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On the Feeding of the Hagfish Myxine Glutinosa in the North Sea

Published online by Cambridge University Press:  11 May 2009

R. G. J. Shelton
Affiliation:
D.A.F.S. Marine Laboratory, P.O. Box 101, Victoria Road, Aberdeen

Extract

The myxinoid cyclostomes, of which the hagfish Myxine glutinosa L. is one of the best known examples, are of unique biological interest as representatives of a group of jawless vertebrates which probably had their origin in the pteraspidomorph ostracoderms of the Ordovician era (Nybelin, 1973). They have been much studied by comparative anatomists and physiologists but somewhat neglected by ecologists. There is, for instance, very little critical information on their normal feeding biology. Perhaps one reason for this is that, although hagfish may be extremely abundant locally (their principal habitat requirements are stable, soft muddy sediments and a salinity in excess of 31 %, (Gustafson, 1935)), they tend to be missed by most exploratory fishing and biological sampling programmes. This is because benthic sampling techniques are often ill-adapted for the capture of large active organisms capable of swimming and burrowing and because, unless blocked by the catch, the cod-end mesh sizes of the trawls used by most British commercial fishermen would easily permit the escape of even the largest hagfish. However, the research otter trawls used by the Department of Agriculture and Fisheries for Scotland (D.A.F.S.) for surveying the North Sea stocks of the deep water pink shrimp, Pandalus borealis Krøyer, are fitted with cod-end covers of small mesh, and it is found that the catches frequently include small numbers of hagfish, presumably caught while swimming close to the bottom, or possibly when buried in the surface of the sediments. The present study is largely based on the examination of hagfish collected during the D.A.F.S. Pandalus surveys of 1975 and 1976. The remaining material was kindly provided by Dr J. B. Buchanan of the Dove Marine Laboratory at Cullercoats, Northumberland.

Type
Research Article
Copyright
Copyright © Marine Biological Association of the United Kingdom 1978

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References

REFERENCES

Adam, H., 1963. Structure and histochemistry of the alimentary canal. In The Biology of Myxine (ed. A., Brodal and R., Fänge), pp. 256288. Oslo: Universitetsforlaget.Google Scholar
Allen, J. A., 1959. On the biology of Pandalus borealis Krøyer, with reference to a population off the Northumberland coast. Journal of the Marine Biological Association of the United Kingdom, 38, 189220.CrossRefGoogle Scholar
Buchanan, J. B., 1963. The bottom fauna communities and their sediment relationships off the coast of Northumberland. Oikos, 14, 154175.CrossRefGoogle Scholar
Dean, B., 1899. On the embryology of Bdellostoma stouti. A general account of myxinoid development from the egg and segmentation to hatching. In Festschrift zum siebenzigsten Geburtstag von Carl von Kupffer, pp. 221276. Jena: Gustav Fischer.Google Scholar
Foss, G., 1962. Some observations on the ecology of Myxine glutinosa L. Preliminary communication. Sarsia, 7, 1722.CrossRefGoogle Scholar
Foss, G., 1968. Behaviour of Myxine glutinosa L. in natural habitat. Investigation of the mud biotope by a suction technique. Sarsia, 31, 113.CrossRefGoogle Scholar
Gustafson, G., 1935. On the biology of Myxine glutinosa. Arkiv för zoologi, 28, 128.Google Scholar
Nybelin, O., 1973. Phylogeny of the hagfish and the lampreys. Ada Regiae Societatis Scientiarum et Litter arum Gothobergensis (Zoologica), 8, 813.Google Scholar
Strahan, R., 1963. The behaviour of myxinoids. Acta zoologica, 44, 73102.CrossRefGoogle Scholar
Warren, P. J. & Sheldon, R. W., 1968. Association between Pandalus borealis and fine-grained sediments off Northumberland. Nature, London, 217, 579580.CrossRefGoogle Scholar