The common sole,
The global capture production of common sole in 2016 was about 32 057 t (FAO 2020). Common sole landings in the Mediterranean Basin amounted to 5227.5 t in 2018 (GFCM 2020). Total landings of common sole in Turkey have dramatically declined in recent years from approximately 1000 t in 2010 to < 500 t in 2019 (TÜİK 2020). Knowledge of the age, growth and reproduction of any species is of great importance for achieving good environmental status and management strategies. Several studies on the age–growth and spawning characteristics of the common sole have been conducted in different regions in recent years (Slastenenko 1956; Nielsen 1972; Quéro et al. 1986; Hoşsucu et al. 1999; Muus & Nielsen 1999; Vallisneri et al. 2000; Cerim & Ateş 2019). On the other hand, there is only one not very recent PhD study on the general biological characteristics of this species in the Sea of Marmara (Oral 1996).
In the Sea of Marmara, the common sole is primarily caught by beam trawls and set gillnets, because bottom trawling has been completely banned for a long time. On the other hand, it is obvious that the existing management policies and strategies (seasonal closures and minimum landing size) have failed to protect critical nursery and spawning areas for many fish species, including the common sole. In addition, these management practices are outdated and ignore region-specific details regarding sexual maturity and reproductive patterns of this species. Estimation of demographic parameters of fish populations, particularly their growth, mortality and spawning rates, is essential for assessing population dynamics and management of fishery resources (Newman & Dunk 2003). After a comprehensive review of the relevant literature, it can be concluded that the material available for this study is extremely scarce. The declining trend in landings further indicates the urgency and necessity for research on common sole. Therefore, the objective of this study was to determine the growth characteristics of the common sole in the Sea of Marmara based on sagittal otolith readings, fish length at the onset of sexual maturity (
Common sole specimens were randomly collected monthly from the Sea of Marmara by commercial fishermen using beam trawls and trammel nets between October 2017 and September 2018. Total length (TL, cm) and total wet weight (TW, g) were recorded for each specimen. Sex was determined macroscopically as male, female and immature (or unidentified). Pairs of “sagittal” otoliths were extracted for age assessment and ground on both sides with two abrasive papers of 35.0 μm and 25.8 μm, respectively. They were then cleaned in distilled water and immersed in glycerin for the age estimation process and viewed using an image analysis system with a circular reflected light source (Leica DFC295 stereomicroscope). For age estimation, annual growth rings on otoliths were evaluated by three experienced age readers, and agreement rates between them were 90–95%. Annuli were counted from the core outward. Each annulus was defined as the location where the opaque zone meets the translucent zone.
The length–weight relationship was determined using the equation TW =
Total instantaneous mortality (
The gonads were dissected and then weighed (GW). Each specimen was macroscopically assigned to a gonadal stage on the basis of a scale consisting of five maturity phases: immature (phase I), developing or regenerating (phase II), spawning capable (phase III), actively spawning (phase IV), and regressing (phase V; Brown-Peterson et al. 2011). To corroborate the macroscopic classification of females, all ovaries were used for histological analysis; specifically, a subsample of an approximately 1.0 cm wide section from the central part of the ovary was preserved in 10% buffered formalin. Tissue sections were washed in a buffer solution, dehydrated in ethanol and
Immature (phase I) ovaries contained oocytes in the primary growth phase and a thin ovarian wall (PG). Oocytes of developing ovaries (phase II) showed the initiation of the secondary growth phase with the formation of cortical alveoli (CA). Entry into the spawning capable phase was characterized by the appearance of Vtg3 oocytes and the actively spawning phase can be used to identify fish that are progressing through germinal vesicle breakdown (GVBD) or hydration. The regressing phase was identified by the presence of oocyte atresia, a reduced number of vitellogenic oocytes, and, in some specimens, postovulatory follicles (POF). The regenerating phase was distinguished from the immature phase by: (i) a thicker ovarian wall (OW), (ii) the presence of more space, interstitial tissue, and capillaries around PG oocytes, and (iii) the presence of muscle bundles (Brown-Peterson et al. 2011).
To determine the spawning season, the gonadosomatic index (
A total of 580 individuals of common sole were measured monthly throughout the year. Total length of all specimens varied from 11.1 to 29.5 cm (mean length 20.91 ± 3.62 cm). No statistically significant differences (
Figure 1
Monthly length–frequency distribution for females and males of

Parameters of the length–weight relationship (W =
Growth type | ||||
---|---|---|---|---|
Pooled | 0.022 | 2.6838 | 0.9456 | Negative Allometric |
F | 0.0349 | 2.5536 | 0.9032 | |
M | 0.0253 | 2.6235 | 0.934 | |
Unidentified | 0.0201 | 2.7179 | 0.941 |
Length-at-age values and the number of individuals in each age class are presented in Table 2. The estimated age ranged from 1 to 3 years, with age class 2 being the most abundant one (52.3%). Females reached a maximum size of 35.8 cm, which is 4 cm larger than males (31.3 cm). This indicates that females grew slightly faster than males (Table 3). In addition, growth parameters for all individuals were calculated for pooled data according to the ELEFAN method and found to be
Length-at-age key for all samples of
Length class (cm) | Age (years) | Total | ||
---|---|---|---|---|
1 | 2 | 3 | ||
11 | 6 | 6 | ||
12 | 9 | 9 | ||
13 | 18 | 18 | ||
14 | 16 | 16 | ||
15 | 13 | 13 | ||
16 | 10 | 10 | ||
17 | 3 | 3 | ||
18 | 5 | 3 | 8 | |
19 | 16 | 16 | ||
20 | 38 | 38 | ||
21 | 77 | 77 | ||
22 | 111 | 111 | ||
23 | 52 | 29 | 81 | |
24 | 67 | 67 | ||
25 | 47 | 47 | ||
26 | 19 | 19 | ||
27 | 15 | 15 | ||
28 | 9 | 9 | ||
29 | 4 | 4 | ||
Total | 80 | 297 | 190 | 567 |
Von Bertalanffy growth parameters calculated for
Sex | N | |||
---|---|---|---|---|
Pooled | 580 | 0.48 | −0.18 | 33.7 |
F | 248 | 0.37 | −0.49 | 35.8 |
M | 294 | 0.57 | 0.03 | 31.3 |
Figure 2
Seasonally oscillating growth curve generated from length–frequency distribution for

Of all collected specimens, 248 specimens (64%) were females with an average length of 23.5 ± 2.08 cm, ranging from 12.6 to 29.5 cm, and 294 specimens (36%) were males with an average length of 22.7 ± 2.92 cm, ranging from 11.8 cm to 27.8 cm. The sex ratio (♂/♀) was 1.18, and was statistically significantly different from the ratio of 1:1 (
Figure 3
Monthly changes in the mean gonadosomatic index (GSI) and condition factor (CF) by sex of

Four different developmental phases of common sole oocytes were identified in this study (Fig. 4), with 71 females collected in May–June and October–November being sexually mature (phases III, IV, and V) and almost all of them being larger than 21 cm. On the other hand, virgin specimens were common during nearly all months. Post-spawning oocytes were first noticed in June–July and December. These findings showed that the spawning activity of the common sole occurs at the end of autumn and spring. In addition, estimates of
Figure 4
Micrographs from cross-sections of immature or virgin gonads, Phase II – Developing (ovaries begin to develop, but are not ready to spawn); Phase III – Spawning capable (fish are developmentally and physiologically capable of spawning); Phase IV – Regressing (cessation of spawning) with hydrated oocytes (HYD); Phase V – Regenerating (characterized by thick ovarian wall); CA = cortical alveolar; GVBD = germinal vesicle breakdown; OW: ovarian wall; POF = postovulatory follicle complex; VTG3 = tertiary vitellogenic

Figure 5
Maturity ogives for males (upper) and females (lower) by total length (TL) for

The present study shows the age composition, growth, and mortality of common sole from the Sea of Marmara. The first attempt at histological analysis of oocyte development and other reproductive aspects of the common sole from the Sea of Marmara are also presented here.
The length range of specimens examined in our study (Table 4) was generally similar to that found in other studies carried out in the Eastern Mediterranean Sea. In addition, we found that the
Length–weight relationships for
Sex | Length (cm) | Length | N | Locality | References | |||
---|---|---|---|---|---|---|---|---|
Eastern Atlantic | ||||||||
0.005 | 3.20 | M + F | 10.0–42.0 | – | 0.975 | 334 | North Sea | Froese & Sampang 2013 |
0.0071 | 3.095 | M + F | 21.0–43.0 | TL | 0.954 | 325 | North Sea coast of Germany | Duncker 1923 |
0.0048 | 3.175 | M + F | 2.0–59.0 | TL | 0.998 | 5804 | Bay of Biscay | Dorel 1986 |
0.0039 | 3.264 | M + F | 3.0–49.0 | TL | 1.000 | 3,799 | East and West Channel | Dorel 1986 |
0.0036 | 3.313 | M + F | 11.0–29.0 | TL | – | 13 | German Bight & Clyde | Coull et al. 1989 |
0.0046 | 3.21 | M + F | – | – | – | 518 | Douarnenez Bay, Brittany | Deniel 1984 |
0.004 | 3.251 | M + F | 9.0–49.0 | TL | – | 945 | North–eastern Atlantic | Mahé et al. 2018 |
0.0078 | 3.08 | M + F | 10.5–38.9 | TL | 0.969 | – | Arade Estuary, Central Algarve | Veiga et al. 2009 |
0.0071 | 3.092 | M + F | 20.5–46.0 | TL | 0.908 | 58 | Nazaré to St André | Mendes et al. 2004 |
Central and Western Mediterranean Sea | ||||||||
0.0086 | 2.99 | F | – | TL | – | – | Gulf of Lion | Campillo 1992 |
0.0109 | 2.94 | M | – | TL | – | – | ||
0.0062 | 3.04 | M + F | 5.0–45.0 | TL | 0.980 | 561 | Gulf of Lion | Vianet et al. 1989 |
0.0106 | 3.062 | M + F | 6.5–25.0 | SL | 0.981 | 82 | Acquitina, Italy | Maci et al. 2009 |
0.0019 | 3.453 | M + F | 19.8–32.5 | TL | 0.946 | 2,130 | Northern Adriatic | Dulčić & Glamuzina 2006 |
0.01 | 2.96 | M + F | 15.0–45.0 | TL | 0.932 | 406 | French Catalan Coast | Crec’hriou et al. 2013 |
Eastern Mediterranean Sea | ||||||||
0.049 | 2.35 | Juvenile | 11.2–24.4 | TL | 0.980 | 13 | Iskenderun Bay | Gökçe et al. 2010 |
0.0117 | 2.988 | M | 8.8–25.0 | TL | 0.922 | 550 | Iskenderun Bay | Türkmen 2003 |
0.0091 | 3.077 | F | 10.5–28.2 | TL | 0.947 | 533 | ||
Aegean Sea | ||||||||
0.0098 | 3.002 | Juvenile | 11.0–22.1 | TL | 0.988 | 21 | Porto-Lagos | Koutrakis & Tsikliras 2003 |
0.0023 | 3.369 | M + F | 18.6–33.7 | TL | 0.920 | 171 | Aegean Sea | Bilge et al. 2014 |
0.0088 | 3.024 | M | 3.1–29.0 | TL | 0.9925 | 529 | Güllük Bay | Cerim 2017 |
0.007 | 3.1013 | F | 7.1–37.0 | TL | 0.9866 | 607 | ||
Sea of Marmara | ||||||||
0.0043 | 3.171 | Juvenile | 6.9–16.0 | TL | 0.928 | 55 | Sea of Marmara | Bök et al. 2011 |
0.0183 | 2.727 | M | 13.0–27.0 | TL | – | 206 | Sea of Marmara | Oral 1996 |
0.0011 | 3.674 | F | 13.0–34.0 | TL | – | 218 | ||
0.0253 | 2.6235 | M | 11.8–27.8 | TL | 0.9 | 294 | Sea of Marmara | This study |
0.0349 | 2.5536 | F | 12.6–29.5 | TL | 0.934 | 248 |
Table 5 shows the age and growth parameters of common sole obtained by several researches. The growth parameters (
Von Bertalanffy growth parameters (L∞ – asymptotic mean length;
Ø′ | Sex | Locality | Reference | |||
---|---|---|---|---|---|---|
Eastern Atlantic | ||||||
34.2 | 0.35 | −1.3 | 2.62 | M | Dutch ports | De Veen 1976 |
35.6 | 0.38 | −0.5 | 2.68 | F | Dutch ports | De Veen 1976 |
36.9 | 0.28 | −2.3 | 2.58 | F | Dutch ports | De Veen 1976 |
37.4 | 0.31 | – | 2.64 | M + F | North Sea | Nielsen 1972 |
39.0 | 0.4 | – | 2.78 | M + F | North Sea | Beverton & Holt 1959 |
39.6 | 0.35 | −0.8 | 2.74 | F | Dutch ports | De Veen 1976 |
42.4 | 0.39 | 0.09 | 2.85 | M | Bay of Biscay | Deniel 1990 |
48.2 | 0.32 | 0.08 | 2.88 | F | Bay of Biscay | Deniel 1990 |
49.8 | 0.13 | – | 2.51 | M + F | Celtic Sea | Jennings et al. 1998 |
Central and Western Mediterranean Sea | ||||||
37.9 | 0.504 | −5.36 | 2.86 | F | Adriatic Sea | Froglia & Giannetti 1986 |
38.3 | 0.492 | −3.57 | 2.86 | M + F | Adriatic Sea | Froglia & Giannetti 1985 |
40.1 | 0.68 | – | 3.04 | M + F | Adriatic Sea | Piccinetti & Giovanardi 1984 |
39.6 | 0.44 | −0.46 | 2.84 | M + F | Northern Adriatic | Colloca et al. 2013 |
35.8 | 0.41 | – | 2.72 | M + F | Tyrrhenian Sea | Wurtz & Matricardi 2020 |
48.8 | 0.24 | −0.77 | 2.76 | M + F | Gulf of Lion | Vianet et al. 1989 |
47.2 | 0.274 | – | 2.79 | F | Gulf of Lion | Girardin et al. 1986 |
38.8 | 0.24 | −1.09 | 2.56 | M | Castellon coast | Ramos 1982 |
46.4 | 0.22 | −0.75 | 2.68 | F | Castellon coast | Ramos 1982 |
Eastern Mediterranean Sea | ||||||
26.0 | 0.221 | −1.31 | 2.17 | M | Iskenderun Bay | Türkmen 2003 |
29.9 | 0.181 | −1.55 | 2.21 | F | ||
30.0 | 0.33 | −1.51 | 2.47 | M + F | Bardawil Lagoon | El-Gammal et al. 1994 |
Aegean Sea | ||||||
31.1 | 0.33 | −1.04 | 2.5 | M | Aegean Sea | Hoşsucu et al. 1999 |
42.5 | 0.17 | −1.96 | 2.49 | F | ||
30.21 | 0.19 | −0,26 | 2.24 | M | Aegean Sea | Cerim & Ateş 2020 |
36.95 | 0.23 | −0,03 | 2.50 | F | ||
34.9 | 0.38 | −0.41 | 2.67 | M + F | Amvrakikos Gulf | Stergiou et al. 1997 |
Sea of Marmara | ||||||
28.63 | 0.62 | −0.91 | 2.71 | M | Sea of Marmara | Oral 1996 |
35.79 | 0.72 | −1.06 | 2.96 | F | ||
31.3 | 0.57 | 0.03 | 2.74 | M | Sea of Marmara | This study |
35.8 | 0.37 | −0.49 | 2.67 | F |
Mortality rates and exploitation ratio for
Fishing technique | Region | Reference | ||||
---|---|---|---|---|---|---|
2.49 | 1.83 | 0.66 | 0.73 | – | Egypt | Mehanna & Salem 2012 |
1.7 | 1.18 | 0.52 | 0.69 | gillnet | Egypt | Mehanna et al. 2015 |
1.32 | 8.2 | 0.5 | 0.6 | bottom trawl | Iskenderun Bay | Türkmen 2003 |
0.97 | 0.66 | 0.31 | 0.68 | gillnet | Güllük Bay | Cerim & Ateş 2019a |
1.42 | 1.01 | 0.47 | 0.68 | beam trawl & gillnet | Sea of Marmara | this study |
Figure 6 shows a spatial pattern generated by log-transformed values of
Figure 6
Scatter plot and regional groupings in terms of log(

The mortality rates (
Our study determined that the reproductive periods of the common sole were between October and December, and between April and June. Figure 7 shows that common sole does not have any spawning activity in the summer months, when the water temperature reaches a maximum (around 23°C) and the spawning season varies by region. The two spawning seasons previously reported for the common sole in the Sea of Marmara (Slastenenko 1956; Oral 1996) and the seasons found in our study partially overlap. The spawning season reported by Slastenenko (1956) coincides with the spring peak (around 12.8°C) determined in our study and the month of December reported by Oral (1996) agrees with our autumn peak (around 19.2°C). Based on these data, it can be concluded that the common sole in the Sea of Marmara shows the maximum reproductive activity in water temperatures above 10°C and below 20°C. In the eastern Atlantic, on the other hand, the reproductive activity generally occurs between March and May, suggesting that the Mediterranean stock has a longer spawning season than the Atlantic stock. These arguments are consistent with the hypothesis that extended spawning may be observed in fish stock closer to the tropics (Tsikliras et al. 2010).
Figure 7
Spawning season of

In this study, histological analysis of the gonads demonstrated that common sole has an asynchronous spawning pattern, and this is consistent with previous studies on the gonads by Cerim & Ateş (2019) and Follesa & Carbonara (2019). In this study, length at the onset of sexual maturity (
As shown in Table 7, the
Length at the onset of sexual maturity (cm) for
Sex | Country | Region | Study | |
---|---|---|---|---|
18.8 | M + F | Germany | North Sea | Froese & Sampang 2013 |
22.0 | M | France | Bay of Biscay | Dorel 1986 |
24.8 | M + F | UK | North Sea | Jennings et al. 1998 |
26.0 | M + F | North Sea | Rijnsdorp & Vethaak 1997 | |
27.0 | M + F | Holland | Dutch ports | De Veen 1976 |
28.0 | F | France | East and West Channel | Dorel 1986 |
29.0 | M + F | UK | Celtic Sea | Anonymous 2001 |
30.0 | M + F | Holland | Dutch ports | De Veen 1976 |
31.0 | F | France | Bay of Biscay | Dorel 1986 |
32.0 | F | France | Douarnenez Bay, Brittany | Deniel 1990 |
20.8 | F | Turkey | Aegean Sea | Kinacigil et al. 2008 |
22.7 | M | |||
20.4 | F | Turkey | Güllük Bay | Cerim & Ateş 2019b |
21.5 | F | Turkey | Sea of Marmara | this study |
18.6 | M |
In the European Union, the minimum conservation reference size (MCRS) for common sole is 24 cm TL (EU 2019). In the current Turkish legislation, on the other hand, this size has been defined since 2006 as 20 cm TL (Yildiz & Ulman 2020b) and we consider that there is no scientific basis for this regulation. Furthermore, it can be concluded that different
A recent assessment study revealed that the common sole stock in the Aegean Sea is in poor condition and is overexploited regionally (Tsikliras et al. 2021). Moreover, a large-scale stock assessment study conducted in the Eastern Mediterranean Sea and the Black Sea showed a dramatic decline in commercial species (Demirel et al. 2020). The common sole has been listed in the IUCN Red List of Threatened Species under the “Data Deficient” category, and its subpopulations in the Mediterranean Sea have recently been assessed as “Least Concern” (Golani et al. 2011). However, common sole populations in the Sea of Marmara are overexploited and high fishing pressure on common sole, mainly from beam trawlers, can reduce the spawning stock biomass below levels sufficient for population productivity. The results of this study may contribute to better fisheries management for the common sole, as well as the entire region, and will then serve as a basis for further research.
Figure 1

Figure 2

Figure 3

Figure 4

Figure 5

Figure 6

Figure 7

Von Bertalanffy growth parameters calculated for S. solea
Sex | N | |||
---|---|---|---|---|
Pooled | 580 | 0.48 | −0.18 | 33.7 |
F | 248 | 0.37 | −0.49 | 35.8 |
M | 294 | 0.57 | 0.03 | 31.3 |
Von Bertalanffy growth parameters (L∞ – asymptotic mean length; k – growth rate; t0 – hypothetic age at zero length) and growth performance index values (Φ′) obtained in different areas for S. solea
Ø′ | Sex | Locality | Reference | |||
---|---|---|---|---|---|---|
Eastern Atlantic | ||||||
34.2 | 0.35 | −1.3 | 2.62 | M | Dutch ports | |
35.6 | 0.38 | −0.5 | 2.68 | F | Dutch ports | |
36.9 | 0.28 | −2.3 | 2.58 | F | Dutch ports | |
37.4 | 0.31 | – | 2.64 | M + F | North Sea | |
39.0 | 0.4 | – | 2.78 | M + F | North Sea | |
39.6 | 0.35 | −0.8 | 2.74 | F | Dutch ports | |
42.4 | 0.39 | 0.09 | 2.85 | M | Bay of Biscay | |
48.2 | 0.32 | 0.08 | 2.88 | F | Bay of Biscay | |
49.8 | 0.13 | – | 2.51 | M + F | Celtic Sea | |
Central and Western Mediterranean Sea | ||||||
37.9 | 0.504 | −5.36 | 2.86 | F | Adriatic Sea | |
38.3 | 0.492 | −3.57 | 2.86 | M + F | Adriatic Sea | |
40.1 | 0.68 | – | 3.04 | M + F | Adriatic Sea | |
39.6 | 0.44 | −0.46 | 2.84 | M + F | Northern Adriatic | |
35.8 | 0.41 | – | 2.72 | M + F | Tyrrhenian Sea | |
48.8 | 0.24 | −0.77 | 2.76 | M + F | Gulf of Lion | |
47.2 | 0.274 | – | 2.79 | F | Gulf of Lion | |
38.8 | 0.24 | −1.09 | 2.56 | M | Castellon coast | |
46.4 | 0.22 | −0.75 | 2.68 | F | Castellon coast | |
Eastern Mediterranean Sea | ||||||
26.0 | 0.221 | −1.31 | 2.17 | M | Iskenderun Bay | |
29.9 | 0.181 | −1.55 | 2.21 | F | ||
30.0 | 0.33 | −1.51 | 2.47 | M + F | Bardawil Lagoon | |
Aegean Sea | ||||||
31.1 | 0.33 | −1.04 | 2.5 | M | Aegean Sea | |
42.5 | 0.17 | −1.96 | 2.49 | F | ||
30.21 | 0.19 | −0,26 | 2.24 | M | Aegean Sea | |
36.95 | 0.23 | −0,03 | 2.50 | F | ||
34.9 | 0.38 | −0.41 | 2.67 | M + F | Amvrakikos Gulf | |
Sea of Marmara | ||||||
28.63 | 0.62 | −0.91 | 2.71 | M | Sea of Marmara | |
35.79 | 0.72 | −1.06 | 2.96 | F | ||
31.3 | 0.57 | 0.03 | 2.74 | M | Sea of Marmara | This study |
35.8 | 0.37 | −0.49 | 2.67 | F |
Parameters of the length–weight relationship (W = a TLb) for all samples, females (F), males (M) and unidentified specimens of S. solea
Growth type | ||||
---|---|---|---|---|
Pooled | 0.022 | 2.6838 | 0.9456 | Negative Allometric |
F | 0.0349 | 2.5536 | 0.9032 | |
M | 0.0253 | 2.6235 | 0.934 | |
Unidentified | 0.0201 | 2.7179 | 0.941 |
Mortality rates and exploitation ratio for S. solea from different geographical areas in the Mediterranean Basin
Fishing technique | Region | Reference | ||||
---|---|---|---|---|---|---|
2.49 | 1.83 | 0.66 | 0.73 | – | Egypt | |
1.7 | 1.18 | 0.52 | 0.69 | gillnet | Egypt | |
1.32 | 8.2 | 0.5 | 0.6 | bottom trawl | Iskenderun Bay | |
0.97 | 0.66 | 0.31 | 0.68 | gillnet | Güllük Bay | |
1.42 | 1.01 | 0.47 | 0.68 | beam trawl & gillnet | Sea of Marmara | this study |
Length–weight relationships for S. solea in different areas
Sex | Length (cm) | Length | N | Locality | References | |||
---|---|---|---|---|---|---|---|---|
Eastern Atlantic | ||||||||
0.005 | 3.20 | M + F | 10.0–42.0 | – | 0.975 | 334 | North Sea | |
0.0071 | 3.095 | M + F | 21.0–43.0 | TL | 0.954 | 325 | North Sea coast of Germany | |
0.0048 | 3.175 | M + F | 2.0–59.0 | TL | 0.998 | 5804 | Bay of Biscay | |
0.0039 | 3.264 | M + F | 3.0–49.0 | TL | 1.000 | 3,799 | East and West Channel | |
0.0036 | 3.313 | M + F | 11.0–29.0 | TL | – | 13 | German Bight & Clyde | |
0.0046 | 3.21 | M + F | – | – | – | 518 | Douarnenez Bay, Brittany | |
0.004 | 3.251 | M + F | 9.0–49.0 | TL | – | 945 | North–eastern Atlantic | |
0.0078 | 3.08 | M + F | 10.5–38.9 | TL | 0.969 | – | Arade Estuary, Central Algarve | |
0.0071 | 3.092 | M + F | 20.5–46.0 | TL | 0.908 | 58 | Nazaré to St André | |
Central and Western Mediterranean Sea | ||||||||
0.0086 | 2.99 | F | – | TL | – | – | Gulf of Lion | |
0.0109 | 2.94 | M | – | TL | – | – | ||
0.0062 | 3.04 | M + F | 5.0–45.0 | TL | 0.980 | 561 | Gulf of Lion | |
0.0106 | 3.062 | M + F | 6.5–25.0 | SL | 0.981 | 82 | Acquitina, Italy | |
0.0019 | 3.453 | M + F | 19.8–32.5 | TL | 0.946 | 2,130 | Northern Adriatic | |
0.01 | 2.96 | M + F | 15.0–45.0 | TL | 0.932 | 406 | French Catalan Coast | |
Eastern Mediterranean Sea | ||||||||
0.049 | 2.35 | Juvenile | 11.2–24.4 | TL | 0.980 | 13 | Iskenderun Bay | |
0.0117 | 2.988 | M | 8.8–25.0 | TL | 0.922 | 550 | Iskenderun Bay | |
0.0091 | 3.077 | F | 10.5–28.2 | TL | 0.947 | 533 | ||
Aegean Sea | ||||||||
0.0098 | 3.002 | Juvenile | 11.0–22.1 | TL | 0.988 | 21 | Porto-Lagos | |
0.0023 | 3.369 | M + F | 18.6–33.7 | TL | 0.920 | 171 | Aegean Sea | |
0.0088 | 3.024 | M | 3.1–29.0 | TL | 0.9925 | 529 | Güllük Bay | |
0.007 | 3.1013 | F | 7.1–37.0 | TL | 0.9866 | 607 | ||
Sea of Marmara | ||||||||
0.0043 | 3.171 | Juvenile | 6.9–16.0 | TL | 0.928 | 55 | Sea of Marmara | |
0.0183 | 2.727 | M | 13.0–27.0 | TL | – | 206 | Sea of Marmara | |
0.0011 | 3.674 | F | 13.0–34.0 | TL | – | 218 | ||
0.0253 | 2.6235 | M | 11.8–27.8 | TL | 0.9 | 294 | Sea of Marmara | This study |
0.0349 | 2.5536 | F | 12.6–29.5 | TL | 0.934 | 248 |
Length at the onset of sexual maturity (cm) for S. solea from different studies
Sex | Country | Region | Study | |
---|---|---|---|---|
18.8 | M + F | Germany | North Sea | |
22.0 | M | France | Bay of Biscay | |
24.8 | M + F | UK | North Sea | |
26.0 | M + F | North Sea | ||
27.0 | M + F | Holland | Dutch ports | |
28.0 | F | France | East and West Channel | |
29.0 | M + F | UK | Celtic Sea | |
30.0 | M + F | Holland | Dutch ports | |
31.0 | F | France | Bay of Biscay | |
32.0 | F | France | Douarnenez Bay, Brittany | |
20.8 | F | Turkey | Aegean Sea | |
22.7 | M | |||
20.4 | F | Turkey | Güllük Bay | |
21.5 | F | Turkey | Sea of Marmara | this study |
18.6 | M |
Length-at-age key for all samples of S. solea based on otolith age readings
Length class (cm) | Age (years) | Total | ||
---|---|---|---|---|
1 | 2 | 3 | ||
11 | 6 | 6 | ||
12 | 9 | 9 | ||
13 | 18 | 18 | ||
14 | 16 | 16 | ||
15 | 13 | 13 | ||
16 | 10 | 10 | ||
17 | 3 | 3 | ||
18 | 5 | 3 | 8 | |
19 | 16 | 16 | ||
20 | 38 | 38 | ||
21 | 77 | 77 | ||
22 | 111 | 111 | ||
23 | 52 | 29 | 81 | |
24 | 67 | 67 | ||
25 | 47 | 47 | ||
26 | 19 | 19 | ||
27 | 15 | 15 | ||
28 | 9 | 9 | ||
29 | 4 | 4 | ||
Total | 80 | 297 | 190 | 567 |