Variation in plant diversity in mediterranean‐climate ecosystems: the role of climatic and topographical stability. (4th November 2014)

• Record Type: Journal Article
• Authors: Cowling, Richard M.; Potts, Alastair J.; Bradshaw, Peter L.; Colville, Jonathan; Arianoutsou, Margarita; Ferrier, Simon; Forest, Felix; Fyllas, Nikolaos M.; Hopper, Stephen D.; Ojeda, Fernando; Procheş, Şerban; Smith, Rhian J.; Rundel, Philip W.; Vassilakis, Emmanuel; Zutta, Brian R.; McGeoch, Melodie
• Is Part Of: Journal of biogeography. Volume 42:Number 3(2015:Mar.)
• Page Start: 552
• Page End: 564
• Publication Date: 2014-11-04
• Subjects: Biogeography -- Periodicals; 578.09
• DOI: 10.1111/jbi.12429
• Languages: English
• ISSNs: 0305-0270

Abstract

<abstract abstract-type="main" id="jbi12429-abs-0001"> <title>Abstract</title> <sec id="jbi12429-sec-0001" sec-type="section"> <title>Aim</title> <p>Although all five of the major mediterranean‐climate ecosystems (MCEs) of the world are recognized as loci of high plant species diversity and endemism, they show considerable variation in regional‐scale richness. Here, we assess the role of stable Pleistocene climate and Cenozoic topography in explaining variation in regional richness of the globe's MCEs. We hypothesize that older, more climatically stable MCEs would support more species, because they have had more time for species to accumulate than MCEs that were historically subject to greater topographic upheavals and fluctuating climates.</p> </sec> <sec id="jbi12429-sec-0002" sec-type="section"> <title>Location</title> <p>South‐western Africa (Cape), south‐western Australia, California, central Chile and the eastern (Greece) and western (Spain) Mediterranean Basin.</p> </sec> <sec id="jbi12429-sec-0003" sec-type="section"> <title>Methods</title> <p>We estimated plant diversity for each MCE as the intercepts of species–area curves that are homogeneous in slope across all regions. We used two down‐scaled global circulation models of the Last Glacial Maximum (LGM) to quantify climate stability by comparing the change in the location of MCEs between the LGM and present. We quantified the Cenozoic topographic stability of each MCE by comparing contemporary topographic profiles with those present in the late Oligocene and the early Pliocene.</p> </sec> <sec id="jbi12429-sec-0004" sec-type="section"> <title>Results</title> <p>The most diverse MCEs – Cape and Australia – had the highest Cenozoic environmental stability, and the least diverse – Chile and California – had the lowest stability.</p> </sec> <sec id="jbi12429-sec-0005" sec-type="section"> <title>Main conclusions</title> <p>Variation in plant diversity in MCEs is likely to be a consequence not of differences in diversification rates, but rather the persistence of numerous pre‐Pliocene clades in the more stable MCEs. The extraordinary plant diversity of the Cape is a consequence of the combined effects of both mature and recent radiations, the latter associated with increased habitat heterogeneity produced by mild tectonic uplift in the Neogene.</p> </sec> </abstract>