Detection of environmental change in a marine ecosystem—evidence from the western English Channel
Detection of environmental change in a marine ecosystem—evidence from the western English Channel
To separate human-induced changes from natural fluctuations in marine life requires long-term research. The western English Channel has been investigated from Plymouth for over 100 years. The abundance of marine life has been recorded and related to physical changes in the environment. By comparing different parts of the ecosystem we can demonstrate historic natural fluctuations, allowing prediction of effects of future global change. From the 1920s to the 1950s there was a period of warming of the sea, with increases in abundance of species of fish, plankton and intertidal organisms that are typically common in warmer waters to the south of Britain. After 1962 the sea cooled down and northern cold-water species became more abundant. Since the 1980s regional sea surface temperature has increased again and warm-water species are once more becoming abundant.
Long-term changes, Climate, Global warming, English Channel, Sea surface temperature
245-256
Hawkins, Stephen J.
758fe1c1-30cd-4ed1-bb65-2471dc7c11fa
Southward, Alan J.
b218af99-0672-45d5-a014-7f44eba261b0
Genner, Martin J.
90547c65-c194-4c93-8ea4-b8523acef1a6
July 2003
Hawkins, Stephen J.
758fe1c1-30cd-4ed1-bb65-2471dc7c11fa
Southward, Alan J.
b218af99-0672-45d5-a014-7f44eba261b0
Genner, Martin J.
90547c65-c194-4c93-8ea4-b8523acef1a6
Hawkins, Stephen J., Southward, Alan J. and Genner, Martin J.
(2003)
Detection of environmental change in a marine ecosystem—evidence from the western English Channel.
Science of the Total Environment, 310 (1-3), .
(doi:10.1016/S0048-9697(02)00645-9).
Abstract
To separate human-induced changes from natural fluctuations in marine life requires long-term research. The western English Channel has been investigated from Plymouth for over 100 years. The abundance of marine life has been recorded and related to physical changes in the environment. By comparing different parts of the ecosystem we can demonstrate historic natural fluctuations, allowing prediction of effects of future global change. From the 1920s to the 1950s there was a period of warming of the sea, with increases in abundance of species of fish, plankton and intertidal organisms that are typically common in warmer waters to the south of Britain. After 1962 the sea cooled down and northern cold-water species became more abundant. Since the 1980s regional sea surface temperature has increased again and warm-water species are once more becoming abundant.
This record has no associated files available for download.
More information
Published date: July 2003
Keywords:
Long-term changes, Climate, Global warming, English Channel, Sea surface temperature
Identifiers
Local EPrints ID: 188389
URI: http://eprints.soton.ac.uk/id/eprint/188389
ISSN: 0048-9697
PURE UUID: 21c2d85b-4f56-47b6-9a3c-c334518f571d
Catalogue record
Date deposited: 24 May 2011 13:53
Last modified: 14 Mar 2024 03:31
Export record
Altmetrics
Contributors
Author:
Alan J. Southward
Author:
Martin J. Genner
Download statistics
Downloads from ePrints over the past year. Other digital versions may also be available to download e.g. from the publisher's website.
View more statistics