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13C excursion in the North American Midcontinent and its regional implications


* Department of Geological Sciences, The Ohio State University, Columbus, Ohio 43210, USA
Department of Geology, GeoBiosphere Science Center, Lund University, Sölvegatan 12, SE-223 62 Lund, Sweden
Author for correspondence: stig{at}geology.ohio-state.edu
The most prominent of the two major global
13C excursions in the Ordovician, the Hirnantian
13C excursion (HICE), which is previously recorded from the uppermost Ordovician in a few sections in Nevada, Quebec, Arctic Canada, Baltoscandia, Scotland and China, is documented for the first time from the North American Midcontinent. Samples through the Girardeau Limestone and Leemon Formation in Missouri and Illinois show elevated
13C values of + 4
to + 5
. Although not determined precisely, the beginning of the HICE is likely to be in the upper part of the Orchard Creek Shale, and it ends in the upper Leemon Formation. Being extraordinarily useful chronostratigraphically, the presence of the HICE makes it possible to provide a firm dating of the study interval, whose age has long been controversial. Comparison between the study sections and coeval HICE sequences in North America and Europe show striking similarities, especially in sea-level history, indicating that major local lowstands reflect eustatic sea-level changes. A comparison with Hirnantian diamictite successions in North and South Africa and Argentina suggests that these lowstands correspond to two major Gondwanan glacial episodes.
Key Words: carbon isotope excursion Hirnantian Upper Ordovician MissouriIllinois Gondwana glaciation sea-level changes
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