Evaluating signatures of glacial refugia for North Atlantic benthic marine taxa

Christine A. Maggs, Rita Castilho, David Foltz, Christy Henzler, Marc Taimour Jolly, John Kelly, Jeanine Olsen, Kathryn E. Perez, Wytze Stam, Risto Väinölä, Frederique Viard, John Wares

Tutkimustuotos: ArtikkelijulkaisuKatsausartikkelivertaisarvioitu

Abstrakti

"A goal of phylogeography is to relate patterns of genetic differentiation to potential historical geographic isolating events. Quaternary glaciations, particularly the one culminating in the Last Glacial Maximum similar to 21 ka (thousands of years ago), greatly affected the distributions and population sizes of temperate marine species as their ranges retreated southward to escape ice sheets. Traditional genetic models of glacial refugia and routes of recolonization include these predictions: low genetic diversity in formerly glaciated areas, with a small number of alleles/haplotypes dominating disproportionately large areas, and high diversity including ""private'' alleles in glacial refugia. In the Northern Hemisphere, low diversity in the north and high diversity in the south are expected. This simple model does not account for the possibility of populations surviving in relatively small northern periglacial refugia. If these periglacial populations experienced extreme bottlenecks, they could have the low genetic diversity expected in recolonized areas with no refugia, but should have more endemic diversity (private alleles) than recently recolonized areas. This review examines evidence of putative glacial refugia for eight benthic marine taxa in the temperate North Atlantic. All data sets were reanalyzed to allow direct comparisons between geographic patterns of genetic diversity and distribution of particular clades and haplotypes including private alleles. We contend that for marine organisms the genetic signatures of northern periglacial and southern refugia can be distinguished from one another. There is evidence for several periglacial refugia in northern latitudes, giving credence to recent climatic reconstructions with less extensive glaciation."
Alkuperäiskielienglanti
LehtiEcology
Vuosikerta89
Numero11
SivutS108-S122
Sivumäärä15
ISSN0012-9658
DOI - pysyväislinkit
TilaJulkaistu - 2008
OKM-julkaisutyyppiA2 Katsausartikkeli tieteellisessä aikakauslehdessä

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  • 118 Biotieteet

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