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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):
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):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Sample code/labelSample labelFoster, Laura CDSDP/ODP/IODP sample designation
3DEPTH, sediment/rockDepth sedmGeocode
4Depth, composite revisedDepth comp rrmcdFoster, Laura C
5Age, relativeAge relkaFoster, Laura Csince CIE (Roehl et al., 2007)
6Oridorsalis umbonatus, penultimate chamber widthO. umbonatus pen chamber wµmFoster, Laura C
7Oridorsalis umbonatus, chamber numberO. umbonatus chamber no#Foster, Laura C
8Oridorsalis umbonatus, size of proloculusO. umbonatus size prolocµmFoster, Laura C
9Oridorsalis umbonatus, maximum test widthO. umbonatus max wµmFoster, Laura C
10Oridorsalis umbonatus, calcite volumeO. umbonatus cal volµm3Foster, Laura C
11Oridorsalis umbonatus, test volumeO. umbonatus test volumeµm3Foster, Laura C
12Oridorsalis umbonatus, penultimate chamber width/maximum test width ratioO. umbonatus pen chamber w/max w%Foster, Laura C
13Calcite, volume normalizedCal vol norm%Foster, Laura C
Size:
186 data points

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