Anomalous flow below 2700 m in the EPICA Dome C ice core detected using delta O-18 of atmospheric oxygen measurements

作者：Dreyfus G B^*; Parrenin F; Lemieux Dudon B; Durand G; Masson Delmotte V; Jouzel J; Barnola J M; Panno L; Spahni R; Tisserand A; Siegenthaler U; Leuenberger M

来源：Climate of the Past, 2007, 3(2): 341-353.

While there are no indications of mixing back to 800 000 years in the EPICA Dome C ice core record, comparison with marine sediment records shows significant differences in the timing and duration of events prior to stage 11 (similar to 430 ka, thousands of years before 1950). A relationship between the isotopic composition of atmospheric oxygen (delta O-18 of O-2, noted delta O-18(atm))and daily northern hemisphere summer insolation has been observed for the youngest four climate cycles. Here we use this relationship with new delta O-18 of O-2 measurements to show that anomalous flow in the bottom 500 m of the core distorts the duration of events by up to a factor of 2. By tuning delta O-18(atm) to orbital precession we derive a corrected thinning function and present a revised age scale for the interval corresponding to Marine Isotope Stages 11-20 in the EPICA Dome C ice core. Uncertainty in the phasing of delta O-18(atm) with respect to insolation variations in the precession band limits the accuracy of this new agescale to +/- 6 kyr (thousand of years). The previously reported similar to 30 kyr duration of interglacial stage 11 is unchanged. In contrast, the duration of stage 15.1 is reduced by a factor of 2, from 31 to 16 kyr.

• 出版日期2007
• 单位中国地震局