|
|||||
|
|
The Quaternary history of the Wash fluvial network, UK |
|
| Authors: | Steve Boreham Tom S White Andy J Howard |
| Institution: | a Department of Geography, University of Cambridge, Downing Place, Cambridge CB2 3EN, UK b Department of Zoology, University of Cambridge, Downing Street, Cambridge CB2 3EJ, UK c Department of Geography, Durham University, Science Laboratories, South Road, Durham DH1 3LE, UK d Institute of Archaeology and Antiquity, University of Birmingham, Edgbaston, Birmingham B15 2TT, UK e Department of Archaeology, Durham University, Science Laboratories, South Road, Durham DH1 3LE, UK |
| Abstract: | This paper appraises and compares the Middle-Upper Pleistocene sedimentary sequences preserved in the fluvial systems draining into the Fenland Basin and the Wash estuary. Of the main Fenland rivers the longest records, which extend back to the initial Anglian (glacial) formation of the basin, are found in the Great Ouse and its tributaries, particularly the Cam and the Nar. These sequences preserve sediments representing all four post-Anglian interglacials. The Nene also has an extensive post-Anglian history, with evidence for a Hoxnian estuary that is presumed to have been the precursor of the Wash. North of the Nene, however, the Welland and Witham (proto-Trent) have relatively short sequences, which are thought to commence with a later (post-Anglian-pre-Devensian) glaciation that affected Lincolnshire and fed the previously-recognized Tottenhill outwash delta south of Kings Lynn. Prior to Devensian deglaciation the Witham valley was occupied by the Trent, which was the trunk river of the late Middle Pleistocene Wash system. During periods of low sea level the river would have extended north-eastwards across what is now the floor of the North Sea, possibly via the Inner Silver Pit. Several of the central Fenland sequences show evidence of infrequent terrace formation during the late Quaternary, although this might in part be due to poor vertical separation between terraces, so that differentiating them has been difficult; this has been exacerbated by mixed biostratigraphical signals due to the preservation of sediments representing more than one interglacial beneath a single terrace surface. In several of the systems there is evidence for valley rejuvenation to the lowest terrace or valley-floor level during the MIS 4-3 transition. The observed differences within what, during the predominant periods of lower sea level, would have been a single Wash river system are difficult to explain. |
| Keywords: | Quaternary River terraces Interglacial deposits Fen Basin Wash rivers |
| 本文献已被 ScienceDirect 等数据库收录！ | |