2004 Articles
Eocene Calibration of Geomagnetic Polarity Time Scale Reevaluated: Evidence from the Green River Formation of Wyoming
We reevaluate the Eocene geomagnetic polarity time scale on the basis of single-crystal 40Ar/39Ar ages for air-fall tuffs from the Wilkins Peak Member of the Green River Formation of Wyoming. Tuff 6 is dated as 49.1 ± 0.2 Ma, and tuff 3 is dated as 50.4 ± 0.3 Ma (maximum estimate). When combined with published magnetostratigraphic constraints, these age determinations suggest that the currently accepted age of chron C22r is 1.5–2.5 m.y. too old, which supports a significantly longer duration for the early Eocene, for the early Eocene climatic optimum, and the Wasatchian North American Land Mammal Age.
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- Machlus.Geology.32.137.pdf application/pdf 425 KB Download File
Also Published In
- Title
- Geology
- DOI
- https://doi.org/10.1130/G20091.1
More About This Work
- Academic Units
- Earth and Environmental Sciences
- Lamont-Doherty Earth Observatory
- Biology and Paleo Environment
- Geochemistry
- Seismology, Geology, and Tectonophysics
- Published Here
- August 28, 2013