Magnesian Conglomerate

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Magnesian Conglomerate
Stratigraphic range: Rhaetian
~208–202 Ma
TypeGeological formation
Lithology
PrimaryBreccia
OtherLimestone
Location
Coordinates51°30′N 2°36′W / 51.5°N 2.6°W / 51.5; -2.6Coordinates: 51°30′N 2°36′W / 51.5°N 2.6°W / 51.5; -2.6
Approximate paleocoordinates35°54′N 0°48′E / 35.9°N 0.8°E / 35.9; 0.8
RegionSouth West England
Country England
ExtentBristol
Type section
Named byHenry Riley & Samuel Stutchbury
Year defined1836
Magnesian Conglomerate is located in England
Magnesian Conglomerate
Magnesian Conglomerate (England)

The Magnesian Conglomerate is a geological formation in Clifton, Bristol in England (originally Avon). It dates back to the Rhaetian stage of the Late Triassic,[1][2] although it may be as old as the Norian stage of the Late Triassic and as young as the Hettangian stage of the Early Jurassic.[citation needed] This formation was first discovered in autumn 1834 and was studied in 1836 by Henry Riley and Samuel Stutchbury.[3]

The Avon Fissure Fill is probably the same formation as the Magnesian Conglomerate.

Vertebrate paleofauna[]

Archosaurs[]

Taxon Species Presence Notes Images
Agnosphitys[2][4] A. cromhallensis[2][4] Geographically present in Avon, England (now Bristol).[2] Its remains include a left ilium (holotype) and a left maxilla, astragalus and humerus (referred specimen).[2] Agnosphitys cromhallensis2 copia.jpg
Agrosaurus[5][2] A. macgillivrayi[5][2] Geographically present in Avon, England (now Bristol). Originally believed to have been found in Cape York Peninsula, Queensland (Australia).[2] A tibia, a claw and some other fragments.[2]
Asylosaurus[2][6] A. yalensis[2][6] Geographically present in Avon, England (now Bristol).[2][7] Dorsal vertebrae, ribs, gastralia, a shoulder girdle, humeri, a partial forearm, and a hand; additional bones from the neck, tail, pelvis, arm and legs that may represent the same individual.[6][2] Asylosaurus NT.jpg
Palaeosaurus[2][6] P. cylindrodon[2][6] Geographically present in Avon, England (now Bristol) and Bristol.[2] Two teeth (one destroyed in 1940).[2] Palaeosaurus both holotypes.png
Rileyasuchus[2][8][9] R. bristolensis[2][8][9] Geographically present in Bristol.[2] Two vertebrae and a humerus.[2]
Theropoda[2] Indeterminate[2] Geographically present in Avon, England (now Bristol) and Bristol.[2] Indeterminate remains.[2]
Thecodontosaurus[2] Indeterminate[2] Geographically present in Avon, England (now Bristol) and Bristol.[2] Indeterminate remains.[2] Thecodontosaurus.jpg

Fish[]

See also[]

References[]

  1. ^ Magnesian Conglomerate in the Paleobiology Database
  2. ^ Jump up to: a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab ac Weishampel et al., 2004, pp. 521–525
  3. ^ Riley & Stutchbury, 1836
  4. ^ Jump up to: a b Nicholas C. Fraser, Kevin Padian, Gordon M. Walkden and A. L. M. Davis, 2002. Basal dinosauriform remains from Britain and the diagnosis of the Dinosauria. Palaeontology. 45(1), 79-95.
  5. ^ Jump up to: a b H. G. Seeley. (1891). On Agrosaurus macgillivrayi (Seeley), a saurischian reptile from the N.E. coast of Australia. Quarterly Journal of the Geological Society of London 47:164-165
  6. ^ Jump up to: a b c d e Galton, Peter (2007). "Notes on the remains of archosaurian reptiles, mostly basal sauropodomorph dinosaurs, from the 1834 fissure fill (Rhaetian, Upper Triassic) at Clifton in Bristol, southwest England". Revue de Paléobiologie. 26 (2): 505–591.
  7. ^ Riley H and Stutchbury S (1836a) "A description of various remains of three distinct saurian animals discovered in the autumn of 1834, in the Magnesian Conglomerate on Durdham Down, near Bristol". Geological Society of London, Proceedings, 2 (45): 397-399.
  8. ^ Jump up to: a b von Huene, F. (1902). Überischt über die Reptilien der Trias. Geologische und Paläontologie Abhandlungen, Neu Folge 8:97-156. [German]
  9. ^ Jump up to: a b Kuhn, O. (1961). Die Familien der rezenten und fossilen Amphibien und Reptilien. Meisenbach:Bamberg, 79 p.
  10. ^ Jump up to: a b c Foffa, D.; D. I. Whiteside; P. A. Viegas, and M. J. Benton. 2014. Vertebrates from the Late Triassic Thecodontosaurus-bearing rocks of Durdham Down, Clifton (Bristol, UK). Proceedings of the Geologists' Association 125. 317–332.

Bibliography[]

  • Foffa, D.; D. I. Whiteside; P. A. Viegas, and M. J. Benton. 2014. Vertebrates from the Late Triassic Thecodontosaurus-bearing rocks of Durdham Down, Clifton (Bristol, UK). Proceedings of the Geologists' Association 125. 317–332.
  • Weishampel, David B.; Peter Dodson, and Halszka Osmólska (eds.). 2004. The Dinosauria, 2nd edition, 1–880. Berkeley: University of California Press. Accessed 2019-02-21. ISBN 0-520-24209-2
  • Riley, H., and S. Stutchbury. 1836. A description of various fossil remains of three distinct saurian animals discovered in the autumn of 1834 in the Magnesian Conglomerate on Durdham Down near Bristol. Proceedings of the Geological Society 2. 397–399.

Further reading[]

  • Riley, H. and Stutchbury, S. 1840. A description of various fossil remains of three distinct saurian animals recently discovered in the Magnesian Conglomerate near Bristol Transactions of the Geological Society of London 5, 349–357
  • W. Buckland. 1824. Reliquiæ Diluvianæ; or, Observations on the Organic Remains Contained in Caves, Fissures, and Diluvial Gravel, and on Other Geological Phenomena, Attesting the Action of an Universal Deluge. Second Edition. John Murray, London 1-303

External links[]

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