Hostname: page-component-586b7cd67f-t7fkt Total loading time: 0 Render date: 2024-11-30T18:48:33.752Z Has data issue: false hasContentIssue false
  • English
  • Français

Ipswichian mammalian fauna from the Beeston Terrace at Boulton Moor, near Derby

Published online by Cambridge University Press:  01 May 2009

P. F. Jones  and
M. F. Stanley
P. F. Jones
Affiliation:
Geology Division, Faculty of Science, Derby College of Art and Technology, Kedleston Road, Derby
M. F. Stanley
Affiliation:
Department of Natural History, Derby Museums and Art Gallery, The Strand, Derby
Get access Rights & Permissions [Opens in a new window]

Summary

Mammalian remains are reported from a Pleistocene terrace deposit in the lower Derwent Valley near Derby, which is a correlative of the Beeston Terrace of the nearby River Trent. The faunal assemblage is characteristic of the Ipswichian interglacial and compares favourably with previous finds at other Ipswichian sites in southern Britain. The discovery is significant as it provides the strongest evidence so far for a dating of the Beeston Terrace which is critical to the Pleistocene chronology of the region.

Type
Articles
Information
Geological Magazine , Volume 111 , Issue 6 , November 1974 , pp. 515 - 520
Copyright
Copyright © Cambridge University Press 1974

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Bemrose, H. H. Arnold & Deeley, R. M. 1896. Discovery of mammalian remains in the Old River Gravels of the Derwent near Derby. Q. Jl. geol. Soc., Lond. 52, 497–510.CrossRefGoogle Scholar
Clayton, K. M. 1953. Glacial chronology of part of the Middle Trent Basin. Proc. Geol. Assoc. 64, 198–207.CrossRefGoogle Scholar
Franks, J. W. 1960. Interglacial deposits at Trafalgar Square, London. New Phytol. 59, 145–52.CrossRefGoogle Scholar
Posnansky, M. 1960. The Pleistocene succession in the Middle Trent Basin. Proc. Geol. Assoc. 71, 285–311.CrossRefGoogle Scholar
Rice, R. J. 1968. The Quaternary era. In: Ford, T. D. & Sylvester-Bradley, P. C. (eds): Geology of the East Midlands, ch. 19, 332–55.Google Scholar
Shotton, F. W. 1973. The English Midlands. In: Mitchell, et al. , A Correlation of Quaternary Deposits in the British Isles. Geol. Soc. Lond., Special Report No. 4.Google Scholar
Straw, A. 1963. The Quaternary evolution of the Lower and Middle Trent. E. Midl. Geogr. 3, 171–89.Google Scholar
Sutcliffe, A. J. 1960. Joint Mitnor Cave, Buckfastleigh. Trans. Torquay Nat. Hist. Soc. 13, 1–26.Google Scholar
Sutcliffe, A. J. 1964. The mammalian fauna. In: Ovey, C. D. (ed): The Swanscombe Skull, ch. 9, 85–111.Google Scholar