Age determination of black bream, Acanthopagrus butcheri (Sparidae), from the Gippsland Lakes of south-eastern Australia indicates slow growth and episodic recruitment

1998 ◽  
Vol 49 (6) ◽  
pp. 491 ◽  
Author(s):  
Alexander K. Morison ◽  
Patrick C. Coutin ◽  
Simon G. Robertson

The age of black bream (Acanthopagrus butcheri) in the Gippsland Lakes of south-eastern Australia was estimated with high precision from sectioned otoliths of fish sampled from 1993 to 1996. Ageing techniques were validated by following the progression of age classes over 4 years. Correct identification of the first increment was aided by reference to the position of the subcupular meshwork fibre zone, and age assignment was confirmed by linear regression analyses of otolith weight against fish age. The growth of black bream was found to be slower, and their natural life span longer, than previously estimated from length–frequency distributions and scale readings. The maximum age recorded was 29 years, with most black bream 4–9 years old and few fish more than 10 years old. There were significant differences between the growth rates of males and females. The von Bertalanffy growth parameters were: L∞ 54.5 cm FL, t0 –5.21 years, K 0.042 year-1 for females and L∞ 38.2 cm FL, t0 –3.70 years, K 0.077 year-1 for males. The current age structure suggests that recruitment has been episodic since 1981 and low for three recent years in succession.

2003 ◽  
Vol 54 (1) ◽  
pp. 57 ◽  
Author(s):  
Kimberley A. Smith ◽  
Kerrie Deguara

The present study used a variety of methods to validate the annual periodicity and to determine the timing of formation of opaque and translucent zones in the sagittal otoliths of sea mullet (Mugil cephalus) from south-eastern Australia. Otoliths of captive juvenile fish were sampled regularly to determine timing of formation of the first opaque zone and ‘marginal increment analysis’ was used to infer timing of formation of subsequent zones. Otoliths of tagged (oxytetracycline injected) and recaptured fish also provided direct observations about the timing and periodicity of otolith zone formation. An ‘increment’ was defined as a translucent zone followed by an opaque zone. The first opaque zone was typically completed in February–March, at an age of 22–23 months. Subsequent opaque zones were completed between November and March, but typically in December. Opaque zones were associated with periods of slow otolith growth during winter and spring. Otoliths of fish aged between 0 and 11 years were examined during the study. Otoliths were sampled from two locations on the south-eastern Australian coast, separated by 5.5° latitude. The transition between opaque and translucent zones appeared more distinct in otoliths from the higher latitude, resulting in greater precision of age estimates at this location. Precision of age estimation was also found to vary with time of year. It is recommended that sampling of otoliths for age determination of Mugil cephalus in south-eastern Australia occur from April to October. Sampling at these times would avoid months in which otolith increments are most difficult to interpret and when the stage of completion of increments is most variable.


2010 ◽  
Vol 61 (11) ◽  
pp. 1243 ◽  
Author(s):  
Eszter Z. Hidas ◽  
David J. Ayre ◽  
Todd E. Minchinton

The abundant-centre hypothesis predicts that species' abundances peak at the centre of their geographical ranges and decline gradually towards their range limits. We tested predictions of this hypothesis for three rocky-shore, intertidal invertebrates with planktonic larvae (the whelk, Morula marginalba, the snail, Afrolittorina pyramidalis, and the barnacle, Tesseropora rosea) by quantifying their patterns of abundance and size, and inferring pulses of recruitment from size-frequency distributions, at multiple spatial scales spanning a 600-km region in south-eastern Australia and encompassing roughly the southern third of their geographical ranges. At the regional scale, abundances for all species were, as predicted, dramatically lower at their range limits. This decline was not gradual, however, because there were large variations in abundance at smaller spatial scales, and abrupt declines at the south-eastern corner of Australia. Size did not change towards the range limit for any species, but size-frequency distributions suggested a decline in the frequency of recruitment events at the range limit for T. rosea. We conclude that the abundant-centre hypothesis is not an appropriate model for abundance distributions of benthic marine invertebrates with planktonic larvae, because of the vagaries of dispersal and recruitment interacting with complex current patterns along non-uniform coastlines.


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