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能够进行好氧硝酸盐呼吸的土壤和沉积物细菌。

Soil and sediment bacteria capable of aerobic nitrate respiration.

作者信息

Carter J P, Hsaio Y H, Spiro S, Richardson D J

机构信息

School of Biological Sciences, University of East Anglia, Norwich, United Kingdom.

出版信息

Appl Environ Microbiol. 1995 Aug;61(8):2852-8. doi: 10.1128/aem.61.8.2852-2858.1995.

Abstract

Several laboratory strains of gram-negative bacteria are known to be able to respire nitrate in the presence of oxygen, although the physiological advantage gained from this process is not entirely clear. The contribution that aerobic nitrate respiration makes to the environmental nitrogen cycle has not been studied. As a first step in addressing this question, a strategy which allows for the isolation of organisms capable of reducing nitrate to nitrite following aerobic growth has been developed. Twenty-nine such strains have been isolated from three soils and a freshwater sediment and shown to comprise members of three genera (Pseudomonas, Aeromonas, and Moraxella). All of these strains expressed a nitrate reductase with an active site located in the periplasmic compartment. Twenty-two of the strains showed significant rates of nitrate respiration in the presence of oxygen when assayed with physiological electron donors. Also isolated was one member of the gram-positive genus Arthrobacter, which was likewise able to respire nitrate in the presence of oxygen but appeared to express a different type of nitrate reductase. In the four environments studied, culturable bacteria capable of aerobic nitrate respiration were isolated in significant numbers (10(4) to 10(7) per g of soil or sediment) and in three cases were as abundant as, or more abundant than, culturable bacteria capable of denitrification. Thus, it seems likely that the corespiration of nitrate and oxygen may indeed make a significant contribution to the flux of nitrate to nitrite in the environment.

摘要

已知几种革兰氏阴性菌的实验室菌株能够在有氧条件下以硝酸盐为呼吸底物,尽管这一过程带来的生理优势尚不完全清楚。有氧硝酸盐呼吸对环境氮循环的贡献尚未得到研究。作为解决这个问题的第一步,已经开发出一种策略,该策略能够分离出在有氧生长后能够将硝酸盐还原为亚硝酸盐的微生物。已从三种土壤和一种淡水沉积物中分离出29株这样的菌株,结果表明它们分属于三个属(假单胞菌属、气单胞菌属和莫拉氏菌属)。所有这些菌株都表达了一种硝酸盐还原酶,其活性位点位于周质区室。当用生理性电子供体进行测定时,其中22株菌株在有氧条件下表现出显著的硝酸盐呼吸速率。还分离出了革兰氏阳性节杆菌属的一个成员,它同样能够在有氧条件下以硝酸盐为呼吸底物,但似乎表达了一种不同类型的硝酸盐还原酶。在所研究的四种环境中,能够进行有氧硝酸盐呼吸的可培养细菌数量可观(每克土壤或沉积物中有10⁴至10⁷个),在三种情况下,其数量与能够进行反硝化作用的可培养细菌一样多或更多。因此,硝酸盐和氧气的共同呼吸作用很可能确实对环境中硝酸盐向亚硝酸盐的通量有显著贡献。

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