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Paleogeography and Paleoenvironment of the Tethyan Realm During the Jurassic Breakup of Pangea

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The Tethys Ocean

Abstract

To reconstitute the evolution of the paleogeography and paleoenvironments of Tethys from 201 Ma until 135 Ma, five maps at a 1:20,000,000 scale were used, four of which were incorporated into the Tethys Atlas of Dercourt et al. (1993). They are (1) the Late Sinemurian map (unpublished), (2) the Mid-Toarcian (Bassoullet et al., 1993), (3) the Callovian (Enay et al., 1993), (4) the Early Kimmeridgian (Cecca et al., 1993), and (5) the Late Tithonian (Fourcade et al., 1991a, 1993). The first and last show periods of relatively low sea level, whereas the three others correspond to periods of relatively high sea level.

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Authors and Affiliations

  1. CNRS URA 1761, Département de Géologie Sédimentaire, Université Pierre et Marie Curie, Paris, France

    Eric Fourcade, Jacques Azéma, Jean-Paul Bassoullet, Fabrizio Cecca & Jean Dercourt

  2. URAM, Université Lyon 1, Villeurbanne, France

    Raymond Enay

  3. Faculté des Sciences, Université d’Avignon, Avignon, France

    René Guiraud

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  1. Eric Fourcade
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  2. Jacques Azéma
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  4. Fabrizio Cecca
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Editors and Affiliations

  1. University of South Carolina, Columbia, South Carolina, USA

    Alan E. M. Nairn

  2. CNRS, Paris, France

    Luc-Emmanuel Ricou  & Bruno Vrielynck  & 

  3. Université Pierre et Marie Curie, Paris, France

    Jean Dercourt

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Fourcade, E. et al. (1995). Paleogeography and Paleoenvironment of the Tethyan Realm During the Jurassic Breakup of Pangea. In: Nairn, A.E.M., Ricou, LE., Vrielynck, B., Dercourt, J. (eds) The Tethys Ocean. Springer, Boston, MA. https://doi.org/10.1007/978-1-4899-1558-0_6

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