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LncRNAs unraveling their sponge role in glioblastoma and potential therapeutic applications
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作者 CAIJUAN LIU XINGHAO LI +3 位作者 YUXUAN WU JINHUI YANG MENGHAN WANG yunqi ma 《BIOCELL》 SCIE 2024年第3期387-401,共15页
Glioblastoma multiforme(GBM),the most common and aggressive primary brain tumor in adults,is the most malignant and still has no cure.However,the novel role of long non-coding RNAs(lncRNAs)in the pathogenesis of gliob... Glioblastoma multiforme(GBM),the most common and aggressive primary brain tumor in adults,is the most malignant and still has no cure.However,the novel role of long non-coding RNAs(lncRNAs)in the pathogenesis of glioblastoma is attracting extensive attention.LncRNAs are transcribed RNA molecules over 200 nucleotides long that do not encode proteins.Unlike small non-coding RNAs,such as microRNAs(miRNAs),lncRNAs have more complex secondary and tertiary structures that enable them to interact with DNA,RNA,and proteins and perform multiple regulatory functions.LncRNAs act as molecular sponges,absorbing and sequestering other biomolecules,particularly miRNAs,thereby preventing these molecules from performing their normal functions.LncRNAs influence glioblastoma through gene expression regulation,molecular sponge capacity,epigenetic modulation,and signaling pathway interactions.In glioblastoma,a large number of lncRNAs have been found to be abnormally expressed,affecting tumor growth,invasion and resistance to treatment.Due to its regulatory role and disease-specific expression patterns,lncRNA has become a potential biomarker for glioblastoma and a promising new therapeutic target.This paper discusses the spongy role of lncRNAs in glioblastoma and its potential therapeutic applications,which will lay a foundation for our understanding of glioblastoma biology and the development of new diagnostic and therapeutic strategies in the future. 展开更多
关键词 LncRNA MIRNA BIOMARKER Molecular sponges Tumor microenvironment
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盐湖卤水中硼同位素分馏因子的第一性原理计算
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作者 顾焕恩 马云麒 魏琦 《中国科学:化学》 CAS CSCD 北大核心 2024年第10期1856-1868,共13页
硼同位素已在物源示踪、古环境研究等方面得到广泛应用.对于盐湖硼同位素研究而言,获得盐湖卤水中不同硼物种(包括B(OH)_(3)、B(OH)_(4)^(–)和多聚硼酸盐阴离子B_(3)O_(3)(OH)_(4)^(–)、B_(3)O_(3)(OH)_(5)^(2–)、B_(4)O_(5)(OH)_(4)... 硼同位素已在物源示踪、古环境研究等方面得到广泛应用.对于盐湖硼同位素研究而言,获得盐湖卤水中不同硼物种(包括B(OH)_(3)、B(OH)_(4)^(–)和多聚硼酸盐阴离子B_(3)O_(3)(OH)_(4)^(–)、B_(3)O_(3)(OH)_(5)^(2–)、B_(4)O_(5)(OH)_(4)^(2–)、B_(5)O_(6)(OH)_(4)^(–))之间准确的硼同位素平衡分馏因子,是开展盐湖硼同位素地球化学研究的基础.本研究利用量子化学计算法精确计算了卤水中B(OH)_(3)和B(OH)_(4)^(–)与多聚硼酸盐阴离子之间的硼同位素平衡分馏因子,并就非谐效应和溶剂化效应对计算结果的贡献进行了校正.结果显示,B(OH)_(3)和B(OH)_(4)^(-)与多聚硼酸盐阴离子之间的平衡硼同位素分馏因子分别为:α_(3-4)=1.0286;α_(3-334)=1.0389;α_(3-335)=1.0717;α_(3-45)=1.0889;α_(3-56)=1.1180;α_(4-334)=0.9545;α_(4-335)=0.9849;α_(4-45)=0.9728;α_(4-56)=0.9711.这些分馏因子的确定,为研究盐湖卤水硼迁移过程的硼同位素分馏行为提供了基础数据和理论指导. 展开更多
关键词 盐湖 多聚硼酸盐阴离子 硼同位素 分馏因子 第一性原理计算
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Distribution and origin of brine-type Li-Rb mineralization in the Qaidam Basin,NW China 被引量:11
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作者 Jiansen LI Tingwei LI +1 位作者 yunqi ma Fukun CHEN 《Science China Earth Sciences》 SCIE EI CSCD 2022年第3期477-489,共13页
The Qaidam Basin on the Qinghai-Tibet Plateau is well endowed with a variety of critical metals,such as Li and Rb.However,little is known about the distribution,source,and enrichment mechanisms of these elements.In th... The Qaidam Basin on the Qinghai-Tibet Plateau is well endowed with a variety of critical metals,such as Li and Rb.However,little is known about the distribution,source,and enrichment mechanisms of these elements.In this paper,we present results of systematic geochemical and H-O-B isotopic analyses of brines in the Tertiary and Quaternary sediments of the Qaidam basin.The results reveal that the paleobrines from oil-bearing anticlines at Dafengshan,Nanyishan,Youquanzi,Jiandingshan,and Jianshishan are significantly enriched in Li and Rb,whose contents are 81.1-128.9 mg L^(-1)and 4.5-29.2 mg L^(-1),respectively,reaching levels of economic significance.High Rb contents(up to 12.5 mg L^(-1))and well-endowment of Li also characterize the Dongtai,Xitai,Yiliping,and Senie salt lakes in the Qaidam Basin.The Tertiary paleobrine average inδD andδ18O at-40.7‰and 2.84‰,respectively.The paleobrine with the highest Li and Rb hasδD andδ^(18)O values close to magmatic water.Theδ^(11)B values are lower than those of river water but close to those of geothermal fluids,suggesting that replenishment by deep magmatic hydrothermal fluid is most likely the key mechanism for the anomalous enrichment of these elements in the paleobrines,though evaporation and water-rock reactions have contributed to the critical metal mineralization.The anomalous enrichment of Li and Rb in modern salt lake brines is closely related to the input of volcanic geothermal water.The relatively high Li and Rb contents of intercrystalline brines in salt lakes of the western Qaidam Basin and the increase of Li and Rb contents with increasing depth were caused by upwelling of local paleobrines along the fault zones. 展开更多
关键词 Li and Rb resources Paleobrine Salt lake brine Hydrogen H-O-B isotopes Qaidam Basin
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