Gard, Gunilla (1987): Nannofossil abundance in sediment core PS1295-5 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.385585, 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
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Silicon Cycling in the World Ocean (SINOPS)
Funding:
Coverage:
Latitude: 77.998200 * Longitude: 2.468200
Date/Time Start: 1985-08-01T00:00:00 * Date/Time End: 1985-08-01T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 5.60 m
Event(s):
PS1295-5 (GIK21295-5 PS07/586) * Latitude: 77.998200 * Longitude: 2.468200 * Date/Time: 1985-08-01T00:00:00 * Elevation: -3112.0 m * Penetration: 10 m * Recovery: 5.63 m * Location: Fram Strait * Campaign: ARK-III/3 (PS07) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 6 core sections: 0-0.79, 0.79-1.78, 1.78-2.79, 2.79-3.79, 3.79-4.79, 4.79-5.63 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:
57 data points
Data
| 1 Depth sed [m] | 2 Nannos abund [#/mm2] |
|---|---|
| 0.01 | 804 |
| 0.10 | 921 |
| 0.20 | 9 |
| 0.30 | 16 |
| 0.40 | 21 |
| 0.50 | 5 |
| 0.60 | 6 |
| 0.70 | 26 |
| 0.80 | 14 |
| 0.90 | 5 |
| 1.00 | 5 |
| 1.10 | 6 |
| 1.20 | 5 |
| 1.30 | 5 |
| 1.40 | 5 |
| 1.50 | 161 |
| 1.60 | 1123 |
| 1.70 | 7 |
| 1.80 | 5 |
| 1.90 | 28 |
| 2.00 | 17 |
| 2.10 | 5 |
| 2.20 | 5 |
| 2.30 | 5 |
| 2.40 | 5 |
| 2.50 | 5 |
| 2.60 | 5 |
| 2.70 | 5 |
| 2.80 | 5 |
| 2.90 | 5 |
| 3.01 | 5 |
| 3.10 | 40 |
| 3.20 | 19 |
| 3.30 | 5 |
| 3.40 | 5 |
| 3.51 | 5 |
| 3.60 | 5 |
| 3.70 | 5 |
| 3.80 | 5 |
| 3.90 | 5 |
| 4.00 | 5 |
| 4.12 | 5 |
| 4.22 | 5 |
| 4.32 | 5 |
| 4.40 | 5 |
| 4.50 | 5 |
| 4.60 | 10 |
| 4.70 | 5 |
| 4.79 | 5 |
| 4.88 | 5 |
| 5.00 | 5 |
| 5.11 | 5 |
| 5.21 | 5 |
| 5.31 | 5 |
| 5.40 | 5 |
| 5.50 | 5 |
| 5.60 | 5 |