Marine Sedimentary Response to the Great Ordovician Biodiversification Event: Examples from North China and South China
- 1 April 2009
- journal article
- Published by The Paleontological Society of Japan in Paleontological Research
- Vol. 13 (1) , 9-21
- https://doi.org/10.2517/1342-8144-13.1.009
Abstract
No abstract availableKeywords
This publication has 44 references indexed in Scilit:
- Ordovician graptolite evolutionary radiation: a reviewGeological Journal, 2006
- Microbial carbonate abundance compared with fluctuations in metazoan diversity over geological timeSedimentary Geology, 2006
- Flat‐pebble conglomerate: its multiple origins and relationship to metre‐scale depositional cyclesSedimentology, 2004
- Microbialite resurgence after the Late Ordovician extinctionNature, 2004
- Comparative diversificationdynamics among Palaeocontinents during the Ordovician RadiationGeobios, 1997
- Patterns in bioclastic accumulation through the Phanerozoic: Changes in input or in destruction?Geology, 1994
- Early Triassic stromatolites as post-mass extinction disaster formsGeology, 1992
- Ordovician increase in extent and depth of bioturbation: Implications for understanding early Paleozoic ecospace utilizationGeology, 1989
- Precambrian Columnar Stromatolite Diversity: Reflection of Metazoan AppearanceScience, 1971
- Phanerozoic Stromatolites: Noncompetitive Ecologic Restriction by Grazing and Burrowing AnimalsScience, 1970