There are many barriers to species' migrations

<p>Temperature-change trajectories are being used to identify the geographic barriers and thermal ‘cul-de-sacs’ that will limit the ability of many species to track climate change by migrating. We argue that there are many other potential barriers to species’ migrations. These include stable e...

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Main Authors: Kenneth J Feeley, Evan M. Rehm, James Stroud
Format: Article
Language:English
Published: International Biogeography Society 2014-06-01
Series:Frontiers of Biogeography
Subjects:
Online Access:http://escholarship.org/uc/item/6x9651xq
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spelling doaj-bd99723ee48941db9350339b15e4d3902020-11-24T23:13:07ZengInternational Biogeography SocietyFrontiers of Biogeography1948-65962014-06-0162ark:13030/qt6x9651xqThere are many barriers to species' migrationsKenneth J Feeley0Evan M. Rehm1James Stroud2Florida International UniversityFlorida International UniversityFlorida International University<p>Temperature-change trajectories are being used to identify the geographic barriers and thermal ‘cul-de-sacs’ that will limit the ability of many species to track climate change by migrating. We argue that there are many other potential barriers to species’ migrations. These include stable ecotones, discordant shifts in climatic variables, human land use, and species’ limited dispersal abilities. To illustrate our argument, for each 0.5° latitude/longitude grid cell of the Earth’s land surface, we mapped and tallied the number of cells for which future (2060–2080) climate represents an analog of the focal cell’s current climate. We compared results when only considering temperature with those for which both temperature and total annual precipitation were considered in concert. We also compared results when accounting for only geographic barriers (no cross-continental migration) with those involving both geographic and potential ecological barriers (no cross-biome migration). As expected, the number of future climate analogs available to each pixel decreased markedly with each added layer of complexity (e.g. the proportion of the Earth’s land surface without any available future climate analogs increased from 3% to more than 36% with the inclusion of precipitation and ecological boundaries). While including additional variables can increase model complexity and uncertainty, we must strive to incorporate the factors that we know will limit species’ ranges and migrations if we hope to predict the effects of climate change at a high-enough degree of accuracy to guide management decisions.</p>http://escholarship.org/uc/item/6x9651xqSpecies migrations, biomes, climate change, global warming, conservation biogeography, climate analogs, dispersal, extinction,
collection DOAJ
language English
format Article
sources DOAJ
author Kenneth J Feeley
Evan M. Rehm
James Stroud
spellingShingle Kenneth J Feeley
Evan M. Rehm
James Stroud
There are many barriers to species' migrations
Frontiers of Biogeography
Species migrations, biomes, climate change, global warming, conservation biogeography, climate analogs, dispersal, extinction,
author_facet Kenneth J Feeley
Evan M. Rehm
James Stroud
author_sort Kenneth J Feeley
title There are many barriers to species' migrations
title_short There are many barriers to species' migrations
title_full There are many barriers to species' migrations
title_fullStr There are many barriers to species' migrations
title_full_unstemmed There are many barriers to species' migrations
title_sort there are many barriers to species' migrations
publisher International Biogeography Society
series Frontiers of Biogeography
issn 1948-6596
publishDate 2014-06-01
description <p>Temperature-change trajectories are being used to identify the geographic barriers and thermal ‘cul-de-sacs’ that will limit the ability of many species to track climate change by migrating. We argue that there are many other potential barriers to species’ migrations. These include stable ecotones, discordant shifts in climatic variables, human land use, and species’ limited dispersal abilities. To illustrate our argument, for each 0.5° latitude/longitude grid cell of the Earth’s land surface, we mapped and tallied the number of cells for which future (2060–2080) climate represents an analog of the focal cell’s current climate. We compared results when only considering temperature with those for which both temperature and total annual precipitation were considered in concert. We also compared results when accounting for only geographic barriers (no cross-continental migration) with those involving both geographic and potential ecological barriers (no cross-biome migration). As expected, the number of future climate analogs available to each pixel decreased markedly with each added layer of complexity (e.g. the proportion of the Earth’s land surface without any available future climate analogs increased from 3% to more than 36% with the inclusion of precipitation and ecological boundaries). While including additional variables can increase model complexity and uncertainty, we must strive to incorporate the factors that we know will limit species’ ranges and migrations if we hope to predict the effects of climate change at a high-enough degree of accuracy to guide management decisions.</p>
topic Species migrations, biomes, climate change, global warming, conservation biogeography, climate analogs, dispersal, extinction,
url http://escholarship.org/uc/item/6x9651xq
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