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磁性细菌趋磁螺菌AMB-1产生铁载体的情况。

Siderophore production by the magnetic bacterium Magnetospirillum magneticum AMB-1.

作者信息

Calugay Ronie J, Miyashita Hideaki, Okamura Yoshiko, Matsunaga Tadashi

机构信息

Department of Biotechnology, Tokyo University of Agriculture and Technology, 2-24-16 Naka-Cho, Koganei, Tokyo, Japan.

出版信息

FEMS Microbiol Lett. 2003 Jan 28;218(2):371-5. doi: 10.1016/S0378-1097(02)01188-6.

Abstract

Siderophore production by the magnetic bacterium Magnetospirillum magneticum AMB-1 is elicited by sufficient iron rather than by iron starvation. In order to clarify this unusual pattern, siderophore production was monitored in parallel to iron assimilation using the chrome azurol sulfonate assay and the ferrozine method respectively. Iron concentration lowered approximately five times less than its initial concentration only within 4 h post-inoculation, rendering the medium iron deficient. A concentration of at least 6 microM Fe(3+) is required to initiate siderophore production. The propensity of M. magneticum AMB-1 for the assimilation of large amounts of iron accounts for the rapid depletion of iron in the medium, thereby triggering siderophore excretion. M. magneticum AMB-1 produces both hydroxamate and catechol siderophores.

摘要

磁性细菌趋磁螺菌AMB-1产生铁载体是由充足的铁引发的,而非铁饥饿。为了阐明这种不寻常的模式,分别使用铬天青磺酸盐测定法和亚铁嗪法,并行监测铁载体产生与铁同化情况。接种后仅4小时内,铁浓度下降幅度约为初始浓度的五分之一,使培养基缺铁。启动铁载体产生需要至少6 microM Fe(3+)的浓度。趋磁螺菌AMB-1大量同化铁的倾向导致培养基中铁迅速耗尽,从而触发铁载体排泄。趋磁螺菌AMB-1同时产生异羟肟酸型和儿茶酚型铁载体。

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