Phylogeography and demographic history of Atherina presbyter (Pisces: Atherinidae) in the North-eastern Atlantic based on mitochondrial DNA
Author(s) -
Sara M. Francisco,
Rita Castilho,
Marisa Porfirio Gomes Soares,
Leonardo Congiu,
Alberto Brito,
Natividade Vieira,
V. C. Almada
Publication year - 2009
Publication title -
marine biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.93
H-Index - 119
eISSN - 1432-1793
pISSN - 0025-3162
DOI - 10.1007/s00227-009-1182-5
Subject(s) - phylogeography , biology , range (aeronautics) , last glacial maximum , demographic history , smelt , population , glacial period , mtdna control region , mitochondrial dna , ecology , pleistocene , refugium (fishkeeping) , genetic structure , colonization , genetic diversity , zoology , fishery , demography , paleontology , phylogenetics , biochemistry , materials science , sociology , habitat , fish <actinopterygii> , genotype , composite material , haplotype , gene
A fragment of the mitochondrial control region was used to assess phylogeographic patterns and historical demography of the sand-smelt Atherina presbyter in the North-eastern Atlantic, covering its geographical range. A striking result is the highly marked diVerentiation between the Canary Islands population and western European
ones. A genetic structure among European populations of A. presbyter was revealed, with a pattern of isolation-by-distance or a gradient eVect at a scale of hundreds kilometres, an uncommon pattern likely related to the biological and life-history traits of the sand-smelt. The northern European populations present a much lower
genetic diversity when compared to southern populations, which is consistent with a recent colonization from southern populations. The results showed signs of Pleistocene signatures, with the population age estimates for the European populations being clearly older than the Last Glacial
Maximum (18,000 years bp). Nevertheless, paleotemperature reconstructions show that the sand-smelt could not have inhabited the western European shores during the last
glacial phase
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