Please use this identifier to cite or link to this item: https://doi.org/10.1086/599292
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dc.titleTransition from Connected to Fragmented Vegetation across an Environmental Gradient: Scaling Laws in Ecotone Geometry
dc.contributor.authorGastner, Michael T
dc.contributor.authorOborny, Beata
dc.contributor.authorZimmermann, DK
dc.contributor.authorPruessner, Gunnar
dc.date.accessioned2020-05-28T00:44:37Z
dc.date.available2020-05-28T00:44:37Z
dc.date.issued2009-07-01
dc.identifier.citationGastner, Michael T, Oborny, Beata, Zimmermann, DK, Pruessner, Gunnar (2009-07-01). Transition from Connected to Fragmented Vegetation across an Environmental Gradient: Scaling Laws in Ecotone Geometry. AMERICAN NATURALIST 174 (1) : E23-E39. ScholarBank@NUS Repository. https://doi.org/10.1086/599292
dc.identifier.issn00030147
dc.identifier.issn15375323
dc.identifier.urihttps://scholarbank.nus.edu.sg/handle/10635/168550
dc.description.abstractA change in the environmental conditions across space-for example, altitude or latitude-can cause significant changes in the density of a vegetation type and, consequently, in spatial connectivity. We use spatially explicit simulations to study the transition from connected to fragmented vegetation. A static (gradient percolation) model is compared to dynamic (gradient contact process) models. Connectivity is characterized from the perspective of various species that use this vegetation type for habitat and differ in dispersal or migration range, that is, "step length" across the landscape. The boundary of connected vegetation delineated by a particular step length is termed the " hull edge." We found that for every step length and for every gradient, the hull edge is a fractal with dimension 7/ 4. The result is the same for different spatial models, suggesting that there are universal laws in ecotone geometry. To demonstrate that the model is applicable to real data, a hull edge of fractal dimension 7/4 is shown on a satellite image of a piñon-juniper woodland on a hillside. We propose to use the hull edge to define the boundary of a vegetation type unambiguously. This offers a new tool for detecting a shift of the boundary due to a climate change. © 2009 by The University of Chicago.
dc.language.isoen
dc.publisherUNIVERSITY CHICAGO PRESS
dc.sourceElements
dc.subjectScience & Technology
dc.subjectLife Sciences & Biomedicine
dc.subjectEcology
dc.subjectEvolutionary Biology
dc.subjectEnvironmental Sciences & Ecology
dc.subjectPatch dynamics
dc.subjectLandscape connectivity
dc.subjectEnvironmental gradient
dc.subjectTree line
dc.subjectFractal geometry
dc.subjectABRUPT POPULATION-CHANGES
dc.subjectSPECIES BORDERS
dc.subjectHABITAT FRAGMENTATION
dc.subjectEXTINCTION THRESHOLDS
dc.subjectMETAPOPULATION DYNAMICS
dc.subjectLANDSCAPE CONNECTIVITY
dc.subjectFRACTAL LANDSCAPES
dc.subjectPHASE-TRANSITIONS
dc.subjectTREELINE ECOTONES
dc.subjectSPATIAL-PATTERNS
dc.typeArticle
dc.date.updated2020-05-27T08:05:53Z
dc.contributor.departmentYALE-NUS COLLEGE
dc.description.doi10.1086/599292
dc.description.sourcetitleAMERICAN NATURALIST
dc.description.volume174
dc.description.issue1
dc.description.pageE23-E39
dc.published.statePublished
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