Deep-water macrofaunal diversity in the Faroe-Shetland region (NE Atlantic): a margin subject to an unusual thermal regime
Deep-water macrofaunal diversity in the Faroe-Shetland region (NE Atlantic): a margin subject to an unusual thermal regime
The Faroe-Shetland Channel, situated in the NE Atlantic, encompasses a number of different sediment types (habitats) as well as being subject to an unusual thermal regime. Our main objective was to assess variations in macrofaunal generic diversity and composition along two transects to gauge the relative influence of regional hydrography and local habitat heterogeneity. We found that generic richness and diversity on a West of Shetland (WoS) transect correlated most strongly with temperature range, whilst along a North of Shetland (NoS) transect, richness and diversity correlated negatively with sedimentary variables, notably total organic carbon. Macrofaunal composition at WoS is also strongly influenced by water temperature with specific genera (e.g. Galathowenia positively associated with the temperature eigenvectors), whereas at NoS it is a combination of temperature, silt + clay fraction and total organic carbon that has an impact on composition (e.g. Proclea and Pseudosphyrapus, showing a negative relationship with the temperature eigenvectors). Although the temperature regime exerts a strong control on regional ecology, local habitat heterogeneity remains a significant factor.
237-246
Narayanaswamy, Bhavani E.
fcecfc2f-1db0-4786-a379-78411de47a3d
Bett, Brian J.
61342990-13be-45ae-9f5c-9540114335d9
Hughes, David J.
374615ee-f4de-4e21-b0a5-df8182d3f110
March 2010
Narayanaswamy, Bhavani E.
fcecfc2f-1db0-4786-a379-78411de47a3d
Bett, Brian J.
61342990-13be-45ae-9f5c-9540114335d9
Hughes, David J.
374615ee-f4de-4e21-b0a5-df8182d3f110
Narayanaswamy, Bhavani E., Bett, Brian J. and Hughes, David J.
(2010)
Deep-water macrofaunal diversity in the Faroe-Shetland region (NE Atlantic): a margin subject to an unusual thermal regime.
Marine Ecology, 31 (1), .
(doi:10.1111/j.1439-0485.2010.00360.x).
Abstract
The Faroe-Shetland Channel, situated in the NE Atlantic, encompasses a number of different sediment types (habitats) as well as being subject to an unusual thermal regime. Our main objective was to assess variations in macrofaunal generic diversity and composition along two transects to gauge the relative influence of regional hydrography and local habitat heterogeneity. We found that generic richness and diversity on a West of Shetland (WoS) transect correlated most strongly with temperature range, whilst along a North of Shetland (NoS) transect, richness and diversity correlated negatively with sedimentary variables, notably total organic carbon. Macrofaunal composition at WoS is also strongly influenced by water temperature with specific genera (e.g. Galathowenia positively associated with the temperature eigenvectors), whereas at NoS it is a combination of temperature, silt + clay fraction and total organic carbon that has an impact on composition (e.g. Proclea and Pseudosphyrapus, showing a negative relationship with the temperature eigenvectors). Although the temperature regime exerts a strong control on regional ecology, local habitat heterogeneity remains a significant factor.
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Published date: March 2010
Organisations:
Marine Biogeochemistry
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Local EPrints ID: 79476
URI: http://eprints.soton.ac.uk/id/eprint/79476
ISSN: 0173-9565
PURE UUID: 8497166b-1821-435a-8550-ffca7e8c6e19
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Date deposited: 16 Mar 2010
Last modified: 14 Mar 2024 00:30
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Author:
Bhavani E. Narayanaswamy
Author:
Brian J. Bett
Author:
David J. Hughes
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