Diester-Haass, Lieselotte (1991): (Table 3) Benthonic/planktonic foraminiferal ratios and fragmentation of planktonic foraminifera from ODP Hole 113-690B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.759813, 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
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
| 2 | Foraminifera, benthic/planktic ratio | Foram benth/plankt | Diester-Haass, Lieselotte | (be.foram/be. + pl.foram) * 100 | ||
| 3 | Fragmentation index, planktic foraminifera | Fragm plankt foram | % | Diester-Haass, Lieselotte |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
82 data points
Data
| 1 Depth sed [m] | 2 Foram benth/plankt | 3 Fragm plankt foram [%] |
|---|---|---|
| 51.10 | 84.7 | 92.6 |
| 52.60 | 71.8 | 76.0 |
| 55.60 | 79.9 | 80.8 |
| 57.10 | 25.0 | 73.9 |
| 58.60 | 37.6 | 51.2 |
| 60.80 | 15.2 | 75.5 |
| 62.30 | 44.4 | 86.4 |
| 65.30 | 45.4 | 84.2 |
| 66.80 | 69.4 | 93.6 |
| 68.30 | 29.4 | 80.2 |
| 70.50 | 51.4 | 87.5 |
| 72.00 | 48.1 | 93.2 |
| 75.00 | 20.7 | 67.4 |
| 76.50 | 44.9 | 88.8 |
| 78.00 | 44.9 | 80.2 |
| 80.00 | 78.0 | 85.8 |
| 81.50 | 84.2 | 95.2 |
| 84.50 | 22.0 | 84.1 |
| 86.00 | 37.7 | 80.5 |
| 87.50 | 40.0 | 84.6 |
| 89.00 | 50.0 | 69.5 |
| 89.70 | 67.1 | 85.8 |
| 91.20 | 59.2 | 77.6 |
| 94.20 | 8.5 | 58.2 |
| 95.70 | 34.6 | 71.6 |
| 97.20 | 30.4 | 64.7 |
| 98.70 | 38.9 | 74.4 |
| 99.40 | 14.4 | 58.8 |
| 100.90 | 30.0 | 74.9 |
| 103.90 | 60.6 | 77.8 |
| 105.40 | 8.9 | 52.4 |
| 109.10 | 7.5 | 43.7 |
| 110.52 | 9.6 | 46.8 |
| 110.60 | 9.7 | 46.0 |
| 113.60 | 6.2 | 44.4 |
| 115.02 | 4.9 | 39.4 |
| 115.10 | 5.2 | 40.5 |
| 120.60 | 5.6 | 44.5 |
| 123.60 | 5.5 | 46.9 |
| 125.10 | 5.3 | 49.4 |
| 126.60 | 4.5 | 46.6 |