Gard, Gunilla (1987): Nannofossil abundance in sediment core PS1294-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.385584, In supplement to: Gard, G (1987): Late Quaternary calcareous nannofossil biostratigraphy and sedimentation patterns: Fram Strait, Arctica. Paleoceanography, 2(5), 519-529, https://doi.org/10.1029/PA002i005p00519
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Project(s):
Silicon Cycling in the World Ocean (SINOPS)
Funding:
Coverage:
Latitude: 78.001600 * Longitude: 5.346700
Date/Time Start: 1985-07-31T00:00:00 * Date/Time End: 1985-07-31T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 5.90 m
Event(s):
PS1294-4 (GIK21294-4 PS07/584) * Latitude: 78.001600 * Longitude: 5.346700 * Date/Time: 1985-07-31T00:00:00 * Elevation: -2677.0 m * Penetration: 9.15 m * Recovery: 6.16 m * Location: Fram Strait * Campaign: ARK-III/3 (PS07) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 7 core sections: 0-1, 1-2, 2-3, 3-4, 4-5, 5-5.65, 5.65-6.16 m
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Nannofossil abundance | Nannos abund | #/mm2 | Gard, Gunilla | Counting |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
60 data points
Data
1 Depth sed [m] | 2 Nannos abund [#/mm2] |
---|---|
0.01 | 860 |
0.10 | 1234 |
0.20 | 5 |
0.30 | 5 |
0.40 | 11 |
0.50 | 14 |
0.60 | 15 |
0.69 | 5 |
0.80 | 52 |
0.90 | 9 |
0.98 | 25 |
1.10 | 10 |
1.20 | 5 |
1.30 | 5 |
1.40 | 5 |
1.50 | 5 |
1.60 | 5 |
1.70 | 5 |
1.80 | 5 |
1.90 | 5 |
2.01 | 134 |
2.11 | 5 |
2.20 | 5 |
2.29 | 5 |
2.40 | 39 |
2.51 | 69 |
2.60 | 5 |
2.70 | 329 |
2.80 | 984 |
2.90 | 1210 |
3.01 | 534 |
3.10 | 14 |
3.20 | 115 |
3.29 | 211 |
3.40 | 197 |
3.49 | 11 |
3.60 | 5 |
3.70 | 5 |
3.81 | 5 |
3.90 | 5 |
3.99 | 5 |
4.10 | 5 |
4.20 | 5 |
4.30 | 5 |
4.50 | 158 |
4.55 | 72 |
4.58 | 54 |
4.70 | 5 |
4.79 | 5 |
4.90 | 5 |
4.98 | 182 |
5.10 | 65 |
5.20 | 5 |
5.30 | 5 |
5.39 | 5 |
5.49 | 5 |
5.61 | 15 |
5.70 | 5 |
5.80 | 5 |
5.90 | 5 |