Late Silurian fish microfossils from Klinta and Rinnebäcks Bro (Scania, south Sweden), with remarks on the morphology of Nostolepis striata trunk scales

The microvertebrate faunas from ten small pieces of rock from the Öved Sandstone Formation at Klinta (1-10) yielded osteostracan, heterostracan, thelodont, and acanthodian remains, dated here as Whitcliffian. The most important age indicators are the heterostracan Archegonaspis and the thelodont zon...

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Bibliographic Details
Main Author: Vergoossen, J.M.J.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2002
Subjects:
Online Access:http://www.repository.naturalis.nl/record/219194
http://www.repository.naturalis.nl/document/46157