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细菌铁氧化还原蛋白进化的新视角。

New perspectives on bacterial ferredoxin evolution.

作者信息

George D G, Hunt L T, Yeh L S, Barker W C

出版信息

J Mol Evol. 1985;22(1):20-31. doi: 10.1007/BF02105801.

Abstract

Recent evidence indicates that a gene transposition event occurred during the evolution of the bacterial ferredoxins subsequent to the ancestral intrasequence gene duplication. In light of this new information, the relationships among the bacterial ferredoxins were reexamined and an evolutionary tree consistent with this new understanding was derived. The bacterial ferredoxins can be divided into several groups based on their sequence properties; these include the clostridial-type ferredoxins, the Azotobacter-type ferredoxins, and a group containing the ferredoxins from the anaerobic, green, and purple sulfur bacteria. Based on sequence comparison, it was concluded that the amino-terminal domain of the Azotobacter-type ferredoxins, which contains the novel 3Fe:3S cluster binding site, is homologous with the carboxyl-terminal domain of the ferredoxins from the anaerobic photosynthetic bacteria. A number of ferredoxin sequences do not fit into any of the groups described above. Based on sequence properties, these sequences can be separated into three groups: a group containing Methanosarcina barkeri ferredoxin and Desulfovibrio desulfuricans ferredoxin II, a group containing Desulfovibrio gigas ferredoxin and Clostridium thermoaceticum ferredoxin, and a group containing Desulfovibrio africanus ferredoxin I and Bacillus stearothermophilus ferredoxin. The last two groups differ from all of the other bacterial ferredoxins in that they bind only one Fe:S cluster per polypeptide, whereas the others bind two. Sequence examination indicates that the second binding site has been either partially or completely lost from these ferredoxins. Methanosarcina barkeri ferredoxin and Desulfovibrio desulfuricans ferredoxin II are of interest because, of all the ferredoxins whose sequences are presently known, they show the strongest evidence of internal gene duplication.(ABSTRACT TRUNCATED AT 400 WORDS)

摘要

最近的证据表明,在祖先序列内基因复制之后的细菌铁氧化还原蛋白进化过程中发生了基因转座事件。鉴于这一新信息,对细菌铁氧化还原蛋白之间的关系进行了重新审视,并得出了与这一新认识相一致的进化树。根据其序列特性,细菌铁氧化还原蛋白可分为几组;这些包括梭菌型铁氧化还原蛋白、固氮菌型铁氧化还原蛋白,以及一组包含来自厌氧、绿色和紫色硫细菌的铁氧化还原蛋白。基于序列比较得出结论,固氮菌型铁氧化还原蛋白的氨基末端结构域含有新的3Fe:3S簇结合位点,与厌氧光合细菌铁氧化还原蛋白的羧基末端结构域同源。许多铁氧化还原蛋白序列并不属于上述任何一组。根据序列特性,这些序列可分为三组:一组包含巴氏甲烷八叠球菌铁氧化还原蛋白和脱硫脱硫弧菌铁氧化还原蛋白II,一组包含巨大脱硫弧菌铁氧化还原蛋白和嗜热醋酸梭菌铁氧化还原蛋白,一组包含非洲脱硫弧菌铁氧化还原蛋白I和嗜热脂肪芽孢杆菌铁氧化还原蛋白。最后两组与所有其他细菌铁氧化还原蛋白的不同之处在于,它们每个多肽仅结合一个Fe:S簇,而其他的结合两个。序列检查表明,这些铁氧化还原蛋白的第二个结合位点已部分或完全丧失。巴氏甲烷八叠球菌铁氧化还原蛋白和脱硫脱硫弧菌铁氧化还原蛋白II之所以令人感兴趣,是因为在目前已知序列的所有铁氧化还原蛋白中,它们显示出内部基因复制的最有力证据。(摘要截于400字)

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