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13 - Lower Devonian Hunsrück Slate of Germany

Published online by Cambridge University Press:  10 November 2010

Hans Hess
Affiliation:
Basel Natural History Museum, Switzerland
William I. Ausich
Affiliation:
Ohio State University
Carlton E. Brett
Affiliation:
University of Cincinnati
Michael J. Simms
Affiliation:
Ulster Museum, Belfast
Hans Hess
Affiliation:
Basel Natural History Museum
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Summary

ROOFS AND TILES

Visitors to this part of Germany cannot fail to notice the dark grey slate roofs and walls in the picturesque towns along the rivers Rhine and Moselle. The Hunsrückschiefer belongs, together with the Lower Jurassic Posidonia Shale and the Upper Jurassic Solnhofen Lithographic Limestone, to those sediments that have been exploited since ancient times for building purposes. The discovery of a large number of world-famous fossils in these strata is, therefore, due to the observation and skilled manual work of quarrymen preparing the slabs and tiles. Fossils wrested from the dark grey Hunsrück Slate are mostly small and, therefore, may not be quite so spectacular as those from some other sites, but they open a fascinating window onto the development of life in these early times.

DECLINE OF A CRAFT

The Hunsrückerschiefer is exposed in the Rheinisches Schiefergebirge between Koblenz, Trier and Mainz. The best localities for well-preserved fossils are the communities of Bundenbach and Gemünden. The slates were widely quarried in former times (slates for roofs, etc.); and during the 19th and present centuries, more than 600, mostly small, pits were exploited. Today, only one quarry remains open in the main fossiliferous region of Bundenbach. Unlike other famous Lagerstätten, the Hunsrück Slate has not undergone detailed sedimentological examination with modern techniques.

THICK SEDIMENTS FROM THE REMAINS OF AN OLD CONTINENT

The slates are of Early Devonian age and were deposited from the Late Siegenian (Late Pragian) Stage and ceased towards the end of the Early Emsian Stage (age about 390 million years). The sediments were deposited in a number of offshore basins separated by swells.

Type
Chapter
Information
Fossil Crinoids , pp. 111 - 121
Publisher: Cambridge University Press
Print publication year: 1999

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