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Geological Formation

Posidonia Shale

Named Rock Formations and Groups

The Posidonia Shale is an Early Jurassic, Toarcian age geological formation found across Germany, northern Switzerland, northwestern Austria, southern Luxembourg and the Netherlands, with its major outcrops near Holzmaden and Dotternhausen in southwestern Germany. It consists of black shales made of fine grained sediments and bituminous limestones deposited in fine alternating layers, along with oil shales, nodular claystone and lime mudstone, laid down 184 to 178 million years ago in a shallow epicontinental sea under strongly reducing, oxygen poor conditions during the Toarcian oceanic anoxic event. These anoxic conditions trapped and exceptionally preserved complete fossils of marine fish and reptiles, making the formation an important source of Jurassic marine fossils. It takes its name from the fossil bivalve historically called Posidonia bronni, though that generic name is now considered invalid.

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Source Posidonia Shale (Wikipedia)

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Source Posidonia Shale (Wikipedia)
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Also in Geography Atlas: where this subject is found.

Also in Geography Atlas: where this subject is found.

Also in Geography Atlas: where this subject is found.

Also in Geography Atlas: where this subject is found.

Sources
Posidonia Shale (Wikipedia)
  • In Discipline: Stratigraphy, Lead paragraph
    The Posidonia Shale (German: Posidonienschiefer, also called Schistes Bitumineux in Luxembourg), is an Early Jurassic (Toarcian) geological formation in Germany, northern Switzerland, northwestern Austria, southern Luxembourg and the Netherlands
  • Caused By: Sedimentation, Lead paragraph
    Posidonia Shale, which was deposited under strongly reducing conditions during the Toarcian oceanic anoxic event, trapped and exceptionally preserved complete fossils of marine fish and reptiles
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