Myers Judith M, Myers Charles R
Department of Pharmacology and Toxicology, Medical College of Wisconsin, Milwaukee, Wisconsin 53226, USA.
Appl Environ Microbiol. 2002 Jun;68(6):2781-93. doi: 10.1128/AEM.68.6.2781-2793.2002.
Anaerobically grown cells of the metal-reducing bacterium Shewanella putrefaciens MR-1 contain multiple outer membrane (OM) cytochromes. A gene replacement mutant (strain OMCB1) lacking the OM cytochrome OmcB is markedly deficient in the reduction of MnO2 and exhibits reduced rates of Fe(III) reduction. The levels of other OM cytochromes are also decreased in OMCB1. Complementation of OMCB1 with wild-type omcB did not restore any of these defects. However, a 21-kb genomic fragment from MR-1, which included omcB and 19 kb of downstream DNA, fully restored MnO2 and Fe(III) reduction and the full complement of OM cytochromes to OMCB1. A 14.7-kb DNA fragment, including omcB and 12 kb of downstream DNA, provided only a modest increase in MnO2 reduction and OM cytochrome content, but it fully restored Fe(III) citrate reduction and partially restored FeOOH reduction. While omcB mRNA was readily detected in this complement, the OmcB protein was not detected in any cellular compartment. The restoration of Fe(III) reduction despite the absence of OmcB suggests that OmcB itself is not required for Fe(III) reduction. Another OM cytochrome, OmcA, was mislocalized to the cytoplasmic membrane of OMCB1. Only the 21-kb genomic fragment was able to restore proper localization of OmcA to the OM. This 21-kb fragment does not contain omcA, but it does contain several open reading frames (ORFs) downstream from omcB. The most downstream of these ORFs (altA) encodes a putative AraC-like transcriptional regulator. However, a gene replacement mutant of altA resembled the wild type with respect to MnO2 reduction, OM cytochrome content, and the localization of OmcA and OmcB to the OM. Since OMCB1 continues to express genes immediately downstream from omcB, the lack of expression of this downstream DNA does not explain its phenotype or the need for the large complementing fragment. The results suggest that the DNA downstream of omcB must be present in cis in order to restore Fe(III) reduction, MnO2 reduction, OM cytochrome content, and the localization of OmcA and OmcB to the OM.
厌氧生长的腐败希瓦氏菌MR-1细胞含有多种外膜(OM)细胞色素。缺乏OM细胞色素OmcB的基因替换突变体(菌株OMCB1)在二氧化锰还原方面明显不足,并且铁(III)还原速率降低。OMCB1中其他OM细胞色素的水平也有所下降。用野生型omcB对OMCB1进行互补并不能恢复这些缺陷中的任何一个。然而,来自MR-1的一个21 kb基因组片段,其中包括omcB和19 kb的下游DNA,完全恢复了OMCB1的二氧化锰和铁(III)还原能力以及OM细胞色素的完整互补。一个14.7 kb的DNA片段,包括omcB和12 kb的下游DNA,仅使二氧化锰还原和OM细胞色素含量略有增加,但它完全恢复了柠檬酸铁还原能力并部分恢复了氢氧化铁还原能力。虽然在这种互补中很容易检测到omcB mRNA,但在任何细胞区室中都未检测到OmcB蛋白。尽管没有OmcB,但铁(III)还原能力的恢复表明Fe(III)还原本身并不需要OmcB。另一种OM细胞色素OmcA被错误定位到OMCB1的细胞质膜上。只有21 kb的基因组片段能够将OmcA正确定位到OM上。这个21 kb的片段不包含omcA,但它确实包含omcB下游的几个开放阅读框(ORF)。这些ORF中最下游的(altA)编码一种假定的类AraC转录调节因子。然而,altA的基因替换突变体在二氧化锰还原、OM细胞色素含量以及OmcA和OmcB在OM上的定位方面与野生型相似。由于OMCB1继续表达omcB下游紧邻的基因,因此该下游DNA缺乏表达并不能解释其表型或对大的互补片段的需求。结果表明,omcB下游的DNA必须以顺式存在,以便恢复铁(III)还原、二氧化锰还原、OM细胞色素含量以及OmcA和OmcB在OM上的定位。