--> Abstract: Dates, Rates and Global Correlation of the Permian of West Texas Based from Coupled U-Pb Carbonate Ages and Sr Chemostratigraphy, by Troy Rasbury, Gary Hemming, Tony Dickson, Jim Barrick, and Art Saller; #90078 (2008)

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Dates, Rates and Global Correlation of the Permian of West Texas Based from Coupled U-Pb Carbonate Ages and Sr Chemostratigraphy

Troy Rasbury1, Gary Hemming2, Tony Dickson3, Jim Barrick4, and Art Saller5
1Geosciences, Stony Brook University, Stony Brook, NY
2SEES, Queens College CUNY, Flushing, NY
3Earth Science, Cambridge University, Cambridge, United Kingdom
4Geosciences, Texas Tech University, Lubbock, TX
5Chevron Corporation, Sugarlands, TX

The Permian Basin of Texas has a marine record that extends through the late Permian. Thus changes in sealevel that, in part, reflect changes in southern ice sheets of Gowdwana are recorded within these Permian low-latitude strata. A U-Pb-carbonate-age-constrained 87Sr/86Sr trend shows a rapid decline from a Pennsylvanian high of 0.70825, to a Carboniferous-Permian boundary value of 0.70815, consistent with published Sr trends and U-Pb zircon ages from the type sections in the Urals. The decline in 87Sr/86Sr is coincident with multiple lines of evidence for increasing aridity in the Pangean tropics, and results from a decrease in continental contributions to the global marine Sr reservoir relative to other sources. This trend of declining Sr is consistent with reduced silicate weathering.

Permian Basin icehouse-style high-amplitude and high-frequency cycles (cyclothems) are replaced by greenhouse-style low-amplitude cycles at Wichita/Abo (Sakmarian) time. This change follows a 17 km step-back of the shelf deposits on the Central Basin Platform that is interpreted as a major transgression. This transgression occurred at a 87Sr/86Sr value of approximately 0.7078, no more than 6 million years after the onset of aridity. A model that links these observations is that reduced silicate weathering caused an increase in pCO2, which has been recognized by terrestrial proxy records, and that the increase in this greenhouse gas was responsible for collapse of the long-lived Carboniferous-Permian glaciers. Transitional type cycles recognized in the Guadalupian may relate to a last pulse of Permian glaciation recognized in Australia.

 

AAPG Search and Discover Article #90078©2008 AAPG Annual Convention, San Antonio, Texas