The complex hybrid zone between the Abisko and Sidensjo chromosome races of Sorex araneus in Sweden

被引:22
作者
Fredga, K [1 ]
Narain, Y [1 ]
机构
[1] Uppsala Univ, Dept Genet, SE-75007 Uppsala, Sweden
关键词
common shrew; G-banding; chromosome polymorphism; colonization history;
D O I
10.1111/j.1095-8312.2000.tb00211.x
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
Six chromosome races of the common shrew occur in Sweden, each with its characteristic arm combination of metacentric chromosomes. G-banded karyotypes were analysed from 201 common shrews in 14 localities of the northern hybrid zone in Sweden. Analyses from another 64 shrews from seven localities outside the hybrid zone were included for comparison. The shrews were classified with respect to karyotype into any of five categories: (1) Abisko race, (2) Sidensjo race, (3) hybrids between the parental races, (4) pseudohybrids (a type of hybrid), and (5) AT with all race-specific chromosomes (h, i, n, o, p, r) present as telocentrics. Hybrids occurred at a frequency close to Hardy-Weinberg expectation in the centre of the hybrid zone. Chromosome polymorphism of Robertsonian type was common and 43 different karyotypes were found among the specimens studied. The polymorphism involved six metacentric pairs in the Abisko and three in the Sidensjo race. The frequency of the Sidensjo race-specific metacentric hi decreased and the frequency of the Abisko race-specific hn increased from south-west to north-east along a transect across the hybrid zone. The number of race-specific telocentrics reached a peak 13km north-east of the hi-hn dine centre. The estimated standardized dine width for chromosomes hi and hn was 16.0 km. The extension of the Sidensjo race is comparatively narrow (c. 50 km in the region of the investigation), and it is regarded to be a 'hybrid race' between the Uppsala race, which colonized Sweden from the south-west, and the Abisko race which arrived from the north-east after the most recent glaciation. The origin of the Sidensjo race is thus less than 10 000 years old, because earlier this area was covered by glacial ice. (C) 2000 The Linnean Society of London.
引用
收藏
页码:285 / 307
页数:23
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