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The Dzikówka Sandstone Quarry outcrop of the formation
The Dzikówka Sandstone Quarry outcrop of the formation
"Pinkiert" quarry sandstone extraction in 1929
"Pinkiert" quarry sandstone extraction in 1929
Spores found on the Polish are mostly from Saprophyte (wood decomposers) fungi, resembling the extant genera like Scutellinia
Spores found on the Polish are mostly from Saprophyte (wood decomposers) fungi, resembling the extant genera like Scutellinia
Example of extant specimen of Viviparus
Example of extant specimen of Viviparus
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