Matzanke B F, Bill E, Müller G I, Trautwein A X, Winkelmann G
Eur J Biochem. 1987 Feb 2;162(3):643-50. doi: 10.1111/j.1432-1033.1987.tb10686.x.
Mössbauer spectra of whole cells of Neurospora crassa arg-5 ota aga (a siderophore-free mutant) show that the siderophore coprogen is accumulated inside the cell as an entity. 57Fe from 57Fe-labeled coprogen is slowly removed from the complex (45% in 27 h). The rate of removal depends on the degree of iron starvation of the cells. The distribution of 55Fe from [55Fe]coprogen in vacuoles, membranes, and cytoplasm has been also determined. From this it is clear that coprogen is accumulated in the cytoplasm. In addition to its role as a siderophore, coprogen serves as an iron-storage compound. No holoferritins could be detected. We therefore conclude that this type of iron-storage protein is lacking in N. crassa. Metabolized iron was found predominantly to exist as an envelope of Fe(II) high-spin (delta = 1.2-1.3 mm s-1; delta EQ = 3.0-3.1 mm s-1 at 4.2 K) and fast-relaxing Fe(III) high-spin species (delta approximately equal to 0.25 mm s-1 and 0.45 mm s-1; delta EQ approximately equal to 0.6 mm s-1 and 0.55 mm s-1, respectively, at 4.2 K). An assignment of these major iron metabolites is difficult. The Mössbauer data of the Fe(II) species do not fit those reported for heme, cytochromes and ferredoxins. We therefore assume that this iron metabolite represents a novel internal iron compound. One of the Fe(III) species becomes the dominant component of the cell spectra after 65 h of metabolization and might correspond to an iron-storage compound with iron oxide cores similar to bacterioferritin. After 27 h of growth in mycelia supplied with 57Fe-labeled coprogen, the siderophore ferricrocin was observed in the cell spectra. This is unexpected, since N. crassa arg-5 ota aga is unable to synthesize ornithine. We assume that ferricrocin is synthesized by the use of coprogen degradation products.
粗糙脉孢菌arg - 5 ota aga(一种无铁载体突变体)全细胞的穆斯堡尔谱表明,铁载体粪卟啉原作为一个整体在细胞内积累。来自57Fe标记粪卟啉原的57Fe从复合物中缓慢去除(27小时内去除45%)。去除速率取决于细胞的缺铁程度。还测定了[55Fe]粪卟啉原中的55Fe在液泡、膜和细胞质中的分布。由此可见,粪卟啉原积累在细胞质中。除了作为铁载体的作用外,粪卟啉原还作为一种铁储存化合物。未检测到全铁蛋白。因此我们得出结论,粗糙脉孢菌缺乏这种类型的铁储存蛋白。发现代谢后的铁主要以Fe(II)高自旋包层(δ = 1.2 - 1.3 mm s-1;在4.2 K时δEQ = 3.0 - 3.1 mm s-1)和快速弛豫的Fe(III)高自旋物种(δ分别约为0.25 mm s-1和0.45 mm s-1;在4.2 K时δEQ分别约为0.6 mm s-1和0.55 mm s-1)的形式存在。很难确定这些主要铁代谢物的归属。Fe(II)物种的穆斯堡尔数据与报道的血红素、细胞色素和铁氧化还原蛋白的数据不符。因此我们假设这种铁代谢物代表一种新型的内部铁化合物。其中一种Fe(III)物种在代谢65小时后成为细胞谱的主要成分,可能对应一种具有类似于细菌铁蛋白的氧化铁核心的铁储存化合物。在用57Fe标记的粪卟啉原供应的菌丝体中生长27小时后,在细胞谱中观察到了铁载体铁铵菌素。这是出乎意料的,因为粗糙脉孢菌arg - 5 ota aga无法合成鸟氨酸。我们假设铁铵菌素是利用粪卟啉原的降解产物合成的。