Dorsal colour pattern variation in Eurasian mountain vipers (genus
Transcription
Dorsal colour pattern variation in Eurasian mountain vipers (genus
Zoologischer Anzeiger 257 (2015) 1–9 Contents lists available at ScienceDirect Zoologischer Anzeiger journal homepage: www.elsevier.com/locate/jcz Dorsal colour pattern variation in Eurasian mountain vipers (genus Montivipera): A trade-off between thermoregulation and crypsis Mahdi Rajabizadeh a,b,c,∗ , Dominique Adriaens a , Mohammad Kaboli d , Jaleh Sarafraz e , Mohsen Ahmadi d a Evolutionary Morphology of Vertebrates, Ghent University, Ghent, Belgium Department of Biodiversity, Institute of Science and High Technology and Environmental Sciences, Graduate University of Advanced Technology, Kerman, Iran c Iranian Plateau Herpetology Research Group (IPHRG), Faculty of Science, Razi University, 6714967346 Kermanshah, Iran d Department of Fishery and Environment, Faculty of Natural Resources, Tehran University, Tehran, Iran e Marine Biology Section, Department of Biology, Ghent University, Ghent, Belgium b a r t i c l e i n f o Article history: Received 21 August 2014 Received in revised form 12 March 2015 Accepted 19 March 2015 Available online 4 April 2015 Keywords: Crypsis Colour Pattern Montivipera Thermoregulation a b s t r a c t Reptile colouration has long been studied as an example of adaptive evolution. Several functions have been proposed for variety of snake colour and pattern with the most common suggestions being camouflage, aposematism and thermoregulation. Montivipera raddei species complex shows a remarkable variation in dorsal colour pattern, but so far there has not been a comprehensive study performed on the adaptive nature of their colour pattern. The dorsal colour pattern of 111 specimens belonging to the M. raddei species complex, originating from 23 localities across its distribution range, were studied to explore intra and interspecific variation in the colour pattern. A generalized linear model analysis showed that there is a significant relationship between the dorsal colour pattern of Montivipera latifii, Montivipera raddei raddei and Montivipera raddei albicornuta, and the environmental factors of the habitat, including elevation, average annual temperature, average annual solar radiation, average annual precipitation, vegetation type and substrate colour. The results suggest that the dorsal colour pattern variation in the M. raddei species complex is affected by a complex trade-off between thermoregulation and crypsis. © 2015 Elsevier GmbH. All rights reserved. 1. Introduction Several functions have been proposed for understanding the variety of snake colour and pattern, with the most common suggestions being camouflage, aposematism and thermoregulation (see Allen et al., 2013). Among visual effects, crypsis may represent the major function (and hence selective pressure) explaining the adaptive nature of colour pattern variation (Vincent, 1982). There are numerous examples of cryptic colour and pattern in reptiles (Brodie, 1992; King, 1992; Shine and Harlow, 1998; Wilson et al., 2006; Farallo and Forstner, 2012; Isaac and Gregory, 2013). Aposematism, the use of bright colours and patterns by noxious animals to deter predators, is documented in reptiles too (Campbell and Lamar, 1989; Savage and Slowinski, 1992; Brodie, 1993; Brodie and ∗ Corresponding author at: Ghent University, Evolutionary Morphology of Vertebrates & Zoology Museum, K L Ledeganckstraat 35, B-9000 Gent, Belgium. Tel.: +98 9388288177. E-mail address: [email protected] (M. Rajabizadeh). http://dx.doi.org/10.1016/j.jcz.2015.03.006 0044-5231/© 2015 Elsevier GmbH. All rights reserved. Janzen, 1995; Valkonen et al., 2011). There are indications that in ectotherms, colour and thermal physiology are co-adapted, meaning that dark individuals with a lower skin reflectance are at an advantage under conditions of low temperature thermoregulation (Gibson and Falls, 1979; Peterson et al., 1993; Lawson and King, 1996; Bittner et al., 2002; Clusella-Trullas et al., 2007, 2009). The Montivipera raddei species complex (MRC) is a group of diurnal mountain dwelling vipers, distributed across north, northwestern and western Iran, southern half of Armenia, south of Azerbaijan, Nakhijavan and adjacent places in eastern Turkey. (Nilson and Andrén, 1986; Stümpel and Joger, 2009; Stümpel, 2012). These vipers show the typical viper’s zigzag pattern on their dorsum, in contrast with a dorsal ground colour. The MRC shows a remarkable variation in dorsal colour pattern, changing from a light dorsal pattern over a dark ground colour, to a dark pattern over a light ground colour. There is also variation in the shape of this dorsal pattern. In taxonomic studies of the MRC (e.g. Nilson and Andrén, 1986) dorsal colour and pattern have been used as important key characters in distinguishing MRC species. Although variation in colour 2 M. Rajabizadeh et al. / Zoologischer Anzeiger 257 (2015) 1–9 Fig. 1. Different populations of the Montivipera raddei species complex and their colour pattern. 1: Montivipera latifii in the central Alborz (D and E), 2: Montivipera raddei albicornuta in the Zanjan valley (F), 3: populations of Montivipera raddei raddei in the Iran and Turkey bordering mountains in the northwestern Iran and adjacent countries (referred to NW) (A and B), 4: populations of Montivipera raddei raddei in the isolated mountains in the northwestern Iran (Sahand, Sabalan, Kordestan and Tekab mountains, briefly referred to SSTK) (C), 5: Montivipera kuhrangica in the central Zagros. Blue markings represent potential distribution of the Montivipera raddei species complex, generated using Maxent modeling software (M. Yousefi, in lit. 2014). Photos A, B, C and E were taken by M. Rajabizadeh; D was taken by R. Behruz; F was taken by M. Kaboli. pattern in populations of the MRC could reflect an underlying level of biodiversity within this group, but reptile colouration has long been studied as an example of adaptive evolution (e.g. Cott, 1940; Rosenblum et al., 2004). So far there has not been a comprehensive study performed on the adaptive nature of intra- and inter-population variation in colour pattern of the MRC. In this paper, we tried to explore to what degree the observed variation in MRC’s colour pattern could be linked to specific environmental factors. Answering this question could also reveal whether colour pattern in the MRC reflects an adaptation to local environmental conditions. 2. Materials and methods 2.1. Taxonomy and distribution of the Montivipera raddei species complex Following Rajabizadeh (2013) small sized species of the MRC (maximum length 99 cm) consist of four taxa: Montivipera latifii (Mertens, Darevsky and Klemmer, 1967), Montivipera kuhrangica (Rajabizadeh et al., 2011), Montivipera raddei raddei (Boettger, 1890) and Montivipera raddei albicornuta (Nilson and Andrén, 1985). To look into the colour pattern variation across the MRC, the dorsal colour pattern in 52 M. raddei raddei, 28 M. raddei albicornuta, 29 M. latifii and two M. kuhrangica from 23 localities across the distribution range of this species complex were studied (Fig. 1, Appendices A–C). In summary, the taxonomy, distribution and dorsal colour pattern of the MRC are as follows: over a light brown or tan dorsal ground colour. A distinct character of this species is a high level of colour polymorphism in its dorsal pattern. So far, four different patterns have been identified in M. latifii (Fig. 1D and E, see also Mertens et al., 1967; Nilson and Andrén, 1986; Rajabizadeh et al., 2012). 2.1.2. Montivipera raddei albicornuta This subspecies inhabits the Zanjan valley (Fig. 1 and Appendix A). The dorsal ground colour is grey, light grey, greyish brown or light brown, with a brown or olive (rarely black), black bordered, zigzag band along the back (Fig. 1F). 2.1.3. Montivipera raddei raddei This subspecies is distributed across easternmost Turkey, northwestern Iran, Naxcivan, southern Armenia and the adjacent area in the Azerbaijan Republic (Fig. 1 and Appendix A). It has a blackish, dark grey, light grey or light brown dorsal ground colour. The dorsal pattern can be a narrow or broad zigzag band, consists of orange to yellow, often round blotches that sometimes, and especially on the lateral side, form a dark edge (Fig. 1A–C). 2.1.4. Montivipera kuhrangica Only three specimens were reported from a small area in the central Zagros mountains. The colour and pattern of this species is similar to that of M. raddei albicornuta (Rajabizadeh et al., 2011). Supplementry material related to this article found, in the online version, at http://dx.doi.org/10.1016/j.jcz.2015.03.006. 2.2. Colour pattern data 2.1.1. Montivipera latifii Current knowledge on the distribution of M. latifii suggests that this species is restricted to a small area in the central Alborz mountain range (Fig. 1 and Appendix A). It has a brown dorsal pattern Colour pattern data collected from live specimens were observed in the field, freshly killed specimens (i.e. road kills), freshly preserved specimens from museum collections and high quality M. Rajabizadeh et al. / Zoologischer Anzeiger 257 (2015) 1–9 3 Table 1 Result of ANOVA showing the relationship between the variation of viper’s colour pattern and the variation of normally distributed environmental data. (DGC): dorsal ground colour, (DPC): dorsal pattern colour and (DPS): shapes of the dorsal pattern. DGC Elevation Temperature Solar Radiation Precipitation DPC DPS Sum of squares df F Sig. Sum of squares df F Sig. Sum of squares df F Sig. 7375482.67 62.39 830712.68 890807.41 2 2 2 2 39.86 49.42 51.85 101.12 0.00 0.00 0.00 0.00 9150526.73 55.35 939177.95 991922.90 2 2 2 2 60.38 39.66 67.40 143.73 0.00 0.00 0.00 0.00 5690596 51.66132 431038.9 722371.1 2 2 2 2 26.25 35.26 18.18 60.26 0.00 0.00 0.00 0.00 pictures, since 2009. Since preserving solutions (i.e. methanol or chloroform) could impact the colour of the preserved viper specimens, colour data of older preserved specimens were not taken into account. To avoid age effect (personal observation) in the analysis, only adult specimens (defined as specimens with snout-vent length above 500 mm) were examined. Since these vipers are darker than usual during shedding, colour data of near to shedding specimens was not considered. Also, because no sexual dimorphism in the dorsal colour have been observed in the MRC (see Nilson and Andrén, 1986), and we did not observe a visible intersexual difference in the colour pattern, the colour pattern data of both sexes were pooled in the analysis. For studying the colour pattern variation in the M. raddei raddei species complex, the dorsal ground colour (DGC), dorsal pattern colour (DPC) and dorsal pattern shape (DPS) were documented. To carry out the statistical relationship analysis linked to environmental conditions, the dorsal ground colour was classified into light, medium and dark categories. To standardize the colour names, the X11 colour name system was used (available at http://en.wikipedia.org/wiki/X11 colour names). In this standard colour naming system, light dorsal ground colour refers to tonalities of tan colour. Dark dorsal ground colour refers to tonalities of grey, dark grey, cool grey, blackish, as well as greyish brown and greyish olive. Medium dorsal ground colour refers to light grey, brown and olive colour. Also the shape of the dorsal blotches was classified in two types: roundish and triangular (Table 1). pastures in north and northwestern Iran (characterized by predominant vegetation of cushion shaped bushes, including the genera Astragalus and Acanthophyllum). To facilitate the analysis of substrate data, the predominant colour of substrate stones in the habitat was regarded as the substrate’s colour. We had observed that in high elevation mountain habitats, with the presence of the MRC, the habitat is covered by stony outcrops, gravel fields and sandy soil admixed with differently sized rubble. Because the colour and composition of gravel fields and sandy soils are strongly related to the colour of parent stones, we used the predominant colour of substrate stones, as the substrate’s colour. Petrologic data were extracted from geology maps of Iran (www.ngdir.com), Turkey (http://www.mta.gov.tr/v2.0/eng/maps.php), Armenia (http://www.lydianinternational.co.uk/editorimages/documents/ GeologicalMapArmenia.pdf) and Azerbaijan (http://www.azenerji. com/en/powersystem/maps/geologicalmap.jpg). These stones were categorized in three colour types (light, medium and dark), based on the petrologic references and field data. In summary, dark stones were defined as stones similar in colour or darker than ophiolite or andesite basalt rocks. Light coloured stones were defined as stones similar in colour or lighter than tuff stones or limestone. Medium-coloured stones were separated as all other stones between dark and light categories, i.e. andesite stones (Appendix E). Supplementry material related to this article found, in the online version, at http://dx.doi.org/10.1016/j.jcz.2015.03.006. 2.3. Environmental factors 2.4. Analysis To investigate the relationship between colour pattern variation in the MRC and environmental factors, one biotic factor (vegetation) and six abiotic factors (elevation, temperature, solar radiation, precipitation and substrate colour), all of which have been proven to be linked to reptile colour pattern variation, were included in the analysis. Vipers of MRC exhibit a diurnal and seasonal movement pattern (Darevsky, 1966; Ettling et al., 2013). Since their minimum home range for a complete season is 32.3 ha ± 13.8 for males and 18.8 ha ± 4.7 for females (Ettling et al., 2013), we considered the average of environmental data from 100 ha (1 km2 ) around each viper’s locality. Data of elevation were extracted from Shuttle Radar Topography Mission elevation model with cell size of 1 km2 . Temperature and precipitation data of each viper’s locality were extracted from the annual mean temperature and annual mean precipitation data, provided by WorldClim (version 1.4, see Hijmans et al., 2005) with a cell size of 1 km2 . Solar radiation data were generated from annual mean temperature data, using ArcGIS (version 9.3) solar radiation extension, depicting total amount of incoming solar radiation (WH/m2 year, see Appendix D). Supplementry material related to this article found, in the online version, at http://dx.doi.org/10.1016/j.jcz.2015.03.006. For each viper’s locality, vegetation data was documented. As the MRC inhabits mountainous pastures or forests with more than 50% density of vegetation, only the vegetation type was considered, grouped in two categories: tree vegetation, referring to forest or shiblik vegetation, and bush vegetation, referring to mountain To evaluate the relationship between the viper’s colour pattern and environmental factors, an analysis of variance (ANOVA) was performed for normally distributed environmental data (elevation, temperature, solar radiation and precipitation) and a Kruskall–Wallis test was used for categorical data (type of vegetation and substrate colour). If an analysis was significant, we performed a LSD post-hoc individual one-way ANOVA test for normally distributed environmental data, and a pairwise Kruskall–Wallis test for categorical data to determine which factors were significantly related. Also, the relationship between viper colour pattern variation and variation of environmental factors were analysed by employing a generalized lineal model (GLM), using the three colour pattern variables as dependent (each by each in three different models) and including elevation, temperature, solar radiation, precipitation, vegetation and substrate colour as independent variables. The generalized linear model was corrected for dispersion under a Poisson distribution with a log link function with the variation of viper colour pattern and environmental factors disturbances as the response variables. For a better schematic presentation of the colour pattern and environmental factors variation across the populations of the MRC, with respect to the populations of the M. latifii in the central Alborz and M. raddei albicornuta in the Zanjan valley, populations of the M. raddei raddei were split into two eastern and western groups. Populations in Iran and Turkey bordering mountains and adjacent 4 M. Rajabizadeh et al. / Zoologischer Anzeiger 257 (2015) 1–9 countries were referred to NW and populations in the isolated mountains in the northwestern Iran (Sahand, Sabalan, Kordestan and Tekab Mountain) referred to SSTK (Fig. 1). M. kuhrangica was excluded from the statistical analysis because of the low number of samples (two specimens). Analyses were performed using SPSS (version 15) statistical software. Pie charts were generated using GraphPad Prism (version 6.05) GraphPad Software (www.graphpad.com). Table 3 Generalize linear model analysis on three colour pattern variables as dependent and an interaction of environmental factors as model: Elevation * Temperature * Solar Radiation * Precipitation * Vegetation Type * Stone Color. AICc: akaiki information criteria corrected for small sample size. DGC DPC DPS Pearson chi-square Log likelihood AICc df Sig. 4.902597 4.51 5.69 −144.763 −136.09 −131.68 345.5741 328.23 319.41 7 5 9 0.00 0.00 0.00 3. Results Studying the frequency of DPC, DPS and DGC in the MRC populations revealed, that specimens of the M. latifii had a dark and mainly triangular dorsal pattern, but rarely a mainly light dorsal ground colour (Fig. 2). At the localities of the Zanjan valley, M. raddei albicornuta had mainly darker dorsal ground colour and lighter dorsal pattern colour than M. latifii colour patterns (Fig. 2). Populations of the M. raddei raddei in the Iran and Turkey neighbouring mountains and adjacent countries (NW) had mainly darker dorsal ground colour and lighter dorsal pattern colour than both the M. raddei albicornuta colour pattern and M. latifii colour pattern, and mostly had a roundish shape in their dorsal pattern. M. raddei raddei in the isolated mountains in the northwestern Iran (SSTK) had both colour and pattern of M. raddei albicornuta of the Zanjan valley and M. raddei raddei in the bordering mountains and adjacent countries of Iran and Turkey (Fig. 2). In habitats of the MRC in the central Alborz towards the Zanjan valley and northwestern Iran, generally the elevation, temperature and solar radiation decreased, the precipitation increased. The pasture vegetation change towards tree vegetation and the predominant medium and light colour stones in the habitat changed to medium and dark colour stones (Figs. 3 and 4). There is a significant relationship between the variation of dorsal pattern colour (DPC), dorsal ground colour (DGC) and shapes of the dorsal pattern (DPS) of MRC species and the variation of environmental factors including elevation, average annual temperature, average annual solar radiation and average annual precipitation (Table 1). The variation of DPC, DGC and DPS in MRC species and variation of substrate colour and vegetation type in MRC habitat were significantly interrelated (Table 2). Pairwise analysis revealed that the variation of all the categories within DGC, DPC and DPS were significantly related to the variation of environmental factors, except that no significant relation was established between the variation of colour traits in M. latifii and M. raddei albicornuta, in relation to variation of vegetation type. No significant relation was observed between the variation of DPS in M. latifii and M. raddei albicornuta, in relation to stone colour variation. Generalized linear model analysis revealed that variation of colour pattern variables were significantly related to the interaction between elevation, temperature, solar radiation, precipitation, vegetation and substrate colour of the viper habitat (Table 3). 4. Discussion The variation of dorsal ground colour (and subsequently dorsal pattern colour) in the species of the M. raddei complex is related to the variation of thermal factors, including temperature and solar radiation. In the MRC distribution range, compared to M. latifii in the central Alborz, M. raddei raddei occupied a habitat located in the higher latitudes that is colder and gets lower solar radiation than central Alborz habitats. The influence of latitude is a major factor that affect the surface air temperature and solar radiation (see Fisher, 1986; Fan and Van den Dool, 2008). Darker colouration of the M. raddei raddei allows them to take more advantage of thermoregulation and radiation absorption, than the lighter M. latifii. A dark colouration in reptiles improves heat absorption over a shorter time (rapid heat absorption, but see Gibson and Falls, 1979; Pough et al., 1998; Lawson and King, 1996; Bittner et al., 2002; Clusella-Trullas et al., 2007, 2009; Norris and Kunz, 2012). Colour patterns within the M. raddei complex revealed relationships to the predominant colour of substrate stones in the habitats. The light dorsal ground colour of M. latifii in the central Alborz mountains is cryptic over the predominant light colour stones in its habitat. These light stones are mainly consisting of tuffaceous stones, which are characteristic of old volcanic activities in the Alborz mountains (Davidson et al., 2004). In the localities of the M. raddei raddei in the Northwestern Iran and adjacent areas, the dark ground colour of M. raddei raddei specimens is cryptic over the predominant dark colour stones. Since the Northwestern Iran localities are close to the closure suture of Tethys Sea ophiolite stones of the Tethys sea basin and basalt stones of the volcanic activities around the closure suture, are the predominant stones of these mountainous habitats (see Rögl, 1999). There are examples of relationships between reptile colour patterns and substrate colour (e.g. Vincent, 1982; Stuart-Fox et al., 2004; McGaugh, 2008; Micheletti et al., 2012; Farallo and Forstner, 2012). Cryptic colour patterns may help to avoid detection by predators (Farallo and Forstner, 2012) and by prey (Götmark, 1987). Although there is some evidence of disruptive colouration function of the viper zigzag patterns (Edmunds, 1974; Shine and Harlow, 1998), it has been shown that even vipers with an aposematic colour pattern (see Andrén and Nilson 1981; Forsman, 1995; Lindell and Forsman, 1996; Wüster et al., 2004; Niskanen and Mappes, 2005; Valkonen et al., 2011; Santos et al., 2014) can appear cryptic against their natural background from a distance (Sherratt and Beatty 2003; Tullberg et al., 2005). Vipers of the MRC are associated with habitat rocks and during the onset of spring and autumn, the snakes are mostly observed close to their hibernation sites between stony outcrops (see Darevsky, 1966; Behruz, 2010). MRC populations can take advantage from the cryptic colouration, which resulted from the association between the dorsal ground colour and the predominant colour of substrate rocks in the habitat. Selective pressure on the background matching (for a definition, see Stevens and Merilaita, 2011) resulting from predation pressure, reduce the Table 2 Result of Kruskall–Wallis analysis showing the relationship between the variation of viper’s colour pattern and the variation of vegetation type and substrate colour categories. (DPC): dorsal pattern colour, (DGC): dorsal ground colour and (DPS): shapes of the dorsal pattern. DGC Vegetation type Stone Color DPC DPS Chi-square df Sig. Chi-square df Sig. Chi-square df Sig. 49.59 58.56 2 2 0.00 0.00 63.63 52.15 2 2 0.00 0.00 60.59 47.39 2 2 0.00 0.00 M. Rajabizadeh et al. / Zoologischer Anzeiger 257 (2015) 1–9 5 Fig. 2. Frequency of the different dorsal colour pattern in the Montivipera raddei species complex and populations.)A): Shapes of the dorsal pattern (DPS), (B): dorsal pattern colour (DPC) and (C): dorsal ground colour (DGC). Number of examined specimens has been presented in the parentheses. 6 M. Rajabizadeh et al. / Zoologischer Anzeiger 257 (2015) 1–9 Fig. 3. Variation of climatic factors across the habitat of examine specimens of the Montivipera raddei species complex. (A): Elevation, (B): Solar Radiation, (C): Temperature, (D): Precipitation. The boxplot use the median and 25% quartiles for ends of the box. The lines (or whiskers) extended to the minimum and maximum values within 1.5 times the spread beyond the quartiles. Number of examined specimens has been presented in the parentheses. contrast between the substrate’s dominant colour and snake colour and patterns (Farallo and Forstner, 2012). The relationship between colour patterns in the species of the M. raddei complex and vegetation type can have a cryptic function. Dark colouration in M. raddei raddei which occurs in forested habitats favours crypsis in the cover of trees in contrast to snakes in the Central Alborz, where bush vegetation offer only limited cover. The light colouration of M. latifii serves mainly as a cryptic colouration over the substrate colour. Differences in the habitat sun exposure, resulting from differences in vegetation type, can affect crypsis as well (see Kark and Werner, 1993; Macedonia, 2001). Various environmental factors that are associated with the colour pattern variation in the MRC include thermal factors, vegetation type and the predominant colour of substrate stones in the habitat. In summary our results suggest that dorsal colour pattern variation in the MRC may be the result of a complex tradeoff between thermoregulation and crypsis. This trade-off between melanistic vs. natural colour pattern is well documented for several snake species (e.g. Gibson and Falls, 1979; Andrén and Nilson, 1981; Lawson and King, 1996; Bittner et al., 2002; Castella et al., 2013). Although M. raddei raddei takes advantage of its dark ground colour in terms of crypsis and thermoregulation. However in M. latifii, selection prefers the light dorsal ground colour that appears cryptic in light substrates, despite it is not aiding thermoregulation. A pale colouration of ectothermic organisms, such as snakes is expected to help primarily during unstable weather conditions such as in early spring when high body temperatures are difficult to achieve and maintain (e.g. Gibson and Falls, 1988). Recent findings support the hypothesis that thermal physiology and behaviour are co-adapted (Clusella-Trullas et al., 2007), enabling reptiles to adjust their behaviour to the thermal condition of the habitat in order to achieve optimum body temperatures (e.g. Adolph, 1990; Peterson et al., 1993). It is known that M. raddei raddei leave their hibernation sites in early spring and start courtship activities at the end of April or beginning of May (Terent év and Chernov, 1965). Courtship of M. latifii starts at warmer weather at about the second half of June (Andrén and Nilson, 1979). Since M. latifii has a pale colouration in comparison to M. raddei raddei, reproductive activities in late spring may help M. latifii to easily achieve its optimum body temperature. Our study confirms previous observations (e.g. Nilson and Andrén, 1986) that dorsal ground colour and dorsal pattern in M. Rajabizadeh et al. / Zoologischer Anzeiger 257 (2015) 1–9 7 Fig. 4. Variation of rock colouration (A) and vegetation structure (B) across the habitat of examine specimens of the Montivipera raddei species complex. Number of examined specimens has been presented in the parentheses. 8 M. Rajabizadeh et al. / Zoologischer Anzeiger 257 (2015) 1–9 Fig. 5. Phylogenetic distribution of different colour pattern morphs in the Montivipera raddei species complex. The figure shows variation of the colour pattern, parallel to dispersal of the Montivipera raddei species complex into central Alborz and in the direction of the northwestern Iran and adjacent area in Armenia and Turkey. Figure shows that dorsal colour pattern of Montivipera raddei populations in Sahand, Sabalan, Kordestan and Tekab mountain, referred to SSTK is a combination of both colour patterns of M. raddei albicornuta of the Zanjan valley and M. raddei raddei of northwestern Iran and adjacent area. Schematic pictures, light, medium and dark dorsal ground colour and dorsal pattern colour are presented as white, grey and dark grey colour. Also, variation of the shape of dorsal pattern is presented similar to natural pattern. Dorsal ground colour, dorsal pattern colour and the shape of dorsal pattern agree with data of Table 1. Phylogenetic tree modified from ‘Stümpel (2012)’. For the map legends, see Fig. 1. the MRC are mainly in contrasting colour with each other. Colour patterns represent a balance between the need for signalling (e.g. aposematic signalling) and the need for crypsis to avoid predation (Stuart-Fox et al., 2004). Hence, although dorsal ground colour in the MRC have thermoregulatory or cryptic functions, dorsal blotch colour serves as a contrasting colour in combination with a dorsal ground colour to keep a signalling function. In a phylogenetic context (following Stümpel, 2012), populations of M. raddei ssp. form a monophyletic lineage, showing different local adaptation and trade-offs with environmental factors leading to different colour pattern morphs (Fig. 5). The occurrence of both colour pattern morphs of M. raddei albicornuta and M. raddei raddei, within populations of the SSTK mountains (Fig. 1) is not accompanied by occurrence of both environmental condition of the Northwestern Iran and the Zanjan valley in the SSTK mountains. We hypothesize that the observed diversity within the colour and pattern of SSTK’s populations can be explained by occurrence of gene flow between the M. raddei ssp. populations, caused by Pleistocene climate oscillations (see Hewitt, 2004). The temperature decreased during Pleistocene cooling periods causing descending elevation shift in the habitat of mountain dwelling species. The SSTK mountains are adjacent to the Zanjan valley and Montivipera populations inhabiting these mountain ranges are isolated by a dry, intra-mountainous plain, named the Ghezel-Ozan basin. Although, at present the basin is not suitable habitat for M. raddei ssp., maybe because Pleistocene cold seasons altered the climate, it was a historical suitable habitat for M. raddei ssp. and mediated connection between Montivipera populations of the Zanjan valley and SSTK mountains. Species of M. raddei complex are an interesting model for studying local adaptation of colour and pattern traits, in response to different environmental factors and trade-off between thermoregulatory, cryptic and signalling function of colour pattern characters. Further studies are needed to determine thermal preferences and thermoregulatory behaviour of M. raddei ssp. and M. latifii to test whether thermoregulation and behaviour or co-adapted in these vipers. Acknowledgements No official funding was used for this research. We greatly thank Hasan Poudineh, Mohsen Ranjbaran, Nikolaus Stümpel, Ruzbeh Behruz, Maoud Yousefi, Benny Trapp, Göran Nilson and Jeff Ettling for their kind cooperation. We would like to thank Alexander Kupfer, Marco Zuffi and an anonymous referee for commenting on earlier manuscript versions. References Adolph, S.C., 1990. Influence of behavioral thermoregulation on microhabitat use by two Sceloporus lizards. Ecology 71, 315–327. Allen, W.L., Baddeley, R., Scott-Samuel, N.E., Cuthill, I.C., 2013. The evolution and function of pattern diversity in snakes. Behav. Ecol. 24, 1237–1250. Andrén, C., Nilson, G., 1979. 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