| Usili Formation | |
| Type: | Geological formation |
| Age: | Lopingian ~ |
| Period: | Lopingian |
| Prilithology: | Sandstone, conglomerate |
| Otherlithology: | Siltstone, mudstone |
| Namedfor: | Usili Mountain |
| Namedby: | Stockley |
| Year Ts: | 1932 |
| Region: | Ruvuma Region |
| Coordinates: | -10.3°N 35.1°W |
| Paleocoordinates: | -55.1°N 15.2°W |
| Unitof: | Songea Group |
| Underlies: | Manda Formation |
| Overlies: | Ruhuhu Formation |
| Thickness: | 260m (850feet) |
| Extent: | Ruhuhu Basin |
The Usili Formation is a Late Permian geologic formation in Tanzania. It preserves fossils of many terrestrial vertebrates from the Permian, including temnospondyls, pareiasaurs, therapsids and the archosauromorph Aenigmastropheus.[1] [2]
One of the first to study rocks of the Usili Formation was British geologist G. M. Stockley. In 1932, Stockley explored the geology of the Ruhuhu Basin in Tanzania. He called a series of layers dating from the Late Carboniferous to the Middle Triassic of the Songea Series and divided it into eight units labelled K1-K8. Stockley was also the first to describe fossils from these rocks, naming an older layer the "Lower Bone Bed" and a younger layer the "Upper Bone Bed".
In 1957, paleontologist Alan J. Charig described many more fossils from the upper bone beds in his Ph.D. thesis for the University of Cambridge.[3] [4] Subsequently, Stockley's units were renamed, Charig (1963) calling unit K6 the Kawinga Formation, K7 the Kingori Sandstones, and K8 the Manda Formation. Fossils were identified in many strata, invalidating Stockley's division into two distinct bone beds. Since Charig's description, the Kawinga Formation has been renamed the Usili Formation, the Kingori Sandstones have become the Kingori Sandstone Member of the Manda Formation, and Charig's original Manda Formation has become a subunit of the formation called the Lifua Member.[5] Six formations and one informal unit are currently recognized in the Songea Group (Ruhuhu basin) rocks range in age from Pennsylvanian to Anisian, including the Idusi (K1), Mchuchuma (K2), Mbuyura (K3), Mhukuru (K4), Ruhuhu (K5), and Usili (K6) formations and the informal Manda Beds, which include the Kingori Sandstone (K7) and Lifua Member (K8).[6]
Recent studies have described the Usili Formation as a 260m (850feet) thick fluvio-lacustrine succession made up of a lowermost conglomeratic interval that is approximately 5 meters thick, grading up into a trough cross-bedded, coarse-grained, sandstone-dominated interval that is 25mto40mm (82feetto130feetm) thick, overlain by massive nodular siltstone and laminated mudstone beds with minor ribbon sandstones forming the bulk of the succession. Since Parrington (1956), the Usili Formation became widely recognized as a Late Permian formation that correlates with the Teekloof and Balfour formations of South Africa, as well as with the Zambian Upper Madumabisa Mudstone (Cistecephalus AZ). Comparison of Usili tetrapods with those of the lower Beaufort Group has suggested a broad biostratigraphic correlation with the Cistecephalus, Dicynodon, and Tropidostoma assemblage zones. Sidor et al. (2010) recognized only one undivided tetrapod faunal assemblage in the Usili Formation, which includes Aenigmastropheus, temnospondyls, pareiasaurs, gorgonopsians, therocephalians, cynodonts, and dicynodonts, whose remains were collected from various localities. This suggests that several therapsid genera have unequal stratigraphic ranges and temporal durations in the Ruhuhu and Karoo basins.[2] [6]
Sidor et al. (2010) and Sidor et al. (2013) noted that it is probable that the Chiweta Beds of Malawi and the Usili Formation of Tanzania represent the same rock unit, separated only by political boundaries and geologic faulting (being located on either side of Lake Nyasa). Except for the burnetiid MAL 240, which is unique to the Chiweta Beds, the Usili Formation hosts identical genera, including Aelurognathus, Dicynodontoides, Rhachiocephalus, Endothiodon cf. E. bathystoma, Oudenodon baini, Gorgonops? dixeyi and an indeterminate tusked dicynodont (SAM-PK-7862, SAM-PK-7863).[1] [6]
| Taxon | Species | Locality | Material | Notes | Images |
|---|---|---|---|---|---|
| Anthodon | A. serrarius | A pareiasaur. Originally named Anthodon minisculus, it was considered a junior synonym of A. serrarius by Lee (1997). | |||
| Pareiasaurus | P. serridens | A pareiasaur. | |||
| Unidentified Parareptilia | Indeterminate | GPIT K72, six or seven dorsal vertebrae with articulated osteoderms | A pareiasaur originally described by von Huene (1944), endemic to this formation. | ||
| Taxon | Species | Locality | Material | Notes | Images |
|---|---|---|---|---|---|
| Compsodon | C. helmoedi[7] | L35, Z04 | A highly damaged mandible as well as articulated craniodental remains (skull and mandible) | First preservation of a mandible for this taxon. | |
| Daptocephalus | D .leoniceps | A dicynodontoid dicynodont, previously considered to be a species of Dicynodon, known only from South Africa. | |||
| D. huenei | B2 (Kingori) | SAM-PK-10630, fragmentary skull and postcrania; 7 additional skulls | A dicynodontoid dicynodont, the holotype was formerly assigned as a species of Dicynodon. | ||
| Dicynodon | Dicynodon lacerticeps | A dicynodontoid dicynodont, known only from South Africa. | |||
| Dicynodon angielczyki | UMZC T1089, a complete skull; 6 additional partial to complete skulls and some possible postcrania | A species named for specimens of Dicynodon formerly assigned to Daptocephalus huenei.[8] | |||
| Dicynodon | D. robertsi | Originally considered to be a species of Dicynodon, but it is a junior synonym of Oudenodon bainii. | |||
| "Dicynodon" tealei | B32 | SAM-PK-10631, fragmentary skull roof | An indeterminate dicynodont, a nomen dubium. | ||
| Dicynodontoides | D. nowacki | Kingori | GPIT/RE/7174, a nearly complete skull; other skulls and skeletons | A kingoriid dicynodont, previously considered to be a species of Dicynodon. | |
| Endothiodon | E. cf. bathystoma | Basal dicynodont, endothiodontid. | |||
| E. sp. nov. | A new, yet unnamed species. | ||||
| E. uniseries | Basal dicynodont, endothiodontid. Originally placed in its own genus Esoterodon. | ||||
| Euptychognathus | E. bathyrhynchus | Kingori | GPIT/RE/7104 (UT K 19), well preserved partial skull | Basal lystrosaurid dicynodont, previously considered to be a species of Dicynodon. | |
| Geikia | G. locusticeps | GPIT K87/UT von HUENE 1942 Abb.3, juvenile partial skull and dentary; GPIT K114, skull and dentary | A geikiine cryptodont, previously considered to be a species of Dicynodon. | ||
| Katumbia | K. parringtoni | B19 (Kingori); B4 (Katumbi); Usili-Berges | GPIT K120/UT Huene 1942 S.155, fragmentary skull; UMZC T761, UMZC T791, incomplete skulls; A dentary | Basal dicynodontoid, endemic to this formation. | |
| Kawingasaurus | K. fossilis | Kingori | UT K 52, skull and dentary; UT K 56, skull; UT K 55, 5 skulls and postcrania | A cistecephalid dicynodont, endemic to this formation. | |
| Oudenodon | O. bainii | Many skulls | Basal oudenodontid cryptodont. | ||
| Pachytegos | P. stockleyi | B32 | SAM 10639, SAM 10642, fragmentary skull elements | Basal dicynodont, endothiodontid, endemic to this formation. | |
| Pristerodon | P. mackayi | NMT RB38 | Basal dicynodont, eumantellid. Previous reports by King (1988, 1992), King and Rubidge (1993), and Gay and Cruickshank (1999) were based on the holotype specimen of Katumbia parringtoni. The first diagnostic specimen of Pristerodon mackayi from this formation, NMT RB38, was discovered in 2008. | ||
| Rhachiocephalus | R. behemoth | GPIT K 15, nearly complete skull; GPIT K 15B, fragmentary skull | A rhachiocephalid cryptodont. | ||
| R. magnus | Many specimens | A rhachiocephalid cryptodont. | |||
| Unnamed Anomodont | Unidentified | NMT RB22, a partial maxilla of an adult. NMT RB156, a nearly complete skull, mandible, and associated postcrania of a subadult. | A new genus and species of a cryptodontian dicynodont. Endemic to this formation. | ||
| Taxon | Species | Locality | Material | Notes | Images |
|---|---|---|---|---|---|
| Silphictidoides | S. ruhuhuensis | Kingori | A baurioid, endemic to this formation. | ||
| Theriognathus | T. microps | Kingori | K 107 and K 84, two fragmentary skulls | ||
| Taxon | Species | Locality | Material | Notes | Images |
|---|---|---|---|---|---|
| Cyonosaurus | C. broomianus | A gorgonopsian | |||
| Dinogorgon | D. rubidgei | Kingori | IGP K 16, nearly complete skull and dentary | A gorgonopsid, endemic to this formation. | |
| "Dixeya" | "Dixeya" nasuta | IGP K 52, nearly complete skull; IGP K 96, fragmentary skull; 6 more skulls | A gorgonopsid, informally given the nomen nudum "Njalila" by Gebauer (2007). Endemic to this formation. | ||
| Gorgonops | G. sp. | A gorgonopsid | |||
| Inostrancevia | I. sp. | NMT RB38, an isolated left premaxilla[9] | A gorgonopsid | ||
| Lycaenops | L. sp. | A gorgonopsid | |||
| Rubidgea | R. atrox | IGP K 46, fragmentary skull | A gorgonopsid, formally named Broomicephalus, endemic to this formation. | ||
| Ruhuhucerberus | R. haughtoni | Katumbi, B4 | MZC T891, nearly complete skull | A gorgonopsid, endemic to this formation. | |
| Sauroctonus | S. parringtoni | Usili-Berges | IGP U 28, complete skull and dentary and fragmentary skeleton | A gorgonopsid, endemic to this formation. | |
| Scylacops | S. capensis | Kingori, B19 | MZC T885/FRP 93, skull and cervical vertebrae | A gorgonopsid | |
| Sycosaurus | S. nowaki | Kingori | IGP K 47, nearly complete skull | A gorgonopsid, endemic to this formation. | |