Lein, Alla Yu; Ivanov, Mikhail V (2009): (Table 4.2.17) Consumption of organic carbon for microbial methane formation in recent bottom sediments of the Baltic Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.771109, In supplement to: Lein, AY; Ivanov, MV (2009): Biogeokhimicheskii Tsikl Metana v Okeane (Biogeochemical Cycle of Methane in the Ocean). Nauka Publ. (Moscow); Lisitzin, A.P. (Ed.), 576 pp.
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 57.724111 * Median Longitude: 20.600950 * South-bound Latitude: 57.350000 * West-bound Longitude: 19.270000 * North-bound Latitude: 58.750000 * East-bound Longitude: 23.591700
Minimum DEPTH, sediment/rock: 0.0005 m * Maximum DEPTH, sediment/rock: 1.8300 m
Event(s):
AK26A-2601 * Latitude: 57.700000 * Longitude: 23.591700 * Elevation: -53.0 m * Location: Gulf of Riga * Campaign: AKU26A * Basis: Akademik Kurchatov * Method/Device: Multiple investigations (MULT)
AK26A-2611 * Latitude: 57.756667 * Longitude: 20.630000 * Elevation: -134.0 m * Location: Baltic Sea * Campaign: AKU26A * Basis: Akademik Kurchatov * Method/Device: Gravity corer (GC)
AK26A-2618 * Latitude: 57.408000 * Longitude: 20.034000 * Elevation: -232.0 m * Location: Baltic Sea * Campaign: AKU26A * Basis: Akademik Kurchatov * Method/Device: Multiple investigations (MULT)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | Elevation of event | Elevation | m | |||
| 5 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 6 | Depth, top/min | Depth top | m | Lein, Alla Yu | ||
| 7 | Depth, bottom/max | Depth bot | m | Lein, Alla Yu | ||
| 8 | Carbon, organic, residual | C org res | mg/kg | Lein, Alla Yu | ||
| 9 | Methane formation rate, sediment | CH4 fr sed | nl/dm3/day | Lein, Alla Yu | Isotopic tracer uptake | |
| 10 | Organic carbon consumption rate, sediment | TOC cr sed | mg/kg/a | Lein, Alla Yu | Calculated | for formatioon of CH4 from CO2 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
124 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Depth sed [m] | 6 Depth top [m] | 7 Depth bot [m] | 8 C org res [mg/kg] | 9 CH4 fr sed [nl/dm3/day] | 10 TOC cr sed [mg/kg/a] |
|---|---|---|---|---|---|---|---|---|---|
| AK26A-2601 | 57.700 | 23.592 | -53 | 0.0025 | 0.000 | 0.005 | 1590 | 16500 | 12.7020 |
| AK26A-2601 | 57.700 | 23.592 | -53 | 0.0775 | 0.005 | 0.150 | 1503 | 27300 | 21.0240 |
| AK26A-2601 | 57.700 | 23.592 | -53 | 0.9000 | 0.800 | 1.000 | 1726 | 21300 | 16.5320 |
| AK26A-2611 | 57.757 | 20.630 | -134 | 0.0005 | 0.000 | 0.001 | 1904 | 6600 | 4.9640 |
| AK26A-2611 | 57.757 | 20.630 | -134 | 0.0150 | 0.010 | 0.020 | 1928 | 13200 | 10.0740 |
| AK26A-2611 | 57.757 | 20.630 | -134 | 0.0850 | 0.020 | 0.150 | 1830 | 1200 | 0.8760 |
| AK26A-2611 | 57.757 | 20.630 | -134 | 0.2000 | 0.150 | 0.250 | 2276 | 800 | 0.5840 |
| AK26A-2611 | 57.757 | 20.630 | -134 | 0.5000 | 0.460 | 0.540 | 3039 | 1600 | 1.1680 |
| AK26A-2611 | 57.757 | 20.630 | -134 | 1.1000 | 1.050 | 1.150 | 2936 | 1100 | 0.7300 |
| AK26A-2611 | 57.757 | 20.630 | -134 | 1.7000 | 1.650 | 1.750 | 3960 | 4100 | 3.2120 |
| AK26A-2631 | 57.380 | 19.270 | -120 | 0.0250 | 0.000 | 0.050 | 2509 | 7300 | 5.5480 |
| AK26A-2631 | 57.380 | 19.270 | -120 | 0.1600 | 0.100 | 0.220 | 2931 | 2000 | 1.4600 |
| AK26A-2631 | 57.380 | 19.270 | -120 | 1.5500 | 1.500 | 1.600 | 5646 | 1500 | 1.0220 |
| AK26A-2636 | 58.750 | 19.900 | -162 | 0.0500 | 0.000 | 0.100 | 1524 | 1300 | 0.8760 |
| AK26A-2636 | 58.750 | 19.900 | -162 | 0.1500 | 0.100 | 0.200 | 1654 | 2200 | 1.6060 |
| AK26A-2636 | 58.750 | 19.900 | -162 | 0.5300 | 0.500 | 0.560 | 4361 | 800 | 0.5840 |
| AK26A-2636 | 58.750 | 19.900 | -162 | 0.8500 | 0.800 | 0.900 | 0 | ||
| AK26A-2618 | 57.408 | 20.034 | -232 | 0.0110 | 0.002 | 0.020 | 1201 | 200 | 0.1460 |
| AK26A-2618 | 57.408 | 20.034 | -232 | 0.2800 | 0.260 | 0.300 | 3549 | 200 | 0.1460 |
| AK26A-2618 | 57.408 | 20.034 | -232 | 0.7750 | 0.700 | 0.850 | 3602 | 100 | 0.0728 |
| AK26A-2618 | 57.408 | 20.034 | -232 | 1.8300 | 1.750 | 1.910 | 5857 | 100 | 0.0728 |
| AK26A-2622 | 57.350 | 20.180 | -240 | 0.0250 | 0.000 | 0.050 | 1870 | 1100 | 0.7300 |
| AK26A-2622 | 57.350 | 20.180 | -240 | 0.1000 | 0.050 | 0.150 | 1870 | 800 | 0.5840 |
| AK26A-2622 | 57.350 | 20.180 | -240 | 0.2750 | 0.150 | 0.400 | 3298 | 0 | |
| AK26A-2622 | 57.350 | 20.180 | -240 | 0.9250 | 0.850 | 1.000 | 1100 | 0.7300 | |
| AK26A-2622 | 57.350 | 20.180 | -240 | 1.5750 | 1.500 | 1.650 | 0 |