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Observations on the Morphology of the Mantle Folds of the Pediveliger of Ostrea Edulis L. and their Function During Settlement

Published online by Cambridge University Press:  11 May 2009

H. J. Cranfield
H. J. Cranfield*
Affiliation:
NERC UNIT of Marine Invertebrate Biology, Marine Science Laboratories, Menai Bridge, Anglesey, U.K.
*
*Present address: Fisheries Research Division, Ministry of Agriculture and Fisheries, P.O. Box 19062, Wellington, New Zealand.
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Extract

Stafford (1913) rejected the view of many early workers (see Ryder, 1883, 1884; Huxley, 1883; Horst, 1886) that oyster larvae cemented themselves to the substratum with secretions of the mantle edge. He thought that the mantle margin could not be extended sufficiently to form the extensive area of cement that he found on the left valve of cemented larvae. Furthermore, he argued that the mantle could not secrete so much material in the short period that larvae took to cement. He deduced from the much reduced state of the ‘byssus gland’ in settled larvae that this gland was the source of the cement and suggested that the cement was spread over the shell by the foot. Nelson (1924), Prytherch (1934), Cole & Knight-Jones (1939) and Cranfield (19736, c) have clarified the role of the foot in cementing. Nelson (1924) also noted that cementing oyster larvae extended the mantle margin over the substratum but considered that this action spread the cement discharged by the foot and that the folds themselves did not secrete more material. The other authors, like Stafford, have dismissed or ignored any part the mantle folds might play in cementing.

Type
Research Article
Information
Journal of the Marine Biological Association of the United Kingdom , Volume 54 , Issue 1 , February 1974 , pp. 1 - 12
Copyright
Copyright © Marine Biological Association of the United Kingdom 1974

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