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- W29220204 abstract "The Basque continental shelf is located in the southeastern part of the Bay of Biscay. It is very narrow, ranging from 7 to 20 km, and comprises the total length of the coastline of ca. 150 km. Structural features dominate the morphology of the continental shelf, where horsts and anticlines, found generally in Cretaceous rocks, form areas starved of soft Neogene sediment. Faults and synclines filled with Tertiary material underlie sandy depressions. Coastal rock lithologies are mainly sandstone, calcareous sandstone, limestone, clay, limonite, marl, and marly limestone. Offshore, the external section of the continental shelf is a sedimentary Neogene and Pleistocene prism, developed by progradation. At shallow-water depth, wave-induced morphologies such as rhythmic surf zone sandbars and troughs, and sandbank morphologies associated to the wave closure depth, could be identified. Regarding macroalgae, the zonation in the intertidal and subtidal zones is determined by tides and exposure to wave action. Rocky bottoms are dominant along the shore and they reach the outer part of the continental shelf; meanwhile, sandbanks are distributed from beaches and river mouths down to muddy depths. Marine habitats along the Basque coast are related to geomorphology and hydrography. The analysis of biological and environmental data shows that wave energy, in the near-bottom, and sedimentary characteristics are the main environmental factors explaining the composition and spatial distribution of sedimentary benthic communities. Within the continental shelf, habitat suitability modeling has been applied, focusing on biological resource management." @default.
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- W29220204 date "2012-01-01" @default.
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- W29220204 title "Rocky Reef and Sedimentary Habitats Within the Continental Shelf of the Southeastern Bay of Biscay" @default.
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- W29220204 doi "https://doi.org/10.1016/b978-0-12-385140-6.00035-9" @default.
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