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在接近中性pH条件下生长的新型铁氧化细菌的分离与鉴定

Isolation and characterization of novel iron-oxidizing bacteria that grow at circumneutral pH.

作者信息

Emerson D, Moyer C

机构信息

American Type Culture Collection, Rockville, Maryland 20852, USA.

出版信息

Appl Environ Microbiol. 1997 Dec;63(12):4784-92. doi: 10.1128/aem.63.12.4784-4792.1997.

Abstract

A gel-stabilized gradient method that employed opposing gradients of Fe2+ and O2 was used to isolate and characterize two new Fe-oxidizing bacteria from a neutral pH, Fe(2+)-containing groundwater in Michigan. Two separate enrichment cultures were obtained, and in each the cells grew in a distinct, rust-colored band in the gel at the oxic-anoxic interface. The cells were tightly associated with the ferric hydroxides. Repeated serial dilutions of both enrichments resulted in the isolation of two axenic strains, ES-1 and ES-2. The cultures were judged pure based on (i) growth from single colonies in tubes at dilutions of 10(-7) (ES-2) (ES-2) and 10(-8) (ES-1); (ii) uniform cell morphologies, i.e., ES-1 was a motile long thin, bent, or S-shaped rod and ES-2 was a shorter curved rod; and (iii) no growth on a heterotrophic medium. Strain ES-1 grew to a density of 10(8) cells/ml on FeS with a doubling time of 8 h. Strain ES-2 grew to a density of 5 x 10(7) cells/ml with a doubling time of 12.5 h. Both strains also grew on FeCO3. Neither strain grew without Fe2+, nor did they grow with glucose, pyruvate, acetate, Mn, or H2S as an electron donor. Studies with an oxygen microelectrode revealed that both strains grew at the oxic-anoxic interface of the gradients and tracked the O2 minima when subjected to higher O2 concentrations, suggesting they are microaerobes. Phylogenetically the two strains formed a novel lineage within the gamma Proteobacteria. They were very closely related to each other and were equally closely related to PVB OTU 1, a phylotype obtained from an iron-rich hydrothermal vent system at the Loihi Seamount in the Pacific Ocean, and SPB OTU 1, a phylotype obtained from permafrost soil in Siberia. Their closest cultivated relative was Stenotrophomonas maltophilia. In total, this evidence suggests ES-1 and ES-2 are members of a previously untapped group of putatively lithotrophic, unicellular iron-oxidizing bacteria.

摘要

采用一种利用Fe2+和O2反向梯度的凝胶稳定梯度法,从密歇根州中性pH值、含Fe(2+)的地下水中分离并鉴定了两种新的铁氧化细菌。获得了两种单独的富集培养物,在每种培养物中,细胞在凝胶中位于好氧-厌氧界面的一个独特的锈色带中生长。这些细胞与氢氧化铁紧密相关。对两种富集培养物进行重复的系列稀释,得到了两个纯菌株,ES-1和ES-2。基于以下几点判断培养物是纯的:(i) 在10(-7)(ES-2)和10(-8)(ES-1)稀释度下,管中单个菌落的生长;(ii) 均匀的细胞形态,即ES-1是能动的细长、弯曲或S形杆状菌,ES-2是较短的弯曲杆状菌;(iii) 在异养培养基上不生长。菌株ES-1在FeS上生长至密度为10(8)个细胞/ml,倍增时间为8小时。菌株ES-2生长至密度为5×10(7)个细胞/ml,倍增时间为12.5小时。两种菌株也能在FeCO3上生长。两种菌株在没有Fe2+的情况下都不生长,以葡萄糖、丙酮酸、乙酸盐、锰或H2S作为电子供体时也不生长。用氧微电极进行的研究表明,两种菌株都在梯度的好氧-厌氧界面生长,当暴露于较高的O2浓度时会追踪O2最小值,表明它们是微需氧菌。从系统发育角度来看,这两种菌株在γ-变形菌纲内形成了一个新的谱系。它们彼此非常密切相关,并且与PVB OTU 1(从太平洋洛伊希海山富含铁的热液喷口系统获得的一个系统型)和SPB OTU 1(从西伯利亚永久冻土土壤获得的一个系统型)同样密切相关。它们最接近的已培养亲缘种是嗜麦芽窄食单胞菌。总的来说,这些证据表明ES-1和ES-2是一个以前未被开发的假定的化能无机营养单细胞铁氧化细菌群体的成员。

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