A hydrographic framework for marine conservation in Scotland

Synopsis Organisms and sea floor sediments respond to a number of physical and physico-chemical factors, the understanding of which permits identification of areas with typical and potentially aberrant habitats and deposits. After a resumé of the bathymetry of Scottish water tides, tidal current and...

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Bibliographic Details
Published in:Proceedings of the Royal Society of Edinburgh. Section B. Biological Sciences
Main Author: McManus, John
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1992
Subjects:
Online Access:http://dx.doi.org/10.1017/s0269727000011040
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0269727000011040
Description
Summary:Synopsis Organisms and sea floor sediments respond to a number of physical and physico-chemical factors, the understanding of which permits identification of areas with typical and potentially aberrant habitats and deposits. After a resumé of the bathymetry of Scottish water tides, tidal current and residual currents stemming from the circulation in the North Atlantic are examined. The salinity and temperature interrelationships in many areas are summarised in open shelf waters, sea lochs and estuaries. Sea floor sediments commonly reflect reworking of glacial deposits coupled with varying indigenous populations of organisms which contribute skeletal debris to the particulate assemblages characterising the bed.