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Manda Formation

Coordinates: 10°18′S 35°12′E / 10.3°S 35.2°E / -10.3; 35.2
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Manda Formation
Stratigraphic range: Anisian
~247–242 Ma
↓
TypeGeological formation
Unit ofCynognathus Assemblage Zone
 Songea Group
Sub-unitsKingori Sandstone Member, Lifua Member
UnderliesNone
OverliesUsili Formation
Lithology
PrimarySandstone
OtherMudstone, siltstone, marl
Location
Coordinates10°18′S 35°12′E / 10.3°S 35.2°E / -10.3; 35.2
Approximate paleocoordinates53°42′S 23°00′E / 53.7°S 23.0°E / -53.7; 23.0
RegionIringa & Ruvuma Regions
Country Tanzania
ExtentRuhuhu Basin

Map of the outcropping Manda Formation

The Manda Formation (also known as the Manda Beds) is a Middle Triassic geologic formation in Tanzania. It preserves fossils of many terrestrial vertebrates from the Triassic, including some of the earliest archosaurs.[1]

History of study

One of the first to study rocks of the Manda 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 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 bone beds in his Ph.D. thesis for the University of Cambridge.[2][3] Charig renamed the youngest of Stockley's units in 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.[1] 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).[4]

Paleobiota

Tetrapods

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Temnospondyls

Taxon Member Material Notes Images
Stanocephalosaurus pronus[5] Lifua Remains of a temnospondyl amphibian previously referred either to Parotosaurus or Eryosuchus[6]

Parareptiles

Taxon Member Material Notes Images
Ruhuhuaria reiszi[7] Lifua CAMZM T997, poorly preserved but complete skull and mandible An owenettid

Archosauromorphs

Taxon Member Material Notes Images
Asperoris mnyama Lifua NHMUK PV R36615, incomplete skull A non-crurotarsan archosauriform of uncertain phylogenetic placement
"Stagonosuchus" tanganyikaensis[8] Lifua Member SAM 11754, right humerus An indeterminate archosauromorph; possibly a rhynchosaur
Stenaulorhynchus stockleyi Lifua A rhynchosaur
Unnamed[5] Lifua NHMUK PV R36619, incomplete skull and partial postcranial skeleton A non-archosaurian archosauriform
Archosaurs
Taxon Member Material Notes Images
Asilisaurus kongwe Lifua A silesaurid dinosauriform
Hypselorhachis mirabilis Lifua NHMUK R16586, a complete dorsal vertebra A sail-backed archosaur possibly belonging to the family Ctenosauriscidae
Mandasuchus tanyauchen[9] Lifua Member NHMUK R6792, partial mandible and postcranial skeletons A paracrocodylomorph
Nundasuchus songeaensis[5][10] Lifua NMT RB48, partial skeleton and skull An archosaur, possibly suchian
Nyasasaurus parringtoni[11] Lifua NHMUK R6856, a right humerus, three partial presacral vertebrae and three sacral vertebrae. SAM-PK-K10654 is also potentially referable - see "Thecodontosaurus" alophos below. A theropod or an ornithischian or the most advanced non-dinosaurian dinosauriform. Possibly the oldest dinosaur.[11]
"Pallisteria angustimentum" Lifua Member NHMUK R36620, partial skull and some postcranial fragments A "rauisuchian"; a nomen nudum first identified as a thecodont
Parringtonia gracilis Lifua NHMUK R8646, a mandible, scapula, partial ischium, twelve vertebrae, and five osteoderms An erpetosuchid
Stagonosuchus nyassicus Lifua GPIT/RE/3831/1-21 and GPIT/RE/3832/1-15, two partial postcranial skeletons A "rauisuchian"
"Stenaulorhynchus" major[8] Lifua Member SAM S337, distal half of a left humerus A subjective senior synonym of Stagonosuchus.[11]
Teleocrater rhadinus Lifua NHMUK R6795, vertebrae, limb bones and other elements. Additional material referred from two other individuals. An early avemetatarsalian[12]
"Thecodontosaurus" alophos[11] Lifua Member SAM-PK-K10654, three neck vertebrae and two rear presacral vertebrae A probable subjective senior synonym of Nyasasaurus, first identified as a sauropodomorph dinosaur.[11]
Unnamed[13] Lifua Nearly complete skull and partial skeleton A stem-aetosaur

Therapsids

Dicynodonts
Taxon Member Material Notes Images
Angonisaurus cruickshanki Lifua A kannemeyeriiform
Kannemeyeria simocephalus Lifua A kannemeyeriid kannemeyeriiform
Sangusaurus parringtonii Lifua A stahleckeriid kannemeyeriiform
?Shansiodon Lifua Skull A shansiodontid kannemeyeriiform
Tetragonias njalilus Lifua A shansiodontid kannemeyeriiform
Cynodonts
Taxon Member Material Notes Images
Aleodon brachyrhamphus Lifua A possible chiniquodontid
Cricodon metabolus Lifua A trirachodontid
Cynognathus crateronotus[14] Lifua A cynognathid
Diademodon tetragonas Lifua A diademodontid
Scalenodon angustifrons Lifua A traversodontid
"Scalenodon" attridgei Lifua A traversodontid; may fall outside the genus Scalenodon and may be a synonym of "Scalenodon" charigi
"Scalenodon" charigi Lifua A traversodontid; may fall outside the genus Scalenodon
Mandagomphodon hirschoni Lifua A traversodontid; originally classified in the genus Scalenodon; named after the Manda Beds

See also

References

  1. ^ a b Butler, R. J.; Barrett, P. M.; Abel, R. L.; Gower, D. J. (2009). "A possible ctenosauriscid archosaur from the Middle Triassic Manda Beds of Tanzania". Journal of Vertebrate Paleontology. 29 (4): 1022–1031. doi:10.1671/039.029.0404.
  2. ^ Charig, A. J. (1957). New Triassic archosaurs from Tanganyika, including Mandasuchus and Teleocrater: Dissertation Abstracts. Cambridge University.
  3. ^ Nesbitt, S. J.; Butler, R. J. (2012). "Redescription of the archosaur Parringtonia gracilis from the Middle Triassic Manda beds of Tanzania, and the antiquity of Erpetosuchidae". Geological Magazine. 150 (2): 225–238. doi:10.1017/S0016756812000362. S2CID 129115107.
  4. ^ Sidor, C. A.; Angielczyk, K. D.; Weide †, D. M.; Smith, R. M. H.; Nesbitt, S. J.; Tsuji, L. A. (2010). "Tetrapod fauna of the lowermost Usili Formation (Songea Group, Ruhuhu Basin) of southern Tanzania, with a new burnetiid record". Journal of Vertebrate Paleontology. 30 (3): 696–703. doi:10.1080/02724631003758086.
  5. ^ a b c Sidor, C. A.; Vilhena, D. A.; Angielczyk, K. D.; Huttenlocker, A. K.; Nesbitt, S. J.; Peecook, B. R.; Steyer, J. S.; Smith, R. M. H.; Tsuji, L. A. (2013). "Provincialization of terrestrial faunas following the end-Permian mass extinction". Proceedings of the National Academy of Sciences. 110 (20): 8129–8133. doi:10.1073/pnas.1302323110. PMC 3657826. PMID 23630295.
  6. ^ Sues, H.-D.; Fraser, N.C. (2010). "Early and early Middle Triassic in Gondwana". Triassic Life on Land: The Great Transition. New York: Columbia University Press. pp. 19–36. ISBN 9780231135221. ISBN 0-231-13522-X
  7. ^ Tsuji, L. A.; Sobral, G.; Müller, J. (2013). "Ruhuhuaria reiszi, a new procolophonoid reptile from the Triassic Ruhuhu Basin of Tanzania". Comptes Rendus Palevol. 12 (7–8): 487–494. doi:10.1016/j.crpv.2013.08.002.
  8. ^ a b Lautenschlager, S.; Desojo, J. B. (2011). "Reassessment of the Middle Triassic rauisuchian archosaurs Ticinosuchus ferox and Stagonosuchus nyassicus". Paläontologische Zeitschrift. 85 (4): 357–381. doi:10.1007/s12542-011-0105-1.
  9. ^ Richard J. Butler; Sterling J. Nesbitt; Alan J. Charig; David J. Gower; Paul M. Barrett (2018). "Mandasuchus tanyauchen, gen. et sp. nov., a pseudosuchian archosaur from the Manda Beds (?Middle Triassic) of Tanzania" (PDF). Journal of Vertebrate Paleontology. 37 (Supplement to No. 6): 96–121. doi:10.1080/02724634.2017.1343728.
  10. ^ Nesbitt, Sterling J.; Sidor, Christian A.; Angielczyk, Kenneth D.; Smith, Roger M. H.; Tsuji, Linda A. (November 2014). "A new archosaur from the Manda beds (Anisian, Middle Triassic) of southern Tanzania and its implications for character state optimizations at Archosauria and Pseudosuchia". Journal of Vertebrate Paleontology. 34 (6): 1357–1382. doi:10.1080/02724634.2014.859622.
  11. ^ a b c d e Nesbitt, S. J.; Barrett, P. M.; Werning, S.; Sidor, C. A.; Charig, A. J. (2013). "The oldest dinosaur? A Middle Triassic dinosauriform from Tanzania". Biol. Lett. 9 (1): 20120949. doi:10.1098/rsbl.2012.0949. PMC 3565515. PMID 23221875.
  12. ^ Nesbitt, Sterling J.; Butler, Richard J.; Ezcurra, Martín D.; Barrett, Paul M.; Stocker, Michelle R.; Angielczyk, Kenneth D.; Smith, Roger M. H.; Sidor, Christian A.; Niedźwiedzki, Grzegorz; Sennikov, Andrey G.; Charig, Alan J. (2017). "The earliest bird-line archosaurs and the assembly of the dinosaur body plan" (PDF). Nature. 544 (7651): 484–487. doi:10.1038/nature22037. PMID 28405026.
  13. ^ Nesbitt, S.J.; Sidor, C.A.; Angielczyk, K.D.; Smith, R.M.; Parker, W. (2012). "Derivation of the aetosaur osteoderm carapace: evidence from a new, exceptionally preserved "stem aetosaur" from the Middle Triassic (Anisian) Manda Beds of southwestern Tanzania". Journal of Vertebrate Paleontology. 32 (Supp. 1): 149. doi:10.1080/02724634.2012.10635175.
  14. ^ Brenen M. Wynd; Brandon R. Peecook; Megan R. Whitney; Christian A. Sidor (2018). "The first occurrence of Cynognathus crateronotus (Cynodontia: Cynognathia) in Tanzania and Zambia, with implications for the age and biostratigraphic correlation of Triassic strata in southern Pangea". Journal of Vertebrate Paleontology. 37 (Supplement to No. 6): 228–239. doi:10.1080/02724634.2017.1421548.
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