Cook, Mea S; Keigwin, Lloyd D; Birgel, Daniel; Hinrichs, Kai-Uwe (2011): (Table S9) Stable carbon isotope composition of tetraether-derived biphytanes of sediment core HLY02-02-51 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.830693, In supplement to: Cook, MS et al. (2011): Repeated pulses of vertical methane flux recorded in glacial sediments from the southeast Bering Sea. Paleoceanography, 26(2), PA2210, https://doi.org/10.1029/2010PA001993
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Coverage:
Latitude: 54.553100 * Longitude: -168.666900
Date/Time Start: 2002-07-03T00:00:00 * Date/Time End: 2002-07-03T00:00:00
Minimum DEPTH, sediment/rock: 5.045 m * Maximum DEPTH, sediment/rock: 5.900 m
Event(s):
HLY02-02-51 * Latitude: 54.553100 * Longitude: -168.666900 * Date/Time: 2002-07-03T00:00:00 * Elevation: -1467.0 m * Recovery: 18.56 m * Location: Bering Sea * Campaign: HLY0202 (HEA02) * Basis: Healy * Method/Device: Jumbo Piston Core (JPC)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Biphytanes, acyclic, δ13C | BPs acyclic δ13C | ‰ PDB | Cook, Mea S | Mass spectrometer Finnigan MAT 252 | with respect to VPDB |
| 3 | Biphytanes, monocyclic, δ13C | BPs monocyclic δ13C | ‰ PDB | Cook, Mea S | Mass spectrometer Finnigan MAT 252 | with respect to VPDB |
| 4 | Biphytanes, bicyclic, δ13C | BPs bicyclic δ13C | ‰ PDB | Cook, Mea S | Mass spectrometer Finnigan MAT 252 | with respect to VPDB |
| 5 | Biphytanes, tricyclic, δ13C | BPs tricyclic δ13C | ‰ PDB | Cook, Mea S | Mass spectrometer Finnigan MAT 252 | with respect to VPDB |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
40 data points
Data
| 1 Depth sed [m] | 2 BPs acyclic δ13C [‰ PDB] | 3 BPs monocyclic δ13C [‰ PDB] | 4 BPs bicyclic δ13C [‰ PDB] | 5 BPs tricyclic δ13C [‰ PDB] |
|---|---|---|---|---|
| 5.045 | -23 | -22 | -22 | -22 |
| 5.180 | -21 | -21 | -21 | -22 |
| 5.260 | -23 | -27 | -22 | -21 |
| 5.330 | -24 | -22 | -21 | -21 |
| 5.420 | -24 | -49 | -23 | -22 |
| 5.500 | -24 | -38 | -22 | -22 |
| 5.570 | -28 | -58 | -25 | -22 |
| 5.660 | -27 | -53 | -23 | -22 |
| 5.820 | -22 | -23 | -21 | -22 |
| 5.900 | -24 | -21 | -22 | -22 |