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Verplanck, Emily P; Farmer, G Lang; Andrews, John T; Dunhill, Gita; Millo, Christian (2009): (Table 1) Nd and Sr isotopic compositions and isotope dilution trace element concentrations of sediment core PS62/017-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.730178, In supplement to: Verplanck, EP et al. (2009): Provenance of Quaternary glacial and glacimarine sediments along the southeast Greenland margin. Earth and Planetary Science Letters, 286(1-2), 52-62, https://doi.org/10.1016/j.epsl.2009.06.012

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Coverage:
Latitude: 67.850300 * Longitude: -24.585000
Date/Time Start: 2002-07-06T10:32:00 * Date/Time End: 2002-07-06T10:32:00
Minimum DEPTH, sediment/rock: 1.415 m * Maximum DEPTH, sediment/rock: 2.815 m
Event(s):
PS62/017-4 * Latitude: 67.850300 * Longitude: -24.585000 * Date/Time: 2002-07-06T10:32:00 * Elevation: -1502.0 m * Recovery: 6.32 m * Location: Iceland Sea * Campaign: ARK-XVIII/1 (PS62) * Basis: Polarstern * Method/Device: Piston corer (PC) * Comment: 7 core sections: 0-1, 1-1.48, 1.48-2.48, 2.48-3.48, 3.48-4.48, 4.48-5.48, 5.48-6.32 m
Comment:
Isotope dilution concentration determinations are accurate to approx. 1% for Rb and Sr, and 0.5% for Sm and Nd. Total procedural blanks averaged apporx. 1 ng for Sr and 100 pg for Nd, during the study period. Measured 87Sr/86Sr ratios were analyzed using four-collector static mode measurements. Thirty measurements of SRM-987 during the study period yielded mean 87Sr/86Sr=0.71032±2. Measured 143Nd/144Nd normalized to 146Nd/144Nd=0.7219. Analyses were dynamic mode, three-collector measurements. Thirty three measurements of the La Jolla Nd standard during the study period yielded a mean 143Nd/144Nd=0.511838±8 (2sigma mean). e-Nd values are calculated using a present-day 143Nd/144Nd (CHUR)=0.512638. Size fraction <63 µm.
Size:
180 data points

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