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Keigwin, Lloyd D (1998): (Table 2) Hydrography of the Okhotsk Sea and Emperor Seamount Cruises [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.857986, In supplement to: Keigwin, LD (1998): Glacial-age hydrography of the far northwest Pacific Ocean. Paleoceanography, 13(4), 323-339, https://doi.org/10.1029/98PA00874

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Coverage:
Median Latitude: 52.474006 * Median Longitude: 150.031206 * South-bound Latitude: 48.003200 * West-bound Longitude: 142.451000 * North-bound Latitude: 57.496200 * East-bound Longitude: 165.083330
Date/Time Start: 1993-09-05T15:57:00 * Date/Time End: 1993-09-13T06:32:00
Minimum DEPTH, water: 0.0 m * Maximum DEPTH, water: 4558.0 m
Event(s):
90BM9316_1/9-1 (HS-09) * Latitude: 48.003200 * Longitude: 150.701500 * Date/Time: 1993-09-05T15:57:00 * Elevation: -3330.0 m * Campaign: 90BM9316_1 * Basis: Akademik A Nesmeyanov * Method/Device: CTD/Rosette (CTD-RO) * Comment: Section P01W
90BM9316_1/13-1 (HS-13) * Latitude: 49.992800 * Longitude: 149.109500 * Date/Time: 1993-09-08T20:55:00 * Elevation: -1110.0 m * Campaign: 90BM9316_1 * Basis: Akademik A Nesmeyanov * Method/Device: CTD/Rosette (CTD-RO) * Comment: Section P01W
90BM9316_1/28-1 (HS-28) * Latitude: 57.496200 * Longitude: 142.810700 * Date/Time: 1993-09-12T05:37:00 * Elevation: -190.0 m * Campaign: 90BM9316_1 * Basis: Akademik A Nesmeyanov * Method/Device: CTD/Rosette (CTD-RO) * Comment: Section P01W
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventKeigwin, Lloyd D
2Latitude of eventLatitudeKeigwin, Lloyd D
3Longitude of eventLongitudeKeigwin, Lloyd D
4Elevation of eventElevationmKeigwin, Lloyd D
5Date/Time of eventDate/TimeKeigwin, Lloyd D
6DEPTH, waterDepth watermKeigwin, Lloyd DGeocode
7Carbon dioxide, totalTCO2µmol/lKeigwin, Lloyd D
8δ13Cδ13C‰ PDBKeigwin, Lloyd D
9SalinitySalKeigwin, Lloyd D
10δ18Oδ18OKeigwin, Lloyd Draw with respect to PDB
11δ18O, standard deviationδ18O std dev±Keigwin, Lloyd D
12ReplicatesRepl#Keigwin, Lloyd D
13δ18O, waterδ18O H2O‰ SMOWKeigwin, Lloyd D
Size:
266 data points

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