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北美东部未受冰川影响地区的比较系统地理学

Comparative phylogeography of unglaciated eastern North America.

作者信息

Soltis Douglas E, Morris Ashley B, McLachlan Jason S, Manos Paul S, Soltis Pamela S

机构信息

Department of Botany, University of Florida, Gainesville, FL 32611, USA.

出版信息

Mol Ecol. 2006 Dec;15(14):4261-93. doi: 10.1111/j.1365-294X.2006.03061.x.

Abstract

Regional phylogeographical studies involving co-distributed animal and plant species have been conducted for several areas, most notably for Europe and the Pacific Northwest of North America. Until recently, phylogeographical studies in unglaciated eastern North America have been largely limited to animals. As more studies emerge for diverse lineages (including plants), it seems timely to assess the phylogeography across this region: (i) comparing and contrasting the patterns seen in plants and animals; (ii) assessing the extent of pseudocongruence; and (iii) discussing the potential applications of regional phylogeography to issues in ecology, such as response to climatic change. Unglaciated eastern North America is a large, geologically and topographically complex area with the species examined having diverse distributions. Nonetheless, some recurrent patterns emerge: (i) maritime - Atlantic vs. Gulf Coast; (ii) Apalachicola River discontinuity; (iii) Tombigbee River discontinuity; (iv) the Appalachian Mountain discontinuity; (v) the Mississippi River discontinuity; and (vi) the Apalachicola River and Mississippi River discontinuities. Although initially documented in animals, most of these patterns are also apparent in plants, providing support for phylogeographical generalizations. These patterns may generally be attributable to isolation and differentiation during Pleistocene glaciation, but in some cases may be older (Pliocene). Molecular studies sometimes agree with longstanding hypotheses of glacial refugia, but also suggest additional possible refugia, such as the southern Appalachian Mountains and areas close to the Laurentide Ice Sheet. Many species exhibit distinct patterns that reflect the unique, rather than the shared, aspects of species' phylogeographical histories. Furthermore, similar modern phylogeographical patterns can result from different underlying causal factors operating at different times (i.e. pseudocongruence). One underemphasized component of pseudocongruence may result from the efforts of researchers to categorize patterns visually - similar patterns may, in fact, not fully coincide, and inferring agreement may obscure the actual patterns and lead to erroneous conclusions. Our modelling analyses indicate no clear spatial patterning and support the hypothesis that phylogeographical structure in diverse temperate taxa is complex and was not shaped by just a few barriers.

摘要

涉及共同分布的动植物物种的区域系统地理学研究已在多个地区开展,最显著的是欧洲和北美太平洋西北部。直到最近,北美东部未受冰川影响地区的系统地理学研究在很大程度上还局限于动物。随着针对不同谱系(包括植物)的研究越来越多,评估该地区的系统地理学似乎恰逢其时:(i)比较和对比动植物中观察到的模式;(ii)评估假一致性的程度;(iii)讨论区域系统地理学在生态问题(如对气候变化的响应)中的潜在应用。北美东部未受冰川影响的地区面积广大,地质和地形复杂,所研究的物种分布多样。尽管如此,还是出现了一些反复出现的模式:(i)沿海地区——大西洋沿岸与墨西哥湾沿岸;(ii)阿巴拉契科拉河间断;(iii)汤比格比河间断;(iv)阿巴拉契亚山脉间断;(v)密西西比河间断;以及(vi)阿巴拉契科拉河和密西西比河间断。尽管这些模式最初是在动物中记录的,但大多数在植物中也很明显,这为系统地理学的概括提供了支持。这些模式通常可能归因于更新世冰川作用期间的隔离和分化,但在某些情况下可能更古老(上新世)。分子研究有时与长期以来关于冰川避难所的假设一致,但也表明还有其他可能的避难所,如阿巴拉契亚山脉南部和靠近劳伦泰德冰盖的地区。许多物种表现出独特的模式,反映了物种系统地理历史中独特而非共有的方面。此外,不同时期运作的不同潜在因果因素(即假一致性)可能导致类似的现代系统地理模式。假一致性中一个未得到充分强调的因素可能源于研究人员试图直观地对模式进行分类——实际上,视觉上相似的模式可能并不完全一致,推断一致性可能会掩盖实际模式并导致错误结论。我们的模型分析表明没有明显的空间模式,并支持这样的假设,即不同温带类群的系统地理结构很复杂,并非仅由少数障碍形成。

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