Population genetic variation in the New Zealand greenshell mussel: locus-dependent conflicting signals of weak structure and high gene flow balanced against pronounced structure and high self-recruitment

A pronounced north–south multitaxon genetic discontinuity occurs in central New Zealand (NZ). Polymorphic microsatellite markers have been used to test the location and structure of this discontinuity in the endemic greenshell mussel, Perna canaliculus . Nine neutral loci revealed limited evidence o...

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Veröffentlicht in:Marine biology 2013-04, Vol.160 (4), p.931-949
Hauptverfasser: Wei, Kaijian, Wood, Ann R., Gardner, Jonathan P. A.
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Sprache:eng
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Zusammenfassung:A pronounced north–south multitaxon genetic discontinuity occurs in central New Zealand (NZ). Polymorphic microsatellite markers have been used to test the location and structure of this discontinuity in the endemic greenshell mussel, Perna canaliculus . Nine neutral loci revealed limited evidence of genetic structure, but one outlier locus ( Pcan1 - 27 ) which may be under selection provided evidence of the discontinuity in central NZ. Whilst the limited multilocus evidence of structure is assumed to result from high levels of gene flow among populations of this continuously distributed species, assignment tests indicated high to very high mean levels of self-recruitment within the 14 populations and the north and south regions. The nine neutral loci were unable to provide further clarification as to the geographic location of the discontinuity, whereas the Pcan1 - 27 locus was particularly informative. These results highlight a tension between limited evidence of genetic structure and presumptive high gene flow among populations versus high levels of self-recruitment and pronounced structure depending on microsatellite loci and analyses in question. Evidence from all 10 loci indicates that the genetic discontinuity is maintained by high levels of self-recruitment, and evidence from Pcan1 - 27 suggests that selection may also be important in explaining the existence of the discontinuity.
ISSN:0025-3162
1432-1793
DOI:10.1007/s00227-012-2145-9