Paukkaungia parva (Sivaladapidae)



Paukkaungia parva ist eine Primatenart innerhalb der Familie Sivaladapidae, die ab dem Paläogen (Eozän) im Bartonium lebte, das vor rund 41,3 Millionen Jahren begann und bis vor 38 Millionen Jahren andauerte.

Fundorte

Systematik

Daten zu den einzelnen Funden von Paukkaungia parva
Sammlung Epoche, Alter Geologie, Formation
Nyaungpinle Bartonian
zwischen 38 und 41.3 Millionen Jahren
Pondaung
Kommentar z. Stratigraphie
The whole sequence of units was originally defined as the ‘Pondaung Sandstones’ by Cotter (1914), but the horizon yielding Eocene vertebrate fossils is now known as the ‘Upper Member’ of the Pondaung Formation (see Maung et al. 2005). The most recent age for this unit is ~39–38 Ma and so it can be regarded as middle Bartonian (see Tsubamoto et al. 2011).
U.a. am Fundort ausgegraben: Afrasia djijidae
Sammlung Kommentar zum Fundort Epoche, Alter Geologie, Formation Kommentar zur Sammlung
Pk2, Pondaung Sandstone approx. 1 km east of Pk1, 1 mi NW of Paukkaung, Paukkaung township Bartonian
zwischen 38 und 41.3 Millionen Jahren
Pondaung Paukkaung kyitchaung 2
Kommentar z. Stratigraphie
The whole sequence of units was originally defined as the ‘Pondaung Sandstones’ by Cotter (1914), but the horizon yielding Eocene vertebrate fossils is now known as the ‘Upper Member’ of the Pondaung Formation (see Maung et al. 2005). The most recent age for this unit is ~39–38 Ma and so it can be regarded as middle Bartonian (see Tsubamoto et al. 2011).
U.a. am Fundort ausgegraben: Bahinia pondaungensis

Literatur

K. C. Beard, L. Marivaux, S. T. Tun, A. N. Soe, Y. Chaimanee, W. Htoon, B. Marandat, H. H. Aung, J.-J. Jaeger 2007, New sivaladapid primates from the Eocene Pondaung Formation of Myanmar and the anthropoid status of Amphipithecidae. Bulletin of Carnegie Museum of Natural History. 39, p. 67 - 76