Kellogg, Thomas B; Duplessy, Jean-Claude; Shackleton, Nicholas J (1978): (Table 1) Stable oxygen isotope ratios of Neogloboquadrina pachyderma sinistral from sediment core V28-14 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.263958, In supplement to: Kellogg, TB et al. (1978): Planktonic foraminiferal and oxygen isotopic stratigraphy and paleoclimatology of Norwegian Sea deep-sea cores. Boreas, 7(1), 61-73, https://doi.org/10.1111/j.1502-3885.1978.tb00051.x
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Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 64.783000 * Longitude: -29.570000
Date/Time Start: 1970-07-19T00:00:00 * Date/Time End: 1970-07-19T00:00:00
Minimum DEPTH, sediment/rock: 0.02 m * Maximum DEPTH, sediment/rock: 6.01 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Neogloboquadrina pachyderma sinistral, δ18O | N. pachyderma s δ18O | ‰ PDB | Shackleton, Nicholas J | Mass spectrometer VG Micromass 602 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
67 data points
Data
1 Depth sed [m] | 2 N. pachyderma s δ18O [‰ PDB] |
---|---|
0.02 | 2.18 |
0.10 | 2.16 |
0.20 | 2.11 |
0.30 | 2.34 |
0.40 | 2.32 |
0.50 | 2.49 |
0.60 | 2.47 |
0.70 | 2.53 |
0.80 | 2.66 |
0.90 | 2.65 |
0.99 | 3.14 |
1.09 | 3.18 |
1.19 | 3.52 |
1.29 | 2.86 |
1.41 | 4.49 |
1.49 | 4.60 |
1.60 | 4.62 |
1.70 | 4.64 |
1.80 | 4.44 |
1.90 | 4.30 |
2.00 | 4.25 |
2.10 | 4.14 |
2.20 | 4.03 |
2.30 | 3.47 |
2.40 | 4.26 |
2.51 | 4.20 |
2.60 | 4.03 |
2.71 | 4.09 |
2.81 | 4.24 |
2.91 | 3.93 |
3.01 | 3.72 |
3.11 | 4.13 |
3.21 | 4.19 |
3.31 | 4.03 |
3.40 | 3.88 |
3.51 | 4.22 |
3.60 | 3.82 |
3.70 | 3.55 |
3.89 | 4.03 |
4.01 | 3.75 |
4.11 | 3.96 |
4.21 | 4.16 |
4.31 | 3.74 |
4.41 | 3.73 |
4.51 | 3.08 |
4.60 | 3.61 |
4.71 | 3.76 |
4.81 | 3.53 |
4.85 | 3.58 |
4.91 | 3.46 |
4.95 | 3.62 |
5.01 | 3.53 |
5.05 | 3.51 |
5.11 | 2.70 |
5.15 | 2.83 |
5.19 | 2.76 |
5.25 | 2.67 |
5.30 | 2.73 |
5.35 | 2.70 |
5.39 | 3.43 |
5.45 | 4.30 |
5.50 | 4.33 |
5.60 | 4.50 |
5.70 | 4.26 |
5.80 | 3.64 |
5.90 | 3.83 |
6.01 | 4.37 |