Dataset for Guillevic et al.: Evidence for a three-phase sequence during Heinrich Stadial 4 using a multiproxy approach based on Greenland ice core records, 2014

Supplementary data to Guillevic et al., 2014, Climate of the Past.This file contains 2 data sets: NEEM ice core 17O-excess covering Dansgaard-Oeschger events 7 to 13 and NEEM ice core d18Oatm covering DO 8 to 10.NEEM ice core 17O-excess data. Measured at LSCE, Laboratoire des Sciences du Climat et de l'Environnement, EMR CEA/CNRS/UVSQ 8212, Gif-sur-Yvette, France. Data referenced against the 2-point calibration scale VSMOW (d18O = 0 permil, 17O-excess = 0 permil) - SLAP (d18O = -55.5 permil, 17O-excess = 0 permil). NEEM ice core, isotopic composition of atmospheric oxygen (d18Oatm). Data measured at LSCE, Laboratoire des Sciences du Climat et de l'Environnement, EMR CEA/CNRS/UVSQ 8212, Gif-sur-Yvette, France. Data referenced versus atmospheric air (d18Oatm = 0 permil). Please cite this reference when using the data: M. Guillevic, L. Bazin, A. Landais, C. Stowasser, V. Masson-Delmotte, T. Blunier, F. Eynaud, S. Falourd, E. Michel, B. Minster, T. Popp, F. Prié, and B. M. Vinther. Evidence for a three-phase sequence during Heinrich Stadial 4 using a multiproxy approach based on Greenland ice core records. Clim. Past, vol. 10, pp. 2115-2133, 2014.