2016
DOI: 10.12681/mms.1562
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Concordant patterns of mtDNA and nuclear phylogeographic structure reveal Pleistocene vicariant event in the green crab Carcinus aestuarii across the Siculo-Tunisian Strait

Abstract: . Concordant patterns of mtDNA and nuclear phylogeographic structure reveal Pleistocene vicariant event in the green crab Carcinus aestuarii across the Siculo-Tunisian Strait.

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Cited by 10 publications
(25 citation statements)
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“…The best known oceanographic discontinuities in the Mediterranean are: (1) the Almería-Oran Front as the main genetic breakpoint between the Atlantic Ocean and the Mediterranean Sea [ 4 , 7 ], (2) the transition between the Western and the Eastern Mediterranean, due to unidirectional water flow at the Siculo-Tunisian Strait [ 5 ], and (3) the hydrographic isolation of the Aegean, Ionian and Adriatic seas [ 5 ]. In addition to these oceanographic barriers, the geological history of the Eastern Atlantic and Mediterranean Sea, including the breaking up of the Tethys Sea, the Messinian Salinity Crisis [ 8 ], and the Pleistocene glaciations [ 9 ], might have left marked footprints on the genetic structure of species and made the Mediterranean region a notably dynamic hotspot of diversity [ 10 12 ]. For example, intensified modifications to the coastline (sea level regressions) during repeated Pleistocene glaciations could have limited the biotic exchange across physical barriers, such as the Gibraltar Strait [ 13 ] and the Siculo-Tunisian Strait [ 14 ], and strongly influenced the formation of distinct phylogenetic lineages within Mediterranean marine species.…”
Section: Introductionmentioning
confidence: 99%
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“…The best known oceanographic discontinuities in the Mediterranean are: (1) the Almería-Oran Front as the main genetic breakpoint between the Atlantic Ocean and the Mediterranean Sea [ 4 , 7 ], (2) the transition between the Western and the Eastern Mediterranean, due to unidirectional water flow at the Siculo-Tunisian Strait [ 5 ], and (3) the hydrographic isolation of the Aegean, Ionian and Adriatic seas [ 5 ]. In addition to these oceanographic barriers, the geological history of the Eastern Atlantic and Mediterranean Sea, including the breaking up of the Tethys Sea, the Messinian Salinity Crisis [ 8 ], and the Pleistocene glaciations [ 9 ], might have left marked footprints on the genetic structure of species and made the Mediterranean region a notably dynamic hotspot of diversity [ 10 12 ]. For example, intensified modifications to the coastline (sea level regressions) during repeated Pleistocene glaciations could have limited the biotic exchange across physical barriers, such as the Gibraltar Strait [ 13 ] and the Siculo-Tunisian Strait [ 14 ], and strongly influenced the formation of distinct phylogenetic lineages within Mediterranean marine species.…”
Section: Introductionmentioning
confidence: 99%
“…In this context, the phylogeography of Mediterranean species underwent a common set of processes resulting from fragmentation within glacial refugia, range expansions via postglacial colonisation, and secondary contact zones among historically divergent lineages [ 4 , 12 , 15 18 ].…”
Section: Introductionmentioning
confidence: 99%
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