[This material embargoed until 5 PM ET June 26, 2006 to coincide with publication in the journal Proceedings of the National Academy of Sciences.]
The locations of ice cores and evidence for abrupt climate change approximately 5,000 years ago discussed in the research are shown, along with areas of large-scale ice retreat. Courtesy of Lonnie Thompson, Ohio State University.
A) Retreat of the Qori Kalis glacier at the Quelccaya ice cap from 1963 to 2005. (B) Retreat records for six other Andean glaciers. (C) The photos document the expansion of the proglacial lake from 1991 to 2005 as Qori Kalis retreated. Courtesy of Lonnie Thompson, Ohio State University.
(A) Decadal averages of O-18 isotopes from low-latitude, high-elevation ice fields are combined for the last 2,000 years. The number of cores contributing to various parts of the 2,000-year record is shown. (B and C) Also shown are the composites for four Tibetan (B) and three Andean (C) cores. (D) These cores are compared to the Northern Hemisphere meteorological observations (red) back to A.D. 1860 (50) and a multiproxy history (blue) back to approximately 200 A.D.(51). Courtesy of Lonnie Thompson, Ohio State University.
The plant Distichia muscoides (dating back 5,138 years B.P., +/- 45 years) collected at the retreating margin of the Quelccaya ice cap in August, 2002 is compared to the modern plant. Courtesy of Lonnie Thompson, Ohio State University.

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