Temperature trends of the late Cambrian through the Middle Ordovician using oxygen isotopic analysis of conodont apatite
Laura E Speir1, Fernanda Serra2, Nicolás Feltes2, Guillermo Albanesi2, Linda C Kah3, Raymond L Ethington1, James F Miller4 and Kenneth G MacLeod1, (1)University of Missouri, Department of Geological Sciences, Columbia, MO, United States, (2)CONICET, Universidad Nacional de Córdoba, CICTERRA, Córdoba, Argentina, (3)University of Tennessee, Department of Earth and Planetary Sciences, Knoxville, TN, United States, (4)Missouri State University, Department of Geography, Geology and Planning, Springfield, MO, United States
