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      Predictors of elevational biodiversity gradients change from single taxa to the multi-taxa community level

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      a , 1 , 2 , 3 , 4 , 1 , 3 , 5 , 6 , 7 , 8 , 1 , 7 , 4 , 1 , 1 , 9 , 3 , 10 , 7 , 11 , 3 , 7 , 5 , 12 , 1 , 1 , 13 , 14 , 15 , 16 , 17 , 14 ,   6 , 18 , 19 , 1 , 6 , 20 , 7 , 4 , 21 , 12 , 3 , 4 , 21 , 5 , 6 , 1
      Nature Communications
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          Abstract

          The factors determining gradients of biodiversity are a fundamental yet unresolved topic in ecology. While diversity gradients have been analysed for numerous single taxa, progress towards general explanatory models has been hampered by limitations in the phylogenetic coverage of past studies. By parallel sampling of 25 major plant and animal taxa along a 3.7 km elevational gradient on Mt. Kilimanjaro, we quantify cross-taxon consensus in diversity gradients and evaluate predictors of diversity from single taxa to a multi-taxa community level. While single taxa show complex distribution patterns and respond to different environmental factors, scaling up diversity to the community level leads to an unambiguous support for temperature as the main predictor of species richness in both plants and animals. Our findings illuminate the influence of taxonomic coverage for models of diversity gradients and point to the importance of temperature for diversification and species coexistence in plant and animal communities.

          Abstract

          Explaining species richness patterns is a key question in ecology. Peters et al. sample diverse plant and animal groups across elevation on Mt. Kilimanjaro to show that, while disparate factors drive distributions of individual taxa, diversity overall decreases with elevation, mostly driven by effects of temperature.

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          Most cited references40

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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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            Global patterns and determinants of vascular plant diversity.

            Plants, with an estimated 300,000 species, provide crucial primary production and ecosystem structure. To date, our quantitative understanding of diversity gradients of megadiverse clades such as plants has been hampered by the paucity of distribution data. Here, we investigate the global-scale species-richness pattern of vascular plants and examine its environmental and potential historical determinants. Across 1,032 geographic regions worldwide, potential evapotranspiration, the number of wet days per year, and measurements of topographical and habitat heterogeneity emerge as core predictors of species richness. After accounting for environmental effects, the residual differences across the major floristic kingdoms are minor, with the exception of the uniquely diverse Cape Region, highlighting the important role of historical contingencies. Notably, the South African Cape region contains more than twice as many species as expected by the global environmental model, confirming its uniquely evolved flora. A combined multipredictor model explains approximately 70% of the global variation in species richness and fully accounts for the enigmatic latitudinal gradient in species richness. The models illustrate the geographic interplay of different environmental predictors of species richness. Our findings highlight that different hypotheses about the causes of diversity gradients are not mutually exclusive, but likely act synergistically with water-energy dynamics playing a dominant role. The presented geostatistical approach is likely to prove instrumental for identifying richness patterns of the many other taxa without single-species distribution data that still escape our understanding.
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              The role of spatial scale and the perception of large-scale species-richness patterns

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                Author and article information

                Journal
                Nat Commun
                Nat Commun
                Nature Communications
                Nature Publishing Group
                2041-1723
                22 December 2016
                2016
                : 7
                : 13736
                Affiliations
                [1 ]Department of Animal Ecology and Tropical Biology, Biocenter, University of Würzburg, Am Hubland , Würzburg 97074, Germany
                [2 ]Department of Plant Systematics, University of Bayreuth , Universitätsstraße 30, Bayreuth 95440, Germany
                [3 ]Environmental Informatics, Faculty of Geography, University of Marburg , Deutschhausstraße 12, Marburg 35032, Germany
                [4 ]Institute for Evolutionary Ecology and Conservation Genomics, University of Ulm , Albert-Einstein-Allee 11, Ulm 89069, Germany
                [5 ]Institute of Plant Sciences, University of Bern , Altenbergrain 21, Bern 3013, Switzerland
                [6 ]Senckenberg Biodiversity and Climate Research Centre (BiK-F) , Senckenberganlage 25, Frankfurt am Main 60325, Germany
                [7 ]Department of Ecology, Animal Ecology, University of Marburg , Karl-von-Frisch-Straße 8, Marburg 35032, Germany
                [8 ]Zoological Museum, Natural History Museum of Denmark, University of Copenhagen , Universitetsparken 15, Copenhagen DK-2100, Denmark
                [9 ]Tanzania Commission for Science and Technology, Department of Life Sciences , Ally Hassan Mwinyi Road, PO Box 4302, Dar es Salaam, Tanzania
                [10 ]Mount Kilimanjaro National Park , PO Box 96, Marangu, Moshi, Tanzania
                [11 ]National Museum of Tanzania , Shaaban Robert Street, Dar es Salaam, Tanzania
                [12 ]Landscape Ecology Group, Institute of Biology and Environmental Sciences, University Oldenburg , Oldenburg 26111, Germany
                [13 ]Molecular Ecology and Fisheries Genetics Lab, School of Biological Sciences, Environment Centre Wales, Bangor University , Bangor LL57 2UW, UK
                [14 ]Museum für Naturkunde, Leibniz Institute for Evolution and Biodiversity Science , Invalidenstraße 43, Berlin 10115, Germany
                [15 ]Agricultural Research Council—Plant Protection Research: Plant Health and Protection , Private Bag X134, Queenswood, Pretoria 0121, South Africa
                [16 ]School of Life Sciences, University of KwaZulu-Natal , Private Bag X01, Scottsville, Pietermaritzburg 3209, South Africa
                [17 ]Zoological Research Museum Alexander Koenig, Department Arthropoda , Adenauerallee 160, Bonn 53113, Germany
                [18 ]Falkenweg 6 , Wachtberg 53343, Germany
                [19 ]Tanzania Wildlife Research Institute , PO Box 661, Arusha, Tanzania
                [20 ]Institute for Ecology, Evolution and Diversity, Goethe University Frankfurt, Biologicum , Max-von-Laue-Straße 13, Frankfurt am Main 60439, Germany
                [21 ]Smithsonian Tropical Research Institute , PO Box 0843-03092, Balboa Ancòn, Republica de Panamà
                Author notes
                [*]

                Deceased 26 September 2011

                Author information
                http://orcid.org/0000-0001-9426-045X
                Article
                ncomms13736
                10.1038/ncomms13736
                5192166
                28004657
                1dc84e06-c8f8-47f8-9b61-45d818927673
                Copyright © 2016, The Author(s)

                This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article's Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

                History
                : 12 January 2016
                : 28 October 2016
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