Riedinger, Natascha; Formolo, Michael J; Lyons, Timothy W; Henkel, Susann; Beck, Antje; Kasten, Sabine (2014): Dissolved inorganic carbon and δ¹³C of dissolved inorganic carbon measured in pore water of sediment core GeoB13820-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.772978, In supplement to: Riedinger, N et al. (2014): An inorganic geochemical argument for coupled anaerobic oxidation of methane and iron reduction in marine sediments. Geobiology, 12(2), 172-181, https://doi.org/10.1111/gbi.12077
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Project(s):
Coverage:
Latitude: -39.301000 * Longitude: -53.967167
Date/Time Start: 2009-06-01T03:12:00 * Date/Time End: 2009-06-01T03:12:00
Minimum DEPTH, sediment/rock: 0.25 m * Maximum DEPTH, sediment/rock: 9.55 m
Event(s):
GeoB13820-1 (397) * Latitude: -39.301000 * Longitude: -53.967167 * Date/Time: 2009-06-01T03:12:00 * Elevation: -3613.0 m * Recovery: 9.66 m * Campaign: M78/3A * Basis: Meteor (1986) * Method/Device: Gravity corer (GC)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Carbon, inorganic, dissolved | DIC | µmol/l | Riedinger, Natascha | Gasbench II (Thermo) coupled to a DELTA V plus isotope ratio mass spectrometer (IRMS) | |
| 3 | δ13C, dissolved inorganic carbon | δ13C DIC | ‰ PDB | Riedinger, Natascha | Gasbench II (Thermo) coupled to a DELTA V plus isotope ratio mass spectrometer (IRMS) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
40 data points
Data
| 1 Depth sed [m] | 2 DIC [µmol/l] | 3 δ13C DIC [‰ PDB] |
|---|---|---|
| 0.25 | 4500 | -9.9 |
| 0.70 | 6800 | -14.2 |
| 1.25 | 13300 | -16.4 |
| 1.70 | 17900 | -17.7 |
| 2.20 | 19700 | -18.8 |
| 2.70 | 25700 | -19.3 |
| 3.20 | 29400 | -19.3 |
| 3.70 | 31000 | -20.1 |
| 4.20 | 35500 | -20.5 |
| 4.70 | 56300 | -20.6 |
| 5.20 | 56900 | -20.8 |
| 5.70 | 81900 | -19.2 |
| 6.20 | 64500 | -16.0 |
| 6.70 | 84000 | -13.0 |
| 7.20 | 66500 | -10.4 |
| 7.70 | 79500 | -7.9 |
| 8.20 | 85600 | -5.5 |
| 8.70 | 100400 | -3.2 |
| 9.20 | 112500 | -1.4 |
| 9.55 | 91400 | -0.6 |