785
Abstract–Age compositions and growth
rates have been determined for populations of Acanthopagrus butcheri in four
estuaries and a saline, coastal lake, all
of which differ markedly in their morphological, physicochemical, and biotic
characteristics. Because the opaque
zones in otoliths were shown to form
annually, the number of these zones
could be used to age individual fish.
However, the otoliths of fish that were
more than six years old had to be sectioned in order to consistently reveal
all opaque zones. The number of annuli
on scales did not provide reliable estimates of age. Acanthopagrus butcheri,
which typically completes its life cycle
in estuaries, was represented in each
of the five water bodies by fish ≥15
years old and lengths and weights >365
mm and >860 g, respectively. The maximum length and weight of A. butcheri
recorded in any of the five water bodies
were 485 mm and 2196 g, respectively.
The values for L∞ in von Bertalanffy
growth equations differed significantly
between females and males in three of
the four estuarine populations (P<0.001
or <0.01), whereas those for both k and
t0 differed significantly between the
sexes in only one population and then
only at P < 0.05. The values for k and
L∞ in the von Bertalanffy growth equations differed significantly among both
females and males in the four estuaries
at either P < 0.001 or P < 0.05. These
parameters also differed significantly
between the males in Lake Clifton and
the males in each estuary, except the
Swan River Estuary. Growth rates in
two of the more northern water bodies
were greater than those in the two
southern and cooler estuaries. The pattern of growth in the Moore River Estuary, as reflected by changes in length
with time, differed from that in the
other four water bodies in that it was
initially slower and subsequently did
not show such a marked tendency to
form an asymptote. The slow initial
rate of increase in length in the Moore
River Estuary may be related to particularly high densities of juvenile A.
butcheri in nearshore, shallow water, as
well as to a relatively lower abundance
of appropriate food or very low salinities, or to both of the latter. The percentage contribution made by fish ≥5
years was the lowest by far in the Swan
River Estuary, which was subjected to
the greatest fishing pressure.
Manuscript accepted 22 March 2000.
Fish. Bull. 98:785–799 (2000).
Variation in age compositions and growth rates
of Acanthopagrus butcheri (Sparidae)
among estuaries: some possible contributing factors
Gavin A. Sarre
Ian C. Potter
School of Biological Sciences and Biotechnology
Murdoch University
Western Australia 6150, Australia
E-mail address (for G. A. Sarre): sarre@central.murdoch.edu.au
The black bream, Acanthopagrus butcheri, which completes its life cycle within
estuaries (Potter and Hyndes, 1999;
Sarre and Potter, 1999) is one of the
most important recreational and commercial fish species in the estuaries
of southern Australia (Lenanton and
Potter, 1987; Kailola et al., 1993). The
fact that the genetic compositions of the
populations of this species in the different estuaries of southwestern Australia
vary, suggests that, although some A.
butcheri are occasionally flushed out of
estuaries during those winters when
freshwater discharge is particularly
heavy, the population in an estuary
remains essentially discrete from those
in other estuaries (Chaplin et al., 1998;
Potter and Hyndes, 1999). The confinement of each population of A. butcheri
to its natal environment means that, if
fishing pressure is sufficiently high in
any one estuary, the population in that
estuary cannot be replenished naturally by immigration from outside that
system. Indeed, there is good evidence
that the abundance of this sparid in
the Blackwood River Estuary in southwestern Australia declined markedly
between the 1970s and 1990s as a
result of a combination of commercial
and recreational fishing activities (see
Valesini et al., 1997; Lenanton et al.,
1999; Lenanton1;Valesini2).
The increasing potential for A. butcheri to become overexploited as recreational fishing in estuaries increases
means that it is now important to have
information on the age compositions of
this species in the various estuaries in
order to ascertain whether the older
age classes are becoming excessively
depleted in some of these estuaries.
Such data are dependent on accurate
estimates of the age of fish. In the
past, such estimates for A. butcheri have
typically been based on the number
of annuli on scales (Butcher, 1945;
Thomson, 1957; Weng, 1971; Hobday
and Moran3). However, no attempt was
made in any of these studies to use
traditional methods to validate that
the growth zones (annuli) on that hard
structure are formed annually—a procedure now considered essential in aging
fish (Beamish and McFarlane, 1983).
Although Morison et al. (1998) have
recently used the number of opaque
zones on otoliths as a criterion of age,
their approach to validating that those
zones were formed annually was based
on the observation that the number of
opaque zones on the otoliths of fish in the
two cohorts that were the most strongly
represented in length-frequency data
for four consecutive years increased by
one in each successive year.
Recent work on A. butcheri in southwestern Australia has focused on populations in four estuaries and a landlocked saline, coastal lake, which vary
1
2
3
Lenanton, R. C. J. 1977. Aspects of the
ecology of fish and commercial crustaceans of the Blackwood River Estuary,
Western Australia. Report 19, Department of Fisheries and Wildlife, Perth, Western Australia, Australia, 72 p.
Valesini, F. J. 1995. Characteristics of
the ichthyofaunas of the Blackwood River
Estuary and Flinders Bay. Unpublished
honours thesis, Murdoch University, Perth,
Western Australia, Australia, 67 p.
Hobday, D., and Moran, M. 1983. Age,
growth and fluctuating year class strength
of black bream in the Gippsland Lakes,
Victoria. Report No. 20. Marine Science
Laboratories, Victoria, Australia, 17 p.
786
markedly in their morphological and physicochemical
characteristics and in the composition of their biota (Sarre
et al., 2000). Thus, two of these water bodies are permanently open to the sea, while one is intermittently closed,
another is normally closed, and one is permanently closed.
Furthermore, the regions where A. butcheri spawns in
these estuaries in the spring and early autumn range in
salinity from as low as 3.5–8.0‰ in the intermittently
open estuary to over 40‰ in the normally closed estuary
and, as a result of their location at different latitudes, they
also differ in water temperature (Young et al., 1997; Sarre
and Potter, 1999). The differences in the biota of these systems are reflected in marked differences in the dietary
composition of A. butcheri, with, for example, the overall
contribution made by macrophytes to the volume of stomach contents ranging from as low as 8.3% in one population to as high as 56.4% in another (Sarre et al., 2000).
The aims of our study on A. butcheri were as follows:
1) to validate that the growth (opaque) zones visible on
sectioned otoliths of A. butcheri are formed annually; 2)
to compare the number of growth (opaque) zones in otoliths prior to and after sectioning in order to determine
whether otoliths always have to be sectioned to reveal
each of their opaque zones; 3) to ascertain whether the
number of annuli on scales corresponds to the number of
opaque zones on sectioned otoliths and can thus likewise
be used for aging this species; 4) to determine the age composition of A. butcheri in the above four estuaries and the
saline, coastal lake, in which the fishing pressure on black
bream varies from zero to substantial, and thereby ascertain whether there is evidence that heavy exploitation of
this species can markedly reduce the proportion of older
fish; and 5) to determine the extent to which the growth
rates and length at age of A. butcheri differ amongst populations in the above five water bodies, which vary markedly in their abiotic and biotic characteristics and amongst
which the dietary compositions of A. butcheri are significantly different.
Materials and methods
Acanthopagrus butcheri was collected from the permanently
open Swan River and intermittently open Moore River
estuaries on the lower west coast of Australia (31–32°S)
and from the permanently open Nornalup Walpole and normally closed Wellstead estuaries (34–35°S) on the southern
coast of Western Australia (see Fig. 1 for locations of these
estuaries). Acanthopagrus butcheri was also collected from
Lake Clifton, a landlocked saline, coastal lake. Because
the Department of Conservation and Land Management
(CALM) restricted the number of A. butcheri that could be
collected from this lake to 100, and because 85 of these 100
fish were males, emphasis was placed on the data obtained
for this sex in this lacustrine environment.
Fish in estuaries were collected from over sand in nearshore, shallow waters (<1.5 m depth) by using a 41-m
seine net with 9-mm mesh in the codend and from offshore, deeper waters (2–5 m depth) by employing composite sunken gill nets containing eight 20 m long × 2 m high
Fishery Bulletin 98(4)
panels, each of which had a different mesh size, i.e. 38, 51,
63, 76, 89, 102, 115, or 127 mm. Sampling in the Swan
River Estuary commenced in September 1993 and was carried out monthly until April 1995 with seine netting and
monthly until February 1995 with gill netting. The same
methods were used to sample A. butcheri in the Moore
River, Nornalup Walpole, and Wellstead estuaries between
the spring of 1993 and the summer of 1996–97 (December–
January). Sampling in the Swan River, Nornalup Walpole,
and Wellstead estuaries was carried out in the saline lower
reaches of the tributary rivers, i.e. upper estuary (Fig. 1),
which, for most of the year, contain the majority of the A.
butcheri found in those estuaries (Sarre and Potter, 1999).
In contrast, sampling was undertaken throughout the short
Moore River Estuary, which does not possess the large central basins that are found in the other three estuaries (Fig.
1). The catches obtained by seine and gill netting in the
above four estuaries were supplemented by up to a further
7% by fish obtained with rod and line. A fine mesh seine
net, which was 5.5 m long and consisted of 1-mm mesh, was
used to collect small A. butcheri from extensive beds of the
macroalgae Gracilaria verrucosa in the downstream and
middle regions of the upper Swan River Estuary between
December 1998 and March 1999. (See “Results” section for
the reason for this additional sampling). The sample of 100
A. butcheri collected from Lake Clifton in November 1996
was obtained exclusively by rod and line, in accordance
with the conditions laid down by CALM.
Both of the sagittal otoliths were removed from each
fish sampled from the four estuaries and Lake Clifton and
these otoliths were immersed in methyl salicylate solution. For sectioning, otoliths were mounted and embedded
in clear epoxy resin and cut into ca 0.5-mm transverse
sections with an Isomet low-speed diamond saw. Sections
were ground on sequentially finer grades of carborundum
paper (400–1200 grade) and mounted on glass slides with
DePX mounting adhesive. Whole otoliths and sectioned
otoliths were placed on a black surface and examined
microscopically under reflected light.
Measurements were made of the distance between the
outer edge of the outermost opaque zone and the periphery
of the otolith in the case of the otoliths that were to be used
for aging fish in the Swan River Estuary. This distance, i.e.
the marginal increment, was then expressed either as a
proportion of the distance between the primordium of the
otolith and the outer edge of the opaque zone, when only
one opaque zone was present, or as a proportion of the distance between the outer edge of the two outermost opaque
zones, when two or more opaque zones were present. All
measurements were recorded to the nearest 0.05 mm. As
with other sparids, a narrow opaque zone is laid down in
the otoliths of A. butcheri during the cool (winter) period
and a wide translucent zone is deposited during the warm
(summer) period (Johnson, 1983; Buxton and Clarke, 1991;
Francis et al., 1992; Booth and Buxton, 1997).
Otoliths from 239 A. butcheri, collected from the Swan
River Estuary and covering a wide size range, were used
for comparing the number of narrow, opaque zones that
could be seen on this hard structure before and after sectioning. The number of opaque zones visible in a subsam-
Sarre and Potter: Variation in age compositions and growth rates of Acanthopagrus butcheri
787
Indian
Ocean
Southern Ocean
Figure 1
Map showing the location of the four estuaries and Lake Clifton in southwestern Australia from which samples
of Acanthopagrus butcheri were collected, together with individual maps of each estuary. The shaded area of the
Swan River Estuary represents the region sampled in our study.
ple of 126 of the sectioned otoliths were then compared
with the numbers of annuli on scales removed from the
same fish. The scales used for these comparisons, which
were obtained from above the lateral line and directly
behind the operculum, were mounted between glass slides
and examined microscopically under reflected light.
788
Fishery Bulletin 98(4)
The number of opaque zones in the whole and sectioned
otoliths of a subsample of 162 of the above 239 fish and the
number of annuli on the scales of a random subsample of
87 of those fish were also counted by a second reader to
determine the level of reproducibility of the counts made
of the growth zones on these hard structures by the senior
author.
The birth date assigned to A. butcheri in each water body
corresponds to peak spawning activity, as estimated from
the trends exhibited by gonadosomatic indices, stages in
gonadal development and pattern of oocyte development
(Sarre and Potter, 1999). Von Bertalanffy growth curves
were fitted to the individual lengths of female and male fish
at their estimated ages at capture by a nonlinear technique
(Gallucci and Quinn, 1979) by using a nonlinear subroutine
in SPSS (SPSS Inc., 1988). The von Bertalanffy equation is
[
]
Lt = L∞ 1 − e− k( t − t ) ,
0
where Lt = the total length at age t (years);
L∞ = the mean of the asymptote predicted by the
equation;
k = the growth coefficient; and
t0 = the hypothetical age at which fish would have
zero length, if growth followed that predicted
by the equation.
The lengths at age of fish whose sex could not be determined under a dissecting microscope were selected at
random and placed alternately in the data sets for female
and male fish.
Each of the growth parameter estimates for female and
male fish in the same estuary and for each sex in the four
estuaries were compared by using a likelihood ratio test
(see Kimura, 1980). Comparisons were also made between
the growth parameters for the males of A. butcheri in Lake
Clifton, the sex which dominated the catches in that lake,
and those of the males of this species in the four estuaries.
The likelihood ratio for the null hypothesis (Kimura,
1980) tests the null hypothesis against the alternative
hypothesis where
Hw states that the parameters L∞, k ,and t0 satisfy some
set of r linear constraints;
HΩ states that the parameters L∞, k, and t0 possibly
satisfy no linear constraints.
The maximum likelihood estimates of the error variances σ̂ 2w and σ̂ 2Ω(r) are given by the sum of squares of
residuals from the iteratively reweighted least squares
procedure used to fit L∞, k, and t0 subject to r linear constraints.
The likelihood ratio test statistic, as described by Cerrato (1990), for two data sets with sample sizes n1 and n2
is given by
–2log(Λ),
where
σˆ 2
Λ = 12ω
σˆ 1Ω
− n1 / 2
σˆ 22ω
σˆ 2
2Ω
− n2 / 2
.
Table 1
The linear constraints and degrees of freedom of each
hypothesis, based on Kimura (1980), where M and F represent males and females, respectively.
Hypothesis
HΩ
Hω 1
Hω 2
Hω β
Linear constraints
Degrees of freedom
none
L∞M = L∞F
kM = kF
t0M = t0F
1
1
1
Under the null hypothesis –2 log(Λ) converges to a χ2(r)
distribution with the degrees of freedom equal to the
number of equations required to specify the linear constraints applied to the model (Kimura, 1980). The null
hypothesis is rejected at the α level of significance when
–2log(Λ) > χ2(r).
The types of linear constraints applied to the von Bertalanffy growth equation, the null and alternative hypotheses associated with each constraint and the degrees of
freedom of the test statistic are given in Table 1.
Results
Validation of annual deposition of opaque zones
in otoliths
The mean monthly marginal increment on sectioned otoliths with one opaque zone declined sharply from 0.57 in
September and October 1993 to 0.11 in November 1993,
before gradually rising to a maximum of 0.93 in October
1994 (Fig. 2). As in 1993, the mean marginal increment
then declined markedly between October and November
1994 and subsequently rose over the ensuing months. The
trends exhibited by the mean monthly marginal increment on otoliths with two and three opaque zones were
the same as those just described for otoliths with one
opaque zone (Fig. 2). Because the number of fish with
otoliths displaying four or more opaque zones in the samples for some months was small, the marginal increments
for all such otoliths in each month were pooled. Although
the trends shown by the mean monthly marginal increments on these otoliths were not quite as “smooth” as
those shown by otoliths with one to three opaque zones,
they still clearly declined precipitously in November of
both 1993 and 1994 and subsequently rose progressively
during the ensuing months between early summer and
mid-autumn (Fig. 2).
The fact that, irrespective of the number of opaque zones
on otoliths, the mean monthly marginal increments on
otoliths underwent a pronounced decline and then a progressive rise only once during the year demonstrates that
a single opaque zone is formed in otoliths each year. Thus,
the number of opaque zones in sectioned otoliths can be
used to determine the age of A. butcheri.
Sarre and Potter: Variation in age compositions and growth rates of Acanthopagrus butcheri
1 opaque zone
Marginal increment
2 opaque zones
3 opaque zones
≥ 4 opaque zones
Month
Figure 2
Mean monthly marginal increments ±1SE for sectioned sagittal otoliths of Acanthopagrus butcheri in
the upper Swan River Estuary. The mean marginal
increment is expressed as a proportion of the distance between the primordium and the edge of the
opaque zone, when only one such zone was present,
and as a proportion of the distance between the outer
edges of the two outermost opaque zones, when two
or more such zones were present. Sample sizes are
given for each month.
Number of growth zones on hard structures
The number of opaque zones detected on a sectioned otolith
of A. butcheri was always the same as the number observed
on the same otolith prior to sectioning, when six or less
such zones were visible on the whole otolith (Fig. 3A). However, the use of whole otoliths would have underestimated
by one year 15% of seven- and eight-year-old fish, collectively, and, by one or two years, 57% of nine- to 13-year-old
fish, collectively. The use of whole otoliths would also have
789
underestimated the age of two 14-year-old fish by three
years, two 15-year-old fish by two years, and one 19- and
one 21-year-old fish by five years each (Fig. 3A).
The numbers of annuli observed on the scales of A.
butcheri differed from those recorded in 27, 67, and 40%
of the sectioned sagittal otoliths of the same fish, when
the otoliths possessed one, two, and three opaque zones,
respectively (Fig. 3B). The number of annuli exceeded that
of the number of opaque zones in 34% of all cases. The
number of annuli on the scales of fish, in which the sectioned otoliths possessed eight to eleven opaque zones,
exceeded by one or two the number of opaque zones on
those otoliths in 70% of cases (Fig. 3B). On the basis of the
number of opaque zones on their sectioned otoliths, one
fish that was estimated as 19 and another as 21 years old,
displayed seven more annuli on their scales than on their
otoliths. Although the number of sectioned otoliths with
more than six opaque zones, that were used for comparisons with scales, was only 18, it is still noteworthy that
the number of opaque zones on more than half of those
otoliths was less than the number of circuli on the scales
obtained from the corresponding fish.
The number of opaque zones recorded independently
by a second “reader” for sectioned otoliths of A. butcheri
with 0–3 zones (50 fish), 4–6 zones (50 fish) and 7–10
zones (40 fish), were always the same as those recorded
by the senior author for the same otoliths. Furthermore,
the second reader recorded the same number of opaque
zones on all but two of the 22 sectioned otoliths that the
senior author had recorded as having 11 or more opaque
zones. Moreover, after reviewing and discussing the two
discrepancies, the second reader agreed that he had failed
to detect one of the least conspicuous opaque zones near
the periphery of the two otoliths for which there were
discrepancies, and therefore his counts agreed with the
counts made by the senior author. However, the number of
annuli counted on the scales by the second reader, that had
previously been recorded by the senior author as having
0–3 annuli (50 fish), 4–10 annuli (30 fish), and ≥11 annuli
(7 fish), differed in 20%, 43%, and 86% of cases, respectively, which reflects the difficulty in detecting annuli on
scales. The differences between counts ranged from one on
scales with 0–3 annuli to more than five on scales with ≥11
annuli.
Trends exhibited by length-frequency data for
different age classes
The data presented earlier demonstrated that the number
of opaque zones on whole otoliths of A. butcheri could be
used for aging this sparid when there were six or less
opaque zones present (Fig. 3A). However, the data in Fig.
3A showed that otoliths had to be sectioned to consistently
reveal all of their opaque zones when they displayed seven
or more such zones prior to sectioning. Thus, to reduce the
margin for producing invalid counts to a minimum, estimates of the age of individual A. butcheri were made by
using whole otoliths, when five or less opaque zones were
present, and by employing sectioned otoliths, when six or
more such zones were present.
Fishery Bulletin 98(4)
.
.
790
Figure 3
Comparisons between (A) the numbers of opaque zones on whole and sectioned
otoliths and (B) the numbers of annuli on scales and the numbers of opaque
zones on sectioned otoliths of Acanthopagrus butcheri from the Swan River
Estuary.
Although seine netting over sand in nearshore, shallow
waters of the upper Swan River Estuary in the summer and
early autumn of both 1993–94 and 1994–95 yielded many A.
butcheri of 50 to 180 mm, it produced only a few smaller individuals of this species. However, sampling of beds of the macroalgae Gracilaria verrucosa in the same period in 1998–99
yielded considerable numbers of A. butcheri that ranged in
length from 16 to 60 mm. Once A. butcheri reached lengths
of ca. 60 mm, they moved from the beds of G. verrucosa to
reside over sand. The lengths of these A. butcheri, which
represented the 0+ recruits resulting from spawning from
November to December of 1998 (Sarre and Potter, 1999), and
thus represented the 1998 year class, increased from 16–32
mm in December 1998 to 26–63 mm in January 1999 to
44–86 mm in February 1999 and to 36–112 mm in March
1999 (Fig. 4). The mean length ±1SE in the latter month, i.e.
76 mm, did not differ significantly (P>0.05) from that of the
0+ age class in March 1994, when a substantial number of
these small fish were also caught (Fig. 5).
Because A. butcheri spawns predominantly between
October and January (spawning peaking in November
[Sarre and Potter, 1999]), the cohort of small A. butcheri
(81–115 mm), that was caught by seine net in the shallow
waters of the Swan Estuary in September 1993 and whose
otoliths did not possess an opaque zone, was the product
of the spawning that took place in the spring to early
summer of the previous year, i.e. 1992 (Fig. 5). The lengths
of this 1992 year class increased from 81–115 mm in
September 1993 to 100–152 mm in November 1993, by
which time a single and narrow opaque zone could be
discerned on the edge of the otoliths of this year class.
Because spawning peaks in November, the members of
this cohort were thus now about one year old. By November and December 1994, the lengths of this 1992 year
class, now representing early 2+ fish, had increased to
170–220 and 189–224 mm, respectively. The 1993 year
class first appeared in seine net catches in March 1994 at
lengths of 67–102 mm and was caught until May, when its
Sarre and Potter: Variation in age compositions and growth rates of Acanthopagrus butcheri
791
Maximum size and age and von Bertalanffy growth
parameters
Figure 4
Length-frequency histograms for juvenile Acanthopagrus butcheri caught with a 5.5-m seine net
(1-mm mesh) in the shallows (<1 m) of the upper
Swan River Estuary between December 1998 and
March 1999. Numbers in parentheses represent the
number of fish measured.
lengths had reached 104–139 mm. When representatives
of the 1993 year class reappeared in catches in September
1994, their lengths were still only 96–135 mm, indicating
that growth had not occurred during the immediately preceding winter months. The lengths of the 1993 year class
subsequently increased to between 136 and 183 mm in
January 1995 (Fig. 5). Although the 1994 year class first
appeared in March 1995, i.e. in the corresponding month
to when the 1993 year class appeared in the previous year,
its numbers were small and it was not represented in the
following month, i.e. April (Fig. 5).
The 1991 year class was well represented in the majority of months (Fig. 5). The lengths of this strong cohort
increased from 163–235 mm in September 1993 to 220–296
mm in September 1994 and to 222–325 mm in November
1994, at which time the fish were entering their fourth
year of life. The 1990 year class was a particularly strong
cohort (Fig. 5). The lengths of this year class increased
from 208–304 mm in September 1993 to 268–349 mm in
September 1994 and 259–360 mm at the commencement
of their fifth year of life in November. The numbers of fish
belonging to earlier year classes, i.e. the 1989, 1988, 1987
year classes, etc., were very low (Fig. 5). Thus, the number
of older fish collectively in the Swan River Estuary was
also low.
The spawning activity of A. butcheri peaked in early
November in the Swan River, Moore River, and Nornalup
Walpole estuaries and in early October in the Wellstead
Estuary (Sarre and Potter, 1999). The von Bertalanffy
growth curves for A. butcheri were thus derived by using a
birth date of 1 November for the first three estuaries and
1 October for the Wellstead Estuary. Because many fully
mature fish were found in Lake Clifton in early November,
and this lake was located near the Swan River Estuary,
a birth date of 1 November was likewise assigned to the
population of A. butcheri in that system.
The lowest maximum lengths of female and male A.
butcheri were 377 and 365 mm, respectively, which were
recorded for fish caught in the Wellstead Estuary, whereas
the greatest maximum lengths of each sex was 480 mm
recorded for a female in the Swan River Estuary and
485 mm recorded for a male in Lake Clifton (Table 2).
The maximum weights of A. butcheri in the five systems
ranged from a low of 862 g for a female in the Wellstead
Estuary to 2196 g for a female in the Swan River Estuary
(Table 2). The maximum age of both sexes in each estuary
was at least 15 years and the maximum age attained in
any system was the 21 years recorded for both a female in
the Swan River Estuary and a male in the Nornalup Walpole Estuary (Table 2).
The growth curves of male A. butcheri in the Swan River,
Nornalup Walpole, and Wellstead estuaries and Lake Clifton followed similar overall trends and thus never crossed
one another, and the same was true for the growth curves
for females in the above three estuaries (Figs. 6 and 7).
The rates of increase in the lengths of both sexes in the
Moore River Estuary were initially slower than in each of
the above three estuaries, and the rate of increase in the
length of males in the Moore River Estuary was also initially less than that of this sex in Lake Clifton. (Note that
there were insufficient data for the females in Lake Clifton
to make similar comparisons with this sex in this system.)
The far slower rate at which length initially increased in
the Moore River Estuary is illustrated by the fact that,
when male fish were 35–37 months old, i.e. three years
in age, their mean length in this estuary was only 151
mm and significantly lower (P<0.001) than the 272 mm
in the Swan River Estuary, 162 mm in the Nornalup Walpole Estuary, 204 mm in the Wellstead Estuary, and 339
mm in Lake Clifton. Likewise, the mean length of females
of A. butcheri in the Moore River Estuary at this age was
only 144 mm and thus significantly lower than the 285,
161, and 212 mm recorded in the Swan, Nornalup Walpole,
and Wellstead estuaries, respectively. It is also noteworthy that the above-mean lengths of males in each of the
five systems were significantly different from each other
in all cases, except for A. butcheri from the Nornalup Walpole and Wellstead estuaries. Corresponding results were
obtained for females in the four estuaries. As A. butcheri
in the Moore River Estuary reached an older age, the
growth curves for males and females in this estuary then
crossed those for fish from the Nornalup Walpole and Well-
Fishery Bulletin 98(4)
Number of fish
792
Total length (mm)
Figure 5
Length-frequency histograms for the different year classes of Acanthopagrus butcheri, with
data derived from samples of males and females collectively that were caught with seine and
gill nets in the upper Swan River Estuary between September 1993 and April 1995. Sample
sizes in each month are given for seine netting (SN), gill netting (GN) and rod and line (RL)
and in parenthesis for the total sample.
stead estuaries. This feature was reflected in significantly
greater asymptotic lengths and lower k values for the
Moore River Estuary population than those derived for
fish in the latter two estuaries (Table 2, Figs. 6 and 7).
The likelihood ratio test demonstrated that neither the
ages at length zero (t0) nor the growth coefficients (k)
in the von Bertalanffy growth equations differed significantly between female and male A. butcheri in either the
Sarre and Potter: Variation in age compositions and growth rates of Acanthopagrus butcheri
793
Table 2
Von Bertalanffy growth parameters and confidence intervals (95%) derived from length-at-age data for female and male Acanthopagrus butcheri caught in the Swan River, Moore River, Nornalup Walpole and Wellstead estuaries and for the males in Lake
Clifton. n is sample size and Lmax, Wmax, and Amax are the maximum lengths (mm), weights (g), and ages, respectively. t0 is the
hypothetical age at which fish would have zero length, k is the growth coefficient, L∞ is the asymptotic length and r2 is the coefficient of determination.
von Bertalanffy parameters
Swan River
Females
95% CL (lower)
95% CL (upper)
Males
95% CL (lower)
95% CL (upper)
Moore River
Females
95% CL (lower)
95% CL (upper)
Males
95% CL (lower)
95% CL (upper)
Nornalup Walpole
Females
95% CL (lower)
95% CL (upper)
Males
95% CL (lower)
95% CL (upper)
Wellstead
Females
95% CL (lower)
95% CL (upper)
Males
95% CL (lower)
95% CL (upper)
Lake Clifton
Males
95% CL (lower)
95% CL (upper)
n
Lmax
Wmax
Amax
t0
k
L∞
733
480
2196
21
894
475
1780
15
–0.13
–0.17
–0.10
–0.15
–0.19
–0.11
0.30
0.28
0.31
0.31
0.29
0.32
437.8
426.0
449.5
419.3
10.7
427.9
345
403
1192
17
387
394
1162
18
–0.54
–0.68
–0.41
–0.61
–0.76
–0.46
0.11
0.09
0.12
0.11
0.09
0.12
451.6
416.3
486.9
429.2
395.9
462.6
346
412
1250
17
265
409
1148
21
–0.60
–0.88
–0.43
–0.31
–0.54
–0.08
0.16
0.14
0.18
0.21
0.19
0.24
367.0
352.5
381.6
323.0
311.8
334.6
324
377
862
15
331
365
1247
15
–0.17
–0.27
–0.07
–0.18
–0.28
–0.08
0.25
0.23
0.27
0.27
0.25
0.29
377.8
365.3
390.3
344.6
335.8
353.4
85
485
1914
18
–0.46
–0.66
–0.26
0.32
0.28
0.36
441.5
453.4
429.6
Swan River, Moore River or Wellstead estuaries (Table 3).
Furthermore, although these two growth parameters did
differ significantly between the two sexes in the Nornalup Walpole Estuary, the probability levels in both cases
were close to 0.05. However, the asymptotic length (L∞) for
female fish was significantly greater than that of male fish
in each estuary except that of the Moore River (Table 3).
The values for k and L∞ for each sex differed significantly among the populations of A. butcheri in the four
estuaries and between those of males in each of these
r2
0.94
0.94
0.93
0.92
0.91
0.90
0.91
0.92
0.96
estuaries and Lake Clifton (P<0.001 or 0.01). Furthermore, the values for t0 for each sex almost invariably
differed significantly (P<0.001 or <0.05) among the populations in the four estuaries and between those of males
in each of these estuaries and Lake Clifton. Because the
three von Bertalanffy parameters for both sexes were each
shown almost invariably to differ significantly among
the different populations, no attempt was made to test
whether there was a common pattern of growth for each
sex in each system.
794
Fishery Bulletin 98(4)
Figure 6
Von Bertalanffy growth curves fitted to length at age data for female and
male Acanthopagrus butcheri caught in the Swan River, Moore River, Nornalup Walpole and Wellstead estuaries.
The values for k for A. butcheri were least in the Moore
River Estuary, i.e. 0.11, and greatest in Lake Clifton, i.e.
0.32 (Table 2). The values for L∞ ranged from a low of
367.0 mm for females and 323.0 mm for males in the Nornalup Walpole Estuary to a high of 451.6 and 441.5 mm
for the corresponding sexes in the Moore River Estuary
and Lake Clifton, respectively (Table 2). Estimates of t0 for
both sexes of A. butcheri in the four estuaries and of the
males of A. butcheri in Lake Clifton all lay within the relatively narrow range of –0.13 to –0.61 years (Table 2).
Length–weight relationships
The equations relating total length and weight of female and
male A. butcheri in each estuary and for males in Lake Clifton are presented below, so that, when required, the approxi-
Sarre and Potter: Variation in age compositions and growth rates of Acanthopagrus butcheri
mate weights of fish of a particular length can be estimated.
Becasue analysis of covariance (ANCOVA) showed that neither the slopes nor the y-intercepts in the equations for
795
female and male fish in each estuary differed significantly
(P>0.05), the equations relating total length and weight for
both sexes combined in each estuary are also presented.
Swan River Estuary
Females:
Males:
Pooled:
log10 W = –5.09 + 3.14 log10 L
log10 W = –5.10 + 3.14 log10 L
log10 W = –5.07 + 3.14 log10 L
(r2=0.99, n=865).
(r2=0.99, n=925).
(r2=0.99, n=1790).
Moore River Estuary
Females:
Males:
Pooled:
log10 W = –5.10 + 3.13 log10 L
log10 W = –5.14 + 3.15 log10 L
log10 W = –5.12 + 3.13 log10 L
(r2=0.99, n=250).
(r2=0.99, n=287).
(r2=0.99, n=537).
Nornalup Walpole Estuary
Females:
Males:
Pooled:
log10 W = –4.99 + 3.07 log10 L
log10 W = –5.03 + 3.09 log10 L
log10 W = –5.00 + 3.08 log10 L
(r2=0.99, n=302).
(r2=0.99, n=234).
(r2=0.99, n=536).
Wellstead Estuary
Females:
Males:
Pooled:
log10 W = –4.84 + 3.01 log10 L
log10 W = –4.89 + 3.03 log10 L
log10 W = –4.85 + 3.02 log10 L
(r2=0.99, n=274).
(r2=0.99, n=278).
(r2=0.99, n=552).
Lake Clifton
Males:
Pooled:
log10 W = –5.12 + 3.14 log10 L
log10 W = –5.10 + 3.13 log10 L
(r2 =0.98, n=85).
(r2=0.99, n=100).
Discussion
Table 3
Validation of the method for aging
Acanthopagrus butcheri
Our study shows that a growth zone is not laid down in the
otoliths of the 0+ age class of Acanthopagrus butcheri until
winter and that this growth zone does not become clearly
delineated until late spring. Because spawning peaks in
early November in the Swan Estuary (Sarre and Potter,
1999), the first growth zone becomes delineated as the
individuals of this species become one year old. Furthermore, the trends exhibited by the marginal increments on
the sectioned otoliths of A. butcheri demonstrate that an
opaque zone is laid down annually in this hard structure.
Our results also demonstrate that the otoliths of A. butcheri do not need to be sectioned in order to consistently
reveal all of the opaque zones until they had reached a size
at which they possessed seven or more such zones. Validation that the opaque zones, which are revealed on the
otoliths of A. butcheri by sectioning, are formed annually,
implies that the estimates of the ages of individual black
bream recorded by Morison et al. (1998) using sectioned
otoliths are valid for fish caught in the Gippsland Lakes in
eastern Australia. However, because the number of annuli
on scales frequently differed from the number of opaque
zones on sectioned otoliths from the same fish, the number
of annuli on scales do not provide a reliable method for
aging A. butcheri. Thus, those estimates of the age of individual A. butcheri, that have been based on the number
Significance levels for comparisons between the von Bertalanffy growth parameters for female and male Acanthopagrus butcheri caught in each of the Swan River,
Moore River, Nornalup Walpole, and Wellstead estuaries
by using the likelihood ratio test. ***=P<0.001, **=P<0.01,
*=P<0.05, NS = Not significant. t0 is the hypothetical age
at which fish would have zero length, k is the growth coefficient, and L∞ is the asymptotic length.
von Bertalanffy growth parameter
Estuary
Swan
Moore
Nornalup Walpole
Wellstead
t0
k
L∞
NS
NS
*
NS
NS
NS
*
NS
**
NS
***
***
of annuli on scales (Butcher, 1945; Thomson, 1957; Weng,
1971; Hobday and Moran3) are, in many cases, probably
invalid.
Differences in age structures amongst populations
Because the majority of A. butcheri obtained from the
Swan River, Moore River, Nornalup Walpole, and Wellstead estuaries were collected by using the same seine and
796
Fishery Bulletin 98(4)
gill net sampling regimes, supplemented with a limited
amount of angling, any gross differences in the age structure of samples from populations in the different estuaries
almost certainly represent real differences. The percentage
of A. butcheri caught at ≥5 years of age in the Swan River
Estuary (5%) was far lower than in either the Moore River
Estuary (30%), approximately 100 km farther north on the
lower west coast of Australia, or the Nornalup Walpole
Estuary (45%) on the south coast of Australia. Note that
the estimate for the Swan River Estuary was restricted
to data collected during the main sampling period and
did not thus include the large samples of small fish that
were caught between December 1998 and March 1999.
The above differences in the proportion of older fish presumably reflect a greater “mortality” of older fish in the
Swan River Estuary than in the other estuaries. It thus
appears highly relevant that the population of A. butcheri
in the Swan River Estuary is exposed to heavy fishing
pressure from the recreational sector throughout the year
and from commercial fishermen during winter and early
spring, whereas the population in the Moore River Estuary is lightly fished and that in the Nornalup Walpole
Estuary is not exposed to commercial fishing (Sarre and
Potter, 1999).
Although representatives of all age classes up to 15+
were recorded for the populations of A. butcheri in each
of the above three estuaries, this was not the case with
the Wellstead Estuary, which is located 300 km to the east
of the Nornalup Walpole Estuary. Thus, in the samples
collected from this estuary in 1995 and 1996, the 1989,
1987, 1986, 1985, and 1984 year classes were not represented, and the 1988 year class was represented by only
two fish (Fig. 6). This strong implication that,
in the Wellstead Estuary, A. butcheri either does
not spawn or has very limited spawning success
in some years parallels the situation recorded
for this species in the Gippsland Lakes in eastern Australia (Morison et al., 1998; Hobday and
Moran3; Coutin et al.4). The work of Morison
et al. (1998) demonstrated that, in that latter
estuary, the commercial catches of A. butcheri
between 1993 and 1996 were dominated by
two year classes and that there had been no
strong recruitment of A. butcheri since 1989.
The absence or weakness of certain year classes
in the Gippsland Lakes, and also in the Hopkins
River Estuary which is also in eastern Australia, has been attributed to the detrimental
influence on spawning success of such unfavourable environmental conditions as heavy freshwater discharge or unsuitable salinities (Newton,
1996; Hobday and Moran3). Thus, in the context
of the absence of the 1984 year class in samples, it appears relevant that, in the Wellstead
Estuary, which has normally remained closed
during the last 30 years, there was, as a result
of “cyclonic rainfall,” an extremely protracted
period of heavy freshwater discharge between
the early spring of 1984 and the autumn of 1985
(Hodgkin and Clark5). This led to a very severe
scouring of the substrate and a breaching of the
bar at the mouth of this estuary, with the result
that this mouth remained open between September 1984 and May 1985. The heavy freshwater
discharge that occurred during and immediately
after the 1985 spawning season of A. butcheri
in the Wellstead Estuary would thus almost cer4
Figure 7
Comparisons between von Bertalanffy growth curves fitted to lengthat-age data for female and male Acanthopagrus butcheri in the Swan
River, Moore River, Nornalup Walpole, and Wellstead estuaries and for
males in Lake Clifton in southwestern Australia.
5
Coutin, P., S. Walker, and A. Morison. 1997.
Black bream—1996. Compiled by the Bay & Inlet
Fisheries and Stock Assessment Group. Fisheries
Victoria Assessment Report 14. Melbourne, Victoria,
Australia, 89 p.
Hodgkin, E. P., and R. Clark. 1987. Wellstead
Estuary, the estuary of the Bremer River. Estuarine
Study Series 1. Environmental Protection Authority,
Perth, Western Australia, 22 p.
Sarre and Potter: Variation in age compositions and growth rates of Acanthopagrus butcheri
tainly have flushed out to sea any eggs or larvae of this
species that were produced during that period. However, it
should also be recognized that freshwater discharge was so
strong during that period that even many large A. butcheri
were flushed out of the estuary, with the result that some
of these fish were subsequently caught by anglers along
the nearby coast (Spurr6). Furthermore, when freshwater
discharge is very high, the salinities fall to such low levels
that they are unlikely to be conducive to spawning by A.
butcheri (Haddy and Pankhurst, 2000). Thus, the absence
of the 1984 year class in samples may be due to the loss of
eggs, larvae, or maturing and mature fish to the ocean in
1984, or to the inhibitory effect of low salinities on spawning, or to a combination of the latter.
The fact that the 1985 year class of A. butcheri was also
not caught may reflect a low return of large A. butcheri to
the estuary by the commencement of the spawning period in
1985. The absence of the 1986, 1987, and 1989 year classes
and the paucity of the 1988 year class can probably be
attributed to the fact that, although freshwater discharge
was not as strong as in 1984, it was still sufficient to breach
the bar at the estuary mouth during the spawning period in
each of those years (Spurr6). It would thus also have been
likely to result in a loss to the ocean of eggs and larvae produced during the spawning periods in those years or to the
emigration of maturing or mature fish, or in both of these
effects (Hodgkin and Clark5). The view that heavy freshwater flushing or very low salinities, or both, were the main
contributors to the lack of spawning success of A. butcheri
between 1984 and 1989 is consistent with the observation
that, when freshwater discharge was not sufficiently strong
to breach the estuary mouth, as was the case between 1990
and 1995 (Spurr6), there was at least a reasonable recruitment of each of the 1990 to 1995 year classes.
Comparisons between von Bertalanffy growth
parameters for females and males
The likelihood ratio test showed that the growth coefficients (k) for female and male fish were significantly different in only one of the four estuaries, i.e. the Nornalup
Walpole Estuary, and even then the probability level was
close to 0.05, which is consistent with the fact that the
values for the 95% confidence intervals for this parameter
for the two sexes overlap in each estuary other than the
Nornalup Walpole Estuary. The lack of a marked distinction between the growth rates of female and male
fish is hardly surprising because A. butcheri undergoes a
substantial amount of growth before the gonads start to
become mature for the first time (Sarre and Potter, 1999).
However, the maximum length and asymptotic length (L∞)
were always greater for female than male fish in each of
the four estuaries, thereby paralleling the situation with
many other fish species in both southwestern Australia
(Laurenson et al., 1994; Wise et al., 1994; Hyndes et al.,
1996; 1998) and elsewhere (e.g. Kenchington and Augustine, 1987; McPherson, 1992; Crabtree et al., 1995).
6
Spurr, P. 1995. Local resident and former commercial fisherman. Personal commun. Bremer Bay, Western Australia.
797
The relatively low values determined for age at length
zero for the two sexes in the four estuaries and for males
in Lake Clifton, i.e. –0.13 to –0.61 years, reflects in part
the good fit of the growth curves to the points for the age
at length of the small fish. These low values for t0 contrast
with the –5.21 years for females and –3.70 years for males
that were calculated by Morison et al. (1998) for A. butcheri in the Gippsland Lakes. Furthermore, the fork lengths
at age zero for female and male fish in the Gippsland
Lakes were ca. 110 and 100 mm, respectively. Thus, the
von Bertalanffy growth equations recorded for A. butcheri
in the Gippsland Lakes do not provide a good description
of the pattern of growth throughout the full size range of
fish.
Variations in von Bertalanffy growth parameters
among populations
Although the patterns of growth of female and male A.
butcheri in the Swan River, Wellstead, and Nornalup Walpole estuaries followed the same overall trends, with length
increasing rapidly with time initially and then forming
asymptotes, the values for k and L∞ for each sex varied
significantly amongst the populations in those estuaries.
The initial rate of increase in length in these three estuaries was greatest in the Swan River Estuary and least in
the Nornalup Walpole Estuary. Although the value for k
for male A. butcheri in Lake Clifton differed significantly
from that of this sex in the Swan River Estuary, the same
was not true for L∞. However, the value for L∞ for male A.
butcheri in Lake Clifton was still similar to that of this sex
in the Swan River Estuary. The above comparisons demonstrate that the growth rate in Lake Clifton was similar
to that in the Swan River Estuary, which is located only
ca. 90 km farther to the north (see also Fig. 1). The von
Bertalanffy growth parameters demonstrated that male A.
butcheri grew more rapidly and attained greater asymptotic lengths in the Swan River Estuary and Lake Clifton
than in either the Wellstead or Nornalup Walpole estuaries. The presence of faster growth rates in the Swan River
Estuary and Lake Clifton, which are located at latitudes
of ca. 32° on the lower west coast of Australia, than in the
Nornalup Walpole and Wellstead estuaries, which are situated much farther south at a latitude of ca. 34° on the
south coast of Western Australia, may reflect the greater
temperatures found in more northern regions.
The pattern of growth of A. butcheri in the Moore River
Estuary differed from those of this species in each of the
other three estuaries and Lake Clifton, in that the increase
in length with time was initially slower and the growth
curve did not exhibit a marked asymptote. This pattern
suggests that some factor or factors were less than optimal for growth during the first few years of life, but that
conditions for growth improved later in life. The slow initial rates of increase in length of A. butcheri in the Moore
River Estuary during early life may be related to the exceptionally high densities of this species in nearshore, shallow
waters, the region which constitutes the typical habitat of
the juveniles of this species (Sarre, 1999). The far greater
density of this species in these waters, than in correspond-
798
ing waters of the other three estuaries, can be gauged from
the fact that, during summer, the densities in such waters
sometimes reached 234 fish per 250 m2 in the Moore River
Estuary, whereas they never exceeded 50 fish per 250 m2 in
any of the other three estuaries. Because A. butcheri tends
to move into offshore and deeper waters as it increases in
size, as is the case with several other fish species in southwestern Australian estuaries (Chubb et al., 1981; Chrystal
et al., 1985; Potter et al., 1988; Wise et al., 1994), it then
becomes more widely dispersed.
Although the high densities of juvenile A. butcheri in
nearshore, shallow waters of the Moore River Estuary
could have contributed to the initially slow rate at which
length increased early in life, it also seems possible that
the low salinities, i.e. generally <7‰ (Young et al., 1997),
and quality of food in this estuary may also have had an
inhibiting influence on the rate at which length increased.
The view that low salinity has had such an effect is based
on a combination of the results of detailed laboratory
trials, which demonstrated that A. butcheri did not grow
as well at 0‰ and 12‰ as at 24‰ (Sarre et al.7) and the
fact that the upstream regions of other estuaries, where
juvenile A. butcheri are located between late spring and
early autumn when most growth occurs, are characterized
by elevated salinities (Potter and Hyndes, 1994; Sarre,
1999). Although low salinities may restrict growth, it is
worth noting that growth in the Wellstead Estuary, which
was the only estuary to become hypersaline, was greater
than in the Nornalup Walpole Estuary, which is likewise
located on the south coast of Western Australia. However,
as mentioned earlier, growth in the Wellstead Estuary was
not as great as in the Swan River Estuary and Lake Clifton farther to the north.
In the context of potential food, it may be relevant that
juvenile A. butcheri feed to a greater extent on algae
in the Moore River Estuary than in other estuaries. As
pointed out by Blaber (1974) during his study of another
sparid, Rhabdosargus holubi, which likewise ingests a
large amount of algal material, the volume of digestible
material consumed is small. However, as A. butcheri
increased in size in the Moore River Estuary, it fed to an
increasing extent on whole large bivalves (Sarre et al.,
2000), a food source that has a particularly high energy
content (Whitfield, 1980).
The age compositions recorded in this paper for A. butcheri in different water bodies have been combined with data
on reproductive biology to determine the lengths and ages
at which black bream typically reach maturity in these
systems, i.e. the L50 and A50 (Sarre and Potter, 1999). The
resultant data showed that, amongst the estuarine populations, the A50 for female A. butcheri was lowest in the
Swan River Estuary (2.2 years), in which the growth was
greatest, and greatest in the Nornalup Walpole Estuary
7
Sarre, G. A., G. J. Partridge, R. C. J. Lenanton, G. I. Jenkins,
and I. C. Potter. 1999. Elucidation of the characteristics of
inland fresh and saline water bodies that influence growth and
survival of black bream. Fisheries Research and Development
Corporation. Research Report, Project 97/309. Canberra, ACT,
Australia, 68 p.
Fishery Bulletin 98(4)
(4.3 years), in which early growth was relatively slow
and the asymptotic length the least. The minimum legal
length (MLL) for the capture of A. butcheri in southwestern Australia, i.e. 250 mm, is attained as early as 2.7 years
in the Swan River Estuary and as late as 6.5 and 6.8
years in the Nornalup Walpole and Moore River estuaries. Because the MLL is well above the L50 for females and
males of A. butcheri at first maturity in each system, it
allows a substantial number of the members of each population to reach maturity before they are likely to be caught
by either recreational or professional fishermen. However,
the relatively small contribution made by A. butcheri ≥5
years old in the heavily fished Swan River Estuary emphasizes the need to keep the upper part of that estuary closed
to commercial fishing and suggests that similar measures
may be necessary in other estuaries as they become more
heavily fished in the future.
Acknowledgments
We thank numerous people, particularly D. Mead-Hunter,
G. Richard, and D. Tiivel for help in collecting black bream,
and N. Hall and M. Platell for helpful comments on the
manuscript. Financial support was provided by the Australian Fisheries Research and Development Corporation,
Fisheries Western Australia, and Murdoch University.
Gratitude is also expressed to two anonymous referees for
constructive criticism of our paper.
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