Metal hyperaccumulation is an uncommon but highly distinctive adaptation found in certain plants that can grow on metalliferous soils. Here we review what is known about evolution of metal hyperaccumulation in plants and describe a population-genetic analysis of the Alyssum serpyllifolium (Brassicaceae) species complex that includes populations of nickel-hyperaccumulating as well as non-accumulating plants growing on serpentine (S) and non-serpentine (NS) soils, respectively. To test whether the S and NS populations belong to the same or separate closely related species, we analysed genetic variation within and between four S and four NS populations from across the Iberian peninsula. Based on microsatellites, genetic variation was similar in S and NS populations (average Ho=0.48). The populations were significantly differentiated from each other (overall FST=0.23), and the degree of differentiation between S and NS populations was similar to that within these two groups. However, high S versus NS differentiation was observed in DNA polymorphism of two genes putatively involved in adaptation to serpentine environments, IREG1 and NRAMP4, whereas no such differentiation was found in a gene (ASIL1) not expected to play a specific role in ecological adaptation in A. serpyllifolium. These results indicate that S and NS populations belong to the same species and that nickel hyperaccumulation in A. serpyllifolium appears to represent a case of adaptation to growth on serpentine soils. Further functional and evolutionary genetic work in this system has the potential to significantly advance our understanding of the evolution of metal hyperaccumulation in plants.
Metal hyperaccumulation in plants
One of the most extraordinary adaptations known in the plant kingdom is the ability of certain plants to hyperaccumulate trace elements in their above-ground biomass. This trait is present in only ∼500 species, representing <0.2% of all angiosperm species (Reeves and Baker, 2000; Verbruggen et al., 2009; Krämer, 2010; Van der Ent et al., 2013). In contrast to metal excluders whose strategy is to control the uptake of metals into the root and prevent metal translocation to aerial organs, hyperaccumulators accumulate metals in the shoot to levels toxic to most other plants (Baker, 1981; Baker and Brooks, 1989; Baker et al., 2000; Pollard et al., 2002; Krämer, 2010; Rascio and Navari-Izzo, 2011). This is remarkable as the photosynthetic apparatus is one of the major targets of metal phytotoxicity, typically resulting in severe symptoms such as chlorosis and necrosis, wilting, abnormal development and reduced growth (Pandey and Sharma, 2002; Rahman et al., 2005; Marschner and Marschner, 2012). These toxic effects are a product of numerous harmful interactions at the cellular level (Haydon and Cobbett, 2007), including nonspecific binding of metals to enzyme functional groups and displacement of other metals from their binding sites, generation of reactive oxygen species by redox-active metals that can lead to disruption of the electron-transport chain (Qadir et al., 2004), lipid peroxidation and subsequent impairment of membrane integrity (Pandolfini et al., 1992; Ros et al., 1992; Gonnelli et al., 2001; Haydon and Cobbett, 2007; Krämer, 2010; Hanikenne and Nouet, 2011).
Of various hypotheses proposed to explain the possible adaptive advantage conferred by hyperaccumulation of metals (Boyd and Martens, 1992), only the herbivore/pathogen ‘elemental defence’ hypothesis has gathered plentiful supporting experimental evidence (Boyd, 2004, 2007). There have been many reports of decreased herbivory or reduced pathogen infection on plants hyperaccumulating metals (Poschenrieder et al., 2006; Boyd, 2007; Fones et al., 2010; Rascio and Navari-Izzo, 2011). However, in some studies no protective effect of metal hyperaccumulation against herbivory was observed (Noret et al., 2007), and designing trials to demonstrate such an effect in the field is particularly challenging, and hence further work is required to substantiate the selective advantage offered by metal hyperaccumulation. Nonetheless, it remains broadly true that hyperaccumulator species show a very high degree of metal tolerance (otherwise the accumulation of such exceptional concentrations of metals in the shoot would be suicidal), and that the degree of metal tolerance of different species or populations tends to be quite closely correlated with the metal content of the natural substrates on which they grow (Antonovics et al., 1971; Roosens et al., 2003; de la Fuente et al., 2007; Pollard et al., 2014).
Two broad hypotheses have been considered in the literature regarding the origin and spread of metallicolous populations, that is, those adapted to soils containing an elevated concentration of a particular metal (Pauwels et al., 2005). One is based on the observation that populations inhabiting metalliferous outcrops are often separated by large geographic distances; this would limit dispersal and genetic exchange between metallicolous populations, and instead would favour evolution of locally adapted metallicolous populations from nearby non-metalliferous sites (Schat et al., 1996) driven by ecological speciation (Rundle and Nosil, 2005). The other hypothesis proposes a single origin of a genetic adaptation to metalliferous substrates, its spread across outlying metalliferous sites and subsequent differentiation between more recently established metallicolous populations because of genetic drift. These alternative views resonate with earlier debates as to whether local populations of metal-tolerant plants occurring on metalliferous outcrops represent ‘neoendemics’ or ‘palaeoendemics’, respectively (equivalent to the ‘insular’ and ‘depleted’ species of Stebbins (1942), as discussed by Kazakou et al. (2008)). Correspondingly, non-metallicolous populations of such species could be either ancestral, as in the first scenario, or locally derived from metallicolous populations, as in the second.
Evolution of metal tolerance in plants
The question of whether metal tolerance is a constitutive trait across all populations of a species, or the degree to which ecotypic differentiation has occurred in response to different substrates, has been one of the most important issues underpinning hypotheses concerning the evolutionary origins of this trait. Two of the most intensively studied species of hyperaccumulator plants, Arabidopsis halleri (L.) O’Kane & Al-Shehbaz (formerly Cardaminopsis halleri (L.) Hayek) and Noccaea caerulescens (J Presl and C Presl) FK Mey. (formerly Thlaspi caerulescens J Presl and C Presl), display a basal, constitutive level of zinc tolerance and hyperaccumulation in both metallicolous and non-metallicolous populations (Meerts and Van Isacker, 1997; Bert et al., 2000, 2002; Escarré et al., 2000; Frérot et al., 2003; Pauwels et al., 2006; Meyer et al., 2010). However, across the geographic range of these species, there is a significant positive correlation between the degree of tolerance and substrate metal concentration, indicative of local adaptation to the natural habitat (Roosens et al., 2003; Pauwels et al., 2005). The relationship between metal tolerance and hyperaccumulation is rather less clear, and although the highest shoot metal concentrations observed in the field are found in populations growing on metalliferous soils, there is some evidence that the level of metal hyperaccumulation shown by these populations may be inversely related to their degree of metal tolerance (Bert et al., 2000; Roosens et al., 2003).
Although it is generally believed that the emergence of the hyperaccumulation trait in these two model species was driven by, and coincident with, the appearance of anthropogenic metal-polluted sites in the mining regions of Europe (Pauwels et al., 2006; Jiménez-Ambriz et al., 2007; Besnard et al., 2009), recent research on A. halleri supports a much more ancient appearance of the trait—or at least selection on major genes responsible for the trait—during the speciation process giving rise to this lineage hundreds of thousands of years ago, and thus pre-dating any human industrial activity (Roux et al., 2011). It has been suggested that major loci involved in metal tolerance and accumulation, such as the HMA4 gene (encoding the plasma membrane ATPase responsible for transporting Zn2+ out of root cells for loading into the xylem and translocation to the shoot), were targets of selection early in the history of the species (Pauwels et al., 2005; Roux et al., 2011). This would have established a basal level of zinc tolerance and accumulation in A. halleri, with local selection subsequently acting on additional genes in each established metallophyte population to enhance metal tolerance and possibly hyperaccumulation capacity still further (cf. Macnair, 2003). This has been supported by the results of genome-scan analyses that have shown the presence of outliers specific to different metallicolous populations of A. halleri (Meyer et al., 2009). Large variation in the degree of zinc tolerance within non-metallicolous populations and individuals can then be explained by either local gene flow from metallicolous to non-metallicolous populations, or as a result of ancestral standing genetic variation present within the non-metallicolous populations, that may have been exploited as the initial basis for metal tolerance in metallicolous populations.
Metal hyperaccumulator plants are known to accumulate zinc, cadmium, copper, cobalt, manganese and the metalloids arsenic, thallium and selenium, but the largest number (~80%) of hyperaccumulator species described are known to accumulate nickel (Reeves and Baker, 2000; Verbruggen et al., 2009; Krämer, 2010), possibly because of its prevalence in ultramafic rocks across the continents (Van der Ent et al., 2013). Ultramafic substrates are derived from igneous rocks with a low silica content but rich in mafic minerals such as magnesium, iron and nickel. Weathering of ultramafic bedrock creates serpentine soils with distinctive physical and chemical characteristics, including particularly high contents of nickel, cobalt and chromium, high Mg/Ca ratio and low levels of the essential macronutrients nitrogen, phosphorus and potassium (Brooks, 1987; Kazakou et al., 2008). Most types of soil show nickel concentrations typically between 7 and 50 mg kg−1, whereas in serpentine soils the nickel content usually ranges from 700 to 8000 mg kg−1 (Reeves, 1992; Reeves and Baker, 2000). This characteristic geochemistry, combined with a characteristically thin soil cover and granular texture, poor water-holding capacity, ready erosion and exposure to high light intensity, makes serpentine soils a notoriously difficult environment for plant growth (Proctor, 1975; Freitas et al., 2004). As a result, serpentine outcrops are treated as ecological islands inhabited by specialised floras. Indeed, the discontinuity between serpentine outcrops, with their sparse vegetation, and neighbouring soils can often be clearly delimited from afar (Kruckeberg, 2004; Brady et al., 2005).
Despite the greater taxonomic abundance of nickel hyperaccumulator species (>400), much more research has so far been conducted on the molecular basis and evolution of zinc and cadmium hyperaccumulation in the de facto model organisms A. halleri and N. caerulescens. However, only 15 described species are known to display zinc hyperaccumulation (Meerts and Van Isacker, 1997; Bert et al., 2000; Krämer, 2010), and nickel hyperaccumulation warrants further research as part of attempts to understand the evolutionary basis of plant adaptation to serpentine (Brady et al., 2005; Kazakou et al., 2008; Turner et al., 2010). The present paper thus focusses on evolution of nickel hyperaccumulation in the genus Alyssum (Brassicaceae) that contains 51 known hyperaccumulator taxa out of ∼190 species, making this the largest number of hyperaccumulating species found within a single genus (Brooks, 1998; Burge and Barker, 2010).
Evolution of nickel hyperaccumulation in genus Alyssum
Hyperaccumulator species within the genus Alyssum are widely distributed on serpentine sites across the entire Mediterranean basin, from the Iberian peninsula in the west to the Irano-Turanian region in the east (Brooks, 1987). It is not clear whether hyperaccumulation ability arose at each serpentine site independently, or whether the trait has evolved just once in an ancestral population and then spread by dispersal and range expansion to serpentine sites scattered over a broad geographical area, but this represents an excellent study group given the history of detailed taxonomic treatments of the genus (Ball and Dudley, 1993).
Several taxa within the genus Alyssum are classed as facultative hyperaccumulators (Pollard et al., 2014), providing an opportunity to study evolution of this trait by comparing hyperaccumulating and non-accumulating ecotypes. Alyssum serpyllifolium represents the best-studied example of facultative nickel hyperaccumulation in the genus. A. halleri and N. caerulescens also belong to the group of facultative metallophytes, as they occur both on and off metalliferous substrates. However, A. serpyllifolium is likely to have a different evolutionary history compared with A. halleri and N. caerulescens that are most characteristically found on metal-contaminated sites created in the last two to three millennia as a result of anthropogenic disturbance (such as mining activities). Serpentine populations of Alyssum, in contrast, typically occupy isolated ultramafic outcrops that have been exposed for many millions of years, at least since the Miocene. In addition, most of the current range of A. serpyllifolium is beyond the maximum advance of the main polar ice cap during the Pleistocene glaciations (Reeves, 1992; Hewitt, 1999), unlike the ranges of A. halleri and N. caeruelscens, possibly offering a more stable habitat and leading to a different evolutionary trajectory. However, glacial ice covered parts of the current range of A. serpyllifolium, including southern Spain, certain regions in central Spain, as well as the Pyrenees and the south of France (Levin, 2013), and hence the Last Glacial Maximum cannot be entirely ruled out as a factor in the phylogenetic history of this taxon. Indeed, an influence of climatic fluctuations can be important for the population dynamics of serpentine species (Kolář et al., 2012). One scenario envisages formerly widespread metallophyte species being excluded from non-serpentine sites during post-glacial reforestation because of their low competitiveness on non-metalliferous soils; the serpentine populations would become separated and disjunct, and because of reduced gene flow progressively differentiate owing to drift and selection. This ‘depleted’ (or palaeoendemic) species scenario proposed by Stebbins (Stebbins, 1942; Stebbins and Major, 1965), and considered in the serpentine context by Kruckeberg (Kruckeberg, 1954), has been shown to have taken place in the serpentine subspecies Minuartia laricifolia ssp. ophiolitica in the Alps (Moore et al., 2013) and in the Streptanthus glandulosus complex (Mayer et al., 1994). In a subsequent phase, non-serpentine progenitors can re-invade and come into secondary contact with serpentine populations (depleted species-recolonisation scenario).
The population history of A. serpyllifolium is likely to have been complicated by various factors. Serpentine substrates inhabited by this species represent relatively small edaphic ‘islands’ up to tens of kilometres in diameter (Brooks, 1987; Flynn, 2013), separated by vast stretches of a non-serpentine ‘sea’ with different geochemistry. As serpentine-adapted plants may not be successful competitors on non-serpentine substrates (Brooks, 1987; Elmendorf and Moore, 2007; Anacker and Harrison, 2012; Anacker, 2014), the populations occupying such serpentine islands would become isolated and could eventually diverge into separate species. Landscape and topography may also contribute to isolation of populations of A. serpyllifolium, as they often occur in mountain ranges such as Sierra de Aguas (population Carratraca-S), Sierra Bermeja de Estapona (Sierra Bermeja-S) and Serra do Careón (Barazón-S). Furthermore, ploidy difference is likely to act as an additional isolating mechanism between some populations of this species. All the Iberian populations analysed in this study are diploid, with n=8 (Fernandes and Queirós, 1973; Küpfer, 1974; Cecchi et al., 2013), but both diploid n=8 (Küpfer, 1974) and tetraploid n=16 (Bonnet, 1963; Puech, 1963) populations have been reported in France. All these factors may contribute to gradual divergence between individual populations, and the plants from different populations show some morphological differences. This has led to earlier proposals to raise the serpentine populations of A. serpyllifolium to the status of distinct subspecies, or even separate species (Dudley, 1986a and 1986b). However, analyses based on chloroplast DNA sequences have been unable to establish clearly resolved relationships between the different A. serpyllifolium populations (Cecchi et al., 2013; Flynn, 2013). In this paper, we have therefore reinvestigated the relationships between serpentine and non-serpentine populations of A. serpyllifolium using population-genetic approaches.
Materials and methods
In this study, four serpentine and four non-serpentine populations (Figure 1 and Supplementary Table S1) were sampled from across the main range of A. serpyllifolium in the Iberian peninsula (Ball and Dudley, 1993). The four serpentine populations originate from the three serpentine areas inhabited by A. serpyllifolium: Trás-os-Montes province in northeastern Portugal (Samil-S population), Melide, Galicia (Barazón-S population) and the western Baetic Cordilleras in Andalucía (Carratraca-S and Sierra Bermeja-S populations) in Spain. The four remaining non-serpentine populations (Alhaurín-NS, León-NS, Morata-NS and Rubiá-NS) were collected from across the Iberian peninsula in varying proximity to the serpentine outcrops. Seeds were collected from fruiting plants in years between 1999 and 2012.
Genomic DNA from dried plant shoots was extracted using a modification of the CTAB (cetyl trimethylammonium bromide) method (Rogers and Bendich, 1985; Porebski et al., 1997) from up to 40 individuals in each of the eight sampled A. serpyllifolium populations. The concentration of DNA in each sample was measured using a NanoDrop 2000 spectrophotometer (Thermo Scientific, Wilmington, DE, USA) following extraction.
Development of microsatellite markers
Perfect microsatellites were detected in the consensus A. serpyllifolium transcriptome assembly (manuscript in preparation) with SciRoKo version 3.4 (Kofler et al., 2007) using the following default settings: dinucleotide pattern: minimum 7 repeats; trinucleotide: minimum 5 repeats; tetra-, penta- and hexa-nucleotide: minimum 4 repeats. Out of 3942 microsatellites detected, 32 were selected based on repeat size (3 or 6 nucleotides, that is, no introduction of frameshift mutation), as well as the function of the target gene being considered unlikely to be important for adaptation to serpentine. Primers were then designed around each locus, and amplification success along with level of polymorphism was tested in 3–4 individuals in each population.
Each individual plant was then genotyped for eight developed microsatellites. The PCR mixture for each individual amplification reaction was assembled with the following reagents: 1.5 μl of 10 × buffer (New England BioLabs, Hitchin, UK), 0.3 μl of 10 mM total dNTPs (Thermo Scientific, Hemel Hempstead, UK), 1.2 μl of 25 mM MgCl2 (New England BioLabs), 0.06 μl of 10 μM forward primer, 0.3 μl of 10 μM reverse primer, 0.3 μl of FAM/HEX/NED labelled universal primer, 0.1 μl of Taq Polymerase (New England BioLabs), 1–2 μl of DNA solution (depending on the concentration, 10–100 ng contained in the reaction) and double-distilled water to 15 μl total volume. Oligonucleotide primers were supplied by Eurofins MWG Operon (Ebersberg, Germany), and in addition to the gene-specific sequences listed in Supplementary Table S2, forward primers contained a 5′ overhang fragment of 5′-IndexTermCACGACGTTGTAAAACGAC-3′ to facilitate incorporation of the dye-labelled universal primer in subsequent PCR cycles. PCR cycling was carried out using the following conditions: (1) initial denaturation (3 min at 95 °C), (2) 10 cycles of touch-down PCR (30 s at 95 °C, 30 s at 65 °C (reduced by one degree per cycle), 1 min at 68 °C), (3) 30 cycles of standard amplification (30 s at 95 °C, 30 s at 55 °C, 1 min at 68 °C) and (4) final extension (5 min at 68 °C).
Genotype scoring and data analysis
PCR-amplified fragments containing target microsatellite repeats were run on an Applied Biosystems (Foster City, CA, USA) Capillary Genetic Analyzer at the Department of Zoology, University of Oxford, UK, with GeneScan 500 LIZ Size Standard (Applied Biosystems) added as a reference and results collected using a DS-30 filter (Applied Biosystems). Microsatellite genotypes were scored manually using GeneMarker version 2.6.3 (SoftGenetics, State College, PA, USA) following the default settings for plant microsatellite scoring. In cases where a genotype could not be established with confidence, PCR products were re-run a second time. Micro-checker version 2.2.3 (Van Oosterhout et al., 2004) was then employed to test for genotyping artefacts—null alleles, stuttering and high-allele dropout levels. All of the individual genotypes were exported from MS Excel into CREATE version 1.37 (Coombs et al., 2008) that was then used to convert the data matrix into formats required for various programs.
First, departures from Hardy–Weinberg equilibrium and linkage disequilibrium were tested in Arlequin version 3.5 (Excoffier et al., 2005) and FSTAT version 18.104.22.168 (Goudet, 1995). Subsequently, two programs were used in calculating basic population genetics parameters: allele frequency, F-statistics, heterozygosity as well as analysis of molecular variance (AMOVA; Arlequin). The presence of an isolation-by-distance pattern (Wright, 1943) was investigated using the Mantel test with 1000 permutations (Mantel, 1967) in Genepop version 4.2 (Raymond and Rousset, 1995) by examining the correlation between log-transformed Euclidean distances between pairs of populations and linearised pairwise genetic distances (FST /(1−FST)). The PHYLIP package version 3.69 (Felsenstein, 2005) was employed to calculate various interpopulation genetic distance metrics with bootstrapping (1000 replicates), whereas Factorial Correspondence Analysis was carried out in Genetix version 4.05 using the default settings (http://www.genetix.univ-montp2.fr/).
Bayesian analysis in Structure version 2.3.3 (Falush et al., 2003) was used to assign individuals to genetic clusters (K). A model was chosen in which individuals had admixed ancestries and correlated allele frequencies to allow detection of more ancient admixture events (Falush et al., 2003). Choosing independent allele frequencies made no significant difference to the structure detected, and hence results based on correlated allele frequencies are reported here. The LocPrior clustering method implemented in the latest version of Structure was used that is not only based on the individual multilocus genotypes but also takes into account the sampling locations. The model is recommended by the authors when the genetic data are not highly informative in order to detect population structure, and was chosen because of a moderate number of microsatellite markers employed in the present study.
The number of genetic clusters (K) was set from a minimum of 2 to a maximum of 10, and five simulations were run for each K value with a burn-in of 100 000 and a main run of 1 000 000 Markov chain Monte Carlo iterations. To define the most probable value of K present in the data, the method proposed by Evanno et al. (2005) was initially used that is based on an ad hoc measure ΔK that depends on the rate of change in the log probability of the data between successive values of K. Second, the number of true clusters was also inferred following L(K) over a number of clusters, and then looking for the signature of L(K) starting to plateau with diminished variance in L(K) (Pritchard et al., 2000). These calculations were carried out by Structure Harvester Web version 0.6.94 (Earl and vonHoldt, 2012) that also generated CLUMPP input files. Subsequently, cluster assignments from across the replicate runs were aligned and averaged using CLUMPP version 1.1 (Jakobsson and Rosenberg, 2007) run with the Greedy algorithm and 1000 permutations of randomised input order. Resulting final cluster assignments were visualised using the program DISTRUCT version 1.1 (Rosenberg, 2004).
Locus selection and primer development
For sequence analyses of selection we chose two loci involved in metal hyperaccumulation and homeostasis in other plant species: natural resistance associated macrophage protein 4 (NRAMP4) and iron-regulated protein 1 (IREG1). On the other hand, 6B-interacting protein 1-like 1 (ASIL1) was selected as a reference gene for comparisons with NRAMP4 and IREG1, as ASIL1 is not expected to play a specific role in ecological adaptation in Alyssum as it is a transcriptional repressor of seed maturation genes in germinating seeds and seedlings in Arabidopsis (Gao et al., 2009). Primers for these genes were developed based on A. serpyllifolium transcriptome sequences of these genes using the PrimerDesignM web server (Yoon and Leitner, 2015) with default settings. For both IREG1 and NRAMP4 genes, amplification primers were also used as sequencing primers (Supplementary Table S3), but in the neutral gene ASIL1 a different reverse primer was used for amplification (ASIL1 R1) and sequencing (ASIL1 INTF1). Sequenced regions in both IREG1 and NRAMP4 were found to contain putative introns, 82 bp long in IREG1 and 145 bp long in NRAMP4, that were excluded from the analyses described below, unless otherwise stated.
Gene fragment amplification and Sanger sequencing
PCR mixture (30 μl) for each sample was assembled with the following reagents: 3 μl of 10 × buffer (New England BioLabs), 0.6 μl of 10 mM total dNTPs (Thermo Scientific), 2.4 μl of 25 mM MgCl2 (New England BioLabs), 0.6 μl of 10 μM forward primer, 0.6 μl of 10 μM reverse primer, 0.2 μl of Taq Polymerase (New England BioLabs), 1 μl of DNA solution (25–250 ng) and 21.6 μl of double-distilled water. In the case of ASIL1, 4.8 μl of 5 M betaine was added to a final concentration of 0.8 M, with concomitant reduction of the water volume, to increase primer annealing specificity and fragment amplification rate (Ralser et al., 2006). PCR cycling was carried out under the following conditions: (1) initial denaturation (3 min at 95 °C); (2) 10 cycles of touch-down PCR (30 s at 95 °C, 30 s at 65 °C (reduced by one degree per cycle), 1 min at 68 °C); (3) 33 cycles (IREG1) or 40 cycles (NRAMP4) of amplification (30 s at 95 °C, 1 min at 45–55 °C, 4 min at 68 °C), or in the case of ASIL1 the first 10 cycles carried out at 42 °C and the final 30 cycles with 50 °C annealing temperature to facilitate permissive primer binding and target region amplification in the initial steps of the PCR reaction; and (4) final extension step (5 min at 68 °C). PCR products of correct size, high purity and concentration were then sequenced at the DNA Sequencing Unit, Department of Zoology, University of Oxford, on an ABI 3730 × l DNA Analyzer (Applied Biosystems).
Raw ABI output chromatograms were examined and exported to the FASTA format using FinchTV software version 1.4 (Perkin-Elmer, Beaconsfield, UK). Consensus DNA contigs from combined forward primer and reverse primer sequencing results were created manually in MEGA (Tamura et al., 2013) from sequences trimmed on base call quality. DnaSP version 5 (Librado and Rozas, 2009) was employed to calculate the relevant population-genetic parameters, carry out tests for selection and phase the diploid sequences with the PHASE algorithm (Stephens et al., 2001). AMOVA was performed in Arlequin version 3.5 (Excoffier et al., 2005) and gene trees based on Nei’s DA (Nei et al., 1983) were prepared in POPTREE2 (Takezaki et al., 2010) with 1000 bootstrap replicates.
Genetic diversity and population structure
To analyse population structure and degree of isolation between the sampled populations of Alyssum serpyllifolium, we genotyped eight microsatellite loci in 272 individuals from four serpentine (Barazón-S, Carratraca-S, Samil-S, Sierra Bermeja-S) and four non-serpentine populations (Alhaurín-NS, León-NS, Morata-NS, Rubiá-NS; see Figure 1 and Supplementary Table S1). This revealed between 4 and 12 alleles per locus, with a mode of 5 alleles. No evidence for genotyping artefacts, such as null alleles, was found with Micro-checker (Van Oosterhout et al., 2004). All microsatellite loci were in linkage equilibrium.
Within-population gene diversity (Ho) ranged from 0.33 to 0.62 (average Ho=0.48) and did not differ significantly between serpentine (average Ho=0.50) and non-serpentine (average Ho=0.46) populations (Table 1). FIS values ranged from 0.07 to 0.35, and for most populations were significantly different from 0, based on 1000 permutations (Table 1), pointing to a non-negligible degree of inbreeding in A. serpyllfolium. These results are in line with expectations for serpentine endemics, reflecting small effective population sizes and small distribution ranges and, as a consequence, low genetic diversity and high levels of inbreeding (Anacker et al., 2011). On the other hand, we found significant FIS in only two of the four serpentine A. serpyllfolium populations studied (Table 1).
The results show relatively high levels of population differentiation, with overall FST=0.23 (95% confidence interval 0.17–0.29). AMOVA results indicated that 23.7% of all genetic variation was partitioned between populations, whereas 16.7% and 59.6% partitioned within populations among and within individuals, respectively. When populations are grouped into serpentine (S) and non-serpentine (NS) ecotypes, only a small proportion of variation is accounted for by differentiation between these groups in microsatellite genetic diversity (Table 2).
Population-genetic structure analysis with Structure software (Falush et al., 2003) revealed two optimal numbers of genetic clusters (K): K=4 (as per ΔK: Supplementary Figure S1) and K=8 (as per LnP(D): Supplementary Figure S2). K=4 results show a trend towards grouping together geographically close populations of the same ecotype, whereas K=8 simply place each population in its own separate cluster (Figure 2). Admixture proportions of individuals in different populations varied in the K=4 solution. Individuals in NS populations (northern Rubiá-NS and southern Alhaurín-NS) belonged to a single cluster each (pink and green clusters, respectively), and so did the S populations Sierra Bermeja-S and Carratraca-S in the south (blue cluster). The other four populations showed varying degrees of admixture. The northern Barazón-S and Samil-S populations mostly belonged to the fourth cluster (brown), with more (Samil-S) or less (Barazón-S) admixture from Alhaurín-NS green cluster. The northern and central NS populations Morata-NS and León-NS contained the highest admixture from Alhaurín-NS green cluster, in addition to smaller admixture from Samil-S and Barazón-S brown cluster and Rubiá-NS pink cluster (only in León-NS).
To investigate whether the pattern of isolation by distance could be detected over all populations, a Mantel test (Mantel, 1967) was carried out on the Weir and Cockerham (1984) FST pairwise distance matrix (Supplementary Table S4). This did not reveal any direct correlation, and the number of populations within each ecotype was too small to allow isolation-by-distance testing for S and NS populations separately within them. No consensus neighbour-joining tree could be obtained with reliable branch support values based on Nei’s DST distance metric (Nei, 1987), and no population structure could be detected using factor analysis in GENETIX (data not shown). Taken together, our data indicate that the analysed A. serpyllifolium populations appear to be more or less equidistant from each other and do not cluster according to S and NS ecotypes.
Patterns of sequence diversity at loci putatively involved in metal hyperaccumulation
Genetic diversity across S and NS populations of A. serpyllifolium was analysed in three genes (Table 3), one of which, ASIL1, was used as a reference locus unlikely to be involved in evolution of the nickel hyperaccumulation trait, whereas the two other loci, NRAMP4 and IREG1, have established roles in metal hyperaccumulation and homeostasis in other plant species.
In individual A. serpyllifolium populations, between 5 and 13 individuals were sequenced for ASIL1, 10 to 12 individuals for IREG1 and 6 to 11 individuals for NRAMP4, with the exception of the León-NS population, for which only 2 individuals were successfully sequenced (Table 3). For this reason, the León-NS population was excluded from most of the analyses focussing on NRAMP4. Overall, similar levels of sequence diversity were obtained for the two candidate genes and the reference gene (Table 3). Within the populations, genetic diversity varied widely in all three genes, with no clearly discernible pattern. Tests for selection did not detect any departures from neutrality in any of the populations (Table 3).
Interestingly, the two genes putatively involved in metal hyperaccumulation revealed striking differentiation between S and NS populations, as measured by FST and DA, in contrast to low differentiation at ASIL1 and the microsatellites (Table 2 and Supplementary Tables S4 and S5). For both NRAMP4 and IREG1, two strongly supported subclades grouping S and NS populations were reconstructed based on Nei et al. (1983) DA (Figure 3 and Supplementary Figure S3). Conversely, no well-supported population tree (all bootstrap support values <60%) could be recovered based on ASIL1, with S and NS populations intermixed on the tree (Figure 3 and Supplementary Figure S3).
Pairwise FST values for ASIL1 did not vary significantly across population pairs regardless of their S or NS origin (Supplementary Table S5). Conversely, for NRAMP4, pairwise comparisons of the S and NS populations resulted in FST >0.9, whereas for pairwise comparisons within S populations much lower differentiation was found, with FST typically <0.125, with the exception of Barazón-S, where NRAMP4 appears to have undergone additional longer sequence evolution than in other S populations (Supplementary Table S5).
AMOVA results (Table 2) confirm the high degree of shared genetic variation in the two candidate genes in populations of the same ecotype. When populations are grouped into S and NS ecotypes, the overwhelming percentage (89.7% in NRAMP4 and 64.5% in IREG1) of genetic variation is split between the two groups, whereas the rest is evenly distributed among populations within groups and within populations. The opposite pattern is found for the reference gene ASIL1 as well as for microsatellites, where S vs NS population grouping explained a very small proportion of overall genetic variation (Table 2).
Both candidate genes also contained a significant proportion of single-nucleotide polymorphisms (SNPs) fixed or nearly fixed between the two ecotypes, with serpentine populations often featuring fixed derived genetic variants (Table 4). In particular, NRAMP4 contains eight SNPs fixed for distinct alleles in S and NS populations. Four of these SNPs encode non-synonymous changes, and in all cases the serpentine alleles are derived relative to the non-accumulators Arabidopsis thaliana and Clypeola jonthlaspi (the latter a member of the same clade within the tribe Alysseae as A. serpyllifolium: Rešetnik et al., 2013; Španiel et al., 2015), and hence could be of adaptive importance. In particular, the Asp→Asn amino acid replacement at position 1190 leads to a change from an amino acid with acidic to neutral side-chain properties in the serpentine populations that may influence protein function. Two further synonymous NRAMP4 SNPs are nearly fixed between the ecotypes: at one SNP (position 343) the serpentine allele is segregating in Rubiá-NS, and at another SNP (position 1222) the serpentine allele is not fixed in Barazón-S. Similarly, IREG1 contained six SNPs fixed or nearly fixed between the S and NS ecotypes, four of which were non-synonymous (Table 4).
Our analyses revealed considerable genetic diversity in A. serpyllifolium populations regardless of their S or NS origin. Such a relatively even distribution of genetic diversity is not expected if either S or NS populations were founded only recently. In particular, our results rule out a scenario of recent colonisation of serpentine environments by local migrants from non-serpentine populations, and indicate that both S and NS populations of A. serpyllifolium have existed for a long time. This is consistent with a relatively minor impact of glaciations on A. serpyllifolium populations in parts of south-western Europe beyond the maximum advance of the main polar ice cap during the Pleistocene glaciations (Reeves, 1992; Hewitt, 1999).
Previous studies of the population genetics of species harbouring metallicolous and non-metallicolous populations have often speculated that, given the scenario of local evolution of metallicolous populations from relatively metal-tolerant, low-frequency genotypes present in non-metallicolous populations, a founder effect may have been present in metallicolous populations when they originally diverged from the source populations (Pauwels et al., 2005), resulting in lower genetic diversity in the metallicolous populations. However, no differences in genetic diversity between metallicolous and non-metallicolous populations have been consistently found in the species investigated to date (Vekemans and Lefèbvre, 1997; Quintela-Sabarís et al., 2010), such as A. halleri (Pauwels et al., 2005), A. bertolonii (Mengoni et al., 2003) and M. laricifolia ssp. ophiolitica (Moore et al., 2013), and neither have they been found here (Table 2). However, the bottlenecks in question would need to have been quite recent to stand out in this way, and gene flow and accumulation of new mutations would later erode the signal of any putative bottlenecks (Vekemans and Lefèbvre, 1997).
Our results reveal relatively high levels of population differentiation in A. serpyllifolium, with overall FST=0.23 (95% confidence interval 0.17–0.29). Moderate-to-high values of FST in A. serpyllifolium are typical of values from other taxa endemic to specific substrates, such as Primulina tabacum (0.3936: Ni et al., 2006), Jurinea pinnata (0.374: Salmerón-Sánchez et al., 2014a) or Convolvulus boisseri (0.395: Salmerón-Sánchez et al., 2014b). An even higher FST range was encountered between western Swiss populations of the model hyperaccumulator N. caerulescens, in which FST reached an average of 0.591 (Besnard et al., 2009). The values observed here provide evidence for moderate-to-low gene flow between the populations of A. serpyllifolium, probably determined by both ecological (serpentine ‘islands’ of endemism) and topographical barriers, such as mountains and canyons, resulting in fragmentation of the species’ range. Consistent with this, AMOVA indicated that population divergence accounts for about one-quarter of all genetic variation in A. serpyllifolium. Similar between-population partitioning of genetic variation (22%) was found in an inter-simple sequence repeat study of four populations of the nickel hyperaccumulator Alyssum lesbiacum on the island of Lesbos (Adamidis et al., 2014). In contrast, another Alyssum hyperaccumulator, A. bertolonii, had over a half (51%) of its genetic variation partitioned between populations in a study of 9 populations in Italy genotyped with chloroplast simple sequence repeats (Mengoni et al., 2003). Between-population variation found in a chloroplast restriction fragment length polymorphism-based study of 28 populations A. halleri (Pauwels et al., 2005) was even higher and amounted to 68%. Thus, the levels of between-population genetic variation revealed in our study are not dissimilar to those found in other metal hyperaccumulator species, indicating that evolution of metal hyperaccumulation in A. serpyllifolium is likely to be representative of the processes driving the evolution of the trait in other hyperaccumulator species as well.
Our analyses based on microsatellites and DNA sequence data from the ASIL1 reference locus demonstrate that differentiation between S and NS ecotypes accounts for very little genetic diversity in A. serpyllifolium populations, indicating that there is little differentiation between the ecotypes across the genome. In contrast, two genes putatively involved in metal hyperaccumulation, NRAMP4 and IREG1, show far higher differentiation between S and NS ecotypes. NRAMP4 expression appears to correlate positively with Ni tolerance (Oomen et al., 2009; Halimaa et al., 2014) in N. caerulescens, one of the metal-hyperaccumulating species of Brassicaceae that can accumulate Ni as well as Zn and Cd. In both A. thaliana and N. caerulescens, NRAMP4 has been shown to encode a tonoplast-localised Zn, Fe, Mn and Cd transporter (Thomine et al., 2000, 2003; Lanquar et al., 2005, 2010; Pottier et al., 2015). In particular, ectopic overexpression of NRAMP4 in transgenic A. thaliana promotes Zn and Cd remobilisation from root vacuoles and decreased metal accumulation in the root (Pottier et al., 2015), thus acting in a process expected to operate at a high level in hyperaccumulator species that preferentially translocate metals to the shoot. The NRAMP4 homologue from the serpentine Ni hyperaccumulator T. japonicum has been shown to transport Ni specifically when heterologously expressed in yeast (Mizuno et al., 2005), and hence this transporter may be directly implicated in Ni transport and/or sequestration in plants specifically adapted to serpentine substrates. Expression of IREG1, another membrane-localised metal-ion transporter, has also been shown to be important for nickel and cobalt detoxification in A. thaliana (Kirchner, 2009), consistent with increased nickel tolerance in IREG1-overexpressing transgenic lines and increased nickel sensitivity in IREG1 knockout lines. In addition, a newly characterised IREG family member in the nickel hyperaccumulator Psychotria gabrielliae (Rubiaceae) appears to confer increased nickel tolerance, possibly by enhancing vacuolar accumulation of Ni (Merlot et al., 2014). Taken together, we hypothesise that both NRAMP4 and IREG1 are likely to be of high adaptive significance for the nickel-hyperaccumulation ability of A. serpyllifolium. Conversely, ASIL1, selected as a reference gene for comparisons with NRAMP4 and IREG1, is a transcriptional repressor of seed maturation genes in germinating seeds and seedlings in Arabidopsis (Gao et al., 2009), and is thus unlikely to play a significant role in nickel tolerance and hyperaccumulation in Alyssum.
Stronger differentiation between S and NS ecotypes at NRAMP4 and IREG1, compared with ASIL1 and microsatellites, is consistent with diversifying selection in NRAMP4 and IREG1 genes driven by local adaptation to S and NS environments. Furthermore, local adaptation at these genes is supported by the presence of derived SNPs, including amino acid replacements that are fixed or nearly fixed in serpentine populations, whereas non-serpentine populations are fixed for the ancestral alleles (Table 4). The question of when and how these putatively adaptive alleles spread across the serpentine populations of A. serpyllifolium is of considerable interest, as this may shed light on the evolution of nickel hyperaccumulation. If the spread were recent (<2Ne generations ago), it would be expected to leave characteristic footprints of a selective sweep, such as reduced variation in and around the loci concerned in serpentine populations. However, no deviations from neutrality were detected in any of the populations, indicating that local adaptation to serpentine conditions in NRAMP4 and IREG1 genes may have occurred relatively early in the history of the species complex. This is consistent with the distribution of serpentine A. serpyllifolium populations on relatively old ultramafic outcrops that have been exposed for many millions of years.
In summary, the present results from the population-genetic analysis of A. serpyllifolium across the Iberian peninsula suggests that the S and NS ecotypes can be regarded as belonging to the same species complex and do not warrant description as distinct taxonomic entities. Although earlier work has demonstrated that the serpentine populations show particular morphological characteristics when growing on these substrates in situ, and that they display a much higher degree of nickel tolerance than the non-serpentine populations when tested under common-garden conditions, the distinctiveness of these ecotypes is not supported by the results of the microsatellite analysis. Rather, all eight populations tested were differentiated from each other to an approximately equal extent, with evidence of a significant degree of inbreeding probably indicative of a relatively long history of isolation of these populations. At the level of DNA polymorphism, however, two candidate genes putatively involved in nickel hyperaccumulation showed signatures of adaptive evolution that may represent an integral part of the mechanism of local adaptation to serpentine substrates.
Our results demonstrate that divergence between S and NS ecotypes of A. serpyllifolium is no greater than among populations of the same ecotype. This does not support earlier suggestions that S and NS A. serpyllifolium populations represent separate species (Dudley, 1986a, 1986b). Although earlier work has demonstrated that the serpentine populations show particular morphological characteristics when growing on these substrates in situ (Dudley, 1986a, 1986b), and that they display a much higher degree of nickel tolerance than the non-serpentine populations when tested under common-garden conditions (Brooks et al., 1981), the distinctiveness of these ecotypes is detectable only at the loci putatively involved in the metal hyperaccumulation trait. Selective pressure at these loci to adapt to highly distinct conditions at S and NS sites has resulted in strong differentiation, with many synonymous and non-synonymous mutations fixed between the two ecotypes. Contrary to this, no such differentiation was detected elsewhere in the genome; all eight populations tested were differentiated from each other to an approximately equal extent and contained similar levels of genetic diversity, providing no support to the hypothesis that populations of one ecotype originated from local populations of the other ecotype. We conclude that adaptation to S and NS environments in A. serpyllifolium populations probably had a long history, but affected only the genes involved in evolution of metal tolerance and hyperaccumulation, whereas patterns of polymorphism in the rest of the genome have been dominated by geographic isolation of these populations. Expanding this analysis to a greater number of genes and populations in the future will help to identify more genes involved in evolution of metal hyperaccumulation and more precisely reconstruct the history of evolution of this peculiar trait.
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This work was supported by a BBSRC postgraduate studentship and a Genetics Society Heredity fieldwork Grant to MK Sobczyk, and by the award of Pilot Project Grant NBAF711 from the NERC Biomolecular Analysis Facility (NBAF-Edinburgh) to JACS. DAF acknowledges support from NERC (project NE/G017646/1). We also thank Carlos Aguiar, Gerardo Albela González, Alfredo Asensi Marfil, Félix Llamas García, Teresa Navarro, Gonzalo Nieto Feliner, Celestino Quintela Sabarís and Julia Sánchez Vilas for assistance with locating material in the field.
The authors declare no conflict of interest.
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Sobczyk, M., Smith, J., Pollard, A. et al. Evolution of nickel hyperaccumulation and serpentine adaptation in the Alyssum serpyllifolium species complex. Heredity 118, 31–41 (2017). https://doi.org/10.1038/hdy.2016.93
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