2018
DOI: 10.23855/preslia.2018.039
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Postglacial history and current population genetic diversity of a central-European forest plant Hacquetia epipactis

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Cited by 15 publications
(9 citation statements)
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“…(Primulaceae; Slovák et al, 2012 ), Hacquetia epipactis (Scop.) DC (Apiaceae; Urbaniak et al, 2018 ), and Knautia drymeia Heuff. (Caprifoliaceae; Rešetnik et al, 2016 ).…”
Section: Discussionmentioning
confidence: 99%
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“…(Primulaceae; Slovák et al, 2012 ), Hacquetia epipactis (Scop.) DC (Apiaceae; Urbaniak et al, 2018 ), and Knautia drymeia Heuff. (Caprifoliaceae; Rešetnik et al, 2016 ).…”
Section: Discussionmentioning
confidence: 99%
“…To date, among the studies including samples from the area only Daneck et al (2016) suggested that a glacial refugium in the eastern part of the Northern Limestone Alps “cannot be excluded” for Rosa pendulina based on somewhat ambiguous Amplified Fragment Length Polymorphism evidence. In contrast, a refugium in the southeastern Alps and the adjacent Balkan Peninsula was strongly supported, for instance, for Cyclamen purpurascens ( Slovák et al, 2012 ) and Hacquetia epipactis ( Urbaniak et al, 2018 ).…”
Section: Introductionmentioning
confidence: 99%
“…It is difficult to ascertain when and how the Allium representatives reached Europe, though most probably from their Asian diversity center, thereby inhabiting new territory and new sites. The migration of plants in this case is a key factor responsible for the observed intraspecific diversity [3,4]. Plants inhabiting new locations and adapting to specific sites often develop local morphologically and/or genetically diverse ecotypes and this seems to be the main reason why many similar populations of rare species were also recognized as having less genetic diversity than more widely distributed species [5].…”
Section: Introductionmentioning
confidence: 99%
“…The present distribution and genetic structure of organisms are consequences of repeated climatic changes in the Pleistocene during the past several million years. The cold periods in the Pleistocene Epoch caused substantial changes in ecosystems, such as organism extinction, habitat fragmentation, and modified vegetation in the colder areas of Europe, America, and the Arctic [1][2][3][4].These climatic changes were also the primary reason for numerous plant or animal migrations to the southern part of Europe or into warmer localities, in front of glaciers, where they were able to survive unfavorable conditions; once favorable conditions returned, they could migrate back to the northern areas [5][6][7]. Such organisms, commonly called glacial relicts, were widely distributed when the climate changed in the Holocene Epoch; the changing climate also caused numerous organisms to adapt to the new climatic conditions and reduced their ranges to smaller refugia, mostly in high mountains, where the arctic boreal conditions and cold climate remained.…”
Section: Introductionmentioning
confidence: 99%