Klerf Formation

The Klerf Formation is an Early Devonian (Emsian) formation that includes a Lagerstätte in the Northern Eifel hills, at Willwerath near Prüm, Rhineland-Palatinate, Germany. In it Jaekelopterus rhenaniae, a giant eurypterid was discovered. The Klerf Formation, comprising greenish and reddish shales, siltstones and sandstones, was first described in 1919 by Rudolf Richter (1881-1957) and reaches a maximum thickness of about 1,300 metres (4,300 ft).[1]

Klerf Formation
Stratigraphic range: Emsian
~409–392 Ma
TypeGeological formation
Sub-unitsReifferscheid Mb.
Altenberg Mb.
Unterpreth Mb.
UnderliesHeisdorf Formation
OverliesSchleiden Formation
Thickness1,300 m (4,300 ft)
Lithology
PrimarySiltstone, shale
OtherSandstone
Location
LocationEifel
Coordinates50°14′48″N 06°27′21″W
RegionRhineland-Palatinate
Country Germany
Type section
Named byRichter
LocationWillwerath near Prüm
Year defined1919
Coordinates50°14′48″N 06°27′21″W
Approximate paleocoordinates27.1°S 09.7°E / -27.1; 09.7
RegionEifel
Country Germany

Avalonia with the Proto-Tethys Ocean (3)

Depositional environment

The siltstone and sandstone formation was deposited in an estuarine to deltaic environment.[2] This was located on the edge of Avalonia bordering the Proto-Tethys Ocean.

Fossil content

Apart from the largest arthropod, Jaekelopterus (shown on the left), found in the formation, it also preserved the fish, bryozoa, brachiopod and ostracod remains,[1] the arachnids Devonotarbus hombachensis, Xenarachne willwerathensis,[2] and Mutationella indet. and flora.[3]

See also

References

This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.