Search

During the metamorphosis of anuran amphibians, the tail resorption process is a necessary and crucial change. One subject that has received relatively little or no attention is the expression patterns of proteins and metabolites in the different tail portions during metamorphosis, especially in highland amphibians. The mechanisms of tail resorption in three portions (the tip, middle and root) of the tail were investigated in N. pleskei G43 tadpole based on two omics (proteomic and metabolomic). Integrin αVβ3 was found to be high expressed in the distal portion of the tail, which could improve the sensitiveness to thyroid hormones in the distal portion of the tail. Muscle regression displayed a spatial pattern with stronger regression in distal and weaker one in proximal portion. Probably, this stronger regression was mainly performed by the proteases of proteasome from the active translation by ribosomes. The suicide model and murder model coexisted in the tail resorption. Meanwhile, fatty acids, amino acids, pyrimidine, and purine which derived from the breakdown of tissues can be used as building blocks or energy source for successful metamorphosis. Our data improved a better comprehension of the tail resorption mechanisms underlying the metamorphism of N. pleskei tadpole through identifying important participating proteins and metabolites. [ABSTRACT FROM AUTHOR]

Zokors in the genus Eospalax, which are endemic to northern and western China, are subterranean rodents that inhabit various niches, including grasslands, high-altitude meadows, forests, and farmlands. Six species in Eospalax were described a century ago but their taxonomy and phylogeny remain controversial. In this study, we performed high-depth whole-genome sequencing of 47 zokor samples, comprising all six previously described species. Genomic analyses revealed a reliable and robust phylogeny of Eospalax and supported the validity of the six named species. According to the inferred phylogenetic relationships, Eospalax first divergent into two clades in the early Pliocene (ca. 4.68 million years ago (Ma)), one inhabiting the highaltitude Qinghai-Xizang (Tibet) Plateau (QTP) and adjacent regions, and the another inhabiting the lowaltitude Loess Plateau and Qinling-Daba Mountains. The most recent divergences occurred between E. baileyi and E. smithii and between E. rufescens and E. rothschildi in the late Pliocene (ca. 2.09 and 2.19 Ma, respectively). We also collected specimens of zokors in the southern Hengduan Mountains (Muli County, Sichuan Province), far from the known distributions of all other zokors. Morphological and molecular analyses strongly suggested that the specimens represent a new species, formally described here as Eospalax muliensis sp. nov. The new species belongs to the high-altitude clade and diverged from closely related species (ca. 4.22 Ma) shortly after the first divergence in Eospalax. Interestingly, Eospalax muliensis sp. nov. possesses more supposedly plesiomorphic characters, suggesting a possible origin of the genus in the Hengduan Mountains. [ABSTRACT FROM AUTHOR]

Firstly, the characteristics and roles of Tibetan traditional ecological culture were introduced, and then the predicament of Tibetan traditional ecological culture when facing modern ecological problems was analyzed, finally some suggestions giving full play to the active roles of Tibetan traditional ecological culture were put forward, such as paying more attention to the beneficial factors of Tibetan traditional ecological culture, capturing the bonding point of Tibetan traditional ecological culture and modern science, and meeting legitimate development demand and rationally developing and utilizing natural resources. [ABSTRACT FROM AUTHOR]

The article presents a study which used magnetostratigraphic and radiochronologic dating to amend the chronology of elevation estimates from the Lunpola Basin in central Tibet. Also cited is the importance of knowing the topographic evolution of the Tibetan Plateau by studying the basin to understand its construction and effects on climate, biodiversity and environment during the Cenozoic period.