Cromer Forest Bed
| Cromer Forest-bed Formation | |
|---|---|
| Stratigraphic range: Early Pleistocene - Middle Pleistocene | |
.JPG) Cromer Forest-bed Formation exposed at the base of the West Runton Cliffs | |
| Type | Geological formation |
| Unit of | Dunwich Group |
| Sub-units | Sheringham Member, Runton Member, West Runton Member, and Bacton Member |
| Underlies | Middle Pleistocene glacial deposits |
| Overlies | Wroxham Crag Formation or unconformity with Chalk Group |
| Thickness | around 6 metres (20 ft) |
| Lithology | |
| Primary | sands and silts |
| Other | peat, mud, silty marl |
| Location | |
| Coordinates | 52°56′28″N 1°15′11″E / 52.941°N 1.253°E |
| Region | Norfolk |
| Country | England |
| Type section | |
| Named for | Cromer |
| Named by | Clement Reid |
| Location | The coast of North Norfolk from Weybourne to Happisburgh |
| Year defined | 1882 |
| Country | England |
The Cromer Forest-bed Formation, sometimes known as the Cromer Forest Bed, is a geological formation in Norfolk, England. It consists of river gravels, estuary and floodplain sediments predominantly silt, sand, and muds as well as peat along the coast of northern Norfolk.[1] The Cromer Forest Bed itself varies in age from about 2 to 0.5 million years ago, from the Early Pleistocene to early Middle Pleistocene,[2] though the most fossiliferous strata, such as the West Runton Freshwater Bed date to towards the end of deposition during the early Middle Pleistocene. The fossiliferous West Runton Freshwater Bed is the type locality for the Cromerian Stage of the early Middle Pleistocene between 0.8 and 0.5 million years ago.[3] Some fossils from the Cromer Forest Bed likely come from Early Pleistocene layers, though many finds are found out of stratigraphic context.[4]
It is about 6 metres (20 ft) thick[1] and is exposed in cliff section near the village of West Runton.
Paleontology and paleobotany
[edit]For over a century this formation, named after the local town of Cromer, has been famous for its assemblage of fossil mammal remains, containing the diverse remains of numerous taxa. Species of deer recovered include those of Eucladoceros, Praemegaceros, Megaloceros/Praedama savini, the early moose relative Cervalces latifrons, as well as red deer, fallow deer, and roe deer.[5] Remains of carnivorans include those of the large lion Panthera fossilis, the sabertooth cat Homotherium, the "European jaguar" Panthera gombaszoegensis the early wolf Canis mosbachensis, cave hyena, brown bear, wildcat (Felis lunensis), and lynx.[3] The large hippopotamus Hippopotamus antiquus has also been recovered probably from Cromerian aged layers.[6] The West Runton Mammoth, a largely complete skeleton of the steppe mammoth (Mammuthus trogontherii) is one of the most best preserved finds found in the West Runton Freshwater Bed. Other proboscideans found in the Cromer Forest Bed include those of the earlier mammoth Mammuthus meridionalis, as well as the straight-tusked elephant (Palaeoloxodon antiquus).[7] The bison Bison schoetensacki has also been found in the Cromer Forest Bed.[8] A variety of birds are also known from the Cromer Forest Bed.[9]
Archaeology
[edit]The oldest human footprints outside Africa, the Happisburgh footprints as well as handaxes and bison bones with cut marks were also found in layers considered to belong to this deposit near Happisburgh, dated to around 1 million to 780,000 years ago.[2]
See also
[edit]References
[edit]- ^ a b "Cromer Forest-bed Formation". The BGS Lexicon of Named Rock Units. British Geological Survey.
- ^ a b Ashton, Nick; Lewis, Simon G.; De Groote, Isabelle; Duffy, Sarah M.; Bates, Martin; Bates, Richard; Hoare, Peter; Lewis, Mark; Parfitt, Simon A.; Peglar, Sylvia; Williams, Craig (7 February 2014). Petraglia, Michael D. (ed.). "Hominin Footprints from Early Pleistocene Deposits at Happisburgh, UK". PLOS ONE. 9 (2): e88329. Bibcode:2014PLoSO...988329A. doi:10.1371/journal.pone.0088329. ISSN 1932-6203. PMC 3917592. PMID 24516637.
- ^ a b Lewis, Mark; Pacher, Martina; Turner, Alan (December 2010). "The larger Carnivora of the West Runton Freshwater Bed". Quaternary International. 228 (1–2): 116–135. Bibcode:2010QuInt.228..116L. doi:10.1016/j.quaint.2010.06.022.
- ^ Bynoe, Rachel; Ashton, Nick M.; Grimmer, Tim; Hoare, Peter; Leonard, Joanne; Lewis, Simon G.; Nicholas, Darren; Parfitt, Simon (February 2021). "Coastal curios? An analysis of ex situ beach finds for mapping new Palaeolithic sites at Happisburgh, UK". Journal of Quaternary Science. 36 (2): 191–210. Bibcode:2021JQS....36..191B. doi:10.1002/jqs.3270. ISSN 0267-8179.
- ^ Lister, Adrian M. (1993). "The stratigraphical significance of deer species in the cromer forest-bed formation". Journal of Quaternary Science. 8 (2): 95–108. Bibcode:1993JQS.....8...95L. doi:10.1002/jqs.3390080202.
- ^ Adams, Neil F.; Candy, Ian; Schreve, Danielle C. (January 2022). "An Early Pleistocene hippopotamus from Westbury Cave, Somerset, England: support for a previously unrecognized temperate interval in the British Quaternary record". Journal of Quaternary Science. 37 (1): 28–41. Bibcode:2022JQS....37...28A. doi:10.1002/jqs.3375. ISSN 0267-8179.
- ^ Stuart, Anthony J.; Lister, Adrian M. (December 2010). "Introduction: The West Runton Freshwater Bed and the West Runton Mammoth". Quaternary International. 228 (1–2): 1–7. Bibcode:2010QuInt.228....1S. doi:10.1016/j.quaint.2010.07.035.
- ^ Sorbelli, Leonardo; Alba, David M.; Cherin, Marco; Moullé, Pierre-Élie; Brugal, Jean-Philip; Madurell-Malapeira, Joan (June 2021). "A review on Bison schoetensacki and its closest relatives through the early-Middle Pleistocene transition: Insights from the Vallparadís Section (NE Iberian Peninsula) and other European localities". Quaternary Science Reviews. 261: 106933. Bibcode:2021QSRv..26106933S. doi:10.1016/j.quascirev.2021.106933.
- ^ Harrison, C. J. O. (May 1979). "Birds of the Cromer Forest Bed Series of the East Anglian Pleistocene" (PDF). Transactions of the Norfolk & Norwich Naturalists' Society. 24: 277–287.
Further reading
[edit]- Bowen, D.Q., 1978, Quaternary geology: a stratigraphic framework for multidisciplinary work. Pergamon Press, Oxford, United Kingdom. 221 pp. ISBN 978-0-08-020409-3
- West, R.G., 1980, The pre-glacial Pleistocene of the Norfolk and Suffolk Coasts Cambridge University Press. ISBN 0-521-21962-0
- Ehlers, J., P. L. Gibbard, and J. Rose, eds., 1991, Glacial deposits in Great Britain and Ireland Balkema, Rotterdam. 580 pp ISBN 978-90-6191-875-2
- Mangerud, J., J. Ehlers, and P. Gibbard, 2004, Quaternary Glaciations: Extent and Chronology 1: Part I Europe, Elsevier, Amsterdam. ISBN 0-444-51462-7
- Sibrava, V., Bowen, D.Q, and Richmond, G.M., 1986, Quaternary Glaciations in the Northern Hemisphere, Quaternary Science Reviews, vol. 5, pp. 1–514.
External links
[edit]Gibbard, P.L., S. Boreham, K.M. Cohen and A. Moscariello, 2007, Global correlation tables for the Quaternary, Subcommission on Quaternary Stratigraphy, Department of Geography, University of Cambridge, Cambridge, England.