[EN] NOVEL MACROCYCLES AS FACTOR XIA INHIBITORS<br/>[FR] NOUVEAUX MACROCYCLES EN TANT QU'INHIBITEURS DU FACTEUR XIA
申请人:BRISTOL MYERS SQUIBB CO
公开号:WO2013022818A1
公开(公告)日:2013-02-14
The present invention provides compounds of Formula (Ia): or a stereoisomer, a tautomer, or a pharmaceutically acceptable salt thereof, wherein all the variables are as defined herein. These compounds are selective factor XIa inhibitors or dual inhibitors of FXIa and plasma kallikrein. This invention also relates to pharmaceutical compositions comprising these compounds and methods of treating thromboembolic and/or inflammatory disorders using the same.
Exploration of the Molecular Origin of the Azinomycin Epoxide: Timing of the Biosynthesis Revealed
作者:Vasudha Sharma、Gilbert T. Kelly、Coran M. H. Watanabe
DOI:10.1021/ol8018852
日期:2008.11.6
Streptomyces sahachiroi whole cell feeding experiments, utilizing putative precursors labeled with stable isotopes, established that the epoxide unit of the DNA cross-linked agents, azinomycin A and B, proceeds via a valine-dependent pathway and that hydroxylation and dehydration precedes formation of the terminal epoxide. Sodium 3-methyl-2-oxobutenoate, formed through a transimination reaction, was shown to be the penultimate precursor incorporated into the azinomycin epoxide.
Sues, Justus Liebigs Annalen der Chemie, 1951, vol. 571, p. 201,212
作者:Sues
DOI:——
日期:——
Foeldi; Kollonitsch, Journal of the Chemical Society, 1948, p. 1684
作者:Foeldi、Kollonitsch
DOI:——
日期:——
Coesite inclusions in zircon from gneisses identified by laser Raman microspectrometer in ultrahigh pressure zone of Dabie Mountains, China
作者:Jingbo Liu、Kai Ye、Bolin Cong、Maruyama Shegnori、Hongrui Fan
DOI:10.1007/bf02901171
日期:2001.11
The mineral inclusions in zircon from gneisses in ultra-high pressure (UHP) zone of the Dable Mountains were identified by using a laser Raman microspectrometer. Coesite occurs as inclusions in zircons from all types of gneiss. Other important minerals, such as jadeite, omphacite, aragonite, barite, and anhydrite were also found as inclusion minerals. These discoveries indicate that (i) gneissic country rocks had metamorphosed at the same time as the enclosed eclogites; and (ii) SO4-2-bearing fluids were present in the UHP metamorphic process, which is manifested by occurrence of barite and anhydrite coexisting with coesite.