Cornbrash
Description
Source: Wikipédia
The Cornbrash Formation is a Middle Jurassic geological formation in England. It ranges in age from Bathonian to Callovian, the uppermost part of the Middle Jurassic. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus. The name Cornbrash is an old English agricultural name applied in Wiltshire to a variety of loose rubble or brash which, in that part of the country, forms a good soil for growing corn. The name was adopted by William Smith for a thin band of shelly limestone which, in the south of England, breaks up in the manner indicated. Although only a thin group of rocks (10–25 feet c. 3–7 m), it is remarkably persistent; it may be traced from Weymouth to the Yorkshire coast, but in north Lincolnshire it is very thin, and probably dies out in the neighborhood of the Humber. It appears again, however, as a thin bed in Gristhorpe Bay, Cayton Bay, Wheatcroft, Newton Dale and Langdale. In the inland exposures in Yorkshire it is difficult to follow on account of its thinness, and the fact that it passes up into dark shales in many places the so-called clays of the Cornbrash, with Avicula echinata. The Cornbrash is of little value for building or road-making, although it is used locally; in the south of England it is not oolitic, but in Yorkshire it is a rubbly, marly, frequently ironshot oolitic limestone. In Bedfordshire it has been termed the Bedford limestone.
Découvertes
Source: The Paleobiology Database
Site(s) correspondant(s) à cette formation: 1Enslow Bridge stegosaur : England - Oxfordshire 12234 12793 13123 16884 29301 62949
"Enslow Bridge", probably Enslow Quarries, about 9.6 km N of Oxford, W bank of Cherwell River, 0.8 km downstream from Enslow Bridge (grid reference SP 42 477 177); Huene (1910) describes it as 200 m E of the Bletchington train station, "a little north of Oxford"; supposedly the same quarry as most of the Cetiosaurus bones from this area.- Stegosauria identifié comme Omosaurus vetustus n. sp.
Publication(s)
La base comprend 6 publication(s).
Source: The Paleobiology Database
- ↑1 2 F. v. Huene. 1910. Über den ältesten Rest von Omosaurus (Dacentrurus) im englischen Dogger [On the oldest remains of Omosaurus (Dacentrurus) from the English Dogger]. Neues Jahrbuch für Mineralogie, Geologie und Paläontologie 1910(1):75-78
- ↑1 P. M. Galton and H. P. Powell. 1983. Stegosaurian dinosaurs from the Bathonian (Middle Jurassic) of England, the earliest record of the family Stegosauridae. Géobios 16(2):219-229 (https://doi.org/10.1016/s0016-6995(83)80020-5)
- ↑1 P. M. Galton. 1985. British plated dinosaurs (Ornithischia, Stegosauridae). Journal of Vertebrate Paleontology 5(3):211-254 (https://doi.org/10.1080/02724634.1985.10011859)
- ↑1 R. Hoffstetter. 1957. Quelques observations sur les stégosaurinés [Some observations on stegosaurines]. Bulletin du Muséum National d'Histoire Naturelle, Paris, 2e série 29(6):537-547
- ↑1 S. C. R. Maidment, D. B. Norman, and P. M. Barrett, P. Upchurch. 2008. Systematics and phylogeny of Stegosauria (Dinosauria: Ornithischia). Journal of Systematic Palaeontology 6(4):367-407 (https://doi.org/10.1017/S1477201908002459)
- ↑1 E. Hennig. 1915. Fossilium Catalogus. I: Animalia. Pars 9: Stegosauria 1:1-16 (https://doi.org/10.1515/9783112609408)
