Foster, Laura C; Schmidt, Daniela N; Thomas, Ellen; Arndt, Sandra; Ridgwell, Andy (2013): (Table S1d) Measured tomographic parameters for Oridorsalis umbonatus during ETM-2 for ODP Holes 208-1263C and 208-1262A. PANGAEA, https://doi.org/10.1594/PANGAEA.817799, In supplement to: Foster, LC et al. (2013): Surviving rapid climate change in the deep sea during the Paleogene hyperthermals. Proceedings of the National Academy of Sciences of the United States of America, 110(23), 9273-9276, https://doi.org/10.1073/pnas.1300579110
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Further details:
Röhl, Ursula; Westerhold, Thomas; Bralower, Timothy J; Zachos, James C (2007): On the duration of the Paleocene - Eocene Thermal Maximum (PETM). Geochemistry, Geophysics, Geosystems, 8(12), Q12002, https://doi.org/10.1029/2007GC001784
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -27.859540 * Median Longitude: 2.178315 * South-bound Latitude: -28.533080 * West-bound Longitude: 1.577000 * North-bound Latitude: -27.186000 * East-bound Longitude: 2.779630
Date/Time Start: 2003-03-24T13:00:00 * Date/Time End: 2003-04-04T18:30:00
Minimum DEPTH, sediment/rock: 100.70 m * Maximum DEPTH, sediment/rock: 253.65 m
Event(s):
208-1262A * Latitude: -27.186000 * Longitude: 1.577000 * Date/Time Start: 2003-03-24T13:00:00 * Date/Time End: 2003-03-26T12:40:00 * Elevation: -4759.0 m * Penetration: 161.5 m * Recovery: 163.53 m * Location: Walvis Ridge, Southeast Atlantic Ocean * Campaign: Leg208 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 17 cores; 161.5 m cored; 0 m drilled; 101.3 % recovery
208-1263C * Latitude: -28.533080 * Longitude: 2.779630 * Date/Time Start: 2003-04-03T13:30:00 * Date/Time End: 2003-04-04T18:30:00 * Elevation: -2717.1 m * Penetration: 290.8 m * Recovery: 122.06 m * Location: Walvis Ridge, Southeast Atlantic Ocean * Campaign: Leg208 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 16 cores; 126.3 m cored; 164.5 m drilled; 96.6 % recovery
Comment:
DEPTH, sediment [m] is given in mbsf. The penultimate chamber was chosen for measurement because the final chamber of foraminifers often shows very thin walls not representative for the overall growth. Where dissolution prevented counting of the number of the chambers, the number is the count of preserved chambers (indicated by >).
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Sample code/label | Sample label | Foster, Laura C | DSDP/ODP/IODP sample designation | ||
3 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
4 | Depth, composite revised | Depth comp r | rmcd | Foster, Laura C | ||
5 | Age, relative | Age rel | ka | Foster, Laura C | since CIE (Roehl et al., 2007) | |
6 | Oridorsalis umbonatus, penultimate chamber width | O. umbonatus pen chamber w | µm | Foster, Laura C | ||
7 | Oridorsalis umbonatus, chamber number | O. umbonatus chamber no | # | Foster, Laura C | ||
8 | Oridorsalis umbonatus, size of proloculus | O. umbonatus size proloc | µm | Foster, Laura C | ||
9 | Oridorsalis umbonatus, maximum test width | O. umbonatus max w | µm | Foster, Laura C | ||
10 | Oridorsalis umbonatus, calcite volume | O. umbonatus cal vol | µm3 | Foster, Laura C | ||
11 | Oridorsalis umbonatus, test volume | O. umbonatus test volume | µm3 | Foster, Laura C | ||
12 | Oridorsalis umbonatus, penultimate chamber width/maximum test width ratio | O. umbonatus pen chamber w/max w | % | Foster, Laura C | ||
13 | Calcite, volume normalized | Cal vol norm | % | Foster, Laura C |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
186 data points