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Palynology of the ‘Lower Old Red Sandstone’ at Glen Coe, Scotland

Published online by Cambridge University Press:  01 May 2009

Charles H. Wellman
Charles H. Wellman
Affiliation:
Department of Palaeontology, the Natural History Museum, London SW7 5BD, UK and Department of Geology, University of Wales College of Cardiff, Cardiff CF3 3YE, UK
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Abstract

‘Lower Old Red Sandstone’ deposits preserved by cauldron subsidence at Glen Coe, Scotland have hitherto lacked secure biostratigraphical age constraint. A sporomorph assemblage recovered from basal sediments of these deposits permits age determination, despite being highly carbonized. The sporomorph assemblage is correlated with the micrornatus-newportensis Sporomorph Assemblage Biozone, indicating a late early-early late Lochkovian age (early Devonian). Sporomorph assemblages from basal sediments of the ‘Lower Old Red Sandstone’ sequence at nearby Lorne, a suggested correlative of the Glen Coe deposits, are older (latest Pridoli-earliest Lochkovian age). However, the new biostratigraphical data do not preclude the possibility that the Glen Coe and Lorne deposits are lithological correlatives and the basal sediments are diachronous.

Type
Rapid Communications
Information
Geological Magazine , Volume 131 , Issue 4 , July 1994 , pp. 563 - 566
Copyright
Copyright © Cambridge University Press 1994

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