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dc.contributor.authorNorder, Sietze J.
dc.contributor.authorProios, Konstantinos
dc.contributor.authorWhittaker, Robert J.
dc.contributor.authorAlonso, María R.
dc.contributor.authorBorges, Paulo A. V.
dc.contributor.authorBorregaard, Michael K.
dc.contributor.authorCowie, Robert H.
dc.contributor.authorFlorens, F. B. Vincent
dc.contributor.authorFrias Martins, António M. de
dc.contributor.authorIbáñez, Miguel
dc.contributor.authorKissling, W. Daniel
dc.contributor.authorNascimento Reyes, Lea de 
dc.contributor.authorOtto, Rüdiger
dc.contributor.authorParent, Christine E.
dc.contributor.authorRigal, François
dc.contributor.authorWarren, Ben H.
dc.contributor.authorFernández-Palacios, José María 
dc.contributor.authorLoon, E. Emiel van
dc.contributor.authorTriantis, Kostas A.
dc.contributor.authorRijsdijk, Kenneth F.
dc.date.accessioned2019-10-23T16:45:16Z
dc.date.available2019-10-23T16:45:16Z
dc.date.issued2018
dc.identifier.issn1466-822X
dc.identifier.urihttp://riull.ull.es/xmlui/handle/915/16817
dc.description.abstractAim: To quantify the influence of past archipelago configuration on present‐day insular biodiversity patterns, and to compare the role of long‐lasting archipelago configurations over the Pleistocene to configurations of short duration such as at the Last Glacial Maximum (LGM) and the present-day. Location: 53 volcanic oceanic islands from 12 archipelagos worldwide—Azores, Canary Islands, Cook Islands, Galápagos, Gulf of Guinea, Hawaii, Madeira, Mascarenes, Pitcairn, Revillagigedo, Samoan Islands and Tristan da Cunha. Time period: The last 800 kyr, representing the nine most recent glacial–interglacial cycles. Major taxa studied: Land snails and angiosperms. Methods: Species richness data for land snails and angiosperms were compiled from existing literature and species checklists. We reconstructed archipelago configurations at the following sea levels: the present‐day high interglacial sea level, the intermediate sea levels that are representative of the Pleistocene and the low sea levels of the LGM. We fitted two alternative linear mixed models for each archipelago configuration using the number of single‐island endemic, multiple‐island endemic and (nonendemic) native species as a response. Model performance was assessed based on the goodness‐of‐fit of the full model, the variance explained by archipelago configuration and model parsimony. Results: Single‐island endemic richness in both taxonomic groups was best explained by intermediate palaeo‐configuration (positively by area change, and negatively by palaeo‐connectedness), whereas non‐endemic native species richness was poorly explained by palaeo‐configuration. Single‐island endemic richness was better explained by intermediate archipelago configurations than by the archipelago configurations of the LGM or present‐dayes_ES
dc.language.isoenes_ES
dc.publisherWileyes_ES
dc.relation.ispartofseriesGlobal Ecology and Biogeography;
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.titleBeyond the Last Glacial Maximum: Island endemism is best explained by long‐lasting archipelago configurationses_ES
dc.typeinfo:eu-repo/semantics/article
dc.identifier.doi10.1111/geb.12835
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.subject.keywordArchipelago configurationes_ES
dc.subject.keywordBiotic interchangees_ES
dc.subject.keywordEndemismes_ES
dc.subject.keywordFlowering plantses_ES
dc.subject.keywordGlacial–interglacial cycleses_ES
dc.subject.keywordLand snailses_ES
dc.subject.keywordLate Quaternaryes_ES
dc.subject.keywordLast environmental changees_ES
dc.subject.keywordSea‐level oscillationses_ES
dc.subject.keywordVolcanic oceanic islandses_ES
dc.type.hasVersioninfo:eu-repo/semantics/acceptedVersiones_ES


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Attribution-NonCommercial-NoDerivatives 4.0 Internacional
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