- Research article
- Open Access
Contrasting evolutionary origins of two mountain endemics: Saxifraga wahlenbergii (Western Carpathians) and S. styriaca (Eastern Alps)
BMC Evolutionary Biology volume 19, Article number: 18 (2019)
The Carpathians and the Alps are the largest mountain ranges of the European Alpine System and important centres of endemism. Among the distinctive endemic species of this area is Saxifraga wahlenbergii, a Western Carpathians member of the speciose genus Saxifraga. It was frequently considered a taxonomically isolated Tertiary palaeopolyploid and palaeoendemic, for which the closest relatives could not yet be traced. A recently described narrow endemic of the Eastern Alps, S. styriaca, was hypothesized to be closely related to S. wahlenbergii based on shared presence of peculiar glandular hairs. To elucidate the origin and phylogenetic relationships of both species we studied nuclear and plastid DNA markers based on multiple accessions and analysed the data in a wide taxonomic context. We applied Sanger sequencing, followed by targeted next-generation sequencing (NGS) for a refined analysis of nrITS variants to detect signatures of ancient hybridization. The ITS data were used to estimate divergence times of different lineages using a relaxed molecular clock.
We demonstrate divergent evolutionary histories for the two mountain endemics. For S. wahlenbergii we revealed a complicated hybrid origin. Its maternal parent belongs to a Western Eurasian lineage of high mountain taxa grouped in subsect. Androsaceae and is most likely the widespread S. androsacea. The putative second parent was most likely S. adscendens, which belongs to the distantly related subsect. Tridactylites. While Sanger sequencing of nrITS only showed S. adscendens-related variants in S. wahlenbergii, our NGS screening revealed presence of sequences from both lineages with clear predominance of the paternal over the maternal lineage.
Saxifraga styriaca was unambiguously assigned to subsect. Androsaceae and is not the sister taxon of S. wahlenbergii. Accordingly, the similarity of the glandular hairs observed in both taxa rests on parallelism and both species do not constitute an example of a close evolutionary link between the floras of the Western Carpathians and Eastern Alps. With the origin of its paternal, S. adscendens-like ITS DNA estimated to ca. 4.7 Ma, S. wahlenbergii is not a relict of the mid-Tertiary climate optimum. Its hybrid origin is much younger and most likely took place in the Pleistocene.
The Carpathians constitute an important part of the European Alpine System (EAS sensu Ozenda ), which includes the Alps, the Pyrenees, the Apennines, and the mountain ranges of the northern Balkan Peninsula. Their location in the middle of the European continent causes richness of biota due to overlapping alpine, arctic-alpine, Mediterranean and Asian elements. Because only the highest massifs of the Carpathians were extensively glaciated during the glacial periods of the Pleistocene (see [2,3,4]), this range is considered an important northern glacial refugium [3, 5, 6]. Along with the Alps, the Carpathians form the largest and biogeographically important part of the EAS. Topography and climate of mountain systems are known to generally favour evolution of endemism  and, accordingly, these two ranges belong to important centres of endemism in Europe . The number of endemics in the Carpathians is estimated at 3–5% of the vascular flora of the area (excluding apomictic complexes [3, 9]). In the Alps, it is higher and reaches 12.6% [10, 11].
In the European mountains, the genus Saxifraga is one of the most endemic-rich plant genera and, notably, it contributes most endemic taxa in the alpine and nival belts . Many species of Saxifraga, representing various infrageneric units, occur in restricted areas throughout the EAS . Although in the Carpathians the general taxonomic richness of this genus is much lower compared to the Alps (e.g., ), S. wahlenbergii Ball is counted among the most distinctive endemic plants of this mountain system (Fig. 1). It occurs only in the Western Carpathians, a significant centre of plant endemism (Fig. 2) [4, 8]. Its distribution is limited to the Tatra Mountains and a few neighbouring massifs . Despite the attention this species has attracted, its taxonomic and biogeographic relationships remained rather obscure. Engler & Irmscher , followed by Pawłowski , considered S. wahlenbergii a distinct relict of the Tertiary flora, mostly on account of its presumed close relationship to the Pyrenean endemic S. praetermissa. Later, Pawłowska  contradicted the apparent morphological similarity evoked to place the two species in the same ‘grex’ or series. However, she maintained the position of the Carpathian taxon as a Tertiary palaeoendemic based on its assumed taxonomic isolation together with its restricted geographical range. In a cytological analysis of the flora of the Tatra Mountains, Skalińska  considered S. wahlenbergii a palaeopolyploid. Although she did not explicitly discuss the species’ age, it was suggested to belong to ‘very ancient groups’, which early accomplished their cytological differentiation.
Saxifraga wahlenbergii is characterised by peculiar pluricellular glandular hairs with wormlike endings, which induced Pawłowska  to accommodate it in the monotypic series Perdurantes (S.Pawł.) S.Pawł. Recently, this specific type of glandular hairs has also been observed in the newly described S. styriaca Köckinger, a narrow endemic of the eastern-most Eastern Alps (Lower Tauern), a region harbouring several rare and disjunctly distributed species (Figs. 1 and 2) [20, 21]. This species was therefore suggested to be a putative closest relative of the Carpathian endemic . Both orophytes are characteristic of high altitudinal zones and have their upper distribution limit in alpine and subnival regions (2400–2500 m a.s.l.). Saxifraga wahlenbergii covers a much wider altitudinal range than S. styriaca, with the lower distribution limits around 800 m and 1860 m, respectively [22, 23]. While S. styriaca prefers base-rich schists, S. wahlenbergii is found on both calcareous and siliceous rocks [13, 22, 24]. A phylogenetic analysis testing whether the two species represent a phylogenetically separate lineage within the genus would be vital to unravel their evolutionary history. It would also contribute to the knowledge of evolution of endemic high mountain taxa and of the biogeography of the EAS.
If the close phylogenetic relationships of S. wahlenbergii and S. styriaca were confirmed, this species pair would provide an important case of floristic and evolutionary links between the Carpathians and the Alps. The floras of both mountains have close connections as reflected, for example, by the presence of common endemic species such as Hypochaeris uniflora Vill. and Pinus cembra L. [25,26,27] and vicariant species from many genera, such as Cochlearia L., Sempervivum L. and Soldanella L. [28,29,30,31]. Biogeographical links are particularly strong between the Carpathians and the Eastern Alps including a large group of common species absent from the Western Alps, for instance Campanula alpina Jacq., Dianthus glacialis DC., Doronicum stiriacum (Vill.) Dalla Torre, Gentiana frigida Haenke and Saponaria pumila Janch. [17, 32,33,34,35,36,37]. Plant populations of these regions often display close phylogeographical connections as demonstrated, for example, in the Arabidopsis arenosa (L.) Lawalrée species complex, Pritzelago alpina (L.) O.Kuntze, Ranunculus alpestris L., R. glacialis L., Rhodiola rosea L. or Salix herbacea L. [38,39,40,41,42,43].
Despite their pertinence for the knowledge on biogeography and evolution of the Central European mountain flora, the relationship and phylogenetic position of S. wahlenbergii and S. styriaca have not been comprehensively studied so far. In a preliminary report, Cieślak et al.  placed both species in sect. Saxifraga and suggested their phylogenetic divergence. In a genus-wide molecular-phylogenetic analysis of Saxifraga, Tkach et al.  covered only a single accession of S. wahlenbergii and supported its sectional placement. Furthermore, due to discordance between the topologies of nuclear and plastid DNA trees, a hybrid origin of this taxon was hypothesised.
In this study, we aim at exploring the relationship of S. wahlenbergii and S. styriaca and their parentage in more depth. We apply molecular methods including Sanger sequencing and targeted next-generation sequencing (NGS) for a refined analysis of nuclear and plastid DNA variation. We use a range-wide sample of accessions of S. wahlenbergii and narrowly distributed S. styriaca, a broad phylogenetic context and temporal calibration of the phylogeny, to address the following questions: (1) Are S. wahlenbergii and S. styriaca closely related and eventually sister taxa, corroborating the morphology-based hypothesis? (2) What are their closest extant relatives? (3) What are the similarities and differences in the evolutionary history of both taxa? (4) Do they support a close biogeographical link between the floras of the Western Carpathians and the Eastern Alps? (5) Is the traditional hypothesis that S. wahlenbergii is a Tertiary relict phylogenetically supported?
Our full dataset comprises 326 taxa. The 14 samples from 13 populations of S. wahlenbergii and four samples from two populations of S. styriaca were collected during field campaigns to the Carpathians and the Alps, respectively. To determine the phylogenetic position of S. wahlenbergii and S. styriaca within the genus Saxifraga, we added the newly generated sequences of these samples to the extensive plastid (trnL–trnF region) and nuclear ribosomal DNA (nrDNA; internal transcribed spacer region, ITS) data matrices generated for Saxifraga by Tkach et al. . Additionally, further accessions of S. adscendens, S. androsacea, S. aphylla, S. depressa, S. facchinii, S. hypnoides, S. praetermissa, S. seguieri and S. tridactylites were studied. To increase phylogenetic tree resolution, an additional plastid non-coding intergenic spacer, rpl32–trnL, which was found informative in an earlier pilot study (E. Cieślak, M. Ronikier, unpubl. data), was studied for all taxa. These large (hereafter: ‘extended’) plastid and nr DNA datasets were rooted with Itea virginica L. and Pterostemon rotundifolius Ramírez, both belonging to Iteaceae J.Agardh.
For a better overview of phylogenetic relationships in the target group, reduced plastid and nuclear datasets including 56 taxa were used. They encompassed S. wahlenbergii, S. styriaca, their closest relatives (S. sect. Saxifraga; see Results) and only a few representatives of other Saxifraga sections as identified in the analyses of the extended datasets. Micranthes nivalis (L.) Small was chosen as outgroup.
A further dataset was created to enable an in-depth analysis of variants, intra-individual variation and interspecific sharing patterns based on the ITS2 region of nrDNA. Here, we employed next-generation sequencing (NGS) of amplicons to efficiently retrieve all distinct ITS2 copies present in the genomes. In the analysis, NGS data were combined with the reduced nrDNA dataset based on Sanger sequences (see above).
For the divergence time estimation, sect. Saxifraga was analysed within the broad phylogenetic framework of Saxifragales using this ITS dataset. It was extended to incorporate other representatives of the families Saxifragaceae, Iteaceae and Grossulariaceae and rooted with Penthorum chinense Pursh (Penthoraceae Rydb. ex Britton), a remotely related taxon from the order Saxifragales Bercht. & J. Presl [46, 47].
The species and accessions studied, voucher information and GenBank/ENA accession numbers for all used sequences (www.ncbi.nlm.nih.gov/genbank/; www.ebi.ac.uk/ena/) are listed in Additional file 1: Table S1. All sequence alignments are available in Additional file 2.
Scanning electron microscope (SEM) analysis
Dried leaves were mounted under an incident light microscope (Zeiss, Germany) on aluminium stubs using double stick carbon conductive tabs (Plano GmbH, Wetzlar, Germany). Images of the uncoated samples were taken with the tabletop scanning electron microscope Hitachi TM-3030Plus (Hitachi Europe Ltd., Maidenhead, UK). The abaxial surface of the leaves and single trichomes were imaged using 15 kV in mixed signal mode (combined secondary and backscattered electron detectors). The following specimens were studied: Saxifraga wahlenbergii (Poland, Western Carpathians, Tatry Zachodnie Mt., R. Letz & P. Mráz, 7 Aug 2004, KRAM636368); S. styriaca (Austria, Alps, Lower Tauern, Rettlkirchspitze, M. Röser 11,356 & N. Tkach, 16 June 2018, HAL).
DNA extraction, PCR amplification and Sanger sequencing
Total genomic DNA was extracted from silica-gel dried plant material and herbarium specimens (Additional file 1: Table S1) using either the NucleoSpin Plant II DNA extraction kit (Macherey-Nagel, Düren, Germany) or the DNeasy Plant Mini Kit (Qiagen, Hilden, Germany), according to the manufacturers’ protocols.
Amplification and DNA sequencing using the Sanger chain-termination method of ITS was performed using the primers ITS-1, ITS-4 and ITS-5 of White et al. . For amplification and sequencing of trnL–trnF including the trnL(UAA) intron and the adjacent intergenic spacer between the trnL(UAA) 3’exon and the trnF(GAA) gene, primers c, d, e and f from Taberlet et al.  were used. The rpl32–trnL region was amplified and sequenced using the primers trnL(UAG) and rpl32-F .
For amplification of ITS and trnL–trnF we followed Tkach et al.  or applied a slightly different ITS protocol based on a touchdown cycling profile as follows: initial denaturation at 94 °C for 3 min, followed by 35 cycles of 30 s at 94 °C, 30 s at 60 °C (with decrease of 1 °C by cycle and constant temperature of 50 °C from the 11th cycle onwards), and 1 min at 72 °C, followed by a final extension at 72 °C for 7 min. The rpl32–trnL region was amplified using the following PCR program: initial denaturation at 94 °C for 2 min, followed by 34 cycles of 94 °C for 30 s, 53 °C for 1 min, and 72 °C for 2 min. The final extension at 72 °C lasted for 10 min.
The quality and quantity of the PCR products were checked spectrophotometrically or on 1% agarose gel. Sequencing of new S. wahlenbergii, S. styriaca and S. adscendens samples was carried out using BigDye 3.1 chemistry (Thermo Fisher Scientific, Waltham, Massachusetts, U.S.A.) and sequences were separated on an ABI 3130 automated sequencer. Sequencing of other samples was performed by LGC Genomics (Berlin, Germany).
The sequences were edited in Sequencher 5.0 (Gene Codes Corporation, Ann Arbor, Michigan, U.S.A.). The new ITS and trnL–trnF sequences were added to the alignments of Tkach et al. . The sequences were automatically aligned using the default settings of ClustalW2  implemented in Geneious 9.1.6 (www.geneious.com) . Subsequently, the alignments were refined manually.
NGS library construction
Our NGS protocol largely followed Suchan et al.  and consisted of two PCR steps. First, the ITS2 region was amplified using a combination of ITS-S2F  and ITS-4R  primers, previously successfully used in barcoding  and metabarcoding studies [56, 57], tailed with a partial Illumina adapter. The second PCR reaction used double-indexing primers to uniquely tag sequences belonging to each specimen analysed. The first reaction consisted of 1 μl of the sample, 1× Q5 buffer, 0.4 U of Q5 Hot-Start polymerase (New England Biolabs, Ipswich, Massachusetts, U.S.A.), 200 μM of each dNTP, and 0.5 μM of each primer in a 10 μl reaction volume, and was amplified using 15 PCR cycles. Each sample was processed in two replicates. Each replicate was amplified in three independent reactions to avoid reaction-specific biases [57, 58]. To avoid contamination, each reaction was set up under a laminar flow cabinet, using only ultra-pure molecular-grade water (Sigma-Aldrich, Darmstadt, Germany) and a separate stock of reagents and plastics.
The reaction products were checked on a 1.5% agarose gel and purified using AMPure XP ratio of 1×. After that, all reactions were pooled, quantified using a Qbit instrument (Thermo Fisher Scientific, Waltham, Massachusetts, U.S.A.), and sequenced with 15% PhiX spike-in on a part of MiSeq sequencer lane (Illumina, San Diego, California, U.S.A.) using the 600-cycle MiSeq Reagent Kit v3 according to the manufacturer’s instructions.
NGS data analyses
The raw paired-end reads were merged using PEAR v. 0.9.8  and only successfully merged reads were used in the next steps. Primers were then trimmed with Cutadapt v. 1.12  and only reads containing primers were kept. Using vsearch v. 2.4.3 , the reads were filtered by the expected error rate (maxe) of 0.5, minimum length of 250 nt and maximum length of 450 nt, dereplicated, and the reads present in only one copy in a given individual were removed. Then, the reads were filtered using a custom Python script, retaining only the reads present in both replicates and in more than 100 copies in each replicate. The parameters were chosen after inspecting the sequences present in blank samples. After filtering, the reads from the duplicates were combined. The reads with 99% similarity were clustered using vsearch and the resulting sequences used in further analyses. The reads were also searched against NCBI database using BLASTn (https://blast.ncbi.nlm.nih.gov/Blast.cgi) to retain only the reads mapping against Saxifraga.
In the first step, phylogenetic reconstructions with Maximum Likelihood (ML), Maximum Parsimony (MP) and Bayesian Inference (BI) methods were conducted for all three molecular marker regions separately and for both the extended and reduced datasets. ML searches and bootstrap estimation of clade support were conducted with RAxML 8.2.X . This tool is provided under the familiar interface RAxML BlackBox with default settings on the CIPRES Science Gateway (www.phylo.org) . On the same platform, we performed a Bayesian analysis employing MrBayes v. 3.1.2  (rates = invgamma, ngen = 5,000,000, samplefreq = 500) to estimate the posterior probabilities (PP) of the Bayesian analyses. MP analyses with bootstrap calculations were performed using Paup* 4.0a152  with the settings used by Tkach et al. . Because the trees of the two plastid markers were identical, the respective sequence data were concatenated and analysed as one dataset. All trees were visualized with FigTree 1.4.3 (http://tree.bio.ed.ac.uk/software/figtree/). We used a bootstrap support (BS) ≥ 70% and PP ≥ 0.98 as thresholds to identify significant incongruence between clades of the plastid and the nrITS phylogenetic trees as previously suggested by Tkach et al. .
The input file was produced with BEAUti, a tool of BEAST v. 1.8.4 , using default settings (see Additional file 2). We applied the uncorrelated lognormal clock model with Yule tree priors following Ebersbach et al. . Four nodes were used as calibration points. The Ribes crown was constrained at 14.5 Ma and the Ribes stem node at minimally 48.9 Ma. We set the Iteaceae crown node constraint to 49 Ma and its stem node to 89 Ma according to Ebersbach et al.  and Gao et al. . The node age prior distributions were always lognormal. Conservative settings (m = 1.5, SD = 1.0) were used to accommodate the degree of uncertainty. Four independent Markov chains were run for 100,000,000 generations and parameters were saved every 10,000th tree. Bayesian dating was performed in BEAST v. 1.8.4 . The results were evaluated in Tracer v. 1.6 for effective sample size values and for determining the stationary phase of the runs . Maximum clade credibility (MCC) trees were summarised in the BEAST tool TreeAnnotator v. 1.8.4 with 20% burn-in . The final chronogram and its 95% highest posterior density (HDP) were visualised in FigTree 1.4.3.
Sanger sequence data characteristics
The 44 new sequences of the trnL–trnF and ITS regions were added to the alignments used by Tkach et al. . Structure and length of the alignments were not altered by the inclusion of these additional data. The alignment of the newly studied plastid region rpl32–trnL consisted of 248 sequences and had the length of 1117 base pairs (bp). The length of the rpl32–trnL sequences obtained varied from 434 bp in S. hirculus (sect. Ciliatae) to 747 bp in S. funstonii (sect. Bronchiales). The considerable variation in sequence length (up to 313 bp) was caused by the presence of numerous long and partly nested structural mutations (indels).
NGS sequencing output
Sequencing yielded 4,469,063 raw paired-end reads, including 7149 reads (0.16%) in blank samples, with an average of 58,709 reads per sample (excluding blank samples; standard deviation [SD]: 40,954; median: 66,261). Most of the paired-end reads were successfully merged for all the studied samples (mean: 94.5%; SD: 12.4%; median: 98.8%), and contained the targeted primer sequences (mean 98.1%; SD: 7.2%; median: 99.9% of merged reads). After quality filtering, a total of 3,110,076 reads were retained, including 5102 (0.16%) reads in blank samples (mean: 41,959; SD: 30,024; median: 45,346; excluding blank samples). No reads in blank samples were present in both technical replicates and in more than 100 copies, and reads from 29 of 38 samples passed the above filter. After clustering the reads with 99% similarity and discarding three sequences identified as fungal, an average of 1.9 ITS2 variants per sample (SD: 0.9; median: 2) was obtained, with the most abundant variant present 1–2 orders of magnitude more often than the less common ones. The 22 nrITS2 variants of S. wahlenbergii (11 samples), ten of S. styriaca (four samples), six of S. androsacea (three samples), three of S. tridactylites (two samples), two each of S. adscendens, S. depressa, S. seguieri (one sample each), one variant each of S. aphylla, S. discolor, S. italica, S. osloensis, S. praetermissa (one sample each) were added to the alignment of the reduced dataset based on Sanger sequences.
Infrageneric placement of S. wahlenbergii and S. styriaca
The topology, resolution and support of the individual trees based on the plastid trnL–trnF and rpl32–trnL regions were similar (not shown); therefore, both datasets were concatenated. The plastid and the nuclear ITS datasets for the entire genus Saxifraga (extended datasets) were analysed under ML, MP and BI. The tree topologies obtained for each dataset using each of the methods were widely corresponding, whereas resolution and branch support varied (see Additional file 3: Figure S1, Additional file 4: Figure S2). The plastid and nrDNA trees showed a congruent topology of major supported branches considering the threshold values of node support as outlined in the Material and methods section. In both trees, S. wahlenbergii and S. styriaca were firmly nested within the section Saxifraga (Additional file 3: Figure S1, Additional file 4: Figure S2), which also received strong support in the reduced datasets (nrITS: ML100/MP96/PP100, plastid: ML100/MP92/PP100; Figs. 3 and 4). Remarkably, this lineage is internally characterised by incongruent placement of several species, including S. wahlenbergii, among the nuclear and plastid DNA trees.
Phylogenetic affinities based on the reduced datasets
The reduced nrDNA tree based on Sanger sequences showed a basal dichotomy of the sect. Saxifraga lineage (Fig. 3). All accessions of S. wahlenbergii were included in the clade (ML99/MP94/PP100) containing the taxa belonging to subsect. Tridactylites: S. adscendens, S. discolor, S. osloensis and S. tridactylites (with accessions of S. tridactylites and one of S. osloensis forming a distinct branch within this clade). The second clade (ML100/MP99/PP100) encompassed all other species of sect. Saxifraga, which clustered in three well supported branches that corresponded to three other subsections: Androsaceae, Arachnoideae and Saxifraga. Accessions of S. styriaca grouped within the clade containing species from subsect. Androsaceae (S. androsacea, S. italica, S. seguieri). S. irrigua was included in a sister branch to the former group.
The plastid tree also revealed a basal split of section Saxifraga but with differences in the placement of some species (Fig. 4). In contrast to the ITS tree, the clade containing representatives of subsect. Tridactylites (ML100/MP99/PP100) did not contain S. wahlenbergii accessions. The sister clade (ML100/MP99/PP100) contained a dichotomy of the other species of this section, including a major subclade (ML77/MP73/PP92) with a polytomy encompassing the representatives of subsect. Androsaceae in accordance with the ITS tree: S. androsacea, S. seguieri and S. styriaca. Additionally, in contrast to the ITS tree, it contained all accessions of S. wahlenbergii grouped in two subclades. The second major subclade (ML64/MP66/PP98) contained the remaining species, namely S. irrigua (subsection placement uncertain), a clade grouping species of subsect. Arachnoideae (S. arachnoidea, S. paradoxa, etc.) and a clade grouping species of subsect. Saxifraga (S. bulbifera, S. conifera, S. hypnoides, S. magellanica, S. praetermissa, S. vayredana, etc.)
Analysis of ITS variation (Sanger and NGS data)
The NGS analysis of 28 samples of twelve species yielded 53 ITS2 variants. The tree based on Sanger ITS sequences and NGS data (Fig. 5) showed a similar topology as the reduced nrDNA dataset (Fig. 3). The majority of ITS2 variants of S. wahlenbergii, including all Sanger-based sequences, formed a coherent branch (node 10; ML72/MP61/PP97) in a clade comprising S. adscendens, S. discolor and S. osloensis (node 9; ML100/MP97/PP100). As in the reduced ITS dataset, the former clade was placed in a dichotomy with the one constituted by S. tridactylites and one accession of S. osloensis (node 8; ML100/MP100/PP100). Also in congruence with the phylogenetic tree based on the reduced ITS dataset (Fig. 3), most sequences of S. styriaca (Sanger and NGS) were placed in a single clade (node 17; ML96/MP97/PP100) with S. androsacea, S. italica, S. seguieri (all Sanger and NGS sequences) and S. depressa (NGS) as closest relatives (Fig. 5). Deviant phylogenetic relationships, not revealed by the Sanger sequencing analysis, were found for the remaining, less abundant, NGS variants of S. wahlenbergii. They were nested in a clade along with NGS variants of S. androsacea, S. depressa, S. seguieri, S. styriaca and the Sanger sequence of S. androsacea (node 12; ML98/MP86/PP100). This clade was represented in the Sanger-based phylogeny by S. androsacea (1) only (Fig. 3). In general, these minority NGS variants of S. wahlenbergii (obtained from seven out of eleven samples = 64%) and all sequences of S. androsacea, S. depressa, S. italica, S. seguieri and S. styriaca fell in one internally diversified clade (node 11; ML72/MP62/PP96) with S. irrigua as sister.
Divergence time estimation
The divergence time estimations of relevant clades in Saxifraga based on the ITS dataset including the NGS reads of ITS2 are shown in Fig. 6. The origin of Saxifraga (stem) was estimated to 74.5 Ma (node 3; 95% HDP = 61.1–86.6) and the Saxifraga crown age to 56.1 Ma (node 4; 95% HDP = 43.6–68.1). The stem age of Saxifraga sect. Saxifraga was estimated to 28.3 Ma (node 5; 95% HDP = 21.2–37.1). These age values are comparable to the results of Ebersbach et al.  and Gao et al. .
Stem ages of Saxifraga subsect. Tridactylites and subsect. Androsaceae were dated to 22.6 Ma (node 6; 95% HDP = 16.3–29.9) and 12.0 Ma (node 11; 95% HDP = 7.5–17.5), respectively. The crown age of subsect. Tridactylites was dated to 15.5 Ma (node 7; 95% HDP = 8.6–23.1), when the lowland species S. tridactylites and one accession of S. osloensis (1) segregated from the alpine species group of S. adscendens, S. discolor, S. wahlenbergii and one accession of S. osloensis (2). Saxifraga wahlenbergii (Tridactylites-related sequence) segregated from S. adscendens at ca. 4.7 Ma (node 10; 95% HDP = 2.4–8.9).
Diversification within the subsect. Androsaceae occurred after 9.1 Ma (node 12; 95% HDP = 5.6–13.8; crown age). The widespread S. androsacea seems to be the oldest species in this section (Fig. 6). Saxifraga styriaca split off the other species from the sister clade to S. androsacea at approximately 6.7 Ma (node 14; 95% HDP = 3.7–10.3).
Phylogenetic position of Saxifraga wahlenbergii and S. styriaca
According to the nuclear and plastid DNA data, the Central European narrow mountain endemics S. wahlenbergii (Western Carpathians) and S. styriaca (Eastern Alps) are firmly nested within the large S. sect. Saxifraga (Figs. 3 and 4; Additional file 3: Figure S1, Additional file 4: Figure S2). This group is one of ca. 13 sections of the genus Saxifraga  and accommodates altogether 70–85 species (about 16% of the total species number) with predominantly European distribution. The phylogenetic placement based on 14 S. wahlenbergii and four S. styriaca samples used in this study corroborates previous preliminary reports [44, 45].
Within S. sect. Saxifraga, the inferred phylogenetic relationships of S. wahlenbergii and S. styriaca are different for the nuclear and plastid data. In the ITS tree based on Sanger sequences, they are placed in two different main subclades (Fig. 3), which does not support their status as sister species hypothesized based on morphological features . In contrast, both species are indeed closely related based on the plastid DNA tree where they belong to the same clade together with several species of S. subsect. Androsaceae (Fig. 4). While the affinity to this subsection is congruently displayed by S. styriaca in the two datasets, S. wahlenbergii has a nrDNA resembling that of S. adscendens, S. discolor, S. osloensis and S. tridactylites (subsect. Tridactylites) and plastid DNA resembling that of S. androsacea, S. italica and S. seguieri (subsect. Androsaceae). This incongruence suggests that S. wahlenbergii originated from hybridisation between representatives of these subsections, supporting the hypothesis of Tkach et al. , which was, however, based on a single sample of this species.
Incidentally, it is worth noting that S. osloensis, a tetraploid species originating from hybridisation between S. adscendens and S. tridactylites [45, 68], is represented in this study by different maternal ITS DNA copies as revealed by comparison of nuclear and plastid DNA trees (Figs. 3 and 4), namely the one of S. tridactylites in accession S. osloensis (1) and the one of S. adscendens in accession S. osloensis (2). For the accession S. osloensis (1) used in this study, the second parental ITS sequence was detected neither in Sanger analysis nor in NGS reads (Fig. 5). The sequence data for S. osloensis (2) were taken from GenBank (Sanger only; see Additional file 1: Table S1). A recurrent origin of this hybrid taxon is likely to explain placement of its accessions in different subclades of our tree.
NGS data provide evidence for introgression
The NGS screening of nuclear ITS2 proved efficient in retrieving within-individual sequence variation and detecting both majority and minority variants present in genomes. It shed further light on the origin of the focal species and provides information not retrieved from the Sanger sequencing. The by far predominant number of the sequence reads (99.8%) in S. wahlenbergii was placed in the lineage comprising the species of S. subsect. Tridactylites, as expected from the Sanger sequencing data (Fig. 5). Here, S. wahlenbergii sequences (Sanger and NGS) formed a subclade most closely related to S. adscendens, S. discolor and one accession of S. osloensis. However, the NGS analysis additionally unravelled a minority set of sequences in S. wahlenbergii, which was placed within the subclade of S. subsect. Androsaceae, thus corroborating the plastid tree. These sequences were far less numerous (0.2%) and were detected in most but not all individuals (64%). They grouped with the majority of S. androsacea reads (98.2%) from various geographical regions and some minority ITS2 variants of S. depressa, S. seguieri, S. styriaca. Minority variants detected in the last-mentioned three species may have arisen via hybridization or introgression from S. androsacea (see below) and the vast majority of their NGS reads (99% in the case of S. styriaca) were placed outside this clade and followed the topology detected in the Sanger-based phylogeny (Fig. 3). The presence of minority ITS2 variants incongruent with the placement of major variants could arguably be suspected as possible sample contamination, but we took a special care, both during the lab procedures and in filtering the obtained reads, keeping only those present in more than 100 copies in both independent reaction replicates.
A minority of the NGS variants in S. depressa and S. styriaca (0.1%) grouped together and mixed up with the Sanger sequence of S. androsacea and NGS variants of S. androsacea, S. seguieri and S. wahlenbergii (ML98/MP86/PP100; Fig. 5).
In general, in the complex pattern of genetic introgression observed between the species constituting the clade of subsect. Androsaceae (Fig. 5), three scenarios were observed. (1) Within S. depressa, S. styriaca and S. wahlenbergii minority ITS variants of S. androsacea were found but not vice versa. (2) Between S. seguieri and S. androsacea, there was reciprocal exchange. (3) Within S. androsacea a copy of nrITS of S. italica was found but not vice versa. This evidence concurs with frequent hybridisation reported for Saxifraga androsacea throughout its range, essentially with species placed in the same subsection. Described hybrids include S. androsacea × S. styriaca = S. ×melzeri Köckinger, S. androsacea × S. depressa = S. ×vierhapperi Handel-Mazetti, S. androsacea × S. seguieri = S. ×padellae Brügger, S. androsacea × S. wahlenbergii = S. ×thrinax Rechinger (the parental taxa of the latter hybrid however are considered uncertain; e.g., ).
The extensive hybridisation within subsect. Androsaceae seems to reflect the geographical distribution of these high-mountain plants. Saxifraga androsacea is the most widespread and its distribution encompasses wide parts of Eurasia including mountains of Europe, the eastern Altai, mountains west of Lake Baikal and the Himalayas of Pakistan. It overlaps with the ranges of the narrowly distributed endemics S. depressa (Eastern Alps: Dolomites), S. seguieri (middle part of the Alpine arc), S. styriaca (Eastern Alps: Lower Tauern), S. wahlenbergii (Western Carpathians). No hybrids between S. androsacea and S. italica were reported, which obviously agrees with the absence of S. androsacea in the Central Apennines, where S. italica occurs. However, an NGS-based ITS copy congruent with S. italica was observed in the Pyrenean accession of S. androsacea in our data set. It is worth noting that the DNA from this S. androsacea sample was isolated in a different laboratory than the sample of S. italica. Therefore, cross-contamination is an unlikely explanation of this pattern.
Saxifraga androsacea is cytogenetically highly variable; chromosome numbers of 2n = 16 (likely erroneous), 66, 88, 105, ca. 112, ca. 120, 124, 128, 154, 192, 198, 206–220, 208, 210, 220 were reported (Chromosome Counts Database [CCDB], http://ccdb.tau.ac.il/ ). The count of 2n = 220 represents the highest chromosome number in Saxifraga . The wide range of chromosome numbers points to an important role of polyploid evolution in S. androsacea and, indeed, allopolyploidy could explain the presence of several different ITS variants found in this species. Chromosome numbers of other species (see ) are rather uniform and clearly based on x = 11, namely S. italica (2n = 66), S. seguieri (2n = 66), S. wahlenbergii (2n = 66); no counts are available for S. depressa and S. styriaca. In the case of S. subsect. Tridactylites – involved in formation of S. wahlenbergii – disregarding the geographically remote, tetraploid S. osloensis (2n = 44), both S. adscendens and S. tridactylites are diploids with 2n = 22 chromosomes.
Morphological similarity of S. wahlenbergii and S. styriaca
Saxifraga wahlenbergii has previously been treated as a separate, monotypic ‘grex’ or series Perdurantes (S.Pawł.) S.Pawł. [18, 71]. The main diagnostic character of Perdurantes was the presence of peculiarly shaped glandular hairs that were later found also in S. styriaca (; Fig. 7) but are absent in all other species of Saxifraga studied so far . This character induced Köckinger  to suggest an intimate relationship between S. styriaca and S. wahlenbergii, which also share characters of the leaf morphology, protogynous flowering and a similar growth form (Fig. 1). Köckinger , however, also noted considerable differences at flowering time when both species are unmistakable. The inflorescences are consistently one-flowered in S. styriaca versus usually several-flowered in S. wahlenbergii, petals are minute and yellowish-green in S. styriaca whereas they are large and white in S. wahlenbergii (Fig. 1a–c). According to our results, the peculiar glandular hairs of S. styriaca and S. wahlenbergii (Fig. 7) are seemingly a homoplasious character and do not represent a synapomorphy of both species but rather have a parallel, independent origin. Alternatively, but less likely, one might assume an extinct S. androsacea-like ancestor with this type of hairs currently found only in S. wahlenbergii and S. styriaca.
The close relationship of S. wahlenbergii and the Pyrenean-Cantabrian S. praetermissa, suggested by Engler , Engler & Irmscher  and Webb & Gornall , who placed both species in a separate series Axilliflorae (Willk.) Pawł., was not supported by our molecular phylogenetic results. Saxifraga praetermissa was placed within a clade containing other species from subsect. Saxifraga, distant to S. wahlenbergii in both plastid and nuclear ITS trees (Figs. 3, 4 and 5). This agrees with differences in the position of the flowering stems (axillary in S. praetermissa and terminal in S. wahlenbergii) as documented by Pawłowska , despite overall similar appearance of both species. In the same line, the suggestion by Pax  that S. wahlenbergii is related to S. moschata was not supported by phylogenetic data. It is important to note that the relationships of S. wahlenbergii found in our study were already considered by Ball  in the original description of S. wahlenbergii. He clearly pointed to its similarities to S. androsacea as well as to S. adscendens (as S. controversa Sternb.) in the case of specimens growing at lower elevations.
Saxifraga styriaca, on the other hand, was initially misidentified as S. aphylla, a more widespread endemic species of the Eastern Alps because of similar 3-lobed cuneate leaves, leafless flowering stems, narrow and short petals . The decumbent stems, later flowering time, protandry, petals longer than sepals, shortly stalked hairs with spherical heads and ecological characteristics of S. aphylla, however, are in contrast to the typical features of S. styriaca. These morphological differences were underscored by the molecular phylogenetic placement of S. aphylla distant to S. styriaca in a clade representing subsect. Arachnoideae (Engl. & Irmscher) Tkach, Röser & M.H.Hoffm. (Figs. 3, 4 and 5).
Hybrid origin of S. wahlenbergii
The combination of plastid and ITS sequences indicates that the paternal ancestor of S. wahlenbergii was a species closely related to S. adscendens (Figs. 3 and 5), if not S. adscendens itself. In contrast to the majority of saxifrages, all species of subsect. Tridactylites are short-lived. Saxifraga tridactylites and S. osloensis are annual, whereas S. adscendens and S. discolor are biennial. It can be assumed that the maternal parent contributing the subsect. Androsaceae-like plastid DNA was perennial, as this is the only life form present in this subsection, and this life form was established in S. wahlenbergii. Nuclear and plastid DNA do not provide an unequivocal indication as to which species of subsect. Androsaceae was the actual parent of S. wahlenbergii. Considering the biogeographical context, it was most likely S. androsacea, because it is currently a widespread species and the only representative of this subsection that inhabits the Western Carpathians. This is further corroborated by the placement of subsect. Androsaceae-like NGS ITS variants of S. wahlenbergii within the clade of S. androsacea.
The occurrence of a significantly lower number of NGS reads of subsect. Androsaceae-like nuclear ITS in S. wahlenbergii (Fig. 5) may suggest that the maternal ITS was mostly replaced by subsect. Tridactylites-like variants following the hybridisation. In four of eleven samples of S. wahlenbergii analysed with NGS subsect. Androsaceae-like variants could not be detected (S. wahlenbergii 6, 8, 11, 14; Fig. 5). Such unidirectional loss through the process of concerted evolution, involving gene conversion and recombination, is frequent in the repetitive ribosomal DNA [76,77,78,79,80,81]. Alternatively, the presence of subsect. Androsaceae-like ITS variants in S. wahlenbergii may result from infrequent cases of more recent introgression. Based on our data it is not possible to discern between these two explanations; also a combination of both processes cannot be ruled out. In any event, hybridisation is clearly witnessed by the exclusive presence of plastid DNA from the S. androsacea lineage in all accessions of S. wahlenbergii.
The presumable paternal parent, S. adscendens, is disjunctly distributed in Fennoscandia, the European Alpine System, Anatolia and the Caucasus as well as in the mountains of western North America. In the Western Carpathians, its distribution overlaps with the range of S. androsacea, which makes it likely that S. wahlenbergii originated in situ in this area. The other species of subsect. Tridactylites nested in the clade of S. wahlenbergii and S. adscendens (Figs. 3 and 5) occupy narrow ranges distant to the Western Carpathians. Saxifraga discolor (syn. S. adscendens var. discolor) occurs in the Balkan Peninsula , while the hybrid species S. osloensis occurs only in a small area of southern Scandinavia . The predominantly lowland plant S. tridactylites, which is also widespread in Europe, can be excluded as parent of S. wahlenbergii due to its distant position in the phylogenetic trees (Figs. 3, 4 and 5).
According to our divergence time estimation, the maximal age of the origin of S. wahlenbergii is set later than 4.7 Ma, when its paternal, S. adscendens-like ITS DNA originated (Fig. 6). The hybridisation with the second parent representing subsect. Androsaceae, occurred necessarily at a later time. It could correspond to the late Pliocene cooling periods or the Pleistocene. The earliest glaciation in Poland is now dated to the uppermost Lower Pleistocene (about 0.9 Ma) when the ice sheet reached the mid-southern part of the country . Even postglacial origin of S. wahlenbergii may be considered, because S. adscendens and S. androsacea presently co-exist in the Tatra Mountains and neighbouring massifs, partly in a similar altitudinal range [84, 85]. However, an older origin of the species seems more likely for several reasons. First, the origin of S. wahlenbergii involves two remotely related taxa for which no contemporary hybridisation has been reported to date . Thus, a hybridisation incident could be expected earlier in their evolutionary history and maybe also in significantly different ecological conditions than those acting today . Second, the subsect. Tridactylites-related sequence of S. wahlenbergii shows some divergence from sequence of the extant S. adscendens lineage (Fig. 5; checked also in additional specimens of S. adscendens growing in sympatry with S. wahlenbergii; E. Cieślak, M. Ronikier, unpubl. data). Finally, some degree of geographically-driven intraspecific diversification observed in S. wahlenbergii (Fig. 4; E. Cieślak & M. Ronikier, unpubl. data) also suggests a longer than postglacial historical context for this taxon.
Saxifraga wahlenbergii was usually considered an ‘ancient’ Tertiary relict of the Western Carpathian flora [17,18,19, 87], even though it was not explicitly implied that it belonged to the circumboreal flora that thrived under warm and wet climatic conditions during the early to mid-Tertiary (65–15 Ma) [88, 89]. Pawłowski  suggested an origin of S. wahlenbergii in the ‘pre-Diluvial’ period and mentioned a time span from Pliocene to Early Pleistocene. Our results on the maximum potential age of this endemic species agree with Pawłowski’s estimation and certainly speak against an origin of S. wahlenbergii during the Tertiary climatic optimum. The Pleistocene glaciations and related importance of stable refuge areas are among important historical events that increase diversity of (endemic) vascular plants as reviewed by Bruchmann & Hobohm . On the other hand, distribution shifts induced by recurrent climatic changes may be particularly important for hybrid speciation.
Dated phylogenies for the Carpathian endemic plants species are still scarce . A recent study on Syringa josikea, an endemic shrub of temperate montane forests in the Apuseni Mountains and the Eastern Carpathians, established an age of ca. 1.9 Ma (Early Pleistocene) for the segregation from its closest relatives . Forest species like Syringa josikea have presumably survived the Last Glacial Maximum (LGM) in lowlands surrounding the Carpathians or even within the mountain range . It can be expected that S. wahlenbergii, a plant reaching alpine and subnival zones, may have survived the (maximally) past 4.7 Ma, a period spanning the entire Pleistocene, in situ in the Western Carpathians by following the shifts of the altitudinal vegetation caused by the glacial-interglacial cycles as discussed for several other alpine species in the region (e.g., [43, 91]). Such vertical migrations are important for in situ survival of alpine plant species. The cold periods have even led to an extensive increase of suitable habitats for alpine plants in lower altitudes of the Carpathians (: Fig. 2). On the other hand, glacial survival within the Western Carpathians is considered likely also for species of the montane woodland zone  suggesting maintenance of a wide range of ecological conditions.
The origin of Saxifraga styriaca (ca. 6.8 Ma) predates the Pleistocene and reaches back to the Late Miocene (Messinian), overlapping with the final phase of the Alpine orogeny that lasted until 2.6 Ma . S. styriaca, with a narrow range covering only ca. 1250 km2, agrees with a typical pattern of an Alpine endemic plant species as it belongs to a lineage otherwise widespread in the European Alpine System . It likely belongs to the elements of the Alpine flora that survived the Pleistocene glaciations in the refuge areas in situ. Its present-day distribution fits largely the most important glacial refuge area for silicicolous plants in the Eastern Alps (region S1 in : Fig. 5; [95, 96]).
The evolutionary history of the Eastern Alpine endemic S. styriaca is strongly different from that of West Carpathian S. wahlenbergii. They are neither sister species that would provide an example of vicariance or dispersal nor do they represent a link between the floras of the Eastern Alps and the Carpathians. Saxifraga styriaca seems to have been even more conservative than the Carpathian endemic in keeping its very restricted present-day range within the refuge area. Our study underlines the importance of multilocus DNA studies in endemic species along with their close relatives to clarify the evolutionary and biogeographical connections between the floras of high mountain regions.
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We thank Laura Freisleben (Halle), Justyna Nowak (Kraków) and Magda Tomaszewicz (Kraków) for their technical support in the laboratory work, Patrik Mráz (Praha) for valuable comments on an earlier version of the manuscript, Filippo Prosser (Rovereto) and Gerald M. Schneeweiss (Vienna) for their help in obtaining herbarium specimens.
MiR, NT, MaR and PS designed the study; NT, EC and TS performed the experimental part; MaR, NT, TS and MiR analysed the data; NT, MaR and MiR wrote the manuscript with contributions from all authors. All authors read and approved the final version.
Collecting of plant samples was carried out based on permits granted by Tatrzański Park Narodowy, Poland (no. Bot-203) and Ministerstvo životného prostredia, Slovakia (no. 1762/565/04–5.1 and 6188/2017–6.3). The study was partly financially supported by the European Commission under the 6th Framework Programme (project IntraBioDiv, no. GOCE-CT-2003-505376) and Polish-Swiss Research Programme (grant no. PSPB-161/2010). MiR, TS and EC were supported by the statutory funds of the W. Szafer Institute of Botany, Polish Academy of Sciences. We acknowledge the financial support within the funding programme Open Access Publishing by the German Research Foundation (DFG).
Availability of data and materials
The Sanger sequences reported in this paper have been deposited in the ENA/GenBank databases (www.ebi.ac.uk/ena/; www.ncbi.nlm.nih.gov/genbank/). The datasets used and/or analysed in this study are available in the electronic supplement of this publication (Additional file 2). Paired-end merged and adapter trimmed sequences are deposited in Short Read Archive of the European Bioinformatics Institute under http://www.ebi.ac.uk/ena/data/view/PRJEB29399.
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Table S1. Taxa included in the phylogenetic analysis. ENA/GenBank accession numbers are given for all ITS, trnL–trnF and rpl32–trnL Sanger sequences used in this study, followed by available ITS2 sequences obtained from NGS (without ENA/GenBank entry). They are denoted as “ITS2 variants A–D”. Missing sequence data are indicated by “NA” (not available). Voucher data (country and region, collector and collection number, herbarium code according to Thiers et al. ) are provided for newly generated sequences, which are in bold print. MR: herbarium of G. & S. Miehe deposited at the Institute of Geography, University Marburg, Germany. (PDF 502 kb)
Sequence alignments (FASTA) used in this study (ITS extended taxon set, ITS reduced taxon set, ITS reduced taxon set with NGS reads, ITS reduced taxon set with NGS reads for molecular clock, trnL–trnF and rpl32–trnL extended taxon set, trnL–trnF and rpl32–trnL reduced taxon set) and the BEAUti-generated XML file. See Methods for details and explanation. (ZIP 189 kb)
Figure S1. Maximum likelihood phylogram of Saxifraga (arrow) and representative genera of Saxifragaceae based on nuclear ribosomal ITS DNA Sanger sequence data. Pterostemon rotundifolius and Itea virginica (Iteaceae) were chosen as outgroups. Maximum likelihood and maximum parsimony bootstrap support values as well as posterior probabilities of Bayesian inference ≥50% are indicated on the branches. The sections of Saxifraga are labelled on the right-hand side. (PDF 2680 kb)
Figure S2. Maximum likelihood phylogram of Saxifraga (arrow) and representative genera of Saxifragaceae based on plastid trnL–trnF and rpl32–trnL Sanger sequence data. Pterostemon rotundifolius and Itea virginica (Iteaceae) were chosen as outgroups. Maximum likelihood and maximum parsimony bootstrap support values as well posterior probabilities of Bayesian inference ≥50% are indicated on the branches. The sections of Saxifraga are labelled on the right-hand side. (PDF 793 kb)
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Tkach, N., Röser, M., Suchan, T. et al. Contrasting evolutionary origins of two mountain endemics: Saxifraga wahlenbergii (Western Carpathians) and S. styriaca (Eastern Alps). BMC Evol Biol 19, 18 (2019). https://doi.org/10.1186/s12862-019-1355-x
- European mountains
- Hybrid speciation
- ITS genomic screening
- Molecular clock
- Tertiary relict