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二氧化碳还原因子和甲蝶呤是甲烷杆菌提取物将二氧化碳还原为甲烷所需的两种辅酶。

Carbon dioxide reduction factor and methanopterin, two coenzymes required for CO2 reduction to methane by extracts of Methanobacterium.

作者信息

Leigh J A, Wolfe R S

出版信息

J Biol Chem. 1983 Jun 25;258(12):7536-40.

PMID:6408076
Abstract

Carbon dioxide reduction (CDR) factor is contained in a low molecular weight fraction of cell extract that is required for methane production from CO2 by resolved cell extracts. This fraction has been separated into two components both of which have been highly purified. One component is methanopterin, and for the other component the name CDR factor is retained. No known coenzymes tested substitute in the methane-producing assay for CDR factor and methanopterin, both of which are stable to boiling and exposure to air. The ultraviolet-visible spectrum of CDR factor has a peak at 273 nm, a shoulder at 280 nm, and at pH 1, a peak at 219 nm. The ultraviolet-visible spectrum of methanopterin isolated from the CDR fraction is similar to the spectrum previously reported for this compound (Keltjens, J. T., and Vogels, G. D. (1981) in Microbial Growth on C1 Compounds (Dalton, H., ed) pp. 152-158, Heyden and Son, Ltd., London). The addition of CDR factor (0.8 micrograms) and methanopterin (50 micrograms) to the assay mixture increased by 12-fold the amount of methane formed from CO2.

摘要

二氧化碳还原(CDR)因子存在于细胞提取物的低分子量组分中,该组分是分离的细胞提取物将二氧化碳转化为甲烷所必需的。该组分已被分离为两个成分,且均已高度纯化。一个成分是甲蝶呤,另一个成分仍保留CDR因子的名称。在甲烷生成试验中,没有经过测试的已知辅酶可替代CDR因子和甲蝶呤,这两者对煮沸和暴露于空气中均稳定。CDR因子的紫外可见光谱在273nm处有一个峰值,在280nm处有一个肩峰,在pH值为1时,在219nm处有一个峰值。从CDR组分中分离出的甲蝶呤的紫外可见光谱与先前报道的该化合物的光谱相似(凯尔延斯,J.T.,和福格尔斯,G.D.(1981年),载于《C1化合物上的微生物生长》(道尔顿,H.编),第152 - 158页,海登父子有限公司,伦敦)。向测定混合物中添加CDR因子(0.8微克)和甲蝶呤(50微克),使由二氧化碳生成的甲烷量增加了12倍。

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