A new magnetofossil approach to trace paleoenvironmental changes across the Paleocene-Eocene Thermal Maximum

Liao Chang, Peking University, School of Earth and Space Sciences, Beijing, China, Richard J Harrison, University of Cambridge, Department of Earth Sciences, Cambridge, United Kingdom, David Heslop, Australian National University, Research School of Earth Sciences, Canberra, ACT, Australia and Andrew P Roberts, Australian National University, Research School of Earth Sciences, Canberra, Australia
Back to: Advances in Biomagnetism, Magnetic Proxy Parameters, and Authigenesis and Diagenesis of Magnetic Minerals I