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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Format: | Article in Journal/Newspaper |
Language: | unknown |
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2002
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Online Access: | http://www.repository.naturalis.nl/record/219194 http://www.repository.naturalis.nl/document/46157 |