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PANGAEA.
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Voelker, Antje H L; de Abreu, Lucia (2011): Stable oxygen and carbon isotope ratios of planktonic foraminifera in MIS 6 of sediment core MD01-2443 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.737173, In supplement to: Voelker, AHL; de Abreu, L (2011): A Review of Abrupt Climate Change Events in the Northeastern Atlantic Ocean (Iberian Margin): Latitudinal, Longitudinal and Vertical Gradients. In: Rashid, H; Polyak, L; Mosley-Thompson, E (eds.), Abrupt Climate Change: Mechanisms, Patterns, and Impacts. Geophysical Monograph Series (AGU, Washington D.C.), 193, 15-37, https://doi.org/10.1029/2010GM001021

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Coverage:
Latitude: 37.881000 * Longitude: -10.176000
Minimum DEPTH, sediment/rock: 14.52 m * Maximum DEPTH, sediment/rock: 16.52 m
Event(s):
MD01-2443 * Latitude: 37.881000 * Longitude: -10.176000 * Elevation: -2925.0 m * Campaign: MD123 (GEOSCIENCES, MARMARCORE) * Basis: Marion Dufresne (1995) * Method/Device: Calypso Corer (CALYPSO)
Comment:
Stable isotope analyses were done in the Godwin Laboratory of the University of Cambridge either in a VG Isotech SIRA - Series II mass spectrometer or a PRISM mass spectrometer, both of which have an analytical precision for the Carrara Marble standard of ±0.08 per mil for delta18O and of ±0.06 per mil for delta13C. Age after Tzedakis et al. (2009, doi:10.1016/j.epsl.2008.10.027).).
Size:
480 data points

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