quadrupedality as the taxon is incomplete.

Paleoenvironment

The holotype of Emausaurus was found in the so-called "Emausaurus type site", which represents a shale ingression from the Lehmhagen Member, dated from the Lower Toarcian. The site is a boundary composed of bituminous shale, representing an ancient seashore-influenced environment, probably lagoonal, and contemporaneous with the Sorthat Formation of the same region. Fossil wood has been

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