The demise of a diverse magnetofossil assemblage across the Eocene-Oligocene Transition in a Northwest Atlantic sediment drift.

Peter C Lippert1, Vicki E Taylor2, Steven M Bohaty2, Courtney Wagner1, Chuang Xuan2 and Paul A Wilson2, (1)University of Utah, Department of Geology and Geophysics, Salt Lake City, UT, United States, (2)University of Southampton, Ocean and Earth Science, Southampton, United Kingdom
Back to: Recent Advances in Environmental and Biogeomagnetism I