†Afrasia djijidae (Afrotarsiidae)
Afrasia djijidae ist eine Primatenart innerhalb der Familie Afrotarsiidae, die ab dem Paläogen (Eozän) im Bartonium lebte, das vor rund 41,3 Millionen Jahren begann und bis vor 38 Millionen Jahren andauerte.
Daten zu den einzelnen Funden von Afrasia djijidae
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: | Paukkaungia parva |
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 |
Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
---|---|---|---|---|
Thamingyauk Kyitchaung | shown on map as north of Magyigan and south of Thamingyauk: coordinate based on Thamingyauk | Bartonian zwischen 38 und 41.3 Millionen Jahren |
Pondaung | Tmk |
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). |