Hostname: page-component-586b7cd67f-dsjbd Total loading time: 0 Render date: 2024-11-27T13:26:21.568Z Has data issue: false hasContentIssue false

Observations on the rate of production of external ridges on the shell of Pecten maximus in the laboratory

Published online by Cambridge University Press:  11 May 2009

LL. D. Gruffydd
Affiliation:
N.E.R.C. Unit of Marine Invertebrate Biology, Marine Science Laboratories, Menai Bridge, Gwynedd

Extract

Laboratory observations on the formation of concentric growth ridges on the shell of small Pecten maximus revealed that their rate of production was related to the size of the shell and to the growth increment in a given period. These factors are related, naturally, and the larger the shell, the greater is the growth increment and the number of ridges produced in a given time. Also, in shells of a similar size the higher the growth rate, the larger is the width of each ridge and the greater is the number of ridges produced. Faster growth is achieved therefore by increasing the width and number of ridges. The rate of ridge production at 10 °C was less than half that at 14·5 °C in conditions which were otherwise identical.

Type
Research Article
Copyright
Copyright © Marine Biological Association of the United Kingdom 1981

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Broom, M. J. & Mason, J., 1978. Growth and spawning in the pectinid Chlamys opercularis in relation to temperature and phytoplankton concentration. Marine Biology 47, 277285.CrossRefGoogle Scholar
Clark, G. R. Ii, 1968. Mollusk shell: daily growth lines. Science, New York, 161, 800802.CrossRefGoogle ScholarPubMed
Clark, G. R. Ii, 1974. Periodic growth and biological rhythms in experimentally grown bivalves. In Growth Rhythms and the History of the Earth's Rotation (ed. Rosenberg, G. D. and Runcorn, S. K.), pp. 103117. London: John Wiley & Sons.Google Scholar
Davenport, C. B., 1938. Growth lines in fossil Pectens as indicators of past climates. Journal of Paleontology, 12, 514515.Google Scholar
Richardson, C. A., Crisp, D. J. & Runham, N. W., 1979. Tidally deposited growth bands in the shell of the common cockle, Cerastoderma edule L. Malacologia, 18, 277290.Google Scholar