Epipelagic chitinozoan biotopes map a steep latitudinal temperature gradient for earliest Late Ordovician seas: Implications for a cooling Late Ordovician climate

T. Vandenbroucke,H. Armstrong,M. Williams,F. Paris,K. Sabbe,J. Zalasiewicz,J. Nõlvak,J. Verniers

Published 2010 in Palaeogeography, Palaeoclimatology, Palaeoecology

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