The vertebrate fauna from the interglacial deposits at Sugworth, near Oxford
- 7 May 1980
- journal article
- research article
- Published by The Royal Society in Philosophical Transactions of the Royal Society of London. B, Biological Sciences
- Vol. 289 (1034) , 87-97
- https://doi.org/10.1098/rstb.1980.0028
Abstract
The fossil vertebrate material from Sugworth comprises freshwater fishes, Amphibia, a snake and fourteen mammalian taxa, including Sorex cf. savini, Beremendia cf. fissidens (the first British record), Mimomys savini, Pliomys episcopalis and Dicerorhinus etruscus. Several taxa are not recorded from later than the Cromerian interglacial and the presence of Mimomys savini indicates a pre-Zone Cr IV age, in agreement with a pollen Zone Cr IIIb age, based on palaeobotanical evidence. The terrestrial vertebrate material was for the most part probably disarticulated and broken by the activities of predators and by transport in the river. The fauna is consistent with the palaeobotanical evidence for regional temperate forest, but shows some differences in taxa from that of West Runton (Zone Cr II), and woodland rodents are relatively much more abundant in the younger deposits, probably due in part to local habitat differences. Sugworth provides the only adequate vertebrate fauna of Zone Cr IIIb age so far known from Britain.*This publication has 4 references indexed in Scilit:
- Cromerian interglacial deposits at Sugworth, near Oxford, England, and their relation to the Plateau Drift of the Cotswolds and the terrace sequence of the Upper and Middle ThamesPhilosophical Transactions of the Royal Society of London. B, Biological Sciences, 1980
- THE PALAEOBOTANY OF INTERGLACIAL DEPOSITS AT SUGWORTH, BERKSHIRENew Phytologist, 1978
- New interglacial site at SugworthNature, 1975
- I.—The British Fossil ShrewsGeological Magazine, 1911