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Wiley InterScience | |||||||||||
![]() Ecology LettersVolume 10 Issue 4, Pages 315 - 331 Published Online: 20 Feb 2007 Journal compilation © 2010 Blackwell Publishing Ltd/CNRS Published on behalf of the Centre National de la Recherche Scientifique
Abstract | References | Full Text: HTML, PDF (Size: 614K) | Related Articles | Citation Tracking REVIEW AND SYNTHESIS Evolution and the latitudinal diversity gradient: speciation, extinction and biogeography Copyright 2007 Blackwell Publishing Ltd/CNRS KEYWORDS Biodiversity • biotic interactions • diversification • evolutionary speed • extinction • geographical isolation • latitudinal diversity gradient • speciation • tropics ABSTRACTA latitudinal gradient in biodiversity has existed since before the time of the dinosaurs, yet how and why this gradient arose remains unresolved. Here we review two major hypotheses for the origin of the latitudinal diversity gradient. The time and area hypothesis holds that tropical climates are older and historically larger, allowing more opportunity for diversification. This hypothesis is supported by observations that temperate taxa are often younger than, and nested within, tropical taxa, and that diversity is positively correlated with the age and area of geographical regions. The diversification rate hypothesis holds that tropical regions diversify faster due to higher rates of speciation (caused by increased opportunities for the evolution of reproductive isolation, or faster molecular evolution, or the increased importance of biotic interactions), or due to lower extinction rates. There is phylogenetic evidence for higher rates of diversification in tropical clades, and palaeontological data demonstrate higher rates of origination for tropical taxa, but mixed evidence for latitudinal differences in extinction rates. Studies of latitudinal variation in incipient speciation also suggest faster speciation in the tropics. Distinguishing the roles of history, speciation and extinction in the origin of the latitudinal gradient represents a major challenge to future research. Editor, Jonathan Chase Manuscript received 31 July 2006 First decision made 5 September 2006 Second decision made 30 December 2006 Manuscript accepted 13 January 2007 |
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