Palynological evidence for Lower Ordovician rocks (Tremadoc and Àrenig) in the Northern Greywacke Zone (Eastern Alps)
1992; Wiley; Volume: 4; Issue: 2 Linguagem: Inglês
10.1111/j.1365-3121.1992.tb00472.x
ISSN1365-3121
AutoresErhard Reitz, R.M. van der Zee Holl,
Tópico(s)Geological formations and processes
ResumoABSTRACT Until recently, only fossils of Caradoc to Carboniferous age have been reported from the Northern Greywacke Zone/Eastern Alps. New medium‐preserved and diversified acritarch assemblages from the Lower Wildschönau Formation indicate a Lower Ordovician (Tremadoc and Arenig) age. These fossil spectra define a well‐constrained time interval for a lower section of the Northern Greywacke Zone for the first time.
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