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Strontium isotopes reveal distant sources of architectural timber in Chaco Canyon, New Mexico

Bibliographic Data

ID23354344
AuthorsNathan B English (0000-0002-6936-8079, School of Renewable Natural Resources, Laboratory of Tree-Ring Research, and Department of Geosciences, University of Arizona, Tucson, AZ 85721; and U.S. Geological Survey, Desert Laboratory, Tucson, AZ 85745), Julio L Betancourt (0000-0002-7165-0743, School of Renewable Natural Resources, Laboratory of Tree-Ring Research, and Department of Geosciences, University of Arizona, Tucson, AZ 85721; and U.S. Geological Survey, Desert Laboratory, Tucson, AZ 85745), Jeffrey S Dean (School of Renewable Natural Resources, Laboratory of Tree-Ring Research, and Department of Geosciences, University of Arizona, Tucson, AZ 85721; and U.S. Geological Survey, Desert Laboratory, Tucson, AZ 85745), Jeffrey Dean (Arizona Geological Survey), Jay Quade (0000-0003-2342-858X, School of Renewable Natural Resources, Laboratory of Tree-Ring Research, and Department of Geosciences, University of Arizona, Tucson, AZ 85721; and U.S. Geological Survey, Desert Laboratory, Tucson, AZ 85745)
Year2001
Volume98
Issue21
Pages11891-11896
Publication date2001-10-09
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueProceedings of the National Academy of Sciences (JOURNAL)
Journal identifiersISSN: 0027-8424 • E-ISSN: 1091-6490
PublisherNational Academy of Sciences (PUBLISHER • US)
DOI10.1073/pnas.211305498
PMID11572943
PMCIDPMC59738
OpenAlexW1987635390
LanguageEN
Citations received75
References cited20

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 87 Sr/ 86 Sr ratios in construction beams from different ruins and building periods to ratios in living trees from the surrounding mountains. 87 Sr/ 86 Sr 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.

Archaeology · Bedrock · Canyon · Geography · Geomorphology · Physical geography · Prehistory · Archaeology and ancient environmental studies · Forestry · Geology · Geology and Paleoclimatology Research · Paleontology · Tree-ring climate responses

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Unique citing works75
Citations per year3,13
Citation span2002 - 2026 (25)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 67
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