Abstract
The vast majority of ectothermic organisms grow larger when developing at cooler environmental temperatures, a pattern frequently referred to as the temperature-size rule (TSR). Assuming that this reaction norm has adaptive significance, life history theory predicts that converse patterns may evolve if favored by natural selection, namely if the costs associated with complying to the TSR outweigh the benefits. Calcifying ectotherms may comprise such an exception not following the TSR, because calcification is expected to be more costly at lower temperatures thus increasing associated costs. To test this hypothesis, we reared wild-caught juveniles of the intertidal gastropod Monetaria annulus and compared their shell sizes at the end of the juvenile stage between two rearing temperatures. Contrary to our prediction, M. annulus does follow the TSR, suggesting that increased calcification costs at lower temperatures are not high enough to break the TSR. Such plastic responses should be considered when interpreting geographical patterns such as latitudinal size clines, which may be caused at least partly by phenotypic plasticity.
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Introduction
Most ectotherms mature at a larger size at lower developmental temperatures, a pattern of wide taxonomic prevalence which has been coined the temperature-size rule (TSR; Atkinson 1994). The TSR may comprise either a non-adaptive physiological interaction of an organism with its environment (van Voorhies 1996; van der Have and de Jong 1996; Zuo et al. 2012) or may have adaptive significance (Partridge and French 1996; Angilletta and Dunham 2003; Walters and Hassall 2006). Seeking for a general explanation applicable to all ectothermic taxa, Angilletta et al. (2004) have reviewed several hypotheses based on, for example, the compound interest hypothesis (Partridge and French 1996; Fischer and Fiedler 2002; Atkinson et al. 2003), differential thermal sensitivities of anabolic and catabolic processes (Angilletta and Dunham 2003; Kozlowski et al. 2004), and a positive correlation between temperature and juvenile mortality (Atkinson 1994, 1995, 1996; Irie and Iwasa 2003). Arendt (2010) demonstrated that the TSR may evolve if fecundity increases more steeply with adult body size in cold than in warm environments. Despite these research efforts, the TSR has remained enigmatic and a general explanation for its widespread occurrence is still lacking.
In order to distinguish between the existing hypotheses outlined above, the study of systems comprising exceptions to the TSR along with the respective species’ ecology should prove particularly valuable. Atkinson (1995), for instance, mentioned six exceptions to the TSR, one marine diatom, one parasitic copepod, and four mayfly species (see also Walters and Hassall 2006; Zuo et al. 2012). Although the suspected causal factors differed among species, all explanations followed the same straight forward logic: ectotherms follow the TSR if the benefits of complying with it outweigh the costs, and exceptions occur in case some “additional costs” invert the balance of fitness. The general benefits and costs of following the TSR might be similar across taxa (Angilletta et al. 2004), while any additional or extraordinary costs may stem from the species-specific ecological background.
Some of the above hypotheses can be tested with optimality models, in which the optimal maturation size at a given temperature is determined by the balance between the benefits of enlarging adult size (referred to as adult size advantage, abbreviated as ASA) and the fitness loss of extending the growth period (the delayed maturation disadvantage, DMD). According to such models, the TSR is evolutionarily maintained, if the optimal maturation size is smaller at higher temperatures (e.g., Kingsolver and Huey 2008). This can be achieved if, for example, the fitness increment of early maturation is larger at higher temperatures (Fig. 1a). More specifically, a positive correlation between temperature and juvenile mortality should select for the TSR, because earlier maturation at higher temperatures mitigates the fitness loss of increased mortality (Atkinson 1994, 1995, 1996; Irie and Iwasa 2003). Moreover, a shorter generation time will increase population growth rate and thereby involves compound interest benefits (Partridge and French 1996; Fischer and Fiedler 2002; Atkinson et al. 2003). However, these effects can be cancelled out, if (1) growth rates decrease very steeply with decreasing temperature and/or if (2) growth rates are simply very slow (see “Appendix 1”). As a result, natural selection may favor thermal reaction norms opposite to the TSR (Fig. 1b). In this case, the very slow growth due to low temperatures can be regarded as the additional cost mentioned above.
One example for such an additional cost which may result in not following the TSR may be calcification, that is, the construction of an exoskeleton in marine ectotherms. We assume two reasons that calcification at low temperatures results in very low growth rates thus selecting against the TSR. First, as the solubility of calcium carbonate (CaCO3) increases with decreasing temperature, calcification is expected to be more costly at lower temperatures (Vermeij 1987; Morse et al. 2007). Accumulating evidence suggests this relationship holds regardless of whether seawater is undersaturated with CaCO3 or not (see “Discussion” section). Thus, the overall growth rates of calcifiers decrease more steeply with decreasing temperature than those of non-calcifiers. Second, somatic growth of calcifiers should always be slower than that of non-calcifiers, when temperature and other conditions are equal (see “Discussion” section). This is a principle deductively reached from the optimal allocation theory assuming the energetic tradeoff between somatic and exoskeletal growth (Irie and Iwasa 2005; Irie et al. 2010). Consequently, the costs may outweigh the benefits of achieving a large adult body size in calcifying ectotherms, resulting in smaller rather than larger size at lower temperatures. Although being straight forward, this hypothesis has not been tested thus far. Note here that most studies on the TSR have focused on (non-calcifying) terrestrial organisms (Partridge and French 1996; Nylin and Gotthard 1998, Karl et al. 2008), while studies on calcifying marine organisms are exceedingly rare (but see O’Dea and Okamura 2000; Hosono 2011).
Against the above background, we here test experimentally whether the gold-ringed cowry, Monetaria annulus (Linnaeus 1758), being a marine intertidal gastropod, follows the TSR and thereby whether the costs associated with calcification may break the TSR. An alternative hypothesis is that such costs are minimal across the thermal range that we employ, and thus, the TSR-type reaction norm appears.
Materials and methods
Study organism
Monetaria annulus is an intertidal gastropod that comprises a well-suited model for studying the TSR and thermal adaptation in general, because this species occurs in a wide range of thermal environments. It has a wide latitudinal distribution throughout the Indo-Pacific tropics and subtropics and is found in different types of habitat, for example, in small tide pools with intense heat stress and in subtidal habitats without thermal stress (Katoh 1989; Irie 2006).
Ontogeny after the planktonic stage consists of the juvenile, the callus-building, and the reproductive stage (Fig. 2). Somatic growth and shell construction take place during the juvenile stage, which starts with a metamorphosis from planktotrophic to benthic lifestyle through settlement and ends with the second metamorphosis at which body size is fixed. All cowries exhibit explicit determinate growth (sensu Kozlowski and Wiegert 1987), because no somatic growth occurs after the juvenile stage. The callus is considered to be built for physical defense against predators (Irie and Iwasa 2003, 2005). Both juvenile shell and callus are purely composed of aragonite (T. Irie, unpublished data). In the present study, we focus on the shell size at the end of the juvenile stage (hereinafter referred to as “size at metamorphosis”), which is a good proxy of soft body size at metamorphosis (Irie and Adams 2007).
Experimental design
We performed three experiments with two constant rearing temperatures each to investigate the effects of developmental temperature on body size in M. annulus (Table 1). Since rearing planktonic larvae is not feasible, we collected juvenile M. annulus from a wild population at the Sesoko coast (see Irie 2006; Irie and Morimoto 2008) during low tides in early winter for each experiment (see Table 1 for sample sizes). Juveniles were immediately transferred to Sesoko Station (Tropical Biosphere Research Center, University of the Ryukyus). Initial shell width (IW; Fig. 3) was measured for incorporating into the statistical model in order to control the effect of growth prior to collection (see “Statistical analyses” below). All juveniles were placed individually into 500-ml plastic bottles supplied with fresh seawater and randomly divided among two temperature-controlled water tanks with a higher or a lower temperature.
In the three experiments, different temperatures were used (cf. Table 1) as (1) no a priori information about minimum and maximum temperatures for juvenile development were available and (2) to test for the effects of different amplitudes on body size. In experiment 1, 21 and 27 °C were used, corresponding to the average ambient temperatures in the coldest and warmest months, respectively, at the field sampling site (see Irie and Fischer 2009). In experiment 2, cowries were reared at 30 and 33 °C for examining patterns in a higher temperature range. In experiment 3, finally, 24 and 34 °C were used, corresponding to maximum temperature per hour in the coldest and warmest month, respectively. We could not use more than two treatments at once because (1) the number of juveniles collected at a time, (2) the amount of algae cultured for ad libitum food supply, and (3) the electric supply to maintain the temperature of running seawater were limited. Temperatures within bottles were recorded hourly by digital data loggers (Thermochron: DS1921G-F50), showing only slight deviations from the preset temperatures (Table 1). Nevertheless, rearing temperatures fluctuated slightly throughout the experiments in response to the thermal fluctuation of incoming seawater (Table 1). Cowries were provided with algae for feeding ad libitum throughout all experiments. See Irie and Morimoto (2008) for detailed information on rearing equipment, daily maintenance, and algae cultures.
At the end of the juvenile stage, cowries dome the final shell whorl upwards and eventually narrow the shell aperture by turning the outer lip inwards. We defined the final day of the juvenile stage (=day of metamorphosis) by the construction of the final outer lip and measured the juvenile shell width at this time (JW; Fig. 3) as size at metamorphosis. Additionally, we measured development time as days to metamorphosis (DTM), that is, from the onset of the rearing experiment until metamorphosis. Following metamorphosis, the external shells of all individuals were broken to determine the sex anatomically, because living cowries cannot be sexed.
Statistical analyses on metamorphic size
To test the null hypothesis that the size at metamorphosis is not significantly different among temperature treatments, metamorphic size (JW) was analyzed by applying an ANCOVA model with experimental year, temperature, and sex as fixed-effect factors and IW as a covariate. To improve the estimation, we incorporated the assumption into the model that the expected JW of the individuals staying in the wild until metamorphosis is identical between the two treatments (see “Appendix 2”; Irie and Morimoto 2008). In this case, the null hypothesis to be tested is that the slopes of the regression lines of JW on IW are identical between the two thermal treatments (i.e., a L = a H; see Fig. 4 and “Appendix 2”). Thus, rejecting the null hypothesis is a necessary condition to demonstrate that M. annulus follows the TSR. The null hypothesis was tested using \(F \equiv \frac{{{{\left( {{\text{RSS}}_{\text{null}} - {\text{RSS}}_{\text{alt}} } \right)} \mathord{\left/ {\vphantom {{\left( {{\text{RSS}}_{\text{null}} - {\text{RSS}}_{\text{alt}} } \right)} {\left( {\theta_{\text{alt}} - \theta_{\text{null}} } \right)}}} \right. \kern-0pt} {\left( {\theta_{\text{alt}} - \theta_{\text{null}} } \right)}}}}{{{{{\text{RSS}}_{\text{alt}} } \mathord{\left/ {\vphantom {{{\text{RSS}}_{\text{alt}} } {\left( {n - \theta_{\text{alt}} } \right)}}} \right. \kern-0pt} {\left( {n - \theta_{\text{alt}} } \right)}}}},\) where \(\theta\) is the number of parameters to be estimated and n is the total number of individuals with available data. The subscript “null” indicates the null model, in which no constraint was imposed on the parameter values of y-intercept (b), but the slope (a) must be identical between the two temperatures (i.e., a L = a H; see Fig. 4 and “Appendix 2”). On the other hand, all the parameters are free in the alternative model, abbreviated with “alt” (see Faraway 2002; Ruppert et al. 2003). Assuming that the residuals in the full model follow a normal distribution, the statistic has an F-distribution with \(\theta_{\text{alt}} - \theta_{\text{null}}\) and \(n - \theta_{\text{alt}}\) degrees of freedom. Please refer to the discussion for a justification of the statistical approach used here.
In addition to the above parametric tests, we used a bootstrap approach because sample sizes in our experiments were relatively low and the mathematical assumptions on residual distributions may not be fully met. Therefore, the F-value calculated from the original data was compared with a bootstrap distribution constructed by repeating the following steps 10,000 times: (1) randomly resample the data with replacement across the two thermal treatments, keeping the sample size of each sex equal to the original one; (2) calculate F for the newly generated data after fitting regression lines. We rejected the null hypothesis at the 5 % level of significance, that is, when the original F-value was in the top 5 % of the bootstrap distribution (Efron and Tibshirani 1993; Davison and Hinkley 1997).
Statistical analyses on growth period
Larger maturation size is often accompanied by a prolonged growth period at lower temperatures. In our experiments, individuals with a small initial size needed longer until metamorphosis, particularly when reared at low temperatures. Consequently, the dispersion of DTM potentially depends on both initial shell size and rearing temperature. We thus assumed that the DTM follows a lognormal distribution, in which the mean and the variance are positively interdependent, in order to test the null hypothesis that the median is identical between the two different temperature regimes.
The null hypothesis that the median DTM is identical between the two rearing temperatures was tested by calculating the likelihood ratio test statistic, given as D = −2ln(L null/L alt) = −2(LL null − LL alt), where L and LL are the maximum likelihood and its logarithm, respectively (see “Appendix 3”). The subscript “null” indicates the null model, in which no constraint was imposed on the parameter values of the scale parameter (\(\sigma^{2}\)), but the location parameters (\(\alpha\) and \(\beta\)) must be identical between the two temperatures (i.e., \(\alpha_{\text{L}} = \alpha_{\text{H}}\) and \(\beta_{\text{L}} = \beta_{\text{H}}\)). On the other hand, all the parameters are free in the alternative model, abbreviated with “alt.” The statistic D approximately follows a \(\chi^{2}\)-distribution with the degree of freedom being equal to the difference in the number of free parameters between the null and alternative model.
Since the \(\chi^{2}\)-approximation may not be sufficiently reliable, we performed again bootstrap tests by comparing the D-value calculated from the original data with a bootstrap distribution constructed by repeating the following steps 10,000 times: (1) randomly resample the data with replacement across the two thermal treatments, keeping the sample size of each sex equal to the original one; (2) calculate D for the newly generated data after fitting the above model. We rejected the null hypothesis at the 5 % level of significance, that is, when the original D-value was in the top 5 % of the bootstrap distribution (Efron and Tibshirani 1993; Davison and Hinkley 1997).
Results
In agreement with the TSR, M. annulus exhibited a remarkable trend toward smaller size at metamorphosis when reared at higher developmental temperatures, particularly so in females (Fig. 5). When pooling across experiments and sexes, this pattern was statistically significant regardless of whether the F-approximation or bootstrapping method was used (Table 2). When analyzing experiments separately though, differences between rearing temperatures were only significant in experiment 3, in which the temperature difference was largest (Table 2). Likewise, when pooling across experiments significant differences were restricted to females, while for males only a trend was detected. The good agreement between F-approximation and bootstrapping (Table 2) is consistent with the residual normality in our data, as tested with a Shapiro–Wilk test (W = 0.993, n = 228, P > 0.05).
Given equal initial shell size, M. annulus had a longer growing period at lower than at higher temperatures, except in experiment 2 (Fig. 6; Table 3). This pattern was statistically significant throughout, except for experiment 2 in which the temperature difference was relatively small (Table 3; Fig. 6c, d). Results of χ2-approximation versus bootstrapping generally yielded very similar results (Table 3).
Discussion
In the present experiments, M. annulus reared at lower temperatures matured at a larger size and had a longer growing period, at least if the thermal difference between the two treatments was sufficiently large. These results suggest that this species does follow the TSR. The notion that M. annulus thus does not comprise an exception from the TSR is consistent with field data, showing that individuals developing in warmer seasons metamorphose at a smaller size than those that grow in cooler seasons (Irie and Fischer 2009). Especially, the results obtained from experiment 3 (10 °C difference) are in good agreement with these field data (Irie and Fischer 2009).
We had assumed in our working hypothesis that lower temperatures entail more energy to precipitate a certain amount of CaCO3. To verify this assumption, the saturation state of seawater with respect to aragonite, Ω ar = [Ca2+][CO3 2−]/K sp, where [Ca2+] and [CO3 2−] are the concentrations of calcium and carbonate ions, respectively, needs to be considered. The solubility product, K sp, increases with decreasing temperature, which is the reason why aragonite becomes more soluble at lower temperatures (e.g., Plummer and Busenberg 1982; Vermeij 1987). Theoretically, aragonite precipitates from seawater when Ω ar > 1 and dissolution occurs when Ω ar < 1 (e.g., Peterson 2010). In fact, there can be no doubt that the surface seawater in Okinawa is oversaturated with respect to aragonite (Ω ar > 3 throughout the year; for example, Ishii et al. 2011; Feely et al. 2012) and so it is in our experiments (i.e., 21–34 °C). Thus, calcification may actually incur very little costs challenging our original hypothesis. However, marine calcifiers are known to keep the Ω ar at the place of calcification much higher than 1. For example, the golfball coral, Favia fragum, maintains the calcifying fluid Ω ar at around 15, when the Ω ar of external seawater is ~2.4 (Cohen et al. 2009; Cohen and Holcomb 2009). In addition, the speed of calcification increases with increasing external Ω ar even when Ω ar > 1 (Marubini and Atkinson 1999; Ohde and Hossain 2004). Marine calcifiers thus seem to pay an energetic cost to elevate the Ω ar in the calcifying fluid by decreasing pH and increasing the calcium ion concentration by a Ca2+/H+ exchanger (Ca2+-ATPase) across the mantle membrane (Cohen and McConnaughey 2003; McConnaughey and Gillikin 2008). This is probably needed because Ω ar > 1 is not sufficient for the precipitation of aragonite (see Cohen and Holcomb 2009). In summary, lower temperatures entail more energy to maintain a constant level of the calcifying fluid Ω ar, because Ω ar decreases with decreasing temperature. This is the rational behind the idea that the overall growth rates of calcifiers decrease more steeply with decreasing temperature than those of non-calcifiers (see “Appendix 1”).
Our working hypothesis also assumes that the very slow growth due to calcification at low temperatures may withdraw any adaptive advantage of the TSR, such that reaction norms converse to the TSR may have evolved in calcifying ectotherms (see “Appendix 1”). Molluscan shells are composed of inorganic crystal (CaCO3) and an organic matrix within and between crystals, both of which require energetic costs to produce (Palmer 1983, 1992). Including the cost of synthesizing the organic component, the total energy to construct shells seems to be quantitatively comparable to that of somatic growth (e.g., Palmer 1992). Accordingly, there is an energetic tradeoff between somatic and skeletal growth (Irie and Iwasa 2005; Irie et al. 2010). This suggests that calcifying ectotherms always grow more slowly than shell-less ones, if energy income and other conditions are equal (but see Bourdeau 2010, proposing a tradeoff-free mechanism that makes thicker shells induced by slower somatic growth due to lower food availability). Furthermore, shell building may limit the rate of somatic growth if low temperatures retard shell building more strongly than somatic growth, because body growth cannot proceed in advance of skeletal growth (Palmer 1981).
Nevertheless, our data do not support the above expectation. An explanation is that the fitness loss due to shell building at low temperatures was not high enough to break the TSR in M. annulus. In other words, the energetic cost of shell building might be too low. On the other hand, low temperatures substantially extended the juvenile stage in our experiments. In experiment 1, for example, the growth period at 21 °C was more than twice as long as at 27 °C, while mean maturation size was nearly the same between the two treatments. Hence, a prolonged growth period may compensate the very slow growth at low temperatures in order to avoid reduced adult size.
Another possible explanation for our results is that there is some fundamental constraint resulting in the TSR. This idea was supported by the finding that larger body size at lower temperature is caused by an increase in cell size, while the number of cells remained constant in Caenorhabditis elegans (van Voorhies 1996). This hypothesis implicitly assumes that the negative relationship between temperature and cell size is invariable due to a genetic or physiological constraint, suggesting that the TSR itself has no adaptive significance. However, this hypothesis was rejected by Kammenga et al. (2007), who discovered a wild-type strain of C. elegans not following the TSR. Even if such a constraint would exist, natural selection should be able to break the TSR by working on the slope of the reaction norm, which is supported by the occurrence of several exceptions to the TSR at the species and population level (Atkinson 1995; Walters and Hassall 2006; Zuo et al. 2012).
Interestingly, females showed a much stronger response to different rearing temperatures than males in our experiments. This might be a consequence of the female-biased sexual size dimorphism in M. annulus (Irie and Adams 2007; Irie and Morimoto 2008). Thus, juvenile males are more developed than females at the start of rearing when initial size is equal between the sexes. Therefore, males may have been exposed to controlled thermal conditions for a shorter period of time than females, leaving less opportunity to respond to a temperature change. Alternatively, the costs and benefits associated with plastic responses to temperature may differ across the sexes (e.g., in butterflies; see Fischer and Fiedler 2000, 2001).
In summary, our results suggest that M. annulus does conform to the TSR. The associated plastic response to differences in the developmental environment may also affect macrogeographic patterns of adult body size in cowries. Tissot (1984) demonstrated that the congener M. caputserpentis exhibits a latitudinal size cline from southeast Africa to the west Pacific, by showing that shell size at metamorphosis correlates negatively with average seawater temperature (see also Irie 1997; Irie and Iwasa 2003). Similar trends were found in other cypraeid species, for example, Cypraea tigris (Kay 1961; Foin 1972), Mauritia arabica (Schilder 1961), and Erronea errones (Schilder and Schilder 1968). It is currently unknown whether such clines result from genetic adaptation or phenotypic plasticity (Tissot 1984, 1988; Irie 1997, 2006; Irie and Iwasa 2003), but our current results suggest that the latter possibility should not be dismissed.
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Acknowledgments
The authors are grateful to P. Kraufvelin, W. C. E. P. Verberk, W. Zuo, and three anonymous reviewers for valuable comments, and to S. Nakamura and Y. Nakano for maintaining the equipment necessary for rearing experiments at Sesoko Station. We also thank K. Baba, Y. Iwasa, K. Sakai, S. Tuljapurkar, and K. Yamahira for helpful discussions. This project was funded by the Japan Society for the Promotion of Science (JSPS).
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Communicated by P. Kraufvelin.
Appendices
Appendix 1: Mathematical proof for the working hypothesis
Assuming that the instantaneous mortality rate, μ, is independent of age or size, the lifetime reproductive success (R 0) of a determinate grower is simply given by
where M x is the age-independent fecundity rate of an individual that matures at age x, L x is the probability that the individual survives until maturity (i.e., L x = e−μx), and t is the age after maturity (i.e., t = −x at birth). Taking the natural logarithm of R 0 leads to
where the first term on the right-hand side can be regarded as the adult size advantage (ASA), if fecundity increases with increasing size. On the other hand, the second term is the delayed maturation disadvantage (DMD), because a longer growth period decreases the survivorship until maturity. Let v(a,x) be the size at maturity of an individual that matures at age x with growth rates, a, where growth rates (a) is passively and uniquely determined by temperature, θ. If \(x^{*}\) and \(v^{*}\) designate the age and size at maturity that maximize the fitness R 0, then the dependency of the optimal size at maturity (\(v^{*}\)) on temperature (θ) is
where ∂μ/∂θ > 0 is assumed to reflect adaptive significance of the TSR.
To illustrate the above results, we assign specific functions to the growth and fecundity functions: dv/dx = av k and M x = v(x)k, respectively. k is a coefficient for metabolism that often takes a value of two-thirds. Approximating the initial size v(0) to zero, maturation size is explicitly given as v(x) = (a(1 − k)x)1/(1−k). From Eq. (2), ASA = k ln v(x) and DMD = − μx = − μv(x)1−k/a(1 − k) in this case (see Fig. 1). Taking the derivative of ln R 0 with respect to x, equation it to zero, and solving it for x gives the optimal age at maturity, \(x^{*}\) = k/(1 − k)μ, and thus \(v^{*}\) = v(\(x^{*}\)) = (ak/μ)1/(1−k). The necessary condition that the TSR is selected against is
which is obtained by setting the right-hand side of Eq. (3) to be positive and then rearranging it. When dv/dx = av k and M x = v(x)k, we have
or equivalently,
This inequality suggests that the TSR is more likely to be broken when (1) growth rates (a) are small, (2) growth rates (a) decrease more steeply with temperature (θ), or (3) both. The same conclusion is reached when assuming the linear growth function [i.e., v(x) = ax], for example.
Appendix 2: Incorporating NJW into the ANCOVA model
Prior to the statistical analyses on metamorphic size, we defined the “native shell width at metamorphosis” (NJW) as the shell width at metamorphosis of the individuals staying in the wild until metamorphosis (Fig. 4; see also Irie and Morimoto 2008). The NJW should be identical between the two treatments, because the individuals who stayed in the wild until metamorphosis were subject to the common environmental conditions. We incorporated this into our statistical model in order to improve the estimation of regression lines. NJW can be estimated as the intersection point between the regression line of JW on IW and the diagonal line (Fig. 4). As the individuals with the same sex and from the same experiment have the same expected NJW, the regression coefficients, a and b, can be estimated by minimizing the total sum of residual squares, \({\text{RSS}} = \phi_{\text{F}} + \phi_{\text{M}}\). The sum of residual squares for females (\(\phi_{\text{F}}\)) and males (\(\phi_{\text{M}}\)) are given as
and
where IW i and JW i are initial shell width and juvenile shell width at metamorphosis, respectively, for i-th individual out of N total individuals. Subscripts F and M signify females and males, respectively. Similarly, subscripts L and H denote the lower and the higher temperature treatments conducted in the same year, respectively. Using the least-square estimates of the regression slope (\(\hat{a}\)) and the y-intercept (\(\hat{b}\)), the expected NJW is calculated as:
Since the expected NJW is identical between the two temperature treatments (but not between the sexes) within one experiment, it follows that:
which reduces the number of parameters to be estimated. All the least-square estimates were numerically computed using Mathematica (version 7 for Windows, Wolfram Research, Champaign, IL).
One may argue that our data could be equally well analyzed by applying an ordinary ANCOVA method with JW as the dependent variable, IW as the covariate, and temperature and sex as fixed-effect factors. In this case, the interaction effect between IW and temperature should be significant if sample size is sufficiently large; then the conformance to the TSR is accepted when a higher rearing temperature leads to smaller y-intercept (see Fig. 4). However, regression lines were sometimes unstable (i.e., slopes were too steep to attain a meaningful interpretation) in our data, probably because our sample sizes were relatively low and IW was not scattered broadly enough. This is the main reason why we implemented a model with a mathematical constraint designated by Eq. (10), instead of performing an ordinary ANCOVA. Except for this point, our method is mathematically equivalent with ANCOVA, which should be noticed by looking at using the least-square regression lines and the F-statistic computed by dividing the explained variance between groups by the unexplained variance within the groups.
Appendix 3: ML estimation of the lognormal regression parameters
If Y (>0) is a random variable that follows a lognormal distribution and linearly depends on a positive covariate, x, its probability density function is expressed as:
where the parameters are \(\alpha \in \Re\), \(\beta \in \Re\), and \(\sigma^{2} > 0\). In this case, the median of Y is given as \({\text{Med}}\left[ Y \right] = \exp \left[ {\alpha + \beta x} \right]\). The maximum likelihood estimates of the parameters are those that maximize the likelihood function:
or its logarithmic form:
where y i is DTM and x i is IW for the i-th individual out of n individuals. Taking the partial derivative of LL with respect to each parameter and equating it to zero yields:
and
respectively (the “hat” indicates the maximum likelihood estimate of each parameter). Simultaneous Eqs. (14a) and (14b) provide an explicit function of \(\hat{\alpha }\):
which also gives the maximum likelihood estimates of \(\beta\) and \(\sigma^{2}\) from Eqs. (14b) and (14c).
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Irie, T., Morimoto, N. & Fischer, K. Higher calcification costs at lower temperatures do not break the temperature-size rule in an intertidal gastropod with determinate growth. Mar Biol 160, 2619–2629 (2013). https://doi.org/10.1007/s00227-013-2256-y
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DOI: https://doi.org/10.1007/s00227-013-2256-y