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Foster, Laura C; Schmidt, Daniela N; Thomas, Ellen; Arndt, Sandra; Ridgwell, Andy (2013): (Table S1b) Measured tomographic parameters for Oridorsalis umbonatus during the PETM for ODP Site 208-1262 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.817796, 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:
Latitude: -27.185833 * Longitude: 1.577000
Date/Time Start: 2003-03-24T00:00:00 * Date/Time End: 2003-03-29T00:00:00
Minimum DEPTH, sediment/rock: 114.06 m * Maximum DEPTH, sediment/rock: 128.23 m
Event(s):
208-1262 * Latitude: -27.185833 * Longitude: 1.577000 * Date/Time Start: 2003-03-24T00:00:00 * Date/Time End: 2003-03-29T00:00:00 * Elevation: -4755.4 m * Penetration: 583.9 m * Recovery: 502.5 m * Location: Walvis Ridge, Southeast Atlantic Ocean * Campaign: Leg208 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 54 cores; 493.9 m cored; 90 m drilled; 101.7 % 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 >). Test with significant dissolution observed in samples 208-1262A-13H-6,30-31 and 208-1262B-15H-3,74-75; represents a minimium estimate of CaCO3.
Parameter(s):
Size:
128 data points

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