2021
DOI: 10.1111/geb.13274
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Post‐glacial determinants of regional species pools in alpine grasslands

Abstract: Aim Alpine habitats support unique biodiversity confined to high‐elevation areas in the current interglacial. Plant diversity in these habitats may respond to area, environment, connectivity and isolation, yet these factors have been rarely evaluated in concert. Here we investigate major determinants of regional species pools in alpine grasslands, and the responses of their constituent species groups. Location European mountains below 50° N. Time period Between 1928 and 2019. Major taxa studied Vascular plants… Show more

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Cited by 27 publications
(47 citation statements)
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References 79 publications
(109 reference statements)
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“…Mountains of León are expected given their geographic proximity . Indeed, the two mountain systems have been recently considered as a single biogeographical unit (Fernández-Prieto et al, 2020) and a single refugia for alpine species in Europe (Jiménez-Alfaro et al, 2021). From cold alpine (1) to cool subalpine (3), submontane (5), warm lowland (7) and warmest (9) temperatures.…”
Section: Ecological Indicatorsmentioning
confidence: 99%
“…Mountains of León are expected given their geographic proximity . Indeed, the two mountain systems have been recently considered as a single biogeographical unit (Fernández-Prieto et al, 2020) and a single refugia for alpine species in Europe (Jiménez-Alfaro et al, 2021). From cold alpine (1) to cool subalpine (3), submontane (5), warm lowland (7) and warmest (9) temperatures.…”
Section: Ecological Indicatorsmentioning
confidence: 99%
“…Global alpine areas can be grouped according to their macroclimate (Testolin et al, 2020), and they are linked to different vegetation zones (Walter & Box, 1976) and biomes characterised by their distinct evolutionary history and own species pools (Mucina, 2019). Indeed, present-day alpine floras are the result of upward shifts of species undergoing regional radiations and long-distance migrations associated with the displacement of cold-climate biomes, such as during the Pleistocene glacial cycles (Billings, 1974;Horandl & Emadzade, 2011;Jiménez-Alfaro et al, 2021). The historical legacy of ancestral species, which may have belonged to different vegetation zones and biogeographic realms, together with the environmental filtering of the current macroclimate, have determined the diversity of alpine trait pools, i.e.…”
Section: Introductionmentioning
confidence: 99%
“…The 'drama' of glaciation and deglaciation of alpine terrain recurred 8-10 times during the last 1 million years, meaning that all but some rock flora on so-called nunatak outcrops [48] that protruded the ice shield became locally eradicated and pushed into refugia at the low elevation edges of the ice shield [49]. Since these refugia were often not connected, the fingerprints of genetic differentiation into clusters of greater similarity within species can still be found in the current alpine flora [4,[50][51][52]. The different routes of re-colonisation added to such patterns [53].…”
Section: Viewing Alpine Plant Life Over Geological Time Scalesmentioning
confidence: 99%