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Consequences of climate-driven biodiversity changes for ecosystem functioning of North European rocky shores

Consequences of climate-driven biodiversity changes for ecosystem functioning of North European rocky shores
Consequences of climate-driven biodiversity changes for ecosystem functioning of North European rocky shores
We review how intertidal biodiversity is responding to globally driven climate change, focusing on long-term data from rocky shores in the British Isles. Physical evidence of warming around the British Isles is presented and, whilst there has been considerable fluctuation, sea surface temperatures are at the highest levels recorded, surpassing previous warm periods (i.e. late 1950s). Examples are given of species that have been advancing or retreating polewards over the last 50 to 100 yr. On rocky shores, the extent of poleward movement is idiosyncratic and dependent upon life history characteristics, dispersal capabilities and habitat requirements. More southern, warm water species have been recorded advancing than northern, cold water species retreating. Models have been developed to predict likely assemblage composition based on future environmental scenarios. We present qualitative and quantitative forecasts to explore the functional consequences of changes in the identity, abundance and species richness of gastropod grazers and foundation species such as barnacles and canopy-forming algae. We forecast that the balance of primary producers and secondary consumers is likely to change along wave exposure gradients matching changes occurring with latitude, thereby shifting the balance between export and import of primary production. Increases in grazer and sessile invertebrate diversity are likely to be accompanied by decreasing primary production by large canopy-forming fucoids. The reasons for such changes are discussed in the context of emerging theory on the relationship between biodiversity and ecosystem functioning.
Climate change, Intertidal, Range shifts, Biodiversity, Ecosystem functioning, Northeast Atlantic
245-259
Hawkins, S.J.
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Sugden, H.E.
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Mieszkowska, N.
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Moore, P.J.
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Poloczanska, E.
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Leaper, R.
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Herbert, R.J.H.
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Genner, M.J.
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Moschella, P.S.
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Thompson, R.C.
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Jenkins, S.R.
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Southward, A.J.
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Burrows, M.T.
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Hawkins, S.J.
758fe1c1-30cd-4ed1-bb65-2471dc7c11fa
Sugden, H.E.
bc782d0d-aa2a-428f-9884-6ed3c38e298f
Mieszkowska, N.
4c91117c-a01f-46a6-81c7-68ef16cbd598
Moore, P.J.
fe1c23c9-c921-447c-8e08-006770409a8c
Poloczanska, E.
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Leaper, R.
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Herbert, R.J.H.
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Genner, M.J.
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Moschella, P.S.
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Thompson, R.C.
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Jenkins, S.R.
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Southward, A.J.
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Burrows, M.T.
89ce4c9d-01e6-4ae8-a4a2-5a0d8bb09ec2

Hawkins, S.J., Sugden, H.E., Mieszkowska, N., Moore, P.J., Poloczanska, E., Leaper, R., Herbert, R.J.H., Genner, M.J., Moschella, P.S., Thompson, R.C., Jenkins, S.R., Southward, A.J. and Burrows, M.T. (2009) Consequences of climate-driven biodiversity changes for ecosystem functioning of North European rocky shores. Marine Ecology Progress Series, 396, 245-259. (doi:10.3354/meps08378).

Record type: Article

Abstract

We review how intertidal biodiversity is responding to globally driven climate change, focusing on long-term data from rocky shores in the British Isles. Physical evidence of warming around the British Isles is presented and, whilst there has been considerable fluctuation, sea surface temperatures are at the highest levels recorded, surpassing previous warm periods (i.e. late 1950s). Examples are given of species that have been advancing or retreating polewards over the last 50 to 100 yr. On rocky shores, the extent of poleward movement is idiosyncratic and dependent upon life history characteristics, dispersal capabilities and habitat requirements. More southern, warm water species have been recorded advancing than northern, cold water species retreating. Models have been developed to predict likely assemblage composition based on future environmental scenarios. We present qualitative and quantitative forecasts to explore the functional consequences of changes in the identity, abundance and species richness of gastropod grazers and foundation species such as barnacles and canopy-forming algae. We forecast that the balance of primary producers and secondary consumers is likely to change along wave exposure gradients matching changes occurring with latitude, thereby shifting the balance between export and import of primary production. Increases in grazer and sessile invertebrate diversity are likely to be accompanied by decreasing primary production by large canopy-forming fucoids. The reasons for such changes are discussed in the context of emerging theory on the relationship between biodiversity and ecosystem functioning.

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Published date: 2009
Keywords: Climate change, Intertidal, Range shifts, Biodiversity, Ecosystem functioning, Northeast Atlantic
Organisations: Ocean and Earth Science

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Local EPrints ID: 187801
URI: http://eprints.soton.ac.uk/id/eprint/187801
PURE UUID: 49c0debc-b41a-439b-b134-9df1bead3bb9

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Date deposited: 18 May 2011 11:17
Last modified: 14 Mar 2024 03:28

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Contributors

Author: S.J. Hawkins
Author: H.E. Sugden
Author: N. Mieszkowska
Author: P.J. Moore
Author: E. Poloczanska
Author: R. Leaper
Author: R.J.H. Herbert
Author: M.J. Genner
Author: P.S. Moschella
Author: R.C. Thompson
Author: S.R. Jenkins
Author: A.J. Southward
Author: M.T. Burrows

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