- Original Article
Age and growth in three populations of Dosinia exoleta (Bivalvia: Veneridae) from the Portuguese coast
Helgoland Marine Research volume 67, pages 639–652 (2013)
The present study aimed at estimating the age and growth in three populations of Dosinia exoleta from the Portuguese coast (Aveiro in the north, Setúbal in the southwest and Faro in the south). Two techniques were compared to ascertain the most suitable method for ageing D. exoleta. Growth marks on the shell surface and acetate peel replicas of sectioned shells were the techniques applied. Two hypotheses were tested: growth parameters present latitudinal variation along the Portuguese coast; growth parameters are influenced by the fishing exploitation. Shell surface rings proved inappropriate for ageing this species, whereas acetate peels provided realistic estimates of the von Bertalanffy growth parameters (K, L ∞ and t 0). A latitudinal gradient in growth rate was detected, with a clear southward increase in the growth coefficient (K) of D. exoleta (Faro > Setúbal and Aveiro) indicating that warmer waters in southern Portugal provide optimal conditions for the growth of this species. Fishing exploitation in northern Portugal targets larger individuals and leaves behind a younger population of smaller individuals, decreasing the asymptotic shell length (L ∞ ) of D. exoleta from Aveiro. The overall growth performance was compared among populations of D. exoleta and with other venerid species worldwide.
The rayed artemis or mature dosinia (Dosinia exoleta Linnaeus, 1758) is distributed from the Norwegian and Baltic Seas, southwards to the Iberian Peninsula, into the Mediterranean, and along the western coast of Africa to Senegal and Gabon (Tebble 1966). This species burrows deeply in sand, mud and gravel bottoms, from the intertidal zone to 70 m depth (Poppe and Goto 1993; Macedo et al. 1999), but can be found up to 150 m depth (Anon 2001). In Portugal, D. exoleta is among the target species of the bivalve dredging fleet operating in the northern coast, whereas along the southwestern and southern coasts, it constitutes a by-catch species of the dredge fishery (Gaspar et al. 2007). Fishery exploitation in the northern coast started around 2007 and since then annual landings ranged between a maximum of 37.0 tons in 2007 and a minimum of 9.4 tons in 2010 (DGPA 2012). The latest statistics available on the landings of D. exoleta in northern Portugal (Matosinhos wholesale market) reported total landings of 15.3 tons in 2011, corresponding to an overall value for first sale of 15.3 thousand euro (DGPA 2012).
Knowledge on the age and growth of commercially exploited bivalve species is a crucial requirement for the successful management of the fishery (Gaspar et al. 2004). In bivalves, growth rings on the shell surface have been widely used to make inferences about age and growth rate (Deval 2001). Although being the most quick and economic method, in some species it is difficult to discern real seasonal growth rings from false rings caused by gonad development and spawning, diseases, extreme temperatures, storms and damage during dredging (Gaspar et al. 1995, 2004; Richardson 2001; Keller et al. 2002; Moura et al. 2009). These constraints have been overcome by analysing internal shell microgrowth banding patterns revealed in acetate peel replicas of sectioned shells (Jones et al. 1990; Ramón and Richardson 1992; Richardson 2001). Although being a time-consuming method, internal growth lines visible in acetate peel replicas generally provide a reliable record of the age and growth history of individuals (Anwar et al. 1990). However, some problems in the identification of the annual ring may also occur, especially in long-lived species. In older specimens, the umbonal region is usually eroded, making impossible to identify the first growth rings (Gaspar et al. 2004). In addition, in older individuals growth becomes slower and the later growth rings are deposited very close together at the shell margin, making them hardly discernible (Deval and Oray 1998; Ezgeta-Balić et al. 2011). Furthermore, in some years clearly defined rings may not be formed (Anwar et al. 1990). In some species, age can also be estimated by counting the growth lines visible in acetate peel replicas of the umbonal region of the shell (e.g. Anwar et al. 1990; Ridgway et al. 2011; Peharda et al. 2012).
Information on the age and growth rate of D. exoleta is very scarce and limited to studies on population dynamics performed in Norway by Tunberg (1979). Initially, this author attempted to find annually deposited growth marks in the shells, using surface rings and acetate peels, but both ageing techniques were unsuccessful (Tunberg 1979). Later, an in situ experiment with marked individuals was performed, but results were not satisfactory due to disturbance of the studied specimens and to the weakness of the regression analysis (Tunberg 1983a). Once again, both surface rings and acetate peels were analysed; however, it was impossible to establish an acceptable correlation between the number of growth marks and individual age (Tunberg 1983a).
Taking into account the current scarcity of information, this study aimed at improving the knowledge on the age and growth of D. exoleta by providing data on shell banding, age and growth rate estimates for three populations from the Portuguese coast (Aveiro in the north, Setúbal in the southwest and Faro in the south). Two techniques (surface rings and acetate peels) were employed and compared in order to ascertain which is the most suitable for ageing this species. This study allowed assessing the occurrence of latitudinal variation in the growth parameters of D. exoleta along the Portuguese coast, as well as comparing growth parameters between fishery-exploited (Aveiro) and unexploited (Setúbal and Faro) populations of this species. Finally, the overall growth performance (OGP) was compared among populations of D. exoleta and with analogous information available for other venerid species worldwide.
Materials and methods
Samples of D. exoleta were collected between May and June 2010 in three areas along the Portuguese coast: Aveiro (40º59′–41º03′N) in the northern coast, Setúbal (38º23′–38º27′N) in the southwestern coast and Faro (36º58′–36º59′N) in the southern coast (Fig. 1). Individuals were caught by the IPMA’s RV “Diplodus” operating bivalve dredges on sandy bottoms between 8 and 12 m depth in the southern coast, 8 and 15 m depth in the southwestern coast and between 15 and 30 m depth in the northern. Following the usual fishing procedures, the dredges were towed for 15 min at a constant speed of 2 knots. The dredges used were identical to those operated by the commercial fleet. In brief, the dredge weighs around 40 kg and consists of a rigid iron structure with a toothed lower bar (15 cm tooth length with an angle of 20º). The catch is retained in a net bag 2.5 m long with diamond mesh size of 25 mm for further details on the dredge design, characteristics and dimensions, see (Gaspar et al. 2003); (Leitão et al. 2009).
In order to assess its influence on the growth of D. exoleta, data on seawater temperature along the Portuguese coast were provided by the Hydrographical Institute (IH). For this purpose were gathered data monitored during 2010 by the oceanographic buoys closest to the bivalve collecting sites (buoys of Leixões in the northern coast, Sines in the southwestern coast and Faro in the southern coast). Mean annual temperature was compared between study areas through analysis of variance (ANOVA). If ANOVA assumptions (normality of data and homogeneity of variances) were not met, the nonparametric Kruskal–Wallis test (ANOVA on ranks) was performed. Whenever significant differences were detected by ANOVA or Kruskal–Wallis test, pairwise multiple comparisons were made using Tukey or Dunn’s tests, respectively (Zar 1999). Statistical analyses were performed with the software package SigmaStat© (version 3.5) with significance considered for P < 0.05.
In the laboratory, a total of 50 individuals from each collecting site were measured for shell length (SL) (maximum distance along the anterior–posterior axis) to the nearest 0.1 mm using a digital calliper. Specimens analysed were within the following SL (ranges Aveiro = 40.4–46.8 mm (42.5 ± 1.7 mm); Setúbal = 41.7–52.0 mm (46.7 ± 3.1 mm); Faro = 36.9–44.3 mm (41.0 ± 2.1 mm)). Subsequently, for estimating age and growth, the rings deposited on the external surface of the shells were counted and measured with the digital calliper. In addition, the internal structure of each shell was analysed using acetate peel replicas of polished and etched sections of resin-embedded valves, following the technique previously adopted with success in other commercially exploited bivalve species from the Portuguese coast (for further details see Gaspar et al. 1995, 2002, 2004; Moura et al. 2009). Based on previous studies with sympatric bivalve species from the Portuguese coast, such as Callista chione (Moura et al. 2009) and Chamelea gallina (Gaspar et al. 2004), it was assumed that the growth marks in the shells of D. exoleta are annual, being deposited in late autumn–early winter when shell growth is slower. Each growth ring observed in the acetate peel was marked on the glass slide. After digitising the entire acetate peel and respective marks, the distance between the umbo and each growth ring was measured to the nearest 0.1 mm using the digital image analysis software ImageJ (version 1.43). In both techniques (shell surface and acetate peels), counting and measuring of growth rings were made by two independent observers and a second reading was performed whenever numbers did not coincide. Since the measurements in acetate peels are relative to shell height (SH), data were converted into SL using the following morphometric relationship (n = 259, r = 0.990; Gaspar et al. 2002):
Von Bertalanffy growth functions (VBGF) were fitted separately to the age–length data obtained using the two ageing methods (shell surface rings and internal growth marks). An iterative curve fitting procedure employing nonlinear least-squares regression (Gauss–Newton method) provides estimates of the growth coefficient (K), asymptotic SL (L ∞ ) and theoretical age at SL (zero (t 0), through the following equation (von Bertalanffy 1938):
Linear methods commonly used in the statistical comparison of growth data (ANCOVA or ANOVA) cannot be employed on the VBGF because of its nonlinear formulation and high degree of correlation between its three parameters (K, L ∞ and t 0) (Chen et al. 1992). Comparisons of VBGF can be performed using two general approaches, either by testing individual parameters or by using likelihood ratio statistics. In the present case, D. exoleta growth equations were compared between populations (Aveiro, Setúbal and Faro) using likelihood ratio tests (Kimura 1980; Cerrato 1990). This method allows testing several hypotheses to compare two growth equations, by analysing each growth parameter separately or all growth parameters simultaneously. Fitting and comparison of VBGF were performed using the packages “nlstools” (Baty and Delignette-Muller 2011), “car” (Fox and Weisberg 2011) and “fishmethods” (Nelson 2011) of the free software R (version 2.14.1) (R Development Core Team 2011).
Individual growth is a nonlinear process that must be described by multiparameter nonlinear models (such as the VBGF), making it difficult to compare growth among different taxa in a definite and statistically proper way (Brey 1999). To overcome this difficulty, several growth performance indices have been developed. In the present study,OGP (P) (Pauly 1979) was employed to compare the growth parameters estimated for D. exoleta in the present study with those available in the literature for other venerid species, using the following equation:
Mean annual seawater temperature (Fig. 1) was significantly different (H = 4292.159, P < 0.001) between collecting sites: Aveiro = 15.4 ± 1.8 °C (11.4–20.4 °C), Setúbal = 17.3 ± 1.2 °C (15.1–21.2 °C) and Faro = 20.2 ± 3.1 °C (14.6–26.6 °C). There was a remarkable thermal range between the northernmost site (minimum of 11.4 °C in December 2010 in Aveiro) and the southernmost site (maximum of 26.6 °C in August 2010 in Faro). As expected, seawater temperature displayed a clear northward decreasing trend: Aveiro < Setúbal (Q = 30.519, P < 0.05) and Setúbal < Faro (Q = 31.826, P < 0.05).
Shell surface rings and acetate peel replicas of D. exoleta shell sections are presented in Fig. 2. Observation of the outer prismatic layer revealed distinct growth patterns deposited parallel to the ventral edge of the shell, but defined lines were not found in the umbonal region. The growth marks formed a growth ring in the outer shell surface that was associated with a cleft, and occasionally, two clefts were associated with an annual growth ring (Fig. 2a). In the acetate peels, the gradual decrease in the growth increment zone was the key to distinguish annual growth rings from false rings (caused by stress or shell damage). The former were characterised by the progressive narrowing of growth bands (Fig. 2b), whereas the latter were characterised by the sudden interruption of the natural growth pattern. In false rings, it is also possible to observe a cleft in the shell surface, but the acetate peel does not display narrowing in the microgrowth increments (Fig. 2c).
The mean length-at-age and respective VBGF of D. exoleta populations from Aveiro, Setúbal and Faro, estimated using both ageing techniques (surface rings and acetate peels), are compiled in Table 1. The VBG parameters obtained from surface rings (Fig. 2d) displayed unrealistically high asymptotic SL’s (Aveiro: L ∞ = 76.6 mm; Setúbal: L ∞ = 65.8 mm; Faro: L ∞ = 53.3 mm), and therefore, this ageing method was considered inappropriate for estimating D. exoleta age and growth. The comparison between shell surface rings and microgrowth patterns revealed by the acetate peel replica of the same individual (Fig. 2a, d) supports this conclusion. In contrast, the VBG parameters (K, L ∞ and t 0) estimated using the acetate peels were fairly realistic (Table 1). Accordingly, VBGF based on growth marks revealed in the acetate peels of the three populations of D. exoleta from the Portuguese coast (Aveiro, Setúbal and Faro) are presented in Fig. 3.
The likelihood ratio tests for comparison of VBG parameters between populations of D. exoleta are compiled in Table 2. When all VBG parameters (K, L ∞ and t 0) were analysed simultaneously (H4:VBGF), all growth curves displayed highly significant differences (P < 0.001) between the populations from Aveiro, Setúbal and Faro. When each VBG parameter was analysed separately, it was possible to determine which parameter (K, L ∞ or t 0) was significantly different among populations. The growth coefficient (H1: K) was significantly higher in D. exoleta from Faro (K = 0.50 year−1) than in the populations from Aveiro (K = 0.28 year−1) and Setúbal (K = 0.30 year−1). The asymptotic SL (H2:L ∞) was slightly higher in D. exoleta from Setúbal (L ∞ = 47.1 mm), although not statistically different from those in the populations from Faro (L ∞ = 42.9 mm) and Aveiro (L ∞ = 43.9 mm). Finally, the theoretical age at SL (zero (H3:t 0), considered the VBG parameter with lower biological significance, only displayed significant differences between the populations from Faro (t 0 = −0.07 years) and Aveiro (t 0 = 0.27 years) (Table 2). Overall, growth rates of D. exoleta presented a latitudinal gradient along the Portuguese coast and were directly related to mean annual seawater temperature at the collecting sites. Indeed, the growth rate was highest in the southernmost and warmest site (Faro: K = 0.50 year−1, temperature = 20.2 °C) and lowest in the northernmost and coldest site (Aveiro: K = 0.28 year−1, temperature = 15.4 °C), with the transitional population at an intermediate position (Setúbal: K = 0.30 year−1, temperature = 17.3 °C).
Two VBG parameters (K and L ∞) were applied to calculate the OGP of D. exoleta along the Portuguese coast. The OGP values obtained for the three studied populations were P = 4.374 in Aveiro, P = 4.496 in Setúbal and P = 4.597 in Faro. The VBG parameters and corresponding OGP values for D. exoleta and other venerid bivalve species are compiled in Table 3 and compared among different taxa in the auximetric grid presented in Fig. 4.
Age and growth of D. exoleta were more accurately estimated based on internal growth marks revealed in acetate peel replicas of sectioned shells than directly from surface growth rings. Although quick and economic, the examination of surface rings proved to be inadequate and unreliable for ageing D. exoleta. The unrealistic VBG parameters obtained from surface rings were already expected, because the growth rate is slower in older individuals making it difficult to distinguish and measure surface rings closer to the edge of the shell (Deval 2001; Gaspar et al. 2004; Moura et al. 2009). Differences between surface and internal growth rings were also observed in Macoma balthica. In this case, the number of annual lines obtained from external rings was always higher compared to the internal rings determined from the acetate peel replicas (Cardoso et al. 2012).
Examination of acetate peel replicas of D. exoleta allowed identifying different phases of shell growth, namely narrow dark lines (slow growth) separated by wider microgrowth increments (rapid growth). Other bivalve species from the Portuguese coast showed the same growth pattern, which has been associated with annual shell growth, including Donax trunculus (Gaspar et al. 1999), C. gallina (Gaspar et al. 2004) and C. chione (Moura et al. 2009). Periods of shell slow growth might be caused by low metabolic rates related to low seawater temperature (Lomovasky et al. 2002), lack of food (Arneri et al. 1998) and/or by diversion of metabolic products into gamete production (Lomovasky et al. 2002). Narrow bands corresponding to shell slow growth are often followed by a reduction in the peripheral layer of the shell, thus forming a cleft (Leontarakis and Richardson 2005). Indeed, in D. exoleta the narrowing of microgrowth bands also appeared to always match with a cleft on the shell surface. Moreover, occasionally two narrow bands were deposited very close together (appearing like a double band) and were reflected by the occurrence of two clefts on the shell surface. This phenomenon has also been detected in C. gallina by Ramón and Richardson (1992) and Gaspar et al. (2004). The occurrence of double clefts on the shell surface further strengthens the acetate peel technique as the most adequate and accurate method for ageing D. exoleta. The examination of acetate peel replicas of sectioned shells also allowed detecting several clefts associated with a sudden interruption of the natural growth pattern and that were interpreted as false rings. On the shell surface, false rings induced by gonad development and spawning, diseases, extreme temperatures, storms, predation or dredging are in most cases indistinguishable from seasonal growth rings (Gaspar et al. 2004). In some bivalve species, age can be estimated by counting the number of growth rings deposited in the umbonal region of the shell (e.g. Anwar et al. 1990; Ridgway et al. 2011; Cardoso et al. 2012; Peharda et al. 2012). However, this was unfeasible with D. exoleta, since in most acetate peels the growth rings in the umbonal region were absent or very difficult to discern. Similarly, in C. gallina, the growth bands in the umbonal region were only observed in a limited number of individuals, making this method inappropriate for ageing this species (Dalgiç et al. 2010).
The VBGF of the population of D. exoleta from Setúbal displayed the highest shell asymptotic length (L ∞), followed by the population from Aveiro. The population from Faro presented the lowest L ∞, but in contrast, showed the highest growth rate (K). The populations from Setúbal and Aveiro showed lower and similar growth rates (K). These different growth features between populations of D. exoleta are probably a consequence of the fishing exploitation and certainly also reflect different environmental conditions between the collecting sites, namely in terms of seawater temperature.
Along the Portuguese coast, only the population of D. exoleta from Aveiro is exploited, whereas in Setúbal and Faro, it constitutes a by-catch species of the dredge fishery (sorted on-board and discarded alive in the fishing beds). Therefore, the fishery targeting D. exoleta in Aveiro certainly causes a decline in the proportion of larger individuals (decreasing L ∞ ). Studies on the fishing impact on bivalve growth were relatively scarce but have increased recently. For instance, fishery exploitation appears to have decreased L ∞ and L max of Anadara tuberculosa from Bahía Magdalena, Mexico (Félix-Pico et al. 2009). Similarly, the decline in the abundance and sizes of A. tuberculosa over the years in Costa Rica suggest that the fishing pressure on this species is too high (Campos et al. 1990; Silva-Benavides and Bonilla-Carrion 2001).
The rayed artemis (or mature dosinia) is distributed along a widespread latitudinal range, from northern European coasts (probable northern limit in Finnmark) (Tunberg 1984) to western African coasts, not being found further south than Congo (Fischer-Piette 1968). This implies that Portugal is fairly within the middle of the latitudinal distribution of this species in the Atlantic Ocean. It is well known that physiological processes are influenced by the environmental conditions, namely temperature and food availability (e.g. Clarke 1987; Sprung 1991; Masilamoni et al. 2002), parameters that usually show an inverse trend with latitude (Barry and Carleton 2001; Jansen et al. 2007). With increasing latitude, it has been observed an increasing trend in reproductive effort, egg and larval size, whereas an opposite trend has been shown for age at first maturity, fecundity, reproductive output, growth rate and mortality (e.g. Clarke 1987; Contreras and Jaramillo 2003; Thatje et al. 2004; Ward and Hirst 2007; Petracco et al. 2010).
In the present study, it was also detected a latitudinal gradient in the growth of the three populations of D. exoleta, with growth rates (K) showing a southward increase (Faro > Setúbal ≈ Aveiro). Latitudinal trends in the physiological performance of marine invertebrates are commonly observed (Santos et al. 2011). Latitude has no environmental meaning by itself, being a proxy of annual solar energy input that translates mainly into average annual seawater temperature (Heilmayer et al. 2003), but also into primary production and related parameters. On a geographical scale, differences in growth rate of bivalves have been frequently associated with latitudinal gradients in seawater temperature. Examples of this phenomenon include C. chione (Hall et al. 1974), M. balthica (Beukema and Meehan 1985), Mercenaria campechiensis and Mercenaria mercenaria (Heck et al. 2002), Mya arenaria (Appeldoorn 1995), Placopecten magellanicus (MacDonald and Thompson 1988), Tivela stultorum (Hall et al. 1974) and Zygochlamys patagonica (Gutiérrez and Defeo 2003).
In the present study along the Portuguese coast, higher seawater temperatures were registered in the south, which may explain the higher growth rate displayed by the population of D. exoleta from Faro compared to the populations from the other two collecting sites. However, the abundance of this species in Faro is very low compared to Setúbal and Aveiro (Fig. 5) (Gaspar et al. 2010a, b, c). This north–south decreasing trend also supports that colder waters constitute a more suitable environment for this species. Indeed, although showing wide thermal range, the optimal environmental conditions for this eurythermal species appear to be shifted northwards. Tunberg (1983a) estimated a shell asymptotic length (L ∞ ) of 51.3 mm for D. exoleta from Eggholmen (western Norway), but this value was considered somewhat small compared to the maximum SL (reached in that area, where this species is abundant with a density of 9.9 ± 2.9 ind m−2 (Tunberg 1983a). Moreover, higher abundances were observed in Raunefjorden (western Norway), where D. exoleta reached an overall density of 17.1 ind m−2 (Tunberg 1984). The higher shell asymptotic length in northern (Norway: L ∞ = 51.3 mm) than in southern populations (Portugal: L ∞ = 42.9–47.1 mm), further confirms that although this species grows faster in warmer waters, higher latitudes provide the most favourable environmental conditions for the development of population of D. exoleta.
Although with a few exceptions, the general consensus is that bivalves from low latitudes grow faster, attain a smaller maximum size and have a shorter lifespan than conspecifics from high latitudes (Newell 1964). In the present study, the calculation of the OGP allowed comparing growth among populations of D. exoleta and with other venerid bivalves. The values of OGP obtained for D. exoleta along the Portuguese coast corroborate the above-mentioned latitudinal gradient in growth and the influence of mean annual seawater temperature at the collecting sites Faro > Setúbal > Aveiro. In terms of intra-specific comparison, the only data available in the literature on the growth of D. exoleta lead to slightly higher OGP in Norway (P = 4.687) compared to the populations along the Portuguese coast (P = 4.374 in Aveiro to P = 4.597 in Faro). In general, worldwide comparisons highlight that OGP increases with decreasing latitude, in a general trend that is correlated with average annual seawater temperature (Heilmayer et al. 2003). However, this trend was not observed in the case of D. exoleta since a higher OGP was determined for Norway compared to that obtained for the Portuguese populations. This may be a consequence of the method used by Tunberg (1983a) to estimate growth. This author applied the mark-recapture method which may lead to bias in growth estimates whenever the data set is not representative of the full size range of the population (Haddon 2001). The growth parameters estimated by Tunberg (1983a) were mainly based on large individuals, therefore are probably biased, which may have resulted in a higher OGP for the Norwegian population of D. exoleta.
Within the genus, D. exoleta both from Portugal and Norway has a slightly higher OGP than the sympatric Dosinia lupinus from western Norway (P = 4.225) (Tunberg 1983b), but lower than D. nipponica (4.702 < P < 5.255) from the Pacific Ocean (Tanabe and Oba 1988). In terms of inter-specific comparison, the auximetric grid revealed that D. exoleta has an average growth performance (within the family Veneridae). Indeed, D. exoleta is within the range of OGP values obtained for Amiantis umbonella, Ameghinomya antiqua, Eurhomalea exalbida, Venerupis corrugata and Venus verrucosa (mainly between 4.5 < P < 5.0). In most cases, the sympatric C. gallina and Chamelea striatula exhibited lower OGP (mostly P < 4.5), whereas Callista brevisiphonata and C. chione (usually P > 5.0) and M. mercenaria (mostly P > 5.0) displayed the highest growth performances within the family Veneridae (Fig. 4).
The present study was the first to successfully estimate age and growth of D. exoleta by using the acetate peel technique, thus making available realistic growth parameters (K and L ∞ ) for this species. Furthermore, the present study showed some differences between the growth parameters of the three populations. Results suggest that growth is influenced by geographical distribution and probably also by fishing exploitation. In general, the latitudinal gradient in the growth features of the three populations revealed that, besides growing faster in warm waters, colder environments are beneficial for this species. It also seems that fishing exploitation affects the asymptotic SL of the populations of D. exoleta (decreasing L ∞ ), but further investigation should be performed to confirm this hypothesis. Knowledge on the age and growth of exploited bivalve species is fundamental for the proposal of fishery management measures. The present study provided the first data available on the growth parameters of D. exoleta, but further studies should be conducted, namely the estimation of the size at first sexual maturity, decisive for establishing a minimum landing size for the catches of this species by the bivalve dredging fleet that operates in northern Portugal.
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The authors would like to acknowledge the technical staff of the IPIMAR’s Delegation of Aveiro for collecting and sampling the bivalves. Recognition is owed to Cte. Ventura Soares (Technical Director of the–IH) for kindly providing data on seawater temperature. Thanks are also due to João Cúrdia for photographing the acetate peel replicas of the shells. Paulo Vasconcelos is funded by a post-doctoral Grant (SFRH/BPD/26348/2006) awarded by the Fundação para a Ciência e Tecnologia (FCT–Portugal). This study was performed within the framework of the project “Desarrollo Sostenible de las Pesquerías Artesanales del Arco Atlántico–PRESPO” (Programme INTERREG IV B, co-financed by EU, ERDF funds). Finally, the authors also acknowledge two anonymous reviewers, for valuable comments and suggestions that improved the revised version of the manuscript.
Communicated by Franke.
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Moura, P., Vasconcelos, P. & Gaspar, M.B. Age and growth in three populations of Dosinia exoleta (Bivalvia: Veneridae) from the Portuguese coast. Helgol Mar Res 67, 639–652 (2013). https://doi.org/10.1007/s10152-013-0350-7
- Dosinia exoleta
- Latitudinal variation
- Fishing effects