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dc.date.accessioned2018-03-12T09:55:14Z
dc.date.available2018-03-12T09:55:14Z
dc.date.created2017-02-09T12:48:26Z
dc.date.issued2017
dc.identifier.citationChala, Desalegn Zimmermann, Niklaus E. Brochmann, Christian Bakkestuen, Vegar . Migration corridors for alpine plants among the `sky islands? of eastern Africa: do they, or did they exist?. Alpine Botany. 2017, Published ahead of print, 1-12
dc.identifier.urihttp://hdl.handle.net/10852/60906
dc.description.abstractThe tropical alpine ecosystem in eastern Africa is highly fragmented among biological ‘sky islands’, where populations of frost-tolerant organisms are isolated from each other by a ‘sea’ of tropical lowlands. One-third of the species in the afroalpine flora are exclusively alpine, but the other species can to varying degrees extend into grasslands and open forests of lower vegetation belts. A long-debated question is whether colonization of the alpine zone of these mountains and subsequent intermountain gene flow entirely depend on long-distance dispersal across unsuitable habitats, or whether suitable habitats shifted far enough downslope under past colder climates to form bridges enabling gradual migration. Here we address this question using a classification tree model. We mapped the extent of the current alpine habitat and projected it to the last glacial maximum (LGM) climate to assess whether gradual migration was possible for exclusively alpine taxa during this glacial period, and thus potentially also during earlier Pleistocene glaciations. Next, we modelled landcover under current and LGM climates to assess whether grassland and open forests could have served as migration corridors for alpine taxa that today extend into lower vegetation belts. We estimated that the LGM treeline was about 1000 m lower and the alpine habitat was about eight times larger than that today. At the LGM, we found that most of the currently fragmented alpine habitat of the Ethiopian highlands was interconnected except across the Great Rift Valley, whereas the solitary mountains of East/Central Africa remained isolated for exclusively alpine species. However, for drought-tolerant alpine species that today extend below the treeline, gradual migration through habitat corridors may have been possible among mountains during the dry glacial periods, and possibly also under the current climate before agriculture transformed the low-lying landscapes. Afroalpine · CART · Gene flow · Habitat connectivity · Last glacial maximum · Treeline This is a post-peer-review, pre-copyedit version of an article published in Alpine Botany. The final authenticated version is available online at: http://dx.doi.org/10.1007/s00035-017-0184-zen_US
dc.languageEN
dc.language.isoenen_US
dc.publisherBirkhaeuser Verlag AG
dc.titleMigration corridors for alpine plants among the `sky islands? of eastern Africa: do they, or did they exist?en_US
dc.typeJournal articleen_US
dc.creator.authorChala, Desalegn
dc.creator.authorZimmermann, Niklaus E.
dc.creator.authorBrochmann, Christian
dc.creator.authorBakkestuen, Vegar
cristin.unitcode185,28,8,5
cristin.unitnameForskningsgruppen Planteevolusjon og DNA Metabarcoding
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.fulltextpreprint
cristin.qualitycode1
dc.identifier.cristin1448878
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Alpine Botany&rft.volume=Published ahead of print&rft.spage=1&rft.date=2017
dc.identifier.jtitleAlpine Botany
dc.identifier.volume127
dc.identifier.issue2
dc.identifier.startpage133
dc.identifier.endpage144
dc.identifier.doihttp://dx.doi.org/10.1007/s00035-017-0184-z
dc.identifier.urnURN:NBN:no-63552
dc.type.documentTidsskriftartikkelen_US
dc.type.peerreviewedPeer reviewed
dc.source.issn1664-2201
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/60906/2/HMP_AlpBot_CleanCristin.pdf
dc.type.versionAcceptedVersion
dc.relation.projectANDRE/Norwegian State Loan Fund (Lånekassen)
dc.relation.projectEI/Natural History Museum, University of Oslo
dc.relation.projectSIU/NUFU 2007/10058


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