Conodont apatite δ18O signatures indicate climatic cooling as a trigger of the Late Devonian mass extinction

Research Article| August 01, 2002 Conodont apatite δ18O signatures indicate climatic cooling as a trigger of the Late Devonian mass extinction Michael M. Joachimski; Michael M. Joachimski 1Institute of Geology and Mineralogy, University of Erlangen, Schlossgarten 5, 91054 Erlangen, Germany Search for other works by this author on: GSW Google Scholar Werner Buggisch Werner Buggisch 1Institute of Geology and Mineralogy, University of Erlangen,...