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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. 30, Fasc. 3-4:151-187. 2001				
				
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|   | The Gliridae (Mammalia) from the oligocene (MP24) of Gröben 3 in the folded molasse of southern GermanyUndine UhligKeywords: Biostratigraphy; Cyrena Beds; folded molasse; Germany; Gliridae; level MP 24; Mammals; Oligocene; PalaeoecologyCite this article: Uhlig U., 2001. The Gliridae (Mammalia) from the oligocene (MP24) of Gröben 3 in the folded molasse of southern Germany. Palaeovertebrata 30 (3-4): 151-187. AbstractThis study describes four taxa of Gliridae from the Oligocene mammal locality Gröben 3: Gliravus tenuis BAI-ILO, 1975, Bransatoglis micio (MISONNE, 1957), B. planus (BAHLO, 1975) and B. heissigi n. sp. Gliravus tenuis from Gröben 3 is somewhat more advanced than the type population found in Heimersheim. This confirms previous research suggesting that Gröben 3 should be dated earlier than Heimersheim (MP 24). The first documented occurrence of B. mício around level MP 24 was found in Gröben 3. An abundance of tooth material from B. planus in Gröben 3 makes it possible, for the first time, to observe evolutionary stages within this species from MP 21 until MP 28. B. heissigi n. sp. is restricted to level MP 24. This species is located between B. mísonnei (MP 20 - 23) and Microdyromys praemurinus (MP 25 - 28). Within the lineage Bransatoglis bahloi - B. misonnei - B. heissigi, a decrease in size is noticeable. Published in Vol. 30, Fasc. 3-4 (2001) |  |