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	stratigraphy and biochronology of Oligo-Miocene of Kazakhstan			
	
	
Eocene otoliths (Clinchfield Formation), Georgia			
	
	
Fossil snakes, Palaeocene, Itaborai, Brazil, Part I			
	
	
Notidanodon tooth (Neoselachii: Hexanchiformes) in the Late Jurassic of New Zealand			
	
	
Abstract book of the 18th Conference of the EAVP			
	
Eocene (57) , Quercy Phosphorites (38) , Systematics (32) , Rodents (29) , Mammalia (27)
 
				
				PalaeovertebrataVol. 32, Fasc. 2-4:121-148. 2003				
				
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					Dating dinosaur oodiversity: chronostratigraphic control of LateCretaceous oospecies succession.Nieves Lopez-MartinezKeywords: Biostratigraphy; Chronology; dinosaur eggshells; Late CretaceousCite this article: Lopez-Martinez N., 2003. Dating dinosaur oodiversity: chronostratigraphic control of LateCretaceous oospecies succession. Palaeovertebrata 32 (2-4): 121-148. AbstractAn increasing fossil record of dinosaur eggs and eggshells allows putting ootaxa within a chronostratigraphic framework, in order to study their distribution pattern leading eventually to their use as biochronological markers. For these purposes, high-quality data exists in four major regions; North America, South America, Europe and Asia (Central Asia and India). Most of the highly diverse dinosaur egg record has been dated as Latest Cretaceous in age (Campanian-Maastrichtian), reaching the Cretaceous-Tertiary boundary closer than the dinosaur bone record. However, dating continental sections is problematic and need to be carefully verified, as it appears when comparing the European dinosaur eggshell record from two well-studied areas. Ootaxa distribution in both sides of the Pyrenees (Tremp and Aix basins) shows comparable oospecies successions, but different chronology. This disagreement probably indicates that one or both successions have a wrong chronostratigraphic calibration. Published in Vol. 32, Fasc. 2-4 (2003)  | 
					
					
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