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* School of Renewable Natural Resources, § Laboratory of
Tree-Ring Research, and ¶ Department of Geosciences,
University of Arizona, Tucson, AZ 85721; and Edited by Jeremy A. Sabloff, University of Pennsylvania Museum of
Archaeology and Anthropology, Philadelphia, PA, and approved August 15, 2001 (received for review June 15, 2001)
Between A.D. 900 and 1150, more than 200,000 conifer trees
were used to build the prehistoric great houses of Chaco Canyon, New
Mexico, in what is now a treeless landscape. More than one-fifth of
these timbers were spruce (Picea) or fir
(Abies) that were hand-carried from isolated
mountaintops 75-100 km away. Because strontium from local dust, water,
and underlying bedrock is incorporated by trees, specific logging sites
can be identified by comparing 87Sr/86Sr
ratios in construction beams from different ruins and building periods
to ratios in living trees from the surrounding mountains. 87Sr/86Sr ratios show that the beams came
from both the Chuska and San Mateo (Mount Taylor) mountains, but not
from the San Pedro Mountains, which are equally close. Incorporation of
logs from two sources in the same room, great house, and year suggest
stockpiling and intercommunity collaboration at Chaco Canyon. The use
of trees from both the Chuska and San Mateo mountains, but not from the San Pedro Mountains, as early as A.D. 974 suggests that selection of
timber sources was driven more by regional socioeconomic ties than by a
simple model of resource depletion with distance and time.
Geology
Strontium isotopes reveal distant sources of architectural timber
in Chaco Canyon, New Mexico
,
,
U.S.
Geological Survey, Desert Laboratory, Tucson, AZ 85745
To whom reprint requests should be addressed at:
School of Renewable Natural Resources, 325 BioSciences East, University
of Arizona, Tucson, AZ 85721. E-mail: nenglish{at}ag.arizona.edu.
www.pnas.org/cgi/doi/10.1073/pnas.211305498
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