Post-Hunnebergian Ordovician carbon isotope trend in Baltoscandia, its environmental implications and some similarities with that of Nevada
- 1 March 2007
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 245 (1-2) , 138-155
- https://doi.org/10.1016/j.palaeo.2006.02.020
Abstract
No abstract availableKeywords
This publication has 29 references indexed in Scilit:
- Long-lived glaciation in the Late Ordovician? Isotopic and sequence-stratigraphic evidence from western LaurentiaGeology, 2005
- Response of Late Ordovician paleoceanography to changes in sea level, continental drift, and atmospheric pCO2: potential causes for long-term cooling and glaciationPalaeogeography, Palaeoclimatology, Palaeoecology, 2004
- Late Ordovician (Turinian–Chatfieldian) carbon isotope excursions and their stratigraphic and paleoceanographic significancePalaeogeography, Palaeoclimatology, Palaeoecology, 2004
- 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
- A weathering hypothesis for glaciation at high atmospheric pCO2 during the Late OrdovicianPalaeogeography, Palaeoclimatology, Palaeoecology, 1999
- Late Ordovician mass extinction: A new perspective from stratigraphic sections in central NevadaGeology, 1999
- Evidence for a widespread carbon isotopic event associated with late Middle Ordovician sedimentological and faunal changes in EstoniaGeological Magazine, 1999
- Isotopic evidence for geochemical decoupling between ancient epeiric seas and bordering oceans: Implications for secular curvesGeology, 1998
- Climatic and oceanographic isotopic signals from the carbonate rock record and their preservationGeological Magazine, 1992
- An oceanic model for lithological and faunal changes tested on the Silurian recordJournal of the Geological Society, 1990