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Continuous Plankton Records: Annual Fluctuations of the Plankton in the Western English Channel, 1958–83

Published online by Cambridge University Press:  11 May 2009

G. A. Robinson  and
H. G. Hunt
G. A. Robinson
Affiliation:
Natural Environment Research Council, Institute for Marine Environmental Research, Prospect Place, The Hoe, Plymouth PL1 3DH
H. G. Hunt
Affiliation:
Natural Environment Research Council, Institute for Marine Environmental Research, Prospect Place, The Hoe, Plymouth PL1 3DH
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Extract

Surveys of the plankton at a depth of 10 m in the western English Channel have been carried out at monthly intervals from 1958 onwards using Continuous Plankton Recorders to provide data on annual fluctuations in abundance of the plankton. Interpretation of these results has been attempted by empirical associations with environmental factors (salinity, sea-surface temperature, radiation, atmospheric pressure patterns, wind speed and current strength). Principal component analysis has been used to extract the main patterns of change and correlation analysis for assessing the relationship between the plankton and the environmental factors. There are complex relationships between the plankton and all environmental factors, supporting previous conclusions that the long-term changes are mediated through interaction between the plankton and the climate. Spectral analysis showed long-term trends and shorter cycles of six and three to four years in both the biological and physical elements, indicating that changes in the western Channel are responding to changes in climate over a much wider area

Type
Research Article
Information
Journal of the Marine Biological Association of the United Kingdom , Volume 66 , Issue 4 , November 1986 , pp. 791 - 802
Copyright
Copyright © Marine Biological Association of the United Kingdom 1986

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References

Aiken, J., 1981. The Undulating Oceanographic Recorder Mark 2. Journal of Plankton Research, 3, 551–560.CrossRefGoogle Scholar
Bainbridge, V., 1963. Continuous plankton records: contribution towards a plankton atlas of the North Atlantic and the North Sea. Part viii: Chaetognatha. Bulletin of Marine Ecology, 6, 40–51.Google Scholar
Colebrook, J. M., 1960. Continuous plankton records: methods of analysis, 1950–1959. Bulletin of Marine Ecology, 5, 51–64.Google Scholar
Colebrook, J. M., 1964. Continuous plankton records: a principal component analysis of the geographical distribution of zooplankton. Bulletin of Marine Ecology, 6, 78–100.Google Scholar
Colebrook, J. M., 1975. The Continuous Plankton Recorder survey: automatic data processing methods. Bulletin of Marine Ecology, 8, 123–142.Google Scholar
Colebrook, J. M., 1978. Continuous plankton records: zooplankton and environment, north-east Atlantic and North Sea, 1948–1975. Oceanologica acta, 1, 9–23.Google Scholar
Colebrook, J. M., 1985. Continuous plankton records: overwintering and annual fluctuations in the abundance of zooplankton. Marine Biology, 84, 261–266.CrossRefGoogle Scholar
Colebrook, J. M., Glover, R. S. & Robinson, G. A., 1961. Continuous plankton records: contributions towards a plankton atlas of the north-eastern Atlantic and the North Sea. General Introduction. Bulletin of Marine Ecology, 5, 67–80.Google Scholar
Colebrook, J. M. & Robinson, G. A., 1963. Ecological differentiation in the plankton of the waters around the British Isles. In Speciation in the Sea, pp. 157–169. Systematics Association publication no. 5.Google Scholar
Colebrook, J. M & Taylor, A. H., 1984. Significant time scales of long-term variability in the plankton and the environment. Rapport et procès-verbaux des reunions. Conseil international pour I'exploration de la mer, 183, 20–26.Google Scholar
EDINBURGH OCEANOGRAPHIC LABORATORY, 1973. Continuous plankton records: a plankton atlas of the North Atlantic and the North Sea. Bulletin of Marine Ecology, 7, 174 pp.Google Scholar
Gieskes, W. W. C, 1971. Ecology of the Cladocera of the north Atlantic and the North Sea. Netherlands Journal of Sea Research, 5, 342–376.CrossRefGoogle Scholar
Glover, R. S., Robinson, G. A. & Colebrook, J. M., 1972. Plankton in the north Atlantic - an example of the problems of analysing variability in the environment. In Marine Pollution and Sea Life (ed. M., Ruivo), pp. 439–445. West Byfleet, Surrey: Fishing News (Books)Ltd.Google Scholar
Hardy, A. C, 1939. Ecological investigations with the Continuous Plankton Recorder: object, plan and methods. Hull Bulletins of Marine Ecology, 1, 1–57.Google Scholar
Laevastu, T. & Hubert, W. E., 1965. Analysis and Prediction of the Depth of the Thermocline and Near Surface Thermal Structure. Monterey, California: Fleet Numerical Weather Facility. [Technical note no. 10.]Google Scholar
Lamb, H. H., 1972. British Isles weather types and a register of the daily sequence of circulation patterns 1861–1971. Geophysical Memoirs, London, 1972, 116 pp.Google Scholar
Lindley, J. A., 1977. Continuous plankton records: the distribution of the Euphasiacea (Crustacea: Malacostraca) in the north Atlantic and the North Sea, 1966–1967. Journal of Biogeography, 4, 121–133.CrossRefGoogle Scholar
Prandle, D., 1978. Monthly-mean residual flows through the Dover Strait, 1949–1972. Journal of the Marine Biological Association of the United Kingdom, 58, 965–973.CrossRefGoogle Scholar
Prandle, D., 1984. Monthly-mean residual flows through the Dover Strait, 1949–1980. Journal of the Marine Biological Association of the United Kingdom, 64, 722–724.CrossRefGoogle Scholar
Rasmusson, E. M. & Wallace, J. M., 1983. Meteorological aspects of the El Nino/Southern Oscillation. Science, New York, 222, 1195–1202.CrossRefGoogle ScholarPubMed
Reid, P. C, 1984. Year-to-year changes in zooplankton biomass, fish yield and fish stock in the North Sea. International Council for the Exploration of the Sea (C. M. Papers and Reports), L:39, 7 pp. [Mimeo.]Google Scholar
Robinson, G. A., 1983. Continuous plankton records: phytoplankton in the North Sea, 1958–1980, with special reference to 1980. British Phycological Journal, 18, 131–139.CrossRefGoogle Scholar
Robinson, G. A., Aiken, J & Hunt, H. G. 1986. Synoptic surveys of the western English Channel. The relationships between plankton and hydrography. Journal of the Marine Biological Association of the United Kingdom, 66, 201–218.CrossRefGoogle Scholar
Robinson, G. A. & Hiby, A. R., 1978. The Continuous Plankton Recorder survey. Monographs on Oceanographic Methodology, UNESCO, 6, 58–63.Google Scholar
Russell, F. S., 1936. On the value of certain plankton animals as indicators of water movements in the English Channel and the North Sea. Journal of the Marine Biological Association of the United Kingdom, 20, 309–331.CrossRefGoogle Scholar
Southward, A. J., 1980. The western English Channel-an inconstant ecosystem? Nature, London, 285, 361–366.CrossRefGoogle Scholar
Taylor, A. H. & Stephens, J. A., 1980. Latitudinal displacement of the Gulf Stream (1966 to 1977) and their relation to changes in temperature and zooplankton abundance in the N.E. Atlantic. Oceanologica acta, 3, 145–149.Google Scholar