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Isotopic analysis of wetland development in the American SouthwestDepartment of Botany, University of Wyoming, Laramie WY 82071, USA, minckley{at}uwyo.edu
Department of Geology and Geophysics, University of Wyoming, Laramie WY 82071, USA
Department of Geography, University of Utah, Salt Lake City UT, USA
Department of Geology and Geophysics, University of Wyoming, Laramie WY 82071, USA
The analysis of stable isotope and elemental fractions of organic material collected from San Bernardino Ciénega was used to understand the history of vegetation composition and climate change within this desert wetland. A 4000-yr record of sediment buildup, based on four 14C measurements, provides unique opportunities for the study of environmental conditions within an arid landscape and documents climate shifts from drier to wetter conditions in the late Holocene.
Key Words: Ciénegas wetland development Chihuahuan Desert isotopes climate change sedimentation Sonoran Desert late Holocene.
The Holocene, Vol. 19, No. 5,
737-745 (2009) |
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13C,