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Full-Text Articles in Paleontology
Assessing Diagenetic Conditions In The Late Triassic Chinle Formation Through Petrographic And Geochemical Analysis Of Phytosaur Teeth, John Fortner
Earth Sciences Theses and Dissertations
The Upper Triassic (Norian; ~227-208 Ma) Chinle Formation of Petrified Forest (PeFo) National Park was deposited during a time of major tectonic breakup and profound changes in atmospheric circulation and faunal compositions. Little has been done however to assess whether surficial paleoenvironmental trends related to deterioration of the Late Triassic Megamonsoon resulted in similar trends in the early diagenetic environment. Here, we use phytosaur tooth dentin as a proxy for diagenetic conditions in the Chinle of PEFO, as its greater susceptibility to chemical alteration relative to enamel makes it an excellent substrate from which changing diagenetic conditions may be studied …
Identifying Dietary And Migratory Patterns Of Illinois Woolly Mammoth Populations Using Isotope Analysis Of Carbon, Oxygen, And Strontium, Matthew Harrington, Chris Widga, Al Wanamaker, Doug Walker
Identifying Dietary And Migratory Patterns Of Illinois Woolly Mammoth Populations Using Isotope Analysis Of Carbon, Oxygen, And Strontium, Matthew Harrington, Chris Widga, Al Wanamaker, Doug Walker
Celebration of Learning
The extinct woolly mammoth (Mammuthus primigenius) ranged from Alaska to the Northeastern Seaboard throughout the Late Pleistocene (100-10 Ka). Although it is recognized that woolly mammoths coincided with and lived in a region heavily influenced by glacial ice sheets, little is known about their dietary or migratory behavior. This study classifies and provides insight into the diet and mobility of Midwestern mammoths by analyzing stable isotopes of carbon, oxygen, and strontium preserved in the tooth enamel of these extinct elephantids. A woolly mammoth tooth from Moline, IL, was bulk-sampled and micromilled to extract the aforementioned isotopes from the …