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- W1569152452 abstract "Publisher Summary The Northern Palaeovalley is an open shelf valley system in the English Channel. It is a distinctive erosional feature within the northern half of the eastern English Channel with a particularly well-defined margin on its northern side and an upper break of slope at a depth of 25–30 m with the valley floor generally at depths of 55–75 m. The valley is >100 km long and varies in width from 8 to 20 km. Its floor lies at depths of 45–90 m, with margins up to 30 m high. Net sediment transport is west to east, with rock and coarse sediment in the valley floor in the west and a gradual eastward increase in sand cover and volume, culminating in two large linear sandbanks up to 28 km long along the northeast margin of the valley. The Palaeovalley supports a rich diversity of infaunal and epifaunal communities. Considerable overlap exists in the infaunal communities associated with the different geomorphic features, while the epifaunal communities exhibit far greater variability in response to the environmental gradients. Interstitial polychaetes dominate the macrobenthic communities across the area reflecting the dominance of mobile sediment deposits. The Palaeovalley as a whole is characterized by comparatively rich macrofaunal communities comprising infaunal and epifaunal species in varying proportions. There is significant overlap between the infaunal communities associated with the five geomorphic features in this area, as all are dominated by interstitial polychaetes, many of which are tolerant of a wide range of sediment classes." @default.
- W1569152452 created "2016-06-24" @default.
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- W1569152452 date "2012-01-01" @default.
- W1569152452 modified "2023-09-26" @default.
- W1569152452 title "Open Shelf Valley System, Northern Palaeovalley, English Channel, UK" @default.
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- W1569152452 doi "https://doi.org/10.1016/b978-0-12-385140-6.00041-4" @default.
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