Mediterranean Marine Science
Vol. 3/2, 2002, 147-158
Age determination and growth of leaping mullet, (Liza saliens R.1810) from the
Messolonghi Etoliko lagoon (western Greece).
G. KATSELIS1,2, C. KOUTSIKOPOULOS1 and P. KASPIRIS1
1Department of Biology, University of Patras, 26500, Patra Greece
2 Department of Aquaculture and Fisheries Technology,
Academic Technological Educational Institute Messolonghiou,
30200 Messolonghi, Greece
e-mail: gkatselis@yahoo.com
Abstract
This study is the first detailed work on the age and growth of the leaping mullet (Liza saliens, Risso 1810)
in the central Mediterranean. During the period 1991-1995 the age and growth of leaping mullet from the
Messolonghi -Etoliko lagoon system (western Greek coast) were studied. Age and growth determinations
were based upon otolith samples taken from 537 fish. Marginal increment analysis was used to validate age
determination. Annulus formation took place around November each year. The back-calculated lengths at
age estimated from the otoliths showed no differences between sub-areas of the lagoon system and the recorded
limited between-years variability showed no persistent temporal pattern. The maximum age of leaping mullet
in the Messolonghi - Etoliko lagoon was 5 years for males and 6 years for females. The von Bertalanffy equation
(L∞=32.99±1.25 cm, k=0.258 ±0.017 year-1, t0=-0.47±0.04 year) accurately describes the growth of the
total length of leaping grey mullet for all life stages (fry, juveniles and adults). A large spread and length overlap
characterized the age groups. The estimated Length-Weight relationships were common for the two sexes
(W=0.0079L3.01).
Keywords: Liza saliens, Mugilidae, leaping mullet, age and growth, Western Greece.
Introduction
The leaping mullet (Liza saliens, Risso
1810, Pisces: Mugilidae) is abundant around
the Mediterranean, the Black Sea coast and
along the Atlantic coast from Morocco to the
Bay of Biscay (TREWAVAS, 1979). It is also
present in the Caspian Sea (BEN TUVIA,
1986) and in the brackish water lakes of Egypt
(EL ZARKA & KAMEL, 1965).
Medit. Mar. Sci., 3/2, 2002, 147-158
Mullet and mullet products have
considerable economic importance at a regional
level, especially around the Mediterranean. The
leaping mullet constitutes an important part
of their production. It is one of the least studied
Mugilids in the central and eastern
Mediterranean. Information on its biology
comes mainly from studies carried out in the
western Mediterranean (CAMBRONY,
1983), southeastern Mediterranean (ZAKY-
147
RAFAIL, 1968; El ZARKA & EL SEDFY,
1970; EL ZARKA et al., 1970; PELMUTTER
et al., 1957) and eastern Mediterranean
(KOUTRAKIS & SINIS, 1994; KOUTRAKIS
et al., 1994; KAYA et al., 2000). The other
references to this species are from the Black
Sea (ALEEV, 1956-cited by THOMSON,
1966), the european Atlantic coast (DRAKE
et al., 1984 a,b) and the Balearic Islands
(CARDONA, 1999 a,b). Most of this
information concerns age, growth,
morphological character, feeding and seasonal
occurrence.
The studies conducted in the central
Mediterranean examine morphological
characters (MINOS et al., 1994; MINOS et al.,
1995; MINOS et al., 2002), seasonal occurrence
of fry, the spawning period of the species
(KATAVIC, 1980; KATSELIS et al., 1994;
MICKOVIC et al., 1994), feeding habits
(TORRICELLI et al., 1988; TOSI and
TORRICELLI, 1988) and dynamic of
population (CONIDES et al., 1992). In this
region, only one study presented information
on the age and growth (GIATNISI, 1985), but
the estimates were of low accuracy.
Age and growth are important input
parameters for stock assessment techniques.
This work is the first detailed study on these
parameters of leaping mullet in the
Messolonghi-Etoliko lagoon, a typical
Mediterranean lagoon, (western Greece,
central Mediterranean).
Materials and Methods
The Messolonghi Etoliko lagoon system is
located along the coast of western Greece
(38Æ18’N-21Æ32’E), and is situated in the
northern part of the Patraikos Gulf. It has a
total surface area of about 150 KmÇ and is one
of the larger lagoon systems in the
Mediterranean. Based on the topography,
hydrology and fish species composition, six
sub-areas can be defined (DIMITRIOU et al.,
2000a) (Fig.1). Except for its northern part
(Etoliko lagoon), the lagoon has an average
depth of 0.8m and the bottom is covered with
Fig 1: The area of study. Letters R1 to R6 indicate the different areas composing the MessolonghiEtoliko lagoon system.
148
Medit. Mar. Sci., 3/2, 2002, 147-158
rich vegetation. The Etoliko lagoon has an
average depth of 12m and a maximum depth
of 33m. The water temperature ranges from
9-32Æ C (DIMITRIOU et al., 2000b) and the
salinity from 15-45 psu.
Exploitation is a common, extensive
culture, based on seasonal entrance to the
lagoons and summer-to-winter offshore fish
migration. The fish are caught in barrier traps
in fenced areas separating the lagoon from the
sea. Gill nets and dip nets are also used in the
lagoon all year long.
During the period from January 1991 to
December 1995, samples of leaping grey mullet
were collected on a monthly basis from four
sub-areas (R2, R3, R5 & R6) of the
Messolonghi-Etoliko lagoon system (Fig. 1).
A total sample of 1133 specimens was caught
using a variety of different types of equipment.
973 specimens were caught in barrier traps,
137 specimens by trammel nets and 23
specimens with total length of less than 100
mm, by 12 x 1.2 m mosquito purse seine.
Total length (L) and standard length (LS)
were measured to the nearest mm, total body
weight (W) to the nearest 0.01 g and the sex
was determined in mature specimens by gonad
colour: orange for females and white for males,
while otoliths were removed from the fish. Age
determination from otolith readings was
performed on 537 randomly collected fish
monthly. Otoliths were read under a binocular
stereoscope with a 25x magnification, using
transmitted light. The opaque zone was used
for ageing, the distances from the otolith
nucleus to the rostrum (maximum radius), and
the radius (distance from the otolith nucleus
to the opaque zone edge, in the same direction
of maximum radius) of each ring were
measured with an optical micrometer. In
otoliths presenting reading difficulties in the
region near the focus (mainly from adult
individuals), matter was removed from the
surface layers of the bezel side of the otolith
by smoothing with 50Ì sandpaper.
The marginal increment index I M =
100*(Rc-Rn)/Rn, was calculated, where Rn is
Medit. Mar. Sci., 3/2, 2002, 147-158
the radius of the last growth ring n and Rc is
the maximum otolith radius.
Relationships between total otolith radius
(Rc) and total length (L) were determined for
males, females and the sexes combined.
Regression analysis was employed and the
significance of the recorded differences was
tested by an analysis of covariance
(ANCOVA). Back-calculated lengths at the
estimated age of individual fish were estimated
from the log transformation length-otolith
radius regression. Differences in backcalculated length at age groups between the
age, the sexes, years of sampling and sub-areas
were tested by analysis of variance (ANOVA)
(ZAR, 1984).
The von Bertalanffy growth equation was
fitted to back-calculated length at age data
using a non Linear Regression Analysis.
Results
The 1133 leaping mullet collected during
the period 1991-1995 ranged from 4 to 29.1 cm
total length. From these, 268 individuals were
identified as male, 216 as female and in 649
immature individuals sexes were not identified.
The overall ratio of males to females was 1: 0.8
and ¯2 analysis (P>0.05) revealed this to be
not significantly different from the expected
1:1 ratio. Females ranged from 15 to 29.1 cm
total length and males from 12 to 24.1 cm (Fig.
2). The regression equations of the
interconversion of L to LS are expressed
linearly and the slopes of the equation did not
differ significantly between the sexes (F=0.16,
P>0.05). The relationship for the sexes
combined is: L=0.456+1.234LS (RÇ=0.96,
SEest=0.74) where SEest is the standard error
of estimates.
The analysis of covariance showed no
significant difference between the males and
females in the Length-Weight relationship
(F=0.14, P>0.05). The obtained equation for
both sexes is the following: W=0.0079L3.01
149
(RÇ=0.97, SEest=0.11), where W is expressed
in g and L in cm.
Age and growth determinations were based
upon otolith samples of 537 fish. Ring reading
was impossible in 42 (7.9%) of them. The
unreadable otoliths were uniformly distributed
throughout the fish size range. The maximum
number of detected rings was 6 for males and
7 for females.
The mean marginal increment index for
the age group II, III and IV showed that one
ring was formed per year. The largest
percentage of individuals with a ring at the edge
of the otolith was found in the November
samples (Fig. 3).
The analysis of covariance showed no
significant difference between the males and
females in the L-Rc relationships (F=4x10-6,
P>0.05). Thus, for the estimation of backcalculated lengths at each age (Table 1) we
used the relationships obtained from the total
sample (ln(L)=-2.13+1.19 ln(Rc), RÇ=0.98,
SEest=0.083).
Analysis of variance confirms that for the
age groups O to V, there are no significant
differences between age groups and sexes for
the back-calculated mean length at each age
from otoliths (P>0.05). The first ring was
formed in otoliths at an average length of 3.8
±1.32 cm. The spawning period of leaping
Fig 2: Total length (L) frequency distribution by sex for the sampled leaping mullet individuals.
Fig 3: Monthly changes in the marginal increment index (IM) estimated from the age groups II, III and IV.
150
Medit. Mar. Sci., 3/2, 2002, 147-158
Table 1
Average back calculated lengths (cm) for each ring in each age group.
Males
Females
Age group
O
I
II
III
IV
V
VI
F
P
Mean
SD
n
growth
Mean
SD
n
growth
Mean
SD
n
growth
F
P
1
3.53
3.74
3.71
3.86
4.91
4.72
2.1
0.06
3.81
1.32
198
11.44
3.7
1.5
39
11.19
4.08
1.52
7
12.23
1.37
0.24
2
3
Otolith rings
4
5
10.81
10.38
10.42
10.55
10.19
10.04
1.51
0.18
10.44
1.09
454
6.63
10.4
1.1
82
6.7
10.44
1.06
145
6.36
0.041
0.84
15.68
15.56
15.77
15.74
15.50
0.34
0.84
15.65
1.35
415
5.21
15.8
1.4
81
5.4
15.84
1.09
146
5.40
2.3
0.63
19.57
19.37
19.69
19.48
0.49
0.68
19.53
1.20
225
3.88
19.5
1.5
26
3.7
19.54
1.03
113
3.70
0.09
0.75
22.37
22.83
22.71
0.88
0.42
22.50
1.40
82
2.97
21.0
1.5
4
1.5
22.46
1.47
41
2.92
3.85
0.06
6
25.49
24.57
3.43
0.07
25.38
0.84
24
2.88
25.1
1
4.2
25.38
1.03
13
2.92
0.059
0.81
7
26.58
26.58
0.97
3
1.20
25.46
1
0.07
n is the number of otolith readings, SD is standard deviation, F is F-ratio and P is significant level.
mullet begins in May-June and the greatest
frequency of specimens with a total length
between 35-70 mm appeared in the coastal
waters of Messolonghi from October December (KATSELIS et al., 1994). Thus, it
can be assumed that the first ring is formed 45 months after spawning and consists of the
‘fry ring’. The individuals that have only this
ring formed the O age group. From the results
presented above and the marginal increment
analysis results, the 1st ring is formed on the
otoliths at an age of 4-5 months, the 2nd at 1617 months and the rest follow at 12 monthly
regular intervals.
The back-calculated lengths at age between
years also presented some variability. In fact,
an analysis of variance showed that for the age
groups I to III there were significant differences
between years (Table 2), but these differences
do not show a persistent temporal pattern. In
Medit. Mar. Sci., 3/2, 2002, 147-158
fact, the smaller group I individuals sampled
in 1994 produce the longer mean values the
next year. Also, ANOVA confirms that for age
groups O to V, there are no significant
differences between sub-areas (P>0.05) for
the back-calculated mean length at each age
from otoliths.
The growth rate was calculated using the
von Bertalanffy growth equation and the
coefficients of the growth are presented in
Table 2. The 95 % confidence intervals of the
von Bertalanffy growth equation parameters
overlap between the years of sampling, which
means that their parameters showed no
significant differences. The ratio of Lmax/L∞
(Lmax is the maximum observed length in the
sample) was 0.88. The estimated value of t0 was
–0.47±0.032 year (5.18-6.1 months) and can
be considered as the time needed to form the
first ring (‘fry ring’) in otoliths.
151
Table 2
Size and age composition of males, females and immature individuals of leaping mullet from
Messolonghi -Etoliko lagoon.
Age group
O
I
II
III
IV
V
N
Observed
range of L
L∞ (cm)
k (year-1)
t0 (year)
n
RÇ
1991
3.09
10.4
15.28
19.07
22.45
25.08
44
1992
4.26
10.7
15.68
19.61
22.9
25.42
113
11.1-29.1
4.5-28.4
31.8±5.02 35.1±3.7
0.27±0.09 0.23±0.05
-0.44±0.17 -0.57±0.12
122
278
0.94
0.93
year of sampling
1993
3.36
10.13
14.9
18.9
21.43
25.14
102
4.2-28.7
32.5±3.07
0.25±0.03
-0.45±0.08
228
0.95
1994
4.18
9.9
15.03
18.92
23.76
26.42
29
1995
3.88
10.49
15.97
19.75
22.41
25.69
205
n
F
P
197 1.82 0.13
450 5.048 0*
411 11.05 0*
221 5.068 0*
78 2.46 0.04*
20 0.54 0.71
12.8-23
47.2±23.9
0.14±0.1
-0.64±0.34
69
0.92
11.5-26.6
32.37±1.77
0.27±0.03
-0.46±0.04
705
0.95
All sampling
32.99±1.25
0.26±0.017
-0.47±0.03
1401
0.95
* Significant difference, N is number of specimens, n is the number of length-age readings
for back calculation, F is F-ratio and P is significant level.
A length-age key for the two sexes and their ramada (5.7%) and Chelon labrosous
combination is presented in Table 3. The age (2.4%)(KATSELIS, unpublished data).
groups were characterised by a large spread
Various methods are used to determine the
and overlapping of length.
age in Mugilidae. Some authors preferred using
length frequency analysis (DRAKE et al., 1984a;
CARDONA, 1999a), but QUIGNARD and
Discussion
FARRUGIO (1981) claimed that these
Studies of the age and growth of fish are methods were useless for mullet because of the
essential for the management of their stocks. difficulty of obtaining samples, and because
Grey mullet make up the most important part spawning takes place over several months.
Both scales and otoliths are used for the
of the fish catch in the Messolonghi - Etoliko
age
determination of Mugilidae. To use otolith,
lagoons. The mean annual production is about
or
any
other structure, for age determination,
1300 – 1500 mt and is provided by 200
the
deposition
of regular detectable age marks
fishermen working at the barrier traps and 700
is
essential.
Otolith
age determination is
fishing in the lagoon. Mullet are estimated to
compose 45 % of the total fish catch considered to be more accurate because
(KOTSONIAS, 1984; DIMITRIOU et al., otoliths have a higher priority in utilization of
1994). Separate catch statistics for each species calcium (CARLANDER, 1987). However the
are available only for barrier trap fish catches. otoliths have rarely been used in mullet because
During the period 1995-1998, 182 mt of fish of the difficulty in reading the rings in the region
per year was caught in the barrier trap of the near the focus of the otolith (ERMAN, 1959;
Messolonghi -Etoliko lagoons, 51.9 % of which KENNEDY & FITZMAURICE, 1969;
were mullet. Among the five mullet species BRULHET, 1974). THONG (1969) indicated
caught barrier trap, L. saliens, Liza aurata and that only 67%, 66% and 64% of the otoliths of
Mugil cephalus were more abundant (18.8%, L. ramada, C. labrosus and L. aurata respectively
14.3 % and 10.7 % respectively) than Liza were readable in the above-mentioned studies.
152
Medit. Mar. Sci., 3/2, 2002, 147-158
Table 3
Size and age composition of males, females and immature individuals of leaping mullet from
Messolonghi -Etoliko lagoon.
L (cm)
I
4-5
5-6
6-7
7-8
8-9
9-10
10-11
11-12
12-13
13-14
14-15
15-16
16-17 1
17-18 1
18-19
19-20
20-21
21-22
22-23
23-24
24-25
25-26
26-27
27-28
28-29
29-30
Total 2
II
males
III IV
V
II
females
III IV
V
VI
O
10
3
10
6
5
4
1
3
12
14
12
10
3
2
3
3
8
6
1
1
2
6
11
9
4
1
1
1
1
1
1
2
8
14
19
15
7
3
2
1
5
5
5
9
2
1
1
56
22
3
1
33
72
28
This difficulty was verified in the present study
and it was partially overcome by smoothing the
bezel side during the preparation of the otolith.
The percentage of reliability of otolith readings
in this study was 92.1%. Following the same
technique KAYA et al. (2000) have increased
the percentage of reliability of otolith readings
to 87.7%. According to our findings, otolith
readings gave correct results and fitted the
growth equation well(Table 2).
The results of the study of the marginal
increment index suggest that rings in leaping
mullet are formed annually around November,
when the water temperature in the lagoon is
between 14 and 21ÆC (DIMITRIOU et al.,
2000b). Thus, the annual ring formation is
related to the decrease of the growth rate of
the species in water temperatures lower than
Medit. Mar. Sci., 3/2, 2002, 147-158
2
1
3
2
3
1
12
I
2
2
5
1
5
5
9
7
3
immature
II III IV
2
8
11
16
23
16
8
14
5
1
1
8
9
10
6
7
6
1
1
39
39
103
V
48
3
4
5
5
3
5
1
1
1
1
2
1
2
1
27
8
VI total
10
3
10
6
5
2
6
6
3
13
16
29
43
38
39
55
53
46
35
27
20
11
7
1
7
1
5
1
2 496
20ÆC (CARDONA, 1999a) and minimal
feeding activity (CARDONA, 1999b). In
addition, ‘fry ring’ formation is possibly caused
by changes in the proteinic composition due
to the different diet that they adopt (from
zooplankton to mixed and finally to vegetarian)
(ALBERTINI-BERHAUT, 1974; DE SILVA,
1980). Other researchers agree that the
formation of the annual ring of mullet takes
place in winter, but in scales this ring is detected
in spring (CAMBRONY, 1983; KOUTRAKIS
& SINIS, 1994).
The length overlap between successive age
classes is expected for species with an extended
reproductive period. The reproduction period
of leaping mullet in western Greece occurs
from May to November (KATSELIS et al.,
1994). This fact reduces the ability to use the
153
length frequency analysis for age estimation
(BAGENAL & TESCH, 1978). However, the
population of leaping mullet fished in the
Messolonghi-Etoliko lagoon system consists
of individuals of different ages, which inhabit
several biotopes with various levels of trophic
importance for fish in adjacent areas of the
Ionian Sea and the Gulf of Patras and which
enter the lagoons each spring. Thus, a high
variability in length at age is expected due to
several growth rates. This mechanism could
partially explain the fact that between the subareas of the lagoon system there were no
differences in lengths at age, the variability of
length at age among the years and the length
overlap between successive age classes.
There are six age classes of leaping mullet
in the Messolonghi – Etoliko lagoons. The
oldest specimens observed in Mediterranean
lagoons (Porto Lagos lagoon: N. Greece)
attained an age of eight years (KOUTRAKIS
& SINIS, 1994), while maximum age estimates
in coastal waters of western Greece was 5 years
(CONIDES et al. 1992) and in other localities
ranges from 3-5 years.
The von Bertalanffy equation obtained in
this study appeared to be an accurate
description of growth in length of leaping
mullet for all stages of its life (fry, juveniles and
adults). In our computation the asymptotic
total length of the leaping mullet was
L∞=32.99±1.25 cm and k=0.258±0.017 year-1.
From other Liza species in the Messolonghi
–Etoliko lagoons the leaping mullet was
estimated to have a smaller L∞ and greater k
value. For L. aurata in the same region the von
Bertalanffy values have been estimated
L∞=69.6 cm, k=0.136 year-1 (HOTOS, 1999),
while for L. ramada L∞=56.3 cm, k=0.179
year-1 (MINOS, 1996). These findings were in
agreement with those in Porto Lagos lagoon
(KOUTRAKIS & SINIS, 1994).
Table 4 shows the results obtained by other
studies concerning the age determination of
leaping mullet. Most of the values of L∞ and k
for leaping mullet that inhabit various
Mediterranean localities fluctuate between 30
154
and 39 cm and 0.23 and 0.30 year-1 respectively.
The majority of the extreme values of L∞ and
k are due to the method for the estimation of
the length at age or the sample quality. For the
leaping mullet inhabiting the Loutsa lagoon
(Epirus: NW Greece), GIATNISI (1985)
estimates L∞ equal to 42.3 cm and k equal to
0.16 year-1 an implication of the overestimation
of L 3 due to small size of the samples (3
specimens). For this reason as well, there are
extreme values of von Bertalanffy equation
parameters in the SE Mediterranean where
the older ages (L4, L5) were demonstrated by
1-2 specimens (EL ZARKA & EL SEDFY,
1970; EL ZARKA et al., 1970), or the
overestimation of the lengths at age in older
ages due to the length frequency analysis used
(DRAKE et al., 1984a; CARDONA, 1999a).
From the results shown above it is clear
that the growth rates of leaping mullet from
different localities can be compared only for
young stages and only in some cases (e.g. the
debatable results discussed above should not
be accepted). Thus, the growth rate of the
young leaping mullet (1 to 3 years) in the
Messolonghi -Etoliko lagoons is lower than
the rates recorded in the other regions of the
Mediterranean coastal areas and lagoons (the
lagoons of the Gulf of Lions, north and eastern
Aegean and the Egyptian coasts). Similar
growth patterns of leaping mullet were
observed in the Black Sea and finally, the
growth of leaping mullet is slightly lower in the
Lakes Edku and Quarun in Egypt than in the
Messolonghi - Etoliko lagoon (Table 5).
Despite the above, we should expect the
water temperature to affect growth in length
(or weight) patterns of leaping mullet related
to latitude because this species does not grow
at water temperatures lower than 20ÆC
(CARDONA, 1999a). The different growth
rates of leaping mullet in different locations
can be assigned to other factors apart from
temperature differences, such as local food
availability and/or density-dependent relations
(EL ZARKA et al., 1970; DRAKE et al.,
1984b). Feeding of mullet is connected to
Medit. Mar. Sci., 3/2, 2002, 147-158
Table 4
Average back calculated lengths (cm) for each year at age and estimate of von Bertalanffy growth
equation parameters (± standard error) for year of sampling and all sampling of leaping mullet
from back calculated length at age data set.
Region
W. Greece lagoons
Messolonghi Etoliko
Loutsa lagoon (Epirus)
Porto Lagos lagoon
(N. Greece)
Lake Vistonida
W. Mediterranean
(France: Lions Gulf)
Atlantic coast (Spain)
Balearic Islands
Method
Ot, vIM
Ot, vIM
Ot, vIM
Sc
Sc, vIM
Sc, vIM
Sc, vIM
Sc, vIM
Sc
Sc
Sc
Pt
Sex
M
F
B
B
M
F
B
B
M
F
B
B
L1
10.5
10.4
10.5
9.9
11.5
11.4
11.4
11.4
8.1
8.1
9.2
6.8
L2
15.77
15.8
15.6
14.4
17.8
18
17.9
17.9
13.8
13.8
16.5
18.3
SE Mediterranean (Egypt)
Pt
Pt
Sc
M 10.2 16.1
F 10.2 16.1
B 7.6 18.7
Lake Quarun (Egypt)
Sc
M
12
16.5
Lake Edku (Egypt)
Sc
Sc
F
M
12
8.2
16.5
13.5
Sc
Ot
Ot
Ot
?
F 9 14.5
M 10.2 15.7
F 9.5 15.5
B 9.8 15.6
B 8.7 14.5
E. Mediterranean
(Turkey: NE Aegean)
Black Sea
Total length (Li)at age i
L3 L4 L5 L6 L7 L8 L∞ k t0 Author
19.49 20.98 25.16
29.9 0.30 -0.42
19.5 22.4 25.4 26.4
32.9 0.25 -0.50 Present study
19.4 22.7 24.6 26.6
32.9 0.26 -0.47
21.1· 22.5
42.3 0.16 -0.82 GIATNISI, (1985)
22.1 25.0 27.4 30.7 32.2
33.8 0.32 -0.34 KOUTRAKIS
22.4 25.8 28.2 30.5 32.1 33 36.7 0.28 -0.40 & SINIS, (1994)
22.3 25.6 28.1 30.3 32 33 36.7 0.28 -0.34
21.8 25.6 28.1
36.7 0.28 -0.34
18.9 22.8 26.3
45.2 0.17 -0.17
18.8 23.5 27.7
66.2 0.10 -0.27 EZZAT, (1965)**
22.2 26.2
38.4 0.29 -0.62 CAMBRONY, (1983)
23.4 26.7 28.5
29.9 0.66 -0.14 DRAKE et al.,
(1984a)
18.1 19.3 22.6
34.25 0.26 -0.44
19.3 22.6 26.5 29.1
38.7 0.20 -0.31 CARDONA, (1999a)
23.6 28.0 32.0
36.4 0.44 0.52 ZAKY-RAFAIL,
(1968)
20
24 27.5
36.9 0.23 -0.75 EL ZARKA & EL
SEDFY, (1970)
22
27
31
53.6 0.14 -0.82
16.7
21.5 0.50 0.05 EL ZARKA et al.,
(1970)
17.6
21.6 0.57 0.06
19.8 22.9 25.1 26.8
31.59 0.29 -0.41
20.0 23.4 25.7 27.7 29.0
33.0 0.29 -0.38 KAYA et al., (2000)
19.9 23.2 25.6 27.5 28.8
33.1 0.28 -0.38
17.9 20.9 23 25.8
32.00 0.26 -0.26 ALEEV, (1956)#
# cited by THOMSON (1966) , **cited by QUIGNARD & FARRUGIO (1981)
Table 5
Growth rate of young leaping mullet in different regions.
Total length (Li) at age i
L1 L2 L3 Increment
from 1 to 3
year (cm)
Lake Quarun (Egypt)
12 16.5 20
8
Lake Edku (Egypt)
8.2 13.5 16.7
8.5
Messolonghi (W. Greece: Ionean Sea) 10.5 15.6 19.4
8.9
Black Sea
8.7 14.5 17.9
9.2
E. Mediterranean (Turkey: NE Aegean) 9.8 15.6 19.9
10.1
Lake Vistonida (N. Aegean)
11.4 17.9 21.8
10.4
W. Mediterranean (Lions Gulf)
8.1 13.8 18.9
10.8
Porto Lagos lagoon (N. Aegean)
11.4 17.9 22.3
10.9
W. Mediterranean (France: Lions Gulf) 9.2 16.5 22.2
13
SE Mediterranean (Egyptian coastal)
11 18.7 23.6
12.6
Region
Author
EL ZARKA & EL SEDFY,
EL ZARKA et al., (1970)
Present study
ALEEV, (1956)#
KAYA et al., (2000)
KOUTRAKIS & SINIS, (1994)
EZZAT, (1965)**
KOUTRAKIS & SINIS, (1994)
CAMBRONY, (1983)
ZAKY-RAFAIL, (1968)
# cited by THOMSON (1966) , **cited by QUIGNARD and FARRUGIO (1981)
Medit. Mar. Sci., 3/2, 2002, 147-158
155
primary productivity because these fish feed
mainly on algae and diatoms, though they
consume zooplankton and zoobenthos as well
(BRUSLE, 1981). Thus, the lower growth rate
which was estimated in this study can be
attributed to the fact that the greater sea region
of the Messolonghi - Etoliko lagoons is
characterised by lower primary productivity
values than the north and northeastern Aegean
seas (DRAKOPOULOS, et al., 2000) and Gulf
of Lions (LEFEVRE, et al., 1997).
Growth in length was similar for males and
females, even though females were predominant
in the older age groups (Table 3). Previous
workers have found both significant (EL
ZARKA & EL SEDFY, 1970) and nonsignificant differences (KOUTRAKIS &
SINIS, 1994; KAYA et al., 2000) in the growth
rates of leaping mullet. This disagreement has
been found for other Mugilidae species but in
these cases the females live longer than males
and are predominant in the older age groups
(QUIGNARD & FARRUGIO, 1981). The
small number of males at older ages can be
related to the significant differences in length
among the sexes. For example, in the first study
(EL ZARKA and EL SEDFY, 1970), the L4
and L 5 was estimated from one male, in
contrast to other studies (KOUTRAKIS &
SINIS, 1994; KAYA et al., 2000) where the
number of male specimens of these ages was
greater. This hypothesis is supported by
findings for other Mugilidae species in the
Mediterranean (KOUTRAKIS & SINIS,
1994; MINOS, 1996; HOTOS, 1999).
Finally, the slope of the length-weight
relationship (b=3.01≈3), shows that leaping
mullet in the Messolonghi –Etoliko lagoons
presented an isometric growth pattern.
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