560 |
2.45 | 1.2990 |
2.50 | 1.0830 |
2.55 | 1.4400 |