Ringeling P L, Davy S L, Monkara F A, Hunt C, Dickson D P, McEwan A G, Moore G R
School of Chemical Sciences, Centre for Metalloprotein Spectroscopy and Biology, University of East Anglia, Norwich, England.
Eur J Biochem. 1994 Aug 1;223(3):847-55. doi: 10.1111/j.1432-1033.1994.tb19061.x.
The water-soluble cytochrome b557 from the photosynthetic bacterium Rhodobacter capsulatus was purified and shown to have the properties of the iron-storage protein bacterioferritin. The molecular mass of R. capsulatus bacterioferritin is 428 kDa and it is composed of a single type of 18-kDa subunit. The N-terminal amino acid sequence of the bacterioferritin subunit shows 70% identity to the sequence of bacterioferritin subunits from Escherichia coli, Nitrobacter winogradskyi, Azotobacter vinelandii and Synechocystis PCC 6803. The absorbance spectrum of reduced bacterioferritin shows absorbance maxima at 557 nm (alpha band), 526 nm (beta band) and 417 nm (Soret band) from the six haem groups/molecule. Antibody assays reveal that bacterioferritin is located in the cytoplasm of R. capsulatus, and its levels stay relatively constant during batch growth under aerobic conditions when the iron concentration in the medium is kept constant. Iron deficiency leads to a decrease in bacterioferritin and iron overload leads to an increase. Bacterioferritin from R. capsulatus has an amorphous iron-oxide core with a high phosphate content (900-1000 Fe atoms and approximately 600 phosphates/bacterioferritin molecule). Mössbauer spectroscopy indicates that in both aerobically and anaerobically (phototrophically) grown cells bacterioferritin with an Fe3+ core is formed, suggesting that iron-core formation in vivo may not always require molecular oxygen.
对光合细菌荚膜红细菌中水溶性细胞色素b557进行了纯化,并证明其具有铁储存蛋白细菌铁蛋白的特性。荚膜红细菌细菌铁蛋白的分子量为428 kDa,由单一类型的18 kDa亚基组成。细菌铁蛋白亚基的N端氨基酸序列与大肠杆菌、维氏硝化杆菌、棕色固氮菌和聚球藻PCC 6803的细菌铁蛋白亚基序列具有70%的同一性。还原型细菌铁蛋白的吸收光谱显示,每个分子的六个血红素基团在557 nm(α带)、526 nm(β带)和417 nm(Soret带)处有最大吸收。抗体检测表明,细菌铁蛋白位于荚膜红细菌的细胞质中,在有氧条件下分批培养期间,当培养基中的铁浓度保持恒定时,其水平保持相对恒定。缺铁会导致细菌铁蛋白减少,铁过载会导致其增加。荚膜红细菌的细菌铁蛋白具有高磷酸盐含量的无定形氧化铁核心(每个细菌铁蛋白分子含有900 - 1000个铁原子和约600个磷酸盐)。穆斯堡尔光谱表明,在需氧和厌氧(光养)生长的细胞中都会形成具有Fe3+核心的细菌铁蛋白,这表明体内铁核心的形成可能并不总是需要分子氧。