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Grünbach Formation

Geological formation in Austria From Wikipedia, the free encyclopedia

Grünbach Formation
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The Grünbach Formation is an Austrian geological formation that dates to the early Campanian age of the Late Cretaceous. it forms part of the Gosau Group, and represents a marine regression event, representing a coastal/brackish environment, being underlain by the marine carbonate Maiersdorf Formation and overlain by the deep marine siliciclastic Piesting Formation. The main lithology is clay, marl, siltstone and sandstone, with a minor conglomerate component. Coal seams have also been noted.[1][2] It is notable for its fossils including those of dinosaurs and plants.

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Vertebrate paleofauna

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All remains have been found at a single locality, which is a thin marl seam in the Konstantin mining tunnel, within the Felbering Mine in the Neue Welt area north west of Muthmannsdorf in Lower Austria.[3] The initial remains were discovered in 1859 after an ornithopod tooth was found in a piece of coal in a dump outside the mine by Professor Ferdinand Stoliczka, and the productive seam discovered thereafter. The first material was described by Emanuel Bunzel in 1871[4] and then additional material was described by Harry Seeley in 1881.[5] Due to mining activity in the area ceasing at the end of the 19th century, no additional remains have been recovered since.

Squamates

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Crocodyliformes

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Choristoderes

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Turtles

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Pterosaurs

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Non-avian dinosaurs

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Flora

Most of these specimens were recovered from mining dumps near Grünbach am Schneeberg in lower Austria. The flora of the formation is considered to represent that of a high humidity subtropical climate, typical of the Euro-Sinian phytogeographical region.[11][12][13]

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Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Bryophytes

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Lycopodiophyta

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Pteridophytes

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Gymnosperms

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Angiosperms

Monocots

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Dicots

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References

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