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QUATERNARY DIVERGENCE AND HOLOCENE SECONDARY CONTACT VIA THE NORTHWEST PASSAGE IN THE CIRCUMPOLAR LATHYRUS JAPONICUS (LEGUMINOSAE)

机译:通过圆环豆科日本豆科(豆科)的西北通道进行四级分流和全新世二次接触

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摘要

We used the geographic distribution of genetic diversity in the beach pea, Lathyrus japonicus (Leguminosae) to reconstruct the location of a Pleistocene refugium and Holocene range expansion. DNA sequence data for the chloroplast ndhF-trnH spacer froma global sample of 22 populations in Asia, North America, and Europe were used to assess broad-scale, circumpolar patterns. The cpDNA data revealed five haplotypes including two largely allopatric, widespread haplotypes (one Pacific, the other Atlanticand inland in the Great Lakes). Three geographically restricted haplotypes were also recovered: one each in New Jersey, Lake Champlain, and the Pacific Northwest. The distribution of isozyme variation at 14 loci for 38 populations of beach peas from theAtlantic and Pacific coasts of North America, Lake Champlain, and the Great Lakes was used to reconstruct a North American history. One subset of allozymes was found on the Atlantic Coast and in the Great Lakes; a second subset was widespread from northwestern North America to Newfoundland. There was a nested pattern to the localization of allozymes along the Atlantic Coast; Cape Cod had the greatest number of allozymes. Pacific and Atlantic isozymes and cpDNA haplotypes occurred together along the coast of Newfoundland and adjacent Labrador. The pattern of genetic variation as assessed from isozymes and cpDNA allow the inferences that: 1) an early divergence yielded Atlantic and Pacific lineages and 2) the Atlantic lineage occupied a Wisconsinan refugium on the now-submerged coast of northeastern North America. Our evidence is consistent with there being Holocene secondary contact between the Atlantic and Pacific lineages in the area where they now overlap. We also suggest that an early post-glacialvicariance event is implicated in the history of the Lake Champlain populations.
机译:我们使用了豌豆,山genetic豆(豆科植物)的遗传多样性的地理分布来重建更新世避难所和全新世范围的扩展位置。来自亚洲,北美和欧洲的22个种群的全球样本中的叶绿体ndhF-trnH间隔区的DNA序列数据用于评估大规模的绕极模式。 cpDNA数据揭示了五种单倍型,包括两种基本上是异相的,广泛的单倍型(一个太平洋,另一个大西洋和大湖内陆)。还回收了三种受地理限制的单倍型:新泽西州,尚普兰湖和西北太平洋各一种。来自北美大西洋和太平洋沿岸,尚普兰湖和五大湖的38个豌豆种群的14个基因座的同工酶变异分布被用于重建北美历史。在大西洋沿岸和五大湖中发现了一种同工酶的子集。第二个子集广泛分布于北美西北部至纽芬兰。大西洋沿岸的同工酶定位存在一个嵌套模式。科德角的同工酶数量最多。太平洋和大西洋同工酶和cpDNA单倍型在纽芬兰沿海和邻近的拉布拉多沿岸同时出现。根据同工酶和cpDNA评估的遗传变异模式可以得出以下推论:1)早期分化产生了大西洋和太平洋沿袭,2)大西洋沿袭占据了现在东北北美沿海的威斯康星州避难所。我们的证据与大西洋和太平洋沿袭现在重叠的区域之间存在全新世次生接触是一致的。我们还建议,早冰川后的变迁事件与尚普兰湖人口的历史有关。

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