Fix:Mediterranean Rupelian.jpg

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English: Paleogeography of the Mediterrenean region during the Rupelian age (33.9 - 28.4 million years ago). The Tethys Ocean between Africa and Europe is closing. Paratethys gets separated from Tethys by the formation of the Alps, Carpathians, Dinarides, Taurus and Elburz mountains (all Alpine orogeny). Black lines indicate present day coastlines.

Drawn by the uploader, after studying several sources, most used were:

  • Rögl, F., 1999. Mediterranean and Paratethys. Facts and hypotheses of an Oligocene to Miocene paleogeography (Short Overview). Geologica Carpathica 50 (4), 339– 349.
  • Schulz, H.-M.; Vakarcs, G. & Magyar, I.; 2005: The birth of the Paratethys during the Early Oligocene: From Tethys to an ancient Black Sea analogue?, Global and Planetary Change 49(3-4), p. 163-176.
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Fonte Obra propre
Autor Woudloper

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Public domain I, the copyright holder of this work, release this work into the public domain. This applies worldwide.
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Paratethys sea during the late Jurassic stage.

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aora12:16, 30 desembre 2011Imajeta per revisa de 12:16, 30 desembre 20111,038 × 747 (294 KB)CiaurlecUniformed colours to other geological maps
21:12, 13 julio 2008Imajeta per revisa de 21:12, 13 julio 20081,038 × 747 (136 KB)Woudloper{{Information |Description={{en|1=Paleogeography of the Mediterrenean region during the Rupelian age (33,9 - 28,4 million years ago). The Tethys Ocean between Africa and Europe is closing. The Paratethys gets separated from the Tethys by the formation of

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