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Quaternary Stratigraphy Near Cincinnati, Ohio, And Its Significance For Paleoclimate Reconstruction. Open Access Deposited
Rare occurences of coeval late Wisconsin glacigenic diamictons and ice-proximal sediments with a diverse faunal assemblage provided an opportunity to test the viability of the glacigenic sediments as proxy paleoclimate indicators.
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- Ph.D.
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- Chair: Thomas Lowell.
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Permanent link to this page: https://scholar.uc.edu/show/n583xv070