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The Pearson product moment coefficient and the Baroni-Urbani-Buser binary similarity coefficient were used to test the relationship between lithofacies and conodont biofacies in the Beaver Bend Limestone in Indiana. This lower Chesterian limestone includes a variety of lithotopes, but no associations were readily recognizable. Possibly this failure resulted from collecting techniques, a factor that we plan to test with further study.

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