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Stable oxygen and carbon isotope ratios of planktonic foraminifera in MIS 6 of sediment core MD01-2443

Antje H L Voelker, Lúcia de Abreu

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Abstract

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).).

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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).).

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Available abstract

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).).

Key concepts: Foraminifera, Sediment core, Plankton, Isotopes of oxygen, Oceanography, Oxygen isotope ratio cycle, Isotopes of carbon, Geology

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