2019
DOI: 10.1016/j.scib.2019.03.029
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Into Africa via docked India: a fossil climbing perch from the Oligocene of Tibet helps solve the anabantid biogeographical puzzle

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Cited by 19 publications
(23 citation statements)
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References 49 publications
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“…The collision of the Arabian and Eurasian plates, leading to the closure of the Tethys Ocean in the Late Eocene (~35 Ma: Allen & Armstrong, 2008), intensified the exchange of freshwater organisms between Asia and Africa (Lavoué, 2020; McLoughlin, 2001; Sil, Aravind, & Karanth, 2020; Wu et al, 2019). This provided the first opportunities for Cyprinidae to disperse into Africa.…”
Section: Discussionmentioning
confidence: 99%
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“…The collision of the Arabian and Eurasian plates, leading to the closure of the Tethys Ocean in the Late Eocene (~35 Ma: Allen & Armstrong, 2008), intensified the exchange of freshwater organisms between Asia and Africa (Lavoué, 2020; McLoughlin, 2001; Sil, Aravind, & Karanth, 2020; Wu et al, 2019). This provided the first opportunities for Cyprinidae to disperse into Africa.…”
Section: Discussionmentioning
confidence: 99%
“…A handful of lineages such as Rasboroides , Malpulutta and Belontia , while confined to the more humid parts of the island, are absent from India. All three show close relationships, instead, to South‐East Asian lineages (Liao, Kullander, & Fang, 2011; Rüber, Britz, & Zardoya, 2006; Tang et al, 2010; Wu, He, Fang, & Deng, 2019). It appears that their ancestors dispersed to the island before the South Indian plains aridified at the end of the Miocene (Ashton, 2014; Morley, 2018).…”
Section: Introductionmentioning
confidence: 99%
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“…Initial estimates constrained the lake surface elevation to have been ~1 km at ~25 Ma ( Wu et al., 2017 ), but this implicitly assumed a modern thermal lapse rate, which is inappropriate for paleoaltimetry ( Meyer, 2007 ; Spicer, 2018 ), and the age is only loosely constrained but likely to be at least late Oligocene if not a little older. Even assuming a late Oligocene age for Eoanabas, this discovery pushed back the origin of the anabantids by at least 20 million years ( Wu et al., 2017 ) and suggests an early Eocene Southeast Asian origin of the group ( Wu et al., 2018 ).…”
Section: The Topographic Evolution Of the Tibetan Regionmentioning
confidence: 99%
“…. 这些研究成果为认识高原生态系统在新生 13,14,24~28] , 能够从生物和环境两个方面刻画更多细 [29] , 这 些盆地虽然普遍面积不大, 但其沉积序列保存了周边 地区构造运动的关键信息, 是研究新生代高原隆升历 史的重要对象, 因而在最近十多年来受到了地学各领 域研究者的高度关注 [5,27,28,30~38] , 其中高原古环境的直 接证据--来自伦坡拉和尼玛盆地(图1)的古生物学系 列 新 发 现 更 是 引 起 了 众 多 地 学 同 行 的 热 切 关 注 [10,13,14,17,18,20,21,26,39] . [10,13,17,20,21,23] .…”
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