Clim. Past, 8, 1031-1045, 2012
www.clim-past.net/8/1031/2012/
doi:10.5194/cp-8-1031-2012
© Author(s) 2012. This work is distributed
under the Creative Commons Attribution 3.0 License.
Volcanic synchronisation between the EPICA Dome C and Vostok ice cores (Antarctica) 0–145 kyr BP
F. Parrenin1,2, J.-R. Petit2, V. Masson-Delmotte3, E. Wolff4, I. Basile-Doelsch5, J. Jouzel3, V. Lipenkov6, S. O. Rasmussen7, J. Schwander8, M. Severi9, R. Udisti9, D. Veres2,10, and B. M. Vinther6
1Laboratoire Chrono-Environnement, UMR6249, Besançon, France
2Laboratoire de Glaciologie et Géophysique de l'Environnement, UMR5183 – CNRS, Grenoble, France
3Laboratoire des Sciences du Climat et de l'Environnement, Gif-sur-Yvette, France
4British Antarctic Survey, Cambridge, UK
5Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement, Aix-en-Provence, France
6Arctic and Antarctic Research Institute, St Petersburg, Russia
7Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark
8Physics Institute, University of Bern, Bern, Switzerland
9Department of Chemistry, University of Florence, Florence, Italy
10Institute of Speleology, Romanian Academy, Cluj-Napoca, Romania

Abstract. This study aims at refining the synchronisation between the EPICA Dome C (EDC) and Vostok ice cores in the time interval 0–145 kyr BP by using the volcanic signatures. 102 common volcanic events were identified by using continuous electrical conductivity (ECM), di-electrical profiling (DEP) and sulfate measurements while trying to minimize the distortion of the glaciological chronologies. This is an update and a continuation of previous works performed over the 0–45 kyr interval that provided 56 tie points to the ice core chronologies (Udisti et al., 2004). This synchronisation will serve to establish Antarctic Ice Core Chronology 2012, the next synchronised Antarctic dating. A change of slope in the EDC-depth/Vostok-depth diagram is probably related to a change of accumulation regime as well as to a change of ice thickness upstream of the Lake Vostok, but we did not invoke any significant temporal change of surface accumulation at EDC relative to Vostok. No significant phase difference is detected between the EDC and Vostok isotopic records, but depth shifts between the Vostok 3G and 5G ice cores prevent from looking at this problem accurately. Three possible candidates for the Toba volcanic super-eruption ~73 kyr ago are suggested in the Vostok and EDC volcanic records. Neither the ECM, DEP nor the sulfate fingerprints for these 3 events are significantly larger than many others in the records.

Citation: Parrenin, F., Petit, J.-R., Masson-Delmotte, V., Wolff, E., Basile-Doelsch, I., Jouzel, J., Lipenkov, V., Rasmussen, S. O., Schwander, J., Severi, M., Udisti, R., Veres, D., and Vinther, B. M.: Volcanic synchronisation between the EPICA Dome C and Vostok ice cores (Antarctica) 0–145 kyr BP, Clim. Past, 8, 1031-1045, doi:10.5194/cp-8-1031-2012, 2012.
 
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