M
Min Xu
Researcher at Chinese Academy of Sciences
Publications - 139
Citations - 2459
Min Xu is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Medicine & Chemistry. The author has an hindex of 25, co-authored 122 publications receiving 1832 citations. Previous affiliations of Min Xu include Nanjing Normal University & Griffith University.
Papers
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Highly Enantioselective Construction of a Quaternary Carbon Center of Dihydroquinazoline by Asymmetric Mannich Reaction and Chiral Recognition
TL;DR: In this paper, a chiral trifluoromethyl quaternary carbon center of dihydroquinazoline was constructed by an asymmetric Mannich reaction and chiral recognition.
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Puerins A and B, two new 8-C substituted flavan-3-ols from Pu-er tea.
TL;DR: Chemical investigation led to the identification of two new 8-C substituted flavan-3-ols, puerins A and B, and two known cinchonain-type phenols, epicatechin-[7,8-bc]-4alpha-(4-hydroxyphenyl)-dihydro-2(3H)-pyranone and cinchesonain Ib.
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Long-Term Effect of Different Fertilization and Cropping Systems on the Soil Antibiotic Resistome.
Fang Wang,Min Xu,Robert D. Stedtfeld,Hongjie Sheng,Jianbo Fan,Ming Liu,Benli Chai,Teotonio Soares de Carvalho,Hui Li,Zhongpei Li,Syed A. Hashsham,James M. Tiedje +11 more
TL;DR: How long-term common soil management practices affect the abundance and type of ARGs and MGEs in two very different soil environments, one aerobic and the other primarily anaerobic is shown.
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The processing of Panax notoginseng and the transformation of its saponin components
TL;DR: In this paper, HPLC analyses on saponin composition of processed notoginseng were conducted, which revealed that, during the steaming process, the five main ginsenosides (ginsenosides Rg(1), Rb-1, Rd, and Re, and notogsenoside R-1) decreased gradually and some other new saponins were formed.
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Detection of hydrological variations and their impacts on vegetation from multiple satellite observations in the Three-River Source Region of the Tibetan Plateau
TL;DR: It was concluded that the hydrological cycle had obviously changed and that more soil water was transferred into the GW since the aquiclude changed due to climate warming, which resulted in increased water storage.