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Littler, Kate; Röhl, Ursula; Westerhold, Thomas; Zachos, James C (2014): X-ray fluorescence (XRF) iron (Fe) core scannings of ODP Site 208-1262 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.833209, In supplement to: Littler, K et al. (2014): A high-resolution benthic stable-isotope record for the South Atlantic: Implications for orbital-scale changes in Late Paleocene–Early Eocene climate and carbon cycling. Earth and Planetary Science Letters, 401, 18-30, https://doi.org/10.1016/j.epsl.2014.05.054

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Further details:
Westerhold, Thomas; Röhl, Ursula; Raffi, Isabella; Fornaciari, Eliana; Monechi, Simonetta; Reale, Viviana; Bowles, Julie; Evans, Helen F (2008): Astronomical calibration of the Paleocene time. Palaeogeography, Palaeoclimatology, Palaeoecology, 257(4), 377-403, https://doi.org/10.1016/j.palaeo.2007.09.016
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: 106.570 m * Maximum DEPTH, sediment/rock: 180.090 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/rock = Depth (mcd).Fe abundance data (XRF) for ODP Site 1262, adapted from Westerhold et al., 2007; 2008. Age model is based on option 1 of Westerhold et al., 2008 (W08), extended in this study to encompass depths 103-113 mcd.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2AGEAgeka BPGeocode
3Iron, area, total countsFe count#Littler, KateX-ray fluorescence core scanner (XRF) II, Bremen, (AVAATECH)
Size:
3837 data points

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