Risebrobakken, Bjørg; Dokken, Trond; Jansen, Eystein (2014): Planktonic foraminifera content during marine isotope stage 5 of sediment core MD99-2303 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.840692, In supplement to: Risebrobakken, B et al. (2005): Extent and variability of the Meridional Atlantic Circulation in the Eastern Nordic Seas during Marine Isotope Stage 5 and its influence on the inception of the last Glacial. Geophysical Monograph Series, 158, 323-339, https://doi.org/10.1029/158GM20
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Project(s):
Coverage:
Latitude: 77.519667 * Longitude: 8.399667
Date/Time Start: 1999-08-01T00:00:00 * Date/Time End: 1999-08-01T00:00:00
Minimum DEPTH, sediment/rock: 9.045 m * Maximum DEPTH, sediment/rock: 9.355 m
Event(s):
MD99-2303 (3182N) * Latitude: 77.519667 * Longitude: 8.399667 * Date/Time: 1999-08-01T00:00:00 * Elevation: -2325.0 m * Recovery: 23.915 m * Location: Spitsbergen slope * Campaign: MD114 (IMAGES V) * Basis: Marion Dufresne (1995) * Method/Device: Calypso Corer (CALYPSO)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | AGE | Age | ka BP | Geocode | ||
3 | Foraminifera, planktic | Foram plankt | #/g | Risebrobakken, Bjørg | Counting 150-500 µm fraction | |
4 | Neogloboquadrina pachyderma sinistral | N. pachyderma s | % | Risebrobakken, Bjørg | Counting 150-500 µm fraction | |
5 | Neogloboquadrina pachyderma dextral | N. pachyderma d | % | Risebrobakken, Bjørg | Counting 150-500 µm fraction | |
6 | Globigerina quinqueloba | G. quinqueloba | % | Risebrobakken, Bjørg | Counting 150-500 µm fraction |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
89 data points
Data
1 Depth sed [m] | 2 Age [ka BP] | 3 Foram plankt [#/g] | 4 N. pachyderma s [%] | 5 N. pachyderma d [%] | 6 G. quinqueloba [%] |
---|---|---|---|---|---|
9.045 | 110.09 | 1664 | 97 | 3 | 0 |
9.055 | 110.22 | 322 | 98 | 2 | 0 |
9.065 | 110.39 | 69 | 98 | 2 | 0 |
9.075 | 110.56 | 135 | 99 | 1 | 0 |
9.085 | 110.74 | 47 | 96 | 2 | 1 |
9.105 | 111.08 | 5 | |||
9.115 | 111.25 | 21 | 96 | 2 | 1 |
9.135 | 111.60 | 1 | |||
9.155 | 111.94 | 4 | |||
9.175 | 112.29 | 0 | |||
9.195 | 112.63 | 15 | 98 | 2 | 0 |
9.205 | 112.80 | 0 | |||
9.225 | 113.18 | 28 | 96 | 2 | 1 |
9.235 | 113.56 | 6 | 100 | 0 | 0 |
9.245 | 113.94 | 83 | 99 | 1 | 0 |
9.255 | 114.32 | 47 | 97 | 3 | 0 |
9.265 | 114.70 | 307 | 99 | 1 | 0 |
9.275 | 115.08 | 291 | 99 | 1 | 0 |
9.285 | 115.40 | 1181 | 99 | 1 | 0 |
9.295 | 116.92 | 468 | 98 | 2 | 0 |
9.305 | 118.43 | 4332 | 96 | 2 | 3 |
9.315 | 119.94 | 3800 | 99 | 1 | 0 |
9.325 | 121.45 | 2816 | 98 | 2 | 0 |
9.335 | 122.97 | 2450 | 97 | 3 | 0 |
9.345 | 124.48 | 1186 | 99 | 1 | 0 |
9.355 | 126.00 | 602 | 100 | 0 | 0 |