Cave Stedocys spitting spiders illuminate the history of the Himalayas and southeast Asia
Yufa Luo and Shuqiang Li
Y. Luo and S. Li (http://orcid.org/000.0002-3290-5416) (firstname.lastname@example.org), Key Laboratory of Zoological Systematics and Evolution, Inst. of Zoology, Chinese Academy of Sciences, Beijing, China.
YL also at: School of Life and Environment Sciences, Gannan Normal Univ., Ganzhou, China.
SL also at: Southeast Asia Biodiversity Research Inst., Chinese Academy of Sciences, Menglun, Mengla, Yunnan, China.
PubYear : 2017
Volume : 40
Publication Name :Ecography
Page number : 001-009
Abstract: Stedocys spitting spiders (Araneae: Scytodidae) inhabit subterranean environments and have poor dispersal abilities.Te Cenozoic Indian – Eurasian collision affected the regional biota of this genus, which occurs in parts of Indochina. Phylogeographical pattern of Stedocys based on multigene DNA sequence datasets reveals how tectonic history drove four biological splits. Te first split dates to the late Paleocene – Eocene and involves the Truong Son Mountain Range and Mekong River. Te other splits associate with the Eocene – Oligocene transition, including the Tonkin (Beibu) Gulf, the Ma River, and the Red River. Tese events indicate four early uplifts of the Himalayas and Tibetan Plateau. Our results cannot reject the hypothesis that uplifting of the Himalayas and Tibetan Plateau region due to crustal thickening and the lateral extrusion of Indochina occurred synchronously during the Paleocene – Oligocene transition in reaction to the Indian – Eurasian collision. Species of Stedocys cluster into groups I and II. Teir evolution involves one dispersal and four vicariance events, which formed the following five Indochinese clades: Hainan clade (I-1); western Yunnan and central Laos clade (I-2); central Vietnam clade (I-3); northern Vietnam and southwestern China clade (I-4); and Tailand clade (II-1). Te lateral extrusion of Indochina is the driver of these events. Te drifting of Hainan Island to its present location owes to its southeastern movement from continental Vietnam and Guangxi, China around the Eocene – Oligocene boundary. Tis biogeographical pattern highlights the significant role geography plays in shaping evolutionary history in southeastern Asia. It also illuminates the how the timing of geological events drives the distributions of species.