Changle Coal Mine, China


Fundort: Changle Coal Mine, China, Shandong, China
Taxon: Asioplesiadapis youngi aus der Familie Plesiadapidae
Fossilien und Beschreibung der Fundstelle:
Macrofossils, There is some debate over whether the Wutu Formation is late Paleocene or early Eocene, but most authors accept an early Eocene age, "coal mine" (Tong et al. 2004)
Geschätztes Alter
der Fundstelle:
zwischen 48,6 und 55,8 Millionen Jahre aus der Wutu Formation in China
Geologie, Sratigraphie Ypresian / Early Eocene / Wutu
Koordinaten: 36° 30 ' 59 '' N, 118° 54 ' 59 '' O

Literatur

J.-F. Fu, J.-W. Wang, Y.-S. Tong 2002, The new discovery of the Plesiadapiformes from the Early Eocene of Wutu Basin, Shandong Province. Vertebrata PalAsiatica. 40:3, p. 219 - 227

Systematik