On the use of δ18Oatm for ice core dating. (1st April 2018)

• Record Type: Journal Article
• Authors: Extier, Thomas; Landais, Amaelle; Bréant, Camille; Prié, Frédéric; Bazin, Lucie; Dreyfus, Gabrielle; Roche, Didier M.; Leuenberger, Markus
• Is Part Of: Quaternary science reviews. Volume 185(2018)
• Page Start: 244
• Page End: 257
• Publication Date: 2018-04-01
• Subjects: Oxygen isotopes -- δ18Oatm -- Glacial terminations -- Water cycle -- Ice core -- Chronology; Geology, Stratigraphic -- Quaternary -- Periodicals; Stratigraphie -- Quaternaire -- Périodiques; 551.79
• DOI: 10.1016/j.quascirev.2018.02.008
• Languages: English
• ISSNs: 0277-3791

Abstract

Abstract: Deep ice core chronologies have been improved over the past years through the addition of new age constraints. However, dating methods are still associated with large uncertainties for ice cores from the East Antarctic plateau where layer counting is not possible. Indeed, an uncertainty up to 6 ka is associated with AICC2012 chronology of EPICA Dome C (EDC) ice core, which mostly arises from uncertainty on the delay between changes recorded in δ 18 Oatm and in June 21 st insolation variations at 65°N used for ice core orbital dating. Consequently, we need to enhance the knowledge of this delay to improve ice core chronologies. We present new high-resolution EDC δ 18 Oatm record (153–374 ka) and δO2 /N2 measurements (163–332 ka) performed on well-stored ice to provide continuous records of δ 18 Oatm and δO2 /N2 between 100 and 800 ka. The comparison of δ 18 Oatm with the δ 18 Ocalcite from East Asian speleothems shows that both signals present similar orbital and millennial variabilities, which may represent shifts in the InterTropical Convergence Zone position, themselves associated with Heinrich events. We thus propose to use the δ 18 Ocalcite as target for δ 18 Oatm orbital dating. Such a tuning method improves the ice core chronology of the last glacial inception compared to AICC2012 by reconciling NGRIP and mid-latitude climatic records. It is especially marked during Dansgaard-Oeschger 25 where the proposed chronology is 2.2 ka older than AICC2012. This δ 18 Oatm – δ 18 Ocalcite alignment method applied between 100 and 640 ka improves the EDC ice core chronology, especially over MIS 11, and leads to lower ice age uncertainties compared to AICC2012. Highlights: Complete EPICA Dome C δ 18 Oatm and δO2 /N2 records between 100 and 800 ka. δ 18 Oatm link to insolation is modulated by occurrence of millennial events. Links between δ 18 Oatm and δ 18 Ocalcite can be used to improve ice core chronology.