Abstract

Marked specimens of the Malaysian cockle Anadara granosa (L.) were placed in buried cages (filled with sediment from the surrounding substratum) which were located in intertidal and subtidal environments in an area between Penang Island and mainland West Malaysia. In the majority of cockle shells examined the number of growth bands deposited was close to the number of tidal periods. Bands in the shells of intertidal animals were more strongly defined than those in shells continuously immersed. The banding pattern in shells from the subtidal environments showed narrow increments during spring tides alternating with a few wider increments during neap tides. The growth increments between bands correspond to tidal periods so they can be used to record growth rates and provide estimates of the ages of the shells. Samples of cockles collected from four sites in a commercial cockle-culture area off the coast of West Malaysia were aged. Two of the sites were located in an estuary where the cockles were periodically exposed to fluctuating salinities during the intermonsoon period. Cockles from the other two sites were situated away from the estuary and experienced full strength sea water. There was good agreement between the calculated estimates of the ages determined from the tidal bands and their known ages. Shells of cockles from the estuary had characteristically marked banding patterns which may be related to shell deposition during the intermonsoon period when the cockles were exposed to sea water of low salinity. Cockle shells collected outside the estuary did not display these patterns.

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