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Comparative phylogeography of coastal limpets across a marine disjunction in New Zealand
Author(s) -
GOLDSTIEN SHARYN J.,
SCHIEL DAVID R.,
GEMMELL NEIL J.
Publication year - 2006
Publication title -
molecular ecology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.619
H-Index - 225
eISSN - 1365-294X
pISSN - 0962-1083
DOI - 10.1111/j.1365-294x.2006.02977.x
Subject(s) - phylogeography , ecology , intraspecific competition , biology , allopatric speciation , range (aeronautics) , disjunct , biogeography , phylogenetic tree , population , biochemistry , materials science , demography , sociology , gene , composite material
Cook Strait, which separates the North and South Island of New Zealand, has been a transient, but re‐occurring feature of the New Zealand land mass throughout the Pleistocene, maintaining its current width and depth for the past 5000 years. Historic land fragmentation coupled with the complex hydrography of the Greater Cook Strait region has created both biogeographic and phylogeographic disjunctions between the North and South Island in several marine species. Here we use mitochondrial cytochrome b DNA sequences of three endemic intertidal limpets, Cellana ornata , Cellana radians and Cellana flava to assess intraspecific phylogeographic patterns across Cook Strait and to look for interspecific concordance of ecological and evolutionary processes among closely related taxa. We sequenced 328–359 bp in 85–321 individuals from 8–31 populations spanning the biogeographic range of the three species. Intraspecific phylogeographic analyses show moderate to strong genetic discontinuity among North and South Island populations due to allopatric fragmentation. This pattern was broadly concordant across the three species and the observed divergence among this group of intertidal limpets (0.3–2.0%) is similar to that of previously studied subtidal organisms. For each species, divergence time calculations suggest contemporary North and South Island lineages diverged from their respective most recent common ancestor approximately 200 000 to 300 000 years before present ( bp ), significantly earlier than previous estimates in other coastal marine taxa that arose from a miscalculation of divergence time.