Otolith microstructure was used to characterize growth in five cohorts of larval Herklotsichthys castelnaui from Townsville, north eastern tropical Australia in spring/summer of 1987. Ontogenetic development of larval H. castelnaui is described, and is correlated with changes in otolith microstructure. Development of fin rays coincided with a period of rapid otolith and somatic growth. Otolith increment width and water temperature series were modelled for each cohort using time series analysis. Cross-correlation functions showed no detectable dependencies between increment widths and temperature. Length-at-age relationships were significantly different among cohorts. Repeated-measures analysis of variance was used to establish differences in increment spacing among cohorts. Measurement of otolith radii allowed back-calculation of absolute growth rates of cohorts over the first 30 d of larval life. Significant differences in growth trajectories were detected among cohorts. Data presented here suggest that growth may vary among cohorts separated by as little as 2 wk, and that these differences are detectable by otolith increment analysis.
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Thorrold et al. (1989) studied this question.