4.2 Article

Evidence of dispersal between the Yenisei and the Lena river basins during the late Pleistocene within the whitefish (Coregonus lavaretus pidschian) complex

Journal

CANADIAN JOURNAL OF ZOOLOGY
Volume 99, Issue 12, Pages 1028-1039

Publisher

CANADIAN SCIENCE PUBLISHING
DOI: 10.1139/cjz-2020-0255

Keywords

pidschian-like whitefish; Coregonus lavaretus complex; Coregonus lavaretus pidschian n. glacialis; Siberian whitefish

Categories

Funding

  1. Russian Science Foundation [19-74-10054]
  2. Russian Foundation for Basic Research [20-40-00610]
  3. Russian Science Foundation [19-74-10054] Funding Source: Russian Science Foundation

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This study compared the distribution of whitefish haplotypes in the Yenisei and Lena river basins in Siberia, finding two distinct clusters but also shared haplotypes suggesting migration and hybridization events. These events likely occurred when the rivers were connected after the last glaciation.
The Coregonus lavaretus (Linnaeus, 1758) complex is a morphologically and genetically diverse group of whitefish. Its taxonomic structure has been controversial for almost a century. At least 25 forms of C. lavaretus have been described in Siberia, but there is still no consensus on their intraspecific structure and taxonomy. Coregonus lavaretus pidschian (Gmelin, 1789) was described as a subspecies of C. lavaretus. Recently, it was assumed that this subspecies is also a complex. The purpose of this study was to compare the distributions of pidschian-like whitefish haplotypes in two basins of large Siberian rivers, Yenisei and Lena, and to assess the gene flow between basins of these rivers, which were connected after the last glaciation. The sequence of the following mitochondrial DNA genes, 16S rRNA (partial), tRNA-Leu (full), NADH dehydrogenase subunit 1 (full), tRNA-Ile (full), and tRNA-Gln (partial), were used for the inference of intraspecific genetic structure of C. I. pidschian. Whitefish haplotypes were clustered into two groups according to their distribution between two large Siberian river basins; however, there were shared haplotypes indicating events of migration and hybridization, which could occur when Bolshoi Yenisei and Lena river systems were connected after the last glaciation (the Late Pleistocene).

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