Polyak, Leonid; Stanovoy, Vladimir V; Lubinski, David J (2003): (Table 3) Stable isotope composition of benthic foraminifera from Kara Sea sediment cores [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.842418, In supplement to: Polyak, L et al. (2003): Stable isotopes in benthic foraminiferal calcite from a river-influenced Arctic marine environment, Kara and Pechora Seas. Paleoceanography, 18(1), 1003, https://doi.org/10.1029/2001PA000752
Always quote citation above when using data! You can download the citation in several formats below.
Further details:
Fairbanks, Richard G (1989): A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation. Nature, 342(6250), 637-642, https://doi.org/10.1038/342637a0
Fairbanks, Richard G; Matthews, R K (1978): The marine oxygen isotope record in Pleistocene coral, Barbados, West Indies. Quaternary Research, 10(2), 181-196, https://doi.org/10.1016/0033-5894(78)90100-X
Coverage:
Median Latitude: 72.262667 * Median Longitude: 72.391122 * South-bound Latitude: 69.250000 * West-bound Longitude: 57.300000 * North-bound Latitude: 74.003500 * East-bound Longitude: 79.952200
Date/Time Start: 1997-09-17T11:16:00 * Date/Time End: 1997-09-17T11:16:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 18.20 m
Event(s):
B212_B218 * Latitude: 69.250000 * Longitude: 57.300000 * Elevation: -20.0 m * Location: Kara Sea * Method/Device: Core (CORE)
BP97-24 * Latitude: 73.534500 * Longitude: 79.921167 * Date/Time: 1997-09-17T11:16:00 * Elevation: -40.0 m * Location: Kara Sea * Campaign: BP97 (KaraSea97) * Basis: Akademik Boris Petrov * Method/Device: Sampling gear, diverse (DIVERSE) * Comment: CTD-1,PN-4,RS-3,LVS-2,OG-2,LBC-1,MUC-2,BD-1
DM49-4401-1 * Latitude: 74.003500 * Longitude: 79.952200 * Elevation: -35.0 m * Location: Kara Sea * Campaign: DM49 (SPASIBAIII) * Basis: Dmitry Mendeleev * Method/Device: Gravity corer (GC)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | AGE | Age | ka BP | Geocode | ||
| 4 | Elphidium excavatum forma clavata, δ13C | E. excavatum f clavata δ13C | ‰ PDB | Polyak, Leonid | Mass spectrometer Finnigan MAT 252 | |
| 5 | Elphidium excavatum forma clavata, δ18O | E. excavatum f clavata δ18O | ‰ PDB | Polyak, Leonid | Mass spectrometer Finnigan MAT 252 | |
| 6 | Elphidium excavatum forma clavata, δ18O | E. excavatum f clavata δ18O | ‰ PDB | Polyak, Leonid | Corrected | corrected for global sea level by -0.011 per mil per meter rise (Fairbanks and Matthews, 1978; Fairbanks, 1989) |
| 7 | Haynesina orbicularis, δ13C | H. orbicularis δ13C | ‰ PDB | Polyak, Leonid | Mass spectrometer Finnigan MAT 252 | |
| 8 | Haynesina orbicularis, δ18O | H. orbicularis δ18O | ‰ PDB | Polyak, Leonid | Mass spectrometer Finnigan MAT 252 | |
| 9 | Haynesina orbicularis, δ18O | H. orbicularis δ18O | ‰ PDB | Polyak, Leonid | Corrected | corrected for global sea level by -0.011 per mil per meter rise (Fairbanks and Matthews, 1978; Fairbanks, 1989) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
124 data points
Data
| 1 Event | 2 Depth sed [m] | 3 Age [ka BP] | 4 E. excavatum f clavata δ13C [‰ PDB] (Mass spectrometer Finnigan MA...) | 5 E. excavatum f clavata δ18O [‰ PDB] (Mass spectrometer Finnigan MA...) | 6 E. excavatum f clavata δ18O [‰ PDB] (corrected for global sea leve...) | 7 H. orbicularis δ13C [‰ PDB] (Mass spectrometer Finnigan MA...) | 8 H. orbicularis δ18O [‰ PDB] (Mass spectrometer Finnigan MA...) | 9 H. orbicularis δ18O [‰ PDB] (corrected for global sea leve...) |
|---|---|---|---|---|---|---|---|---|
| B212_B218 | 1.20 | 1.62 | -0.65 | 2.01 | 1.99 | |||
| B212_B218 | 3.40 | 4.60 | -0.23 | 2.54 | 2.49 | |||
| B212_B218 | 3.70 | 4.79 | -1.47 | 2.67 | 2.61 | |||
| B212_B218 | 4.00 | 4.98 | -1.27 | 2.72 | 2.66 | |||
| B212_B218 | 4.60 | 5.36 | -1.96 | 2.43 | 2.36 | |||
| B212_B218 | 5.30 | 5.80 | -2.09 | 1.55 | 1.46 | |||
| B212_B218 | 6.30 | 6.21 | -2.64 | 1.95 | 1.84 | |||
| B212_B218 | 7.00 | 6.46 | -3.27 | 1.31 | 1.18 | |||
| B212_B218 | 9.40 | 7.04 | -3.28 | 1.17 | 1.00 | |||
| B212_B218 | 10.40 | 7.28 | -4.86 | 1.77 | 1.57 | |||
| B212_B218 | 10.90 | 7.40 | -3.03 | 1.96 | 1.74 | |||
| B212_B218 | 12.00 | 7.67 | -3.32 | 0.00 | -0.24 | |||
| B212_B218 | 12.40 | 7.76 | -4.00 | 1.00 | 0.75 | |||
| B212_B218 | 12.90 | 7.88 | -3.38 | 0.43 | 0.17 | |||
| B212_B218 | 13.30 | 7.98 | -3.74 | 0.52 | 0.25 | |||
| B212_B218 | 14.50 | 8.24 | -3.74 | 0.93 | 0.60 | |||
| B212_B218 | 15.10 | 8.36 | -6.08 | -1.22 | -1.59 | |||
| B212_B218 | 15.60 | 8.45 | -4.60 | -0.62 | -1.03 | |||
| B212_B218 | 16.20 | 8.56 | -4.66 | -2.85 | -3.31 | |||
| B212_B218 | 17.80 | 8.86 | -5.65 | -0.53 | -1.12 | |||
| B212_B218 | 18.20 | 8.93 | -3.54 | 0.92 | 0.31 | |||
| BP97-24 | 0.00 | -3.82 | 0.93 | -1.66 | 2.53 | |||
| DM49-4401-1 | 0.03 | 0.11 | -3.17 | 2.26 | 2.26 | -0.98 | 2.02 | 2.02 |
| DM49-4401-1 | 0.18 | 0.74 | -2.97 | 1.94 | 1.93 | -0.68 | 1.98 | 1.97 |
| DM49-4401-1 | 0.33 | 1.37 | -2.93 | 2.23 | 2.22 | -0.97 | 2.59 | 2.58 |
| DM49-4401-1 | 0.73 | 3.06 | -0.60 | 2.41 | 2.38 | |||
| DM49-4401-1 | 1.17 | 5.25 | -0.92 | 1.88 | 1.82 | |||
| DM49-4401-1 | 1.53 | 7.04 | -1.38 | 1.45 | 1.28 | |||
| DM49-4401-1 | 1.74 | 7.30 | -3.50 | 2.24 | 2.04 | -1.97 | 1.57 | 1.37 |
| DM49-4401-1 | 1.84 | 7.43 | -3.82 | 1.87 | 1.65 | -1.46 | 1.80 | 1.58 |
| DM49-4401-1 | 3.43 | 9.33 | -4.74 | 1.24 | 0.72 | -1.87 | 1.47 | 0.95 |
| DM49-4401-1 | 3.73 | 9.69 | -5.62 | -5.23 | -5.83 | -4.70 | -5.74 | -6.34 |
| DM49-4401-1 | 4.03 | 10.05 | -5.33 | -5.56 | -6.21 | |||
| DM49-4401-1 | 4.08 | 10.12 | -7.37 | -6.96 | -7.62 |