Comments on “Early Holocene glacier advance, southern Coast Mountains, British Columbia” by Menounos et al

Using atmospheric methane and the isotopic composition of O sub(2) as correlation tools, we place the delta D record of ice from the Siple Dome (West Antarctica) ice core on a precise common chronology with the GISP2 (Greenland) ice core for the period from 9 to 57 ka. The onset of major millennial...

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Published in:Quaternary science reviews 2005-07, Vol.24 (12), p.1521-1526
Main Authors: Kovanen, Dori J., Begét, James E.
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description Using atmospheric methane and the isotopic composition of O sub(2) as correlation tools, we place the delta D record of ice from the Siple Dome (West Antarctica) ice core on a precise common chronology with the GISP2 (Greenland) ice core for the period from 9 to 57 ka. The onset of major millennial warming events in Siple Dome preceded major abrupt warmings in Greenland, and the pattern of millennial change at Siple Dome was broadly similar, though not identical, to that previously observed for the Byrd ice core (also in West Antarctica). The addition of Siple Dome to the database of well-dated Antarctic paleoclimate records supports the case for a coherent regional pattern of millennial-scale climate change in Antarctica during much of the last ice age and glacial-interglacial transition.
doi_str_mv 10.1016/j.quascirev.2004.12.007
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title Comments on “Early Holocene glacier advance, southern Coast Mountains, British Columbia” by Menounos et al
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