A 120,000-year long climate record from a NW-Greenland deep ice core at ultra-high resolution

International audience We report high resolution measurements of the stable isotope ratios of ancient ice ( δ 18 O, δ D) from the N orth Greenland Eem ian 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...

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Published in:Scientific Data
Main Authors: Gkinis, Vasileios, Vinther, Bo, Popp, Trevor, Quistgaard, Thea, Faber, Anne-Katrine, Holme, Christian, Jensen, Camilla-Marie, Lanzky, Mika, Lütt, Anine-Maria, Mandrakis, Vasileios, Ørum, Niels-Ole, Pedersen, Anna-Sofie, Vaxevani, Nikol, Weng, Yongbiao, Capron, Emilie, Dahl-Jensen, Dorthe, Hörhold, Maria, Jones, Tyler, Jouzel, Jean, Landais, Amaëlle, Masson-Delmotte, Valérie, Oerter, Hans, Rasmussen, Sune, Steen-Larsen, Hans Christian, Steffensen, Jørgen-Peder, Sveinbjörnsdóttir, Árný-Erla, Svensson, Anders, Vaughn, Bruce, White, James W. C.
Other Authors: Niels Bohr Institute Copenhagen (NBI), Faculty of Science Copenhagen, University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH), Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA), University of Manitoba Winnipeg, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI), University of Colorado Boulder, Glaces et Continents, Climats et Isotopes Stables (GLACCIOS), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Institut Pierre-Simon-Laplace (IPSL (FR_636)), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), University of Iceland Reykjavik, ANR-07-VULN-0009,NEEM,NEEM-FRANCE(2007), ANR-19-MPGA-0001,HOTCLIM,Characterisation & Dynamics of Past Warm Climates(2019), European Project: 243908,EC:FP7:ENV,FP7-ENV-2009-1,PAST4FUTURE(2010), European Project: 246815,EC:FP7:ERC,ERC-2009-AdG,WATERUNDERTHEICE(2010), European Project: 610055,EC:FP7:ERC,ERC-2013-SyG,ICE2ICE(2014)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2021
Subjects:
Online Access:https://hal.science/hal-03238378
https://hal.science/hal-03238378/document
https://hal.science/hal-03238378/file/s41597-021-00916-9.pdf
https://doi.org/10.1038/s41597-021-00916-9
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Summary:International audience We report high resolution measurements of the stable isotope ratios of ancient ice ( δ 18 O, δ D) from the N orth Greenland Eem ian 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 δ 18 O and δ D.