Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/121030
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dc.contributor.authorFordham, D.-
dc.contributor.authorBrown, S.-
dc.contributor.authorWigley, T.-
dc.contributor.authorRahbek, C.-
dc.date.issued2019-
dc.identifier.citationCurrent Biology, 2019; 29(10):R356-R357-
dc.identifier.issn0960-9822-
dc.identifier.issn1879-0445-
dc.identifier.urihttp://hdl.handle.net/2440/121030-
dc.description.abstractThe stability of regional climates on millennial timescales is theorised to be a primary determinant of nearby diversification [1-5]. Using simulated patterns of past temperature change at monthly timescales [6], we show that the locations of climatically stable regions are likely to have varied considerably across and within millennia during glacial-interglacial cycles of the Late Quaternary. This result has important implications for the role of regional climate stability in theories of speciation, because long-term climate refugia are typically presumed to be 'cradles' of diversity (areas of high speciation) only if they remain stable across Milankovitch climate oscillations [1-5], which operate on multi-millennial time scales [7].-
dc.description.statementofresponsibilityDamien A. Fordham, Stuart C. Brown, Tom M.L. Wigley and Carsten Rahbek-
dc.language.isoen-
dc.publisherElsevier-
dc.rights© 2019 Elsevier Ltd.-
dc.subjectBiodiversity-
dc.subjectClimate-
dc.subjectClimate Change-
dc.titleCradles of diversity are unlikely relics of regional climate stability-
dc.typeJournal article-
dc.identifier.doi10.1016/j.cub.2019.04.001-
dc.relation.granthttp://purl.org/au-research/grants/arc/DP180102392-
dc.relation.granthttp://purl.org/au-research/grants/arc/FT140101192-
dc.relation.granthttp://purl.org/au-research/grants/arc/DP130103261-
pubs.publication-statusPublished-
dc.identifier.orcidFordham, D. [0000-0003-2137-5592]-
dc.identifier.orcidBrown, S. [0000-0002-0669-1418]-
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