新鲜和福尔马林标本的系统基因组学解决了旧大陆泥蛇的系统分类学问题,并扩展了生物地理推断

Justin M. Bernstein, Hugo De Souza, John Murphy, Harold Voris, Rafe Brown, Edward Myers, Sean Harrington, Kartik Shanker, Sara Ruane
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摘要

我们对亚洲和澳大拉西亚生物多样性的认识随着对不同类群的系统分类学及其生物地理学的研究而不断扩大。历史上,海平面的波动和现在分离的陆地的循环连接和分离被用来解释物种泵机制下生物多样性的积累。然而,最近的研究表明,大陆的地质变化和物种扩散事件可能是这些地区生物多样性的更好解释。我们利用研究较少和地理上广泛分布的泥蛇(蛇类:Homalopsidae),利用从新鲜组织中捕获约4,800个核位点的目标捕获方法和从博物馆标本的福尔马林组织中补充的线粒体数据,研究了这些过程。我们利用这些数据集重建了该类群的第一个确定的系统发育,确定了它们的生物地理起源,并测试了关于海平面变化和栖息地选择对其多样化作用的假设。辐散定年和祖先范围估计支持渐新世起源,并在2000万年前从东南亚大陆和巽他兰的后尖齿群中多样化,然后向东和向西扩散。GeoHiSSE模型表明,祖先的后尖牙谱系在水生环境中的生态位扩展并未影响其多样化率。我们的研究结果强调,更新世海平面的变化和栖息地的特殊性并不是导致Homalopsidae现存物种丰富度的主要原因,相反,东南亚大陆的地质变化可能是该类群多样性的主要驱动力。我们还强调使用新鲜和降解组织,以及核和线粒体DNA的重要性,以填补鲜为人知但高度多样化和概念上重要的群体的知识空白。在这里,Homalopsidae代表了一个非传统但有效的模型研究系统,用于理解陆地,海洋和淡水环境之间的过渡。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Phylogenomics of Fresh and Formalin Specimens Resolves the Systematics of Old World Mud Snakes (Serpentes: Homalopsidae) and Expands Biogeographic Inference
Our knowledge of the biodiversity of Asia and Australasia continues to expand with more focused studies on systematics of various groups and their biogeography. Historically, fluctuating sea levels and cyclic connection and separation of now-disjunct landmasses have been invoked to explain the accumulation of biodiversity via species pump mechanisms. However, recent research has shown that geological shifts of the mainland and species dispersal events may be better explanations of the biodiversity in these regions. We investigate these processes using the poorly studied and geographically widespread Mud Snakes (Serpentes: Homalopsidae) using a target capture approach of ~4,800 nuclear loci from fresh tissues and supplemental mitochondrial data from formalin tissues from museum specimens. We use these datasets to reconstruct the first resolved phylogeny of the group, identify their biogeographic origins, and test hypotheses regarding the roles of sea-level change and habitat selection on their diversification. Divergence dating and ancestral range estimation yielded support for an Oligocene origin and diversification from mainland Southeast Asia and Sundaland in the rear-fanged group ~20 million years ago, followed by eastward and westward dispersal. GeoHiSSE models indicate that niche expansion of ancestral, rear-fanged lineages into aquatic environments did not impact their diversification rates. Our results highlight that Pleistocene sea-level changes and habitat specificity did not primarily lead to the extant species richness of Homalopsidae and that, alternatively, geological shifts in mainland Southeast Asia may have been a major driver of diversity in this group. We also emphasize the importance of using fresh and degraded tissues, and both nuclear and mitochondrial DNA, for filling knowledge gaps in poorly known but highly diverse and conceptually important groups. Here, Homalopsidae represents a non-traditional but effective model study system for understanding transitions between terrestrial, marine, and freshwater environments.
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