2011
DOI: 10.1111/j.1095-8312.2011.01710.x
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Cryptic diversity within the endemic prehensile-tailed geckoUrocotyledon inexpectataacross the Seychelles Islands: patterns of phylogeographical structure and isolation at the multilocus level

Abstract: The deciphering of the process of genetic differentiation of species with insular distributions is relevant for biogeographical and conservation reasons. Despite their importance as old gondwanic islands and part of the western Indian Ocean biodiversity hotspot, little is known about the genetic structure of taxa from the Seychelles Islands. We have examined the patterns of structure and isolation within Urocotyledon inexpectata (Reptilia: Geckkonidae), an endemic species from this archipelago. Genetic diversi… Show more

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Cited by 24 publications
(37 citation statements)
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“…The oscillating sea level changes during the Pliocene and Pleistocene epochs in the Seychelles were characterised by cyclic periods of contact and isolation between different groups of islands (Rocha et al 2011). When freshwater crabs first reached the Seychelles between 2.5 and 5.3 MY ago sea levels oscillated between 30 m below and 20 m above their present levels, but Silhouette was separated from Mahé throughout this time by a deep ocean channel ( Fig.…”
Section: Dispersal Within Seychelles: Vicariance More Likely Than Ovementioning
confidence: 99%
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“…The oscillating sea level changes during the Pliocene and Pleistocene epochs in the Seychelles were characterised by cyclic periods of contact and isolation between different groups of islands (Rocha et al 2011). When freshwater crabs first reached the Seychelles between 2.5 and 5.3 MY ago sea levels oscillated between 30 m below and 20 m above their present levels, but Silhouette was separated from Mahé throughout this time by a deep ocean channel ( Fig.…”
Section: Dispersal Within Seychelles: Vicariance More Likely Than Ovementioning
confidence: 99%
“…Silhouette is separated from Mahé by a deep ocean and these two islands would not have formed a single landmass even during the Pleiocene (2.5 to 5.3 MY ago) when sea levels oscillated between 30 m below and 20 m above their present levels. However, Silhouette would have been connected to the rest of the Seychelles Bank during the Pleistocene (2.5 MY ago to 11 700 years ago) when sea levels oscillated between 80 m and 30 m below their present levels (Rocha et al 2011).…”
Section: Distributionmentioning
confidence: 99%
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