Evidence map›Paper›PMID 30634910›Full record

ArticleBMC evolutionary biology2019

Contrasting evolutionary origins of two mountain endemics: Saxifraga wahlenbergii (Western Carpathians) and S. styriaca (Eastern Alps).

Natalia Tkach, Martin Röser, Tomasz Suchan, Elżbieta Cieślak, Peter Schönswetter, Michał Ronikier

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Article in BMC evolutionary biology, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.

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5 citing papers in PubMed.

  1. Glacial history ofPhytoKeys · 2024
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6 authors.

Natalia TkachInstitute of Biology, Martin Luther University Halle-Wittenberg, Neuwerk 21, 06108, Halle, Germany. natalia.tkach@botanik.uni-halle.de.ORCID 0000-0002-4627-0706
Martin RöserInstitute of Biology, Martin Luther University Halle-Wittenberg, Neuwerk 21, 06108, Halle, Germany.
Tomasz SuchanW. Szafer Institute of Botany, Polish Academy of Sciences, Lubicz 46, 31-512, Krakow, Poland.
Elżbieta CieślakW. Szafer Institute of Botany, Polish Academy of Sciences, Lubicz 46, 31-512, Krakow, Poland.
Peter SchönswetterDepartment of Botany, University of Innsbruck, Sternwartestraße 15, 6020, Innsbruck, Austria.
Michał RonikierW. Szafer Institute of Botany, Polish Academy of Sciences, Lubicz 46, 31-512, Krakow, Poland. m.ronikier@botany.pl.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

backgroundThe 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.

resultsWe 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.

conclusionsSaxifraga 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.

Indexed as

Biological EvolutionEcosystemEvolution, MolecularGenetic MarkersGenetic VariationGeographyLikelihood FunctionsPhylogenyPlant StemsSaxifragaceaeSequence Analysis, DNATime FactorsGenetic MarkersAlpsCarpathiansEndemicsEuropean mountainsHybrid speciationITS genomic screeningMolecular clockNGSPhylogeneticsTertiary relict

Identifiers

PMID30634910
PMCPMC6329101

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