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

DOI

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).).

Identifier
DOI https://doi.org/10.1594/PANGAEA.737173
Related Identifier https://doi.org/10.1594/PANGAEA.737449
Related Identifier https://doi.org/10.1029/2010GM001021
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.737173
Provenance
Creator Voelker, Antje H L ORCID logo; de Abreu, Lucia
Publisher PANGAEA
Publication Year 2011
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 480 data points
Discipline Earth System Research
Spatial Coverage (-10.176 LON, 37.881 LAT)