Xu Xin, Liu Fengxiang, Cheng Ren-Chung, Chen Jian, Xu Xiang, Zhang Zhisheng, Ono Hirotsugu, Pham Dinh Sac, Norma-Rashid Y, Arnedo Miquel A, Kuntner Matjaž, Li Daiqin
Centre for Behavioural Ecology and Evolution (CBEE), College of Life Sciences, Hubei University, Wuhan, People's Republic of China.
Evolutionary Zoology Laboratory, Biological Institute ZRC SAZU, Ljubljana, Slovenia.
Proc Biol Sci. 2015 Jun 7;282(1808):20142486. doi: 10.1098/rspb.2014.2486.
Living fossils are lineages that have retained plesiomorphic traits through long time periods. It is expected that such lineages have both originated and diversified long ago. Such expectations have recently been challenged in some textbook examples of living fossils, notably in extant cycads and coelacanths. Using a phylogenetic approach, we tested the patterns of the origin and diversification of liphistiid spiders, a clade of spiders considered to be living fossils due to their retention of arachnid plesiomorphies and their exclusive grouping in Mesothelae, an ancient clade sister to all modern spiders. Facilitated by original sampling throughout their Asian range, we here provide the phylogenetic framework necessary for reconstructing liphistiid biogeographic history. All phylogenetic analyses support the monophyly of Liphistiidae and of eight genera. As the fossil evidence supports a Carboniferous Euramerican origin of Mesothelae, our dating analyses postulate a long eastward over-land dispersal towards the Asian origin of Liphistiidae during the Palaeogene (39-58 Ma). Contrary to expectations, diversification within extant liphistiid genera is relatively recent, in the Neogene and Late Palaeogene (4-24 Ma). While no over-water dispersal events are needed to explain their evolutionary history, the history of liphistiid spiders has the potential to play prominently in vicariant biogeographic studies.
活化石是指在很长一段时间内保留了祖征性状的谱系。人们预计,这类谱系在很久以前就已经起源并分化。最近,一些活化石的教科书示例对这种预期提出了挑战,特别是现存的苏铁类植物和腔棘鱼。我们采用系统发育方法,测试了地蛛科蜘蛛的起源和分化模式。地蛛科蜘蛛由于保留了蛛形纲的祖征,并且在中纺亚目(所有现代蜘蛛的古老姊妹分支)中单独成组,被认为是活化石。在对其整个亚洲分布范围进行原始采样的帮助下,我们在此提供了重建地蛛科生物地理历史所需的系统发育框架。所有系统发育分析均支持地蛛科和八个属的单系性。由于化石证据支持中纺亚目起源于石炭纪的欧美地区,我们的年代测定分析推测,在古近纪(3900-5800万年前),地蛛科蜘蛛从欧美地区向东进行了长时间的陆地扩散,到达亚洲。与预期相反,现存地蛛科各属内的分化相对较新,发生在新近纪和晚古近纪(400-2400万年前)。虽然不需要跨水扩散事件来解释它们的进化历史,但地蛛科蜘蛛的历史有可能在替代生物地理学研究中发挥重要作用。