FOSSIL VERTEBRATE FAUNAS OF THE BRITISH RHAETIAN (LATEST TRIASSIC)

被引:53
作者
STORRS, GW
机构
[1] University of Bristol, Department of Geology, Bristol, BS8 1RJ, Wills Memorial Building, Queens Road
关键词
ACTINOPERYGII; BLUE ANCHOR FORMATION; CHORISTODERA; DINOSAURIA; DIPNOI; HARAMYIDAE; HOLOCEPHALI; HYBODONTIFORMES; ICHTHYOSAURIA; LILSTOCK FORMATION; PLAEONISCIFORMES; PENARTH GROUP; PLESIOSAURIA; SELACHII; WESTBURY FORMATION;
D O I
10.1111/j.1096-3642.1994.tb00319.x
中图分类号
Q95 [动物学];
学科分类号
071002 ;
摘要
Rhaetian fossil vertebrate faunas of Britain represent rich but biased samples of taxonomic diversity during uppermost Triassic time. Review of the Westbury Formation, Penarth Group, in particular, reveals a combination of marine, littoral, and terrestrial elements. Minimally, six species of shark are preserved along with a myriacanthid holocephalan, at least four actinopterygian taxa, a characteristic lungfish, ichthyosaurs, plesiosaurs, dinosaurs, and potentially the earliest representative of the Choristodera. Rare mammalian occurrences in the Westbury beds are also possible. Severnichthys gen. nov. is a large osteichthyan, probably a palaeonisciform chondrostean, which historically has been mistaken for a labyrinthodont amphibian. At least two additional actinopterygian species and a holocephalan are known from the Lilstock Formation, and a mammal or mammal-like reptile is recorded from the uppermost Blue Anchor Formation. Analysis of element abundance in the disarticulated Westbury Formation assemblage indicates that many parts of some taxa are never preserved while other elements of the same form are common. Such preservational bias suggests that many species may he missing entirely from this long-studied but poorly understood taphocoenosis. Possibly contemporaneous cave faunas from nearby upland areas give a similarly biased picture of the terrestrial fauna during this time of widespread marine transgression.
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页码:217 / 259
页数:43
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