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The Fe-Isotope System and Its Applicability as a BiosignatureHigh precision (0.05) Fe isotope analyses show that igneous rocks and loess are invariant but chemical sediments have variable compositions. The relative roles of abiologic and biologic fractionations that produced this range are discussed. Additional information is contained in the original extended abstract.
Document ID
20010044906
Acquisition Source
Jet Propulsion Laboratory
Document Type
Conference Paper
Authors
Beard, Brian L. (Wisconsin Univ. Madison, WI United States)
Johnson, Clark M. (Wisconsin Univ. Madison, WI United States)
Skulan, Joseph (Wisconsin Univ. Madison, WI United States)
Taylor, Lawerence A. (Tennessee Univ. Knoxville, TN United States)
Sun, Henry (Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Cox, Lea (Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Nealson, Kenneth H. (Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Sinha, Mahadeva P. (Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Gerdenich, Michael J. (Michigan Univ. Ann Arbor, MI United States)
Date Acquired
August 20, 2013
Publication Date
January 1, 2001
Publication Information
Publication: Lunar and Planetary Science XXXII
Subject Category
Lunar And Planetary Science And Exploration
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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