Late Ordovician global warming—The Boda event
- 1 January 2005
- journal article
- Published by Geological Society of America in Geology
- Vol. 33 (5) , 405
- https://doi.org/10.1130/g21180.1
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- The impact of paleogeography, pCO2, poleward ocean heat transport and sea level change on global cooling during the Late OrdovicianPalaeogeography, Palaeoclimatology, Palaeoecology, 2004
- Pre‐Hirnantian Ashgill climatically warm event in the Mediterranean regionLethaia, 2003
- High-resolution stable isotope stratigraphy of Upper Ordovician sequences: Constraints on the timing of bioevents and environmental changes associated with mass extinction and glaciationGSA Bulletin, 2003
- Palaeontological evidence bearing on global Ordovician–Silurian continental reconstructionsPublished by Elsevier ,2002
- Earth geography from 500 to 400 million years ago: a faunal and palaeomagnetic reviewJournal of the Geological Society, 2002
- The late Ordovician carbonate sedimentation as a major triggering factor of the Hirnantian glaciationBSGF - Earth Sciences Bulletin, 2002
- Euconodont paleobiogeography and the closure of the Iapetus OceanGeology, 2002
- High-latitude pelmatozoan–bryozoan mud-mounds from the late Ordovician northern Gondwana platformGeological Journal, 1998
- An atmospheric pCO2 threshold for glaciation in the Late OrdovicianGeology, 1997
- The ecological, significance of variation in the generic composition of Rawtheyan (late Ordovician) trilobite faunas from North Wales, U.K.Geological Journal, 1984