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巴塔哥尼亚獭 Lontra provocax 的系统地理学:对海洋生境的适应性分化还是南方冰川避难所的特征?

Phylogeography of the Patagonian otter Lontra provocax: adaptive divergence to marine habitat or signature of southern glacial refugia?

机构信息

Departamento de Ecología y Biodiversidad, Facultad de Ecología y Recursos Naturales, Universidad Andrés Bello, Republica 440, Santiago, Chile.

出版信息

BMC Evol Biol. 2011 Feb 28;11:53. doi: 10.1186/1471-2148-11-53.

DOI:10.1186/1471-2148-11-53
PMID:21356052
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3056781/
Abstract

BACKGROUND

A number of studies have described the extension of ice cover in western Patagonia during the Last Glacial Maximum, providing evidence of a complete cover of terrestrial habitat from 41°S to 56°S and two main refugia, one in south-eastern Tierra del Fuego and the other north of the Chiloé Island. However, recent evidence of high genetic diversity in Patagonian river species suggests the existence of aquatic refugia in this region. Here, we further test this hypothesis based on phylogeographic inferences from a semi-aquatic species that is a top predator of river and marine fauna, the huillín or Southern river otter (Lontra provocax).

RESULTS

We examined mtDNA sequences of the control region, ND5 and Cytochrome-b (2151 bp in total) in 75 samples of L. provocax from 21 locations in river and marine habitats. Phylogenetic analysis illustrates two main divergent clades for L. provocax in continental freshwater habitat. A highly diverse clade was represented by haplotypes from the marine habitat of the Southern Fjords and Channels (SFC) region (43°38' to 53°08'S), whereas only one of these haplotypes was paraphyletic and associated with northern river haplotypes.

CONCLUSIONS

Our data support the hypothesis of the persistence of L. provocax in western Patagonia, south of the ice sheet limit, during last glacial maximum (41°S latitude). This limit also corresponds to a strong environmental change, which might have spurred L. provocax differentiation between the two environments.

摘要

背景

多项研究描述了巴塔哥尼亚西部冰盖在末次冰盛期的延伸情况,提供了从南纬 41°到 56°的陆地栖息地完全被冰雪覆盖以及两个主要避难所的证据,一个在火地岛的东南部,另一个在智利岛的北部。然而,巴塔哥尼亚河流物种的高遗传多样性的最新证据表明,该地区存在水生避难所。在这里,我们根据半水生物种的系统地理学推断进一步检验了这一假设,该物种是河流和海洋动物群的顶级捕食者,即南河獭(Lontra provocax)。

结果

我们检查了来自河流和海洋栖息地 21 个地点的 75 个 L. provocax 样本的控制区、ND5 和细胞色素-b 的 mtDNA 序列(共 2151bp)。系统发育分析表明,L. provocax 在大陆淡水栖息地有两个主要的分歧支系。一个高度多样化的支系由南峡湾和海峡(SFC)地区(南纬 43°38'到 53°08')的海洋栖息地的单倍型代表,而这些单倍型中只有一个是并系的,与北部河流的单倍型有关。

结论

我们的数据支持了 L. provocax 在巴塔哥尼亚西部,冰盖限以南,末次冰盛期(南纬 41°)持续存在的假设。这一限制也对应着一个强烈的环境变化,这可能促使 L. provocax 在两种环境之间发生分化。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dfc3/3056781/e4d67941a201/1471-2148-11-53-5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dfc3/3056781/0e847927e74f/1471-2148-11-53-1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dfc3/3056781/7a28fdf49b07/1471-2148-11-53-2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dfc3/3056781/e56e5d55b79a/1471-2148-11-53-3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dfc3/3056781/89741ff5debe/1471-2148-11-53-4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dfc3/3056781/e4d67941a201/1471-2148-11-53-5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dfc3/3056781/0e847927e74f/1471-2148-11-53-1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dfc3/3056781/7a28fdf49b07/1471-2148-11-53-2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dfc3/3056781/e56e5d55b79a/1471-2148-11-53-3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dfc3/3056781/89741ff5debe/1471-2148-11-53-4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/dfc3/3056781/e4d67941a201/1471-2148-11-53-5.jpg

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