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作为进化舞台的山脉:模式、新兴方法、范式转变及其对青藏高原-喜马拉雅地区植物系统地理学研究的启示

Mountains as Evolutionary Arenas: Patterns, Emerging Approaches, Paradigm Shifts, and Their Implications for Plant Phylogeographic Research in the Tibeto-Himalayan Region.

作者信息

Muellner-Riehl Alexandra N

机构信息

Department of Molecular Evolution and Plant Systematics & Herbarium (LZ), Leipzig University, Leipzig, Germany.

German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Leipzig, Germany.

出版信息

Front Plant Sci. 2019 Mar 18;10:195. doi: 10.3389/fpls.2019.00195. eCollection 2019.

DOI:10.3389/fpls.2019.00195
PMID:30936883
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6431670/
Abstract

Recently, the "mountain-geobiodiversity hypothesis" (MGH) was proposed as a key concept for explaining the high levels of biodiversity found in mountain systems of the Tibeto-Himalayan region (THR), which comprises the Qinghai-Tibetan Plateau, the Himalayas, and the biodiversity hotspot known as the "Mountains of Southwest China" (Hengduan Mountains region). In addition to the MGH, which covers the entire life span of a mountain system, a complementary concept, the so-called "flickering connectivity system" (FCS), was recently proposed for the period of the Quaternary. The FCS focuses on connectivity dynamics in alpine ecosystems caused by the drastic climatic changes during the past ca. 2.6 million years, emphasizing that range fragmentation and allopatric speciation are not the sole factors for accelerated evolution of species richness and endemism in mountains. I here provide a review of the current state of knowledge concerning geological uplift, Quaternary glaciation, and the main phylogeographic patterns ("contraction/recolonization," "platform refugia/local expansion," and "microrefugia") of seed plant species in the THR. In addition, I make specific suggestions as to which factors future avenues of phylogeographic research should take into account based on the fundamentals presented by the MGH and FCS, and associated complementary paradigm shifts.

摘要

最近,“山地地质生物多样性假说”(MGH)被提出,作为解释在青藏高原-喜马拉雅地区(THR)山地系统中发现的高生物多样性水平的关键概念,该地区包括青藏高原、喜马拉雅山脉以及被称为“中国西南山地”(横断山脉地区)的生物多样性热点地区。除了涵盖山地系统整个生命周期的MGH之外,最近还针对第四纪时期提出了一个补充概念,即所谓的“闪烁连接系统”(FCS)。FCS关注过去约260万年剧烈气候变化导致的高山生态系统中的连接动态,强调范围破碎化和异域物种形成并非山地物种丰富度和特有性加速进化的唯一因素。在此,我对有关地质隆升、第四纪冰川作用以及THR种子植物物种的主要系统发育地理模式(“收缩/重新定殖”、“平台避难所/局部扩张”和“微避难所”)的当前知识状况进行了综述。此外,我根据MGH和FCS提出的基本原理以及相关的补充范式转变,就未来系统发育地理研究的途径应考虑哪些因素提出了具体建议。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7d/6431670/dac809c67b1b/fpls-10-00195-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7d/6431670/d89c05b14c7e/fpls-10-00195-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7d/6431670/06ed71dbf582/fpls-10-00195-g002.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7d/6431670/e5de859f9797/fpls-10-00195-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7d/6431670/c47604f98b83/fpls-10-00195-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7d/6431670/dac809c67b1b/fpls-10-00195-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7d/6431670/d89c05b14c7e/fpls-10-00195-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7d/6431670/06ed71dbf582/fpls-10-00195-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7d/6431670/46e732cd1d0e/fpls-10-00195-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7d/6431670/e5de859f9797/fpls-10-00195-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7d/6431670/c47604f98b83/fpls-10-00195-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd7d/6431670/dac809c67b1b/fpls-10-00195-g006.jpg

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