A pre-Hirnantian (Late Ordovician) interval of global cooling - the Boda Event re-assessed
Facies analysis suggests that the early–mid Ashgill (Late Ordovician) ‘Boda event’ of Fortey and Cocks [Fortey, R.A., Cocks, L.R.M., 2005. Late Ordovician global warming—The Boda event. Geology 33 (5), 405–408] was an episode of global cooling, not of warming as they proposed. Limestones are widely...
| Published in: | Palaeogeography, Palaeoclimatology, Palaeoecology |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
Elsevier
2007
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| Subjects: | |
| Online Access: | https://orca.cardiff.ac.uk/id/eprint/1312/ https://doi.org/10.1016/j.palaeo.2007.04.010 |