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Gruetzner, Jens; Higgins, Sean M (2010): Element intensities and concentrations of K, Ti and Ca, true molar ratios of these elements and derived CaCO3 at IODP Site 306-U1314 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.770381, In supplement to: Gruetzner, J; Higgins, SM (2010): Threshold behavior of millennial scale variability in deep water hydrography inferred from a 1.1 Ma long record of sediment provenance at the southern Gardar Drift. Paleoceanography, 25, PA4204, https://doi.org/10.1029/2009PA001873

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Coverage:
Latitude: 56.364000 * Longitude: -27.888000
Date/Time Start: 2005-04-07T00:00:00 * Date/Time End: 2005-04-10T00:00:00
Minimum DEPTH, sediment/rock: 0.19 m * Maximum DEPTH, sediment/rock: 83.14 m
Event(s):
306-U1314 * Latitude: 56.364000 * Longitude: -27.888000 * Date/Time Start: 2005-04-07T00:00:00 * Date/Time End: 2005-04-10T00:00:00 * Elevation: -2800.0 m * Recovery: 765.63 m * Location: North Atlantic * Campaign: Exp306 (North Atlantic Climate 2) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE)
Comment:
Sediment depth is given in mbsf. Element intensities were measured with X-ray fluorescence core scanning in Bremen (core scanner XRF2) at 10 kV. True molar ratios and concentrations were derived from a log ratio calibration with 54 quantitative XRF measurements on discrete samples.
Size:
100524 data points

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