Juan Carlos SILVA-TAMAYO
Department of Geological and Environmental Sciences, Stanford University, USA/Department of Earth and Environment, University of Leeds, U.K.Stefan WEYER
Institut fur Mineralogie, Leibniz Universitat Hannover, GermanyPaul B. WIGNALL
Department of Earth and Environment, University of Leeds, U.KJonathan L. PAYNE
Department of Geological and Environmental Sciences, Stanford University, USARobert J.NEWTON
Department of Earth and Environment, University of Leeds, U.K.Nadjia NEUBERT
Institut fur Mineralogie, Leibniz Universitat Hannover, GermanyAnnika BRUESKE
Institut fur Mineralogie, Leibniz Universitat Hannover, GermanyKimberly LAU
Department of Geological and Environmental Sciences, Stanford University, USAKatharine MAHER
Department of Geological and Environmental Sciences, Stanford University, USAJuan Carlos SILVA-TAMAYO, Stefan WEYER, Paul B. WIGNALL, Jonathan L. PAYNE, Robert J. NEWTON, Nadjia NEUBERT, Annika BRUESKE, Kimberly LAU, Katharine MAHER.2013. Mo and U Isotope Evidence of Ocean Euxinia during the End-Permian Mass Extinction[J]. Acta Geologica Sinica(),87(Z1):903
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