Recalibrated legacy 40Ar/39Ar ages for the Upper Jurassic Morrison Formation, Western Interior, U.S.A.

  • Kelli C. Trujillo Uinta Paleontological Associates, Inc.
  • Bart J. Kowallis Department of Geological Sciences, Brigham Young University
Keywords: Uranium-Lead Dating, Argon-Argon, Morrison

Abstract

As a result of recent updating of decay constants and standard ages used for 40Ar/39Ar dating, it is necessary to recalibrate legacy ages obtained with older methods. These recalibrations bring legacy 40Ar/39Ar ages into better agreement with ages obtained using 238U/206Pb dating methods. We present nine recalibrated 40Ar/39Ar ages for the Upper Jurassic Morrison Formation of the Western Interior, U.S.A., along with the individual geographic and stratigraphic locations for each sample. These recalibrated ages will be useful for researchers looking to place better age constraints on the flora and fauna of the Morrison Formation, as well as for those working to understand stratigraphic relationships across the formation. The recalibrated ages also can now be used reliably for comparisons with newer 238U/206Pb ages obtained for the Morrison Formation.

Morrison Formation near Notom looking towards the east with the Henry Mountains in the far background. The upper Salt Wash and colorful Brushy Basin Members of the Morrison can be seen in the foreground with the Cedar Mountain Formation and Mancos Shale above. The Tidwell and lower Salt Wash Members are not seen in the photo. Photograph by Bart J. Kowallis.
Published
2015-01-20
How to Cite
Trujillo , K., and Kowallis , B., 2015, Recalibrated legacy 40Ar/39Ar ages for the Upper Jurassic Morrison Formation, Western Interior, U.S.A.: Geology of the Intermountain West, v. 2, p. 1-8., doi: 10.31711/giw.v2.pp1-8.