Mitochondrial DNA in Siberian conifers indicates multiple postglacial colonization centers

Author:

Semerikov Vladimir L.1,Semerikova Svetlana A.1,Putintseva Yuliya A.2,Oreshkova Natalia V.234,Krutovsky Konstantin V.2567

Affiliation:

1. Institute of Plant and Animal Ecology, Ural Branch of the Russian Academy of Sciences, Ekaterinburg 620144, Russia.

2. Laboratory of Forest Genomics, Genome Research and Education Center, Siberian Federal University, Krasnoyarsk 660036, Russia.

3. Laboratory of Forest Genetics and Selection, V.N. Sukachev Institute of Forest, Federal Research Center “Krasnoyarsk Science Center” of the Siberian Branch of the Russian Academy of Sciences, Krasnoyarsk 660036, Russia.

4. Laboratory of Genomic Research and Biotechnology, Federal Research Center “Krasnoyarsk Science Center of the Siberian Branch of the Russian Academy of Sciences”, Krasnoyarsk 660036, Russia.

5. Laboratory of Population Genetics, N.I. Vavilov Institute of General Genetics, Russian Academy of Sciences, Moscow 119333, Russia.

6. Department of Forest Genetics and Forest Tree Breeding, Georg-August University of Göttingen, Göttingen 37077, Germany.

7. Department of Ecosystem Science and Management, Texas A&M University, College Station, TX 77843-2138, USA.

Abstract

The geographic variation of the mitochondrial DNA in Siberian fir (Abies sibirica Ledeb.) was studied using the newly developed markers and compared with the phylogeographic pattern of another previously studied Siberian conifer, Siberian larch (Larix sibirica Ledeb.). Similar to Siberian larch, the distribution of mtDNA haplotypes in Siberian fir revealed clear differentiation among distinct geographic regions of southern Siberia and the Urals, likely indicating postglacial recolonization from several sources. The northern part of the range of both species was genetically homogeneous, which is probably due to its recent colonization from one of the glacial refugia. This conclusion is in agreement with published pollen and macrofossil data in Siberian fir and with the reconstruction of environmental niches indicating a dramatic reduction of the range and a likely survival of fir in certain southern areas during the Last Glacial Maximum (LGM), 21 thousand years ago. Although the modeling of the Siberian larch ecological niche reconstructed a shift of the range to the south at that period, the paleontological data indicated the presence of this species in most areas of the current range during LGM, which corresponds to the results of a previous historical demographic study suggesting that the population expansion preceding the LGM.

Publisher

Canadian Science Publishing

Subject

Ecology,Forestry,Global and Planetary Change

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