Diester-Haass, Lieselotte (1991): (Table 2) Composition of the sand fraction from ODP Hole 113-690B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.759812, In supplement to: Diester-Haass, L (1991): Eocene/Oligocene paleoceanography in the Antarctic Ocean, Atlantic sector (Maud Rise, ODP Leg 113, Site 689B and 690B). Marine Geology, 100(1-4), 249-276, https://doi.org/10.1016/0025-3227(91)90235-V
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -65.161000 * Longitude: 1.204900
Date/Time Start: 1987-01-20T03:15:00 * Date/Time End: 1987-01-21T07:00:00
Minimum DEPTH, sediment/rock: 51.10 m * Maximum DEPTH, sediment/rock: 126.60 m
Event(s):
113-690B * Latitude: -65.161000 * Longitude: 1.204900 * Date/Time Start: 1987-01-20T03:15:00 * Date/Time End: 1987-01-21T07:00:00 * Elevation: -2925.0 m * Penetration: 213.4 m * Recovery: 214.75 m * Location: South Atlantic Ocean * Campaign: Leg113 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 25 cores; 213.4 m cored; 0 m drilled; 100.6 % recovery
Comment:
Sediment depth is given in mbsf. Originally given as cumulative plot.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Diatoms | Diatoms | % | Diester-Haass, Lieselotte | ||
| 3 | Radiolarians | Rad | % | Diester-Haass, Lieselotte | ||
| 4 | Foraminifera, planktic | Foram plankt | % | Diester-Haass, Lieselotte | ||
| 5 | Benthos, other | Benthos oth | % | Diester-Haass, Lieselotte | ||
| 6 | Fish remains | Fish rem | % | Diester-Haass, Lieselotte | ||
| 7 | Bolboforma spp. | Bolboforma spp. | % | Diester-Haass, Lieselotte | ||
| 8 | Terrigenous | Terr | % | Diester-Haass, Lieselotte | ||
| 9 | Pyrite, FeS2 | Py | % | Diester-Haass, Lieselotte |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
328 data points
Data
| 1 Depth sed [m] | 2 Diatoms [%] | 3 Rad [%] | 4 Foram plankt [%] | 5 Benthos oth [%] | 6 Fish rem [%] | 7 Bolboforma spp. [%] | 8 Terr [%] | 9 Py [%] |
|---|---|---|---|---|---|---|---|---|
| 51.10 | 0.5 | 86.1 | 1.7 | 9.6 | 0.8 | 0.0 | 0.5 | 0.8 |
| 52.60 | 0.0 | 73.9 | 7.0 | 18.4 | 0.3 | 0.0 | 0.1 | 0.3 |
| 55.60 | 0.9 | 51.4 | 7.8 | 33.6 | 0.4 | 0.0 | 0.5 | 5.4 |
| 57.10 | 0.1 | 41.5 | 41.4 | 14.6 | 0.9 | 0.6 | 0.8 | 0.1 |
| 58.60 | 0.0 | 32.2 | 41.3 | 25.3 | 0.5 | 0.3 | 0.0 | 0.4 |
| 60.80 | 0.1 | 32.2 | 55.7 | 10.5 | 0.4 | 0.0 | 0.0 | 1.1 |
| 62.30 | 0.3 | 44.0 | 30.1 | 25.0 | 0.3 | 0.0 | 0.1 | 0.2 |
| 65.30 | 0.0 | 64.9 | 17.9 | 16.1 | 0.4 | 0.0 | 0.0 | 0.7 |
| 66.80 | 0.9 | 80.6 | 5.3 | 13.0 | 0.1 | 0.0 | 0.0 | 0.1 |
| 68.30 | 0.0 | 58.0 | 27.5 | 12.6 | 0.5 | 0.0 | 0.0 | 1.4 |
| 70.50 | 0.0 | 62.6 | 17.3 | 18.8 | 0.2 | 0.0 | 0.0 | 1.1 |
| 72.00 | 0.7 | 50.7 | 24.1 | 23.0 | 0.6 | 0.0 | 0.2 | 0.7 |
| 75.00 | 0.1 | 33.3 | 51.6 | 14.2 | 0.4 | 0.0 | 0.0 | 0.4 |
| 76.50 | 0.5 | 32.4 | 45.4 | 20.0 | 0.8 | 0.0 | 0.1 | 0.8 |
| 78.00 | 0.0 | 36.5 | 33.7 | 28.7 | 0.4 | 0.0 | 0.1 | 0.6 |
| 80.00 | 0.0 | 28.9 | 13.9 | 49.8 | 0.3 | 0.0 | 0.0 | 7.1 |
| 81.50 | 0.0 | 43.7 | 8.4 | 45.6 | 0.9 | 0.0 | 0.1 | 1.3 |
| 84.50 | 0.2 | 28.1 | 54.9 | 15.9 | 0.4 | 0.0 | 0.0 | 0.5 |
| 86.00 | 4.3 | 69.1 | 16.0 | 10.1 | 0.1 | 0.0 | 0.0 | 0.4 |
| 87.50 | 3.1 | 66.2 | 17.5 | 12.1 | 0.1 | 0.0 | 0.0 | 1.0 |
| 89.00 | 0.0 | 29.6 | 34.2 | 34.6 | 0.8 | 0.0 | 0.0 | 0.8 |
| 89.70 | 0.5 | 32.1 | 21.5 | 44.4 | 0.1 | 0.0 | 0.0 | 1.4 |
| 91.20 | 0.0 | 14.3 | 33.8 | 50.4 | 0.2 | 0.0 | 0.0 | 1.3 |
| 94.20 | 0.0 | 0.7 | 68.5 | 6.8 | 0.1 | 1.2 | 0.0 | 22.7 |
| 95.70 | 0.2 | 1.3 | 53.4 | 28.9 | 0.8 | 14.8 | 0.5 | 0.1 |
| 97.20 | 0.0 | 0.1 | 59.7 | 26.8 | 0.1 | 5.2 | 0.0 | 8.1 |
| 98.70 | 0.0 | 0.1 | 41.5 | 26.7 | 0.8 | 28.5 | 0.0 | 2.4 |
| 99.40 | 0.0 | 0.0 | 77.3 | 13.5 | 0.3 | 8.8 | 0.0 | 0.1 |
| 100.90 | 0.0 | 0.1 | 57.2 | 24.9 | 0.9 | 16.8 | 0.0 | 0.1 |
| 103.90 | 0.0 | 0.5 | 31.8 | 52.9 | 3.2 | 10.5 | 0.1 | 1.0 |
| 105.40 | 0.0 | 0.0 | 85.5 | 10.2 | 0.7 | 3.5 | 0.0 | 0.1 |
| 109.10 | 0.0 | 0.0 | 89.4 | 8.5 | 0.6 | 0.0 | 1.1 | 0.4 |
| 110.52 | 0.0 | 0.0 | 88.2 | 11.0 | 0.3 | 0.4 | 0.0 | 0.1 |
| 110.60 | 0.0 | 0.0 | 87.9 | 11.2 | 0.4 | 0.0 | 0.5 | 0.0 |
| 113.60 | 0.0 | 0.0 | 91.9 | 7.0 | 0.3 | 0.0 | 0.8 | 0.0 |
| 115.02 | 0.0 | 0.0 | 90.4 | 6.3 | 0.4 | 0.0 | 2.9 | 0.0 |
| 115.10 | 0.0 | 0.0 | 92.8 | 6.1 | 0.2 | 0.0 | 0.9 | 0.0 |
| 120.60 | 0.0 | 1.3 | 89.0 | 5.8 | 0.4 | 0.0 | 3.5 | 0.0 |
| 123.60 | 0.0 | 0.0 | 92.5 | 6.4 | 0.6 | 0.0 | 0.5 | 0.0 |
| 125.10 | 0.0 | 0.0 | 93.0 | 5.6 | 0.1 | 0.0 | 1.3 | 0.0 |
| 126.60 | 0.0 | 0.0 | 90.1 | 4.9 | 0.4 | 0.0 | 4.6 | 0.0 |