Earth:Nsungwe Formation
| Nsungwe Formation Stratigraphic range: Oligocene ~25.2 Ma | |
|---|---|
| Type | Geological formation |
| Unit of | Red Sandstone Group (Rukwa Rift Basin) |
| Sub-units | Utengule Member, Songwe Member |
| Underlies | Unconformity with Lake Beds Sequence |
| Overlies | Unconformity with Galula Formation |
| Thickness | 400 m (1,300 ft) |
| Lithology | |
| Primary | Sandstone |
| Other | Conglomerate, mudstone, siltstone, tuff |
| Location | |
| Location | Rukwa, Mbeya Region |
| Region | African Great Lakes |
| Country |  Tanzania |
| Type section | |
| Named for | Nsungwe River |
| Named by | Roberts et al. |
| Year defined | 2010 |
| Thickness at type section | ~400 m |
The Nsungwe Formation is a formation in the Rukwa Rift Basin of the East African Rift System, it is Oligocene in age based on U-Pb dating of a tuff horizon within the formation. It is part of the Red Sandstone Group along with the uncomfortably underlying Mid-Cretaceous Galula Formation It is divided into two members, the lower Utengule Member, and the upper Songwe member. It is notable for being one of the most important Paleogene fossil deposits in Sub-Saharan Africa.
Geology
The lithology of the two members are quite different, representing different fluvial environments. The Utengule member is 85 m thick and predominantly consists of red-orange sandstones and matrix to clast supported conglomerates. The overlying Songwe Member is approximately twice as thick as the Utengule member, being 310–320 m thick in the type section. It is much finer grained, consisting of red-orange and grey green claystones, siltstones, mudstones, lenticular sandstones and tuffs. The sediments of the Songwe Member are noted for their fossil content.[1]
Fossil content
Important fossils have come out of the formation, including the rodent Kahawamys,[2] some of the oldest records of the frog genus Xenopus,[3] the hyaenodont Pakakali,[4] the elephant shrews Oligorhynchocyon and Rukwasengi,[5] and the primates Nsungwepithecus and Rukwapithecus, some of the earliest crown catarrhines.[6]
References
- ↑ Roberts, Eric M.; O’Connor, Patrick M.; Stevens, Nancy J.; Gottfried, Michael D.; Jinnah, Zubair A.; Ngasala, Sifael; Choh, Adeline M.; Armstrong, Richard A. (May 2010). "Sedimentology and depositional environments of the Red Sandstone Group, Rukwa Rift Basin, southwestern Tanzania: New insight into Cretaceous and Paleogene terrestrial ecosystems and tectonics in sub-equatorial Africa". Journal of African Earth Sciences 57 (3): 179–212. doi:10.1016/j.jafrearsci.2009.09.002. Bibcode: 2010JAfES..57..179R.
- ↑ Stevens, Nancy J.; Holroyd, Patricia A.; Roberts, Eric M.; O'connor, Patrick M.; Gottfried, Michael D. (2009-06-12). "Kahawamys mbeyaensis (n. gen., n. sp.) (Rodentia: Thryonomyoidea) from the late Oligocene Rukwa Rift Basin, Tanzania" (in en). Journal of Vertebrate Paleontology 29 (2): 631–634. doi:10.1671/039.029.0219. ISSN 0272-4634.
- ↑ Blackburn, David C.; Paluh, Daniel J.; Krone, Isaac; Roberts, Eric M.; Stanley, Edward L.; Stevens, Nancy J. (2019-05-15). "The Earliest Fossil of the African Clawed Frog (Genus Xenopus) from Sub-Saharan Africa". Journal of Herpetology 53 (2): 125. doi:10.1670/18-139. ISSN 0022-1511.
- ↑ Borths, Matthew R.; Stevens, Nancy J. (2017-10-11). Smith, Thierry. ed. "The first hyaenodont from the late Oligocene Nsungwe Formation of Tanzania: Paleoecological insights into the Paleogene-Neogene carnivore transition" (in en). PLOS ONE 12 (10): e0185301. doi:10.1371/journal.pone.0185301. ISSN 1932-6203. PMID 29020030. Bibcode: 2017PLoSO..1285301B.
- ↑ Stevens, Nancy J.; O’Connor, Patrick M.; Mtelela, Cassy; Roberts, Eric M. (2021-07-23). "Macroscelideans (Myohyracinae and Rhynchocyoninae) from the late Oligocene Nsungwe formation of the Rukwa Rift Basin, southwestern Tanzania". Historical Biology: 1–7. doi:10.1080/08912963.2021.1938565. ISSN 0891-2963.
- ↑ Stevens, Nancy J.; Seiffert, Erik R.; O'Connor, Patrick M.; Roberts, Eric M.; Schmitz, Mark D.; Krause, Cornelia; Gorscak, Eric; Ngasala, Sifa et al. (2013). "Palaeontological evidence for an Oligocene divergence between Old World monkeys and apes". Nature 497 (7451): 611–614. doi:10.1038/nature12161.
 |  |
