The entire wiki reimagined as a visual magazine with video discovery · Watch your interests come alive
The entire wiki reimagined as a visual magazine with video discovery · Watch your interests come alive
Head of a modern Serpula vermicularis
Head of a modern Serpula vermicularis
Reconstructed specimens
Reconstructed specimens
Turbo petholatus Voavah
Turbo petholatus Voavah
Uptonia jamesoni ESV
Uptonia jamesoni ESV
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