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      Why are there so many species in the tropics?

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          Abstract

          Known for centuries, the geographical pattern of increasing biodiversity from the poles to the equator is one of the most pervasive features of life on Earth. A longstanding goal of biogeographers has been to understand the primary factors that generate and maintain high diversity in the tropics. Many 'historical' and 'ecological' hypotheses have been proposed and debated, but there is still little consensus. Recent discussions have centred around two main phenomena: phylogenetic niche conservatism and ecological productivity. These two factors play important roles, but accumulating theoretical and empirical studies suggest that the single most important factor is kinetics: the temperature dependence of ecological and evolutionary rates. The relatively high temperatures in the tropics generate and maintain high diversity because 'the Red Queen runs faster when she is hot'.

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          TOWARD A METABOLIC THEORY OF ECOLOGY

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            Processes and patterns of oceanic nutrient limitation

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              Evolution and the latitudinal diversity gradient: speciation, extinction and biogeography.

              A 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.
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                Author and article information

                Journal
                J. Biogeogr.
                Journal of biogeography
                Wiley
                0305-0270
                0305-0270
                Jan 2014
                : 41
                : 1
                Affiliations
                [1 ] Department of Biology, University of New Mexico Albuquerque, NM, 87131, USA.
                Article
                10.1111/jbi.12228
                4320694
                25684838
                3c97a269-1a61-4856-aec1-52d20a21c395
                History

                species diversity,metabolic theory,latitudinal diversity gradient,Janzen–Connell dynamics,Ecological interactions,tropics,Red Queen,evolutionary rates

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