Grant S. Boardman
University of Nebraska-Lincoln, Lincoln, NE
Activity
2012
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MINIMAL CHANGE IN VEGETATION STRUCTURE ACROSS THE EOCENE-OLIGOCENE BOUNDARY IN NEBRASKA AS INDICATED BY STABLE ISOTOPES IN MAMMALS
4 Advances in Our Understanding of Paleogene Climate and Vegetative Change in the North American Mid-Continent and Rocky Mountain RegionWednesday, 9 May 20128:30 AM - 11:15 AMAlvarado H
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EARLY OLIGOCENE PALEOSOLS AND FLUVIAL CHANNELS AT TOADSTOOL GEOLOGIC PARK, NORTHWEST NEBRASKA: EVIDENCE FOR STATIC CLIMATE THROUGH CHANGING STYLE OF SEDIMENTATION
4 Advances in Our Understanding of Paleogene Climate and Vegetative Change in the North American Mid-Continent and Rocky Mountain RegionWednesday, 9 May 20128:30 AM - 11:15 AMAlvarado H
2011
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A PRELIMINARY STABLE ISOTOPE ECOLOGY BASED ON TOOTH ENAMEL FOR LATEST EOCENE AND EARLIEST OLIGOCENE PERISSODACTYLS (MAMMALIA) FROM THE WHITE RIVER GROUP OF NORTHWESTERN NEBRASKA
27 The Mammalian Fossil Record of UtahFriday, 20 May 20118:00 AM - 1:00 PMElm