| Literature DB >> 34040008 |
Vasileios Gkinis1, Bo M Vinther2, Trevor J Popp2, Thea Quistgaard2, Anne-Katrine Faber2,3, Christian T Holme2, Camilla-Marie Jensen2,4, Mika Lanzky2,5, Anine-Maria Lütt2, Vasileios Mandrakis2,4, Niels-Ole Ørum2, Anna-Sofie Pedersen2, Nikol Vaxevani2, Yongbiao Weng2,3, Emilie Capron2,6, Dorthe Dahl-Jensen2,7, Maria Hörhold8, Tyler R Jones9, Jean Jouzel10, Amaëlle Landais10, Valérie Masson-Delmotte10, Hans Oerter8, Sune O Rasmussen2, Hans Christian Steen-Larsen2,3, Jørgen-Peder Steffensen2, Árný-Erla Sveinbjörnsdóttir11, Anders Svensson2, Bruce Vaughn9, James W C White9.
Abstract
We report high resolution measurements of the stable isotope ratios of ancient ice (δ18O, δD) from the North Greenland Eemian deep ice core (NEEM, 77.45° N, 51.06° E). The record covers the period 8-130 ky b2k (y before 2000) with a temporal resolution of ≈0.5 and 7 y at the top and the bottom of the core respectively and contains important climate events such as the 8.2 ky event, the last glacial termination and a series of glacial stadials and interstadials. At its bottom part the record contains ice from the Eemian interglacial. Isotope ratios are calibrated on the SMOW/SLAP scale and reported on the GICC05 (Greenland Ice Core Chronology 2005) and AICC2012 (Antarctic Ice Core Chronology 2012) time scales interpolated accordingly. We also provide estimates for measurement precision and accuracy for both δ18O and δD.Entities:
Year: 2021 PMID： 34040008 DOI： 10.1038/s41597-021-00916-9
Source DB: PubMed Journal: Sci Data ISSN： 2052-4463 Impact factor: 6.444