Lein, Alla Yu; Ivanov, Mikhail V (2009): (Table 5.1.10) Methane formation and consumption in the upper meter sediment layer of the Bering Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.771203, 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.
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 58.178333 * Median Longitude: -178.646667 * South-bound Latitude: 53.750000 * West-bound Longitude: 170.000000 * North-bound Latitude: 63.000000 * East-bound Longitude: -174.083333
Minimum DEPTH, sediment/rock: 0.5 m * Maximum DEPTH, sediment/rock: 0.5 m
Event(s):
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 | Methane formation rate, integrated, sediment | CH4 fr int sed | µmol/m2/day | Lein, Alla Yu | Isotopic tracer uptake | |
9 | Methane consumption rate, integrated, sediment | CH4 cr int sed | µmol/m2/day | Lein, Alla Yu | Isotopic tracer uptake | |
10 | Percentage | Perc | % | Lein, Alla Yu | Calculated | methane consumed of methane formed |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
50 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 CH4 fr int sed [µmol/m2/day] | 9 CH4 cr int sed [µmol/m2/day] | 10 Perc [%] |
---|---|---|---|---|---|---|---|---|---|
IL-BS-1 | 58.00 | 170.00 | -1320 | 0.5 | 0.0 | 1.0 | 0.83 | 0.09 | 11 |
IL-BS-9 | 58.47 | 170.93 | -870 | 0.5 | 0.0 | 1.0 | 1.46 | 0.31 | 21 |
IL-BS-20 | 58.50 | -174.08 | -120 | 0.5 | 0.0 | 1.0 | 1.24 | 0.15 | 12 |
IL-BS-22 | 57.50 | -174.08 | -1200 | 0.5 | 0.0 | 1.0 | 0.86 | 0.26 | 30 |
IL-BS-26 | 58.50 | -176.72 | -300 | 0.5 | 0.0 | 1.0 | 1.19 | 0.29 | 24 |
IL-BS-27 | 58.00 | -175.03 | -2350 | 0.5 | 0.0 | 1.0 | 6.90 | 0.18 | 3 |
IL-BS-28 | 55.25 | -177.00 | -3850 | 0.5 | 0.0 | 1.0 | 16.90 | 0.68 | 4 |
IL-BS-32 | 53.75 | -176.17 | -3850 | 0.5 | 0.0 | 1.0 | 12.80 | 0.25 | 2 |
IL-BS-IIn | 63.00 | -177.60 | -89 | 0.5 | 0.0 | 1.0 | 0.67 | 0.15 | 22 |
IL-BS-In | 60.82 | -176.72 | -3000 | 0.5 | 0.0 | 1.0 | 5.80 | 0.40 | 7 |