This is an example of one of the rarer brittle stars from the Hunsrück Slate, Euzonosoma tischbeinianum. It has been naturally pyritized and measures 5.2″ wide. The fossil is folded in half within the rock and one of the arms broke free onto the negative during collection.
It comes with an acrylic display stand.
The lower Devonian (lower Emsian) slates from Bundenback have been quarried for roofing material for centuries. Quarrying continued until the 1960s, when the competition from cheaper synthetic or imported slate resulted in production decline. The last pit closed in 2000. Mining of Hunsrück slate was important for the discovery of Paleozoic fossils. Although not rare, fossils can only be found through extensive mining and time-consuming preparation: fossils are hard to see lying under the surface of dark slate. But in 1970, Wilhelm Stürmer, a chemical physicist and radiologist, developed a new method to examine the Hunsrück slate fossils using medium energy X-rays.
The Bundenbach “Hunsruck Slate” is famous for yielding one of the most important assemblages of Paleozoic fossils, representing 260 animal species including mollusks, echinoderms and arthropods, of which the phacopid trilobite Chotecops is certainly the most abundant.













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