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Korsodde section of the Sorthat Formation, where the local Toarcian anoxic event stratum is located
Korsodde section of the Sorthat Formation, where the local Toarcian anoxic event stratum is located
Sorthat Formation layers, mainly mudstones, claystones, and sandstone bands
Sorthat Formation layers, mainly mudstones, claystones, and sandstone bands
Late Pliensbachian–Early Toarcian Fennoscandinavia, with flora based on the Sorthat Formation and fauna from the Lehmhagen Member, Grimmen Formation a
Late Pliensbachian–Early Toarcian Fennoscandinavia, with flora based on the Sorthat Formation and fauna from the Lehmhagen Member, Grimmen Formation and Drzewica Formation.
The Sorthat Fm was a cold, humid y forested setting, whose best modern analogs can be found in New Zealand
The Sorthat Fm was a cold, humid y forested setting, whose best modern analogs can be found in New Zealand
Anchisauripus footprints belong to a genus similar to Procompsognathus
Anchisauripus footprints belong to a genus similar to Procompsognathus
Therangospodus footprints can belong to relative of Magnosaurus
Therangospodus footprints can belong to relative of Magnosaurus
Ctenis specimen
Ctenis specimen
Otozamites Anina jurassic
Otozamites Anina jurassic