摘要
从黄石磁湖底部泥水样中分离到一株杆状好氧趋磁细菌HM-1,在pH7.0~8.0、30℃振荡培养的条件下培养时,每升培养基含4g柠檬酸,0.5g硝酸钠和50mmol·L-1FeSO4,分别是它生长和磁小体合成的最适碳源、氮源和铁源;此菌为G-,氧化酶和过氧化物酶阳性,不积累聚-β-羟丁酸,G+C的摩尔分数为64.08(HPLC);磁小体含一种矿质元素Fe.
A rod shaped magnetic bacterium was isolated from freshwater sediment and a pure culture was obtained. The organism was cultured in a chemical defind medium containing citric acid (4 g·L -1 ), nitrate (0 5 g·L -1 ) and FeSO 4 (50 mmol·L -1 ) as the carbon, nitrogen and iron soures respectivelly. This magnetotactic bacterium was G - and able to form white colonies on ager plate and grow in O 2 contained atmosphere (shaked at 200 r·min -1 ). In this condition, it synthsised magnetosomes, showed catalase and oxidase activities. Microaerophili condition was influeuce for its growth and magnetosomes formation. Intracellalar poly β hydroxybutyrate is not formed. The X G+C of the DNA is 64.08 (HPLC). The entrgy profiles of X ray showed by electron excitation in TEM indicating that its magnetosome consists of one mineral element Fe only.
出处
《武汉大学学报(自然科学版)》
CSCD
1997年第6期775-780,共6页
Journal of Wuhan University(Natural Science Edition)
基金
国家自然科学基金
关键词
超磁细菌
好氧趋磁细菌
分离
生物学特性
magnetotactic bacterium
magnetosome
aerobic magnetotactic bacterium