Title of article
New MIS 19 EPICA Dome C high resolution deuterium data: Hints for a problematic preservation of climate variability at sub-millennial scale in the “oldest ice”
Author/Authors
Pol، نويسنده , , K. and Masson-Delmotte، نويسنده , , V. and Johnsen، نويسنده , , S. and Bigler، نويسنده , , M. A. Cattani-Lorente، نويسنده , , O. and Durand، نويسنده , , G. and Falourd، نويسنده , , S. and Jouzel، نويسنده , , J. and Minster، نويسنده , , B. and Parrenin، نويسنده , , F. and Ritz، نويسنده , , C. and Steen-Larsen، نويسنده , , H.C. and Stenni، نويسنده , , B.، نويسنده ,
Issue Information
روزنامه با شماره پیاپی سال 2010
Pages
9
From page
95
To page
103
Abstract
Marine Isotope Stage 19 (MIS 19) is the oldest interglacial period archived in the EPICA Dome C ice core (~ 780 ky BP) and the closest “orbital analogue” to the Holocene — albeit with a different obliquity amplitude and phase with precession. New detailed deuterium measurements have been conducted with a depth resolution of 11 cm (corresponding time resolution of ~ 130 years). They confirm our earlier low resolution profile (55 cm), showing a relatively smooth shape over the MIS 20 to MIS 18 time period with a lack of sub-millennial climate variability, first thought to be due to this low resolution. The MIS 19 high resolution profile actually reveals a strong isotopic diffusion process leading to a diffusion length of at least ~ 40 cm erasing sub-millennial climate variability. We suggest that this diffusion is caused by water-veins associated with large ice crystals at temperatures above −10 °C, temperature conditions in which the MIS 19 ice has spent more than 200 ky. This result has implications for the selection of the future “oldest ice” drilling site.
Keywords
water stable isotopes , Ice cores , Isotopic diffusion , Antarctica
Journal title
Earth and Planetary Science Letters
Serial Year
2010
Journal title
Earth and Planetary Science Letters
Record number
2328555
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