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dc.contributor.authorDavies, A. L.
dc.contributor.authorSmith, M. A.
dc.contributor.authorFroyd, C. A.
dc.contributor.authorMcCulloch, R. D.
dc.identifier.citationDavies , A L , Smith , M A , Froyd , C A & McCulloch , R D 2017 , ' Microclimate variability and long-term persistence of fragmented woodland ' , Biological Conservation , vol. 213 , no. Part A , pp. 95-105 .
dc.identifier.otherPURE: 250484896
dc.identifier.otherPURE UUID: 453fee29-cdd5-4526-ab8d-f8eea639a495
dc.identifier.otherScopus: 85021900092
dc.identifier.otherORCID: /0000-0002-8982-7471/work/52888768
dc.identifier.otherWOS: 000410014100012
dc.descriptionThis work was conducted with funding from The Woodland Trust.en
dc.description.abstractFavourable microclimates are predicted to buffer fragmented populations against the effects of environmental change, but ecological timeseries are often too short to establish the extent to which such microsites facilitate population persistence through multiple climate shifts. We investigate the effects of microclimatic heterogeneity on woodland resilience through millennial climate and disturbance shifts near northwest European woodland range limits. We use palaeoecological data from northern Scotland to study the effects of fragmentation on community composition and diversity in a potentially favourable microclimate, and compare palynological timeseries of tree abundance from five sites to assess the effects of favourable (low-lying sheltered) versus more marginal (higher altitude) settings on population persistence and stability. The sheltered site shows persistence of tree cover through Holocene climatic and anthropogenic shifts, including climatically-driven regional woodland contraction around 4400 cal BP (calendar years before present), when surviving woods became compositionally differentiated into upland pine and low-lying deciduous communities. A favourable microclimate can thus buffer woodlands against environmental shifts and increase continuity of canopy cover, but it does not generate stable communities. Compositional reorganisation is an essential stress response mechanism and should be accommodated by conservation managers. The replacement of deciduous taxa by Pinus sylvestris after 1060 cal BP represents the decoupling of pine distribution from climate drivers by management intervention. As a result, current microrefugial woodland composition reflects late Holocene human intervention. Alternative models of community composition and behaviour from palaeoecology provide a stronger foundation for managing microsite communities than relict woods in contrasting environmental settings.
dc.relation.ispartofBiological Conservationen
dc.rights© 2017 Elsevier Ltd. All rights reserved. This work has been made available online in accordance with the publisher’s policies. This is the author created, accepted version manuscript following peer review and may differ slightly from the final published version. The final published version of this work is available at
dc.subjectClimate changeen
dc.subjectGE Environmental Sciencesen
dc.subjectQH301 Biologyen
dc.subjectAgricultural and Biological Sciences(all)en
dc.subjectSDG 13 - Climate Actionen
dc.titleMicroclimate variability and long-term persistence of fragmented woodlanden
dc.typeJournal articleen
dc.contributor.institutionUniversity of St Andrews. Geography & Sustainable Developmenten
dc.description.statusPeer revieweden

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