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Spruce trees from a melting ice patch: evidence for Holocene climatic change in the Colorado Rocky Mountains, USA

( Center for Mountain Archeology, 8297 Overland Road, Ward CO 80481, USA

Robert J. Benedict

8684 Thunderhead, C<9 Boulder CO 80302, USA

Craig M. Lee

Institute of Arctic and Alpine Research, University of Colorado, Boulder CO 80309, USA

Dennis M. Staley

US Geological Survey, 1711 Illinois Street, Golden CO 80401, USA

In September, 2006, we found the remains of timber-sized spruce trees ( Picea engelmannii) on the floors of melting ice patches at altitudes of 3465—3480 m in the Mummy Range of north-central Colorado. The ice patches occupy northeast-facing recesses in which windblown snow, scoured from a tundra upland to the southwest, accumulates deeply. We hypothesize that the upland was timbered during the early to middle Holocene. Dense forest vegetation intercepted snow, preventing it from blowing to the recesses, and allowing trees to become established there. Neoglacial cooling led to gradual deforestation of the upland, renewed transport and deposition of snow by wind, and death of the ice-patch trees. Radiocarbon dates show that the trees died between 3860 ± 15 and 3780 ± 20 ¹⁴C yr BP (c. 4200 cal. yr BP). The trunks show decay similar to that of historic log structures built above timberline during the late nineteenth and early twentieth centuries, suggesting that they have been protected by ice for all but a small portion of the past 4200 years. A series of warm summers and dry winters led to their recent emergence. The study illustrates the importance of monitoring glaciers and ice patches for floral, faunal and archaeological remains whenever severe melting occurs.

Key Words: Ice patches • climatic change • Colorado Front Range • Picea engelmannii • sclerotia • snowbed loess • timberline fluctuations • windblown snow • Holocene.

The Holocene, Vol. 18, No. 7, 1067-1076 (2008)
DOI: 10.1177/0959683608095578


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