| Literature DB >> 26728391 |
Junxing Yang1, Xiaoli Chen2, Jie Bai3,4,5, Dongming Fang6,7, Ying Qiu8,9,10, Wansheng Jiang11, Hui Yuan12, Chao Bian13,14, Jiang Lu15,16, Shiyang He17,18, Xiaofu Pan19, Yaolei Zhang20,21, Xiaoai Wang22, Xinxin You23,24, Yongsi Wang25, Ying Sun26,27, Danqing Mao28, Yong Liu29, Guangyi Fan30, He Zhang31, Xiaoyong Chen32, Xinhui Zhang33,34, Lanping Zheng35, Jintu Wang36, Le Cheng37,38, Jieming Chen39,40, Zhiqiang Ruan41,42, Jia Li43,44,45, Hui Yu46,47,48, Chao Peng49,50, Xingyu Ma51,52, Junmin Xu53,54, You He55, Zhengfeng Xu56, Pao Xu57, Jian Wang58,59, Huanming Yang60,61, Jun Wang62,63, Tony Whitten64, Xun Xu65, Qiong Shi66,67,68,69.
Abstract
BACKGROUND: An emerging cavefish model, the cyprinid genus Sinocyclocheilus, is endemic to the massive southwestern karst area adjacent to the Qinghai-Tibetan Plateau of China. In order to understand whether orogeny influenced the evolution of these species, and how genomes change under isolation, especially in subterranean habitats, we performed whole-genome sequencing and comparative analyses of three species in this genus, S. grahami, S. rhinocerous and S. anshuiensis. These species are surface-dwelling, semi-cave-dwelling and cave-restricted, respectively.Entities:
Mesh:
Year: 2016 PMID: 26728391 PMCID: PMC4698820 DOI: 10.1186/s12915-015-0223-4
Source DB: PubMed Journal: BMC Biol ISSN: 1741-7007 Impact factor: 7.431
Fig. 1Comparison of biological traits, habitat and basic genomic information for the three sequenced Sinocyclocheilus species. They are representative of surface-dwelling (Sg), semi-cave-dwelling (Sr) and cave-restricted (Sa) species, respectively. Please note the regressive characters in the adult Sa, such as loss of eyes, little scale covering and translucent skin
Fig. 2Phylogenomic analysis and demographic histories of the three Sinocyclocheilus species. a Phylogenomic relationships inferred from 3,181 orthologous genes of the three Sinocyclocheilus and six other teleost species (Homo sapiens was the outgroup), with the branch lengths scaled to estimated divergence times (numbers in blue show median and range values). The numbers besides the branch indicated expanded (green) and contracted (red) gene families since the split from a most recent common ancestor (MRCA). b Demographic histories were reconstructed using the pairwise sequentially Markovian coalescent (PSMC) model. The uplift process of the Qinghai-Tibet Plateau since 3.6 Ma was obtained from a published paper [11] and other significant environmental events, such as the atmospheric surface air temperature and Eurasian ice volume for the past 3 Ma, were taken from the National Centers for Environmental Information (NCEI; http://www.ncdc.noaa.gov/). The time range of three rounds of intense uplift (Qingzang, Kunhuang and Gonghe Movement) is highlighted in lilac. All three species have similar patterns of decrease under the Qingzang and Kunhuang Movement, but a subsequent divergent trend under the Gonghe Movement
Fig. 3Comparison of retinal structures among the three Sinocyclocheilus species. Phenotypes and H&E stained sections of eyes from top to bottom are those in a Sg, b Sr and c Sa, respectively. GCL, ganglion cell layer; INL, inner nuclear layer; IPL, inner plexiform layer; IS, inner segment; ONL, outer nuclear layer; OPL, outer plexiform layer; OS, outer segment; RCL, relict cell layer; RPE, retinal pigmented epithelium
Fig. 4I The distributions of superficial neuromasts on the head and II morphology of saccular otolith in the inner ear among the three Sinocyclocheilus species. The superficial neuromasts after DASPEI staining from the plates I-(a–c), I-(d–f) and I-(g–i) represent Sg, Sr and Sa, respectively. The photos from left to right show the lateral view, dorsal view and ventral view. These figures show that the numbers of neuromasts in the adult fishes decline in the following order: Sg > Sr > Sa. The morphology of the saccular otoliths was reconstructed based on synchrotron X-ray microtomography. The plates II-(a–c), II-(d–f) and II-(g–i) represent Sg, Sr and Sa, respectively. The photos from left to right show the location of saccular otoliths in the inner ear, the dorsal view and ventral view of its morphology. The ventral of saccular otolith in Sa is seriously aberrant, with a deep and expanded central pit, encircled by another lateral sulcus. The degree of corrosion increase is in the following order: Sg < Sr < Sa. Scale bar: 1 mm
Fig. 5Summary of the most important genetic changes in the cave-restricted Sa. The main results are outlined as follows: Lws2, Rh2-1, Rh2-2 and Rh2-4 are lost in Sa. Several crystallin genes, including Crygmx in the Sr and Cryball1, Crygm2d2, Crygm7 and Crygmx in Sa, have evolved into pseudogenes. Sa has two Hsp90α genes while Sg and Sr have only one; meanwhile, the expression of Hsp90α in Sa eyes is higher than that in Sg and Sr. Mpv17 has a deletion in the signal region in the Sa genome. Ush2a has two amino acid changes, i.e. R334S and V382A. Tyr has a nucleotide mutation (G420R) in one copy of the Sa genome. Two copies of Edar gene in Sa represent deletions, and Lamb3 and Col7a were lost. Two copies of Skp1 protein in Sa have deletions in the N-terminal end. Prox1 and Tast1r2-1 are under expansions in the three Sinocyclocheilus species genomes, and Tas1r1 and Tas2r200-2 are specifically duplicated in the Sa genome. Red, gene loss; green, gene expansion; purple, pseudogene; orange, mutation or deletion