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低 pH 值下聚集化化能自养细菌的硝化作用。

Nitrification at Low pH by Aggregated Chemolithotrophic Bacteria.

机构信息

Institute for Ecological Research, P.O. Box 40, 6666 ZG Heteren, and Laboratory for Electron Microscopy, Biological Centre, University of Groningen, 9751 NN Haren, The Netherlands, and Abteilung für Mikrobiologie, Institut für Allgemeine Botanik der Universität Hamburg, D-2000 Hamburg 52, Germany.

出版信息

Appl Environ Microbiol. 1991 Dec;57(12):3600-4. doi: 10.1128/aem.57.12.3600-3604.1991.

Abstract

A study was performed to gain insight into the mechanism of acid-tolerant, chemolithotrophic nitrification. Microorganisms that nitrified at pH 4 were enriched from two Dutch acid soils. Nitrate production in the enrichment cultures was indicated to be of a chemolithoautotrophic nature as it was (i) completely inhibited by acetylene at a concentration as low as 1 mumol/liter and (ii) strongly retarded under conditions of carbon dioxide limitation. Electron microscopy of the enrichment cultures showed the presence of bacteria that were morphologically similar to strains of known chemolithotrophic nitrifying genera. Many of the enriched bacteria, in particular those that were identified as ammonium oxidizers, were aggregated. Filtration experiments indicated that aggregated cells were able to nitrify at low pH, whereas single cells were not. It is hypothesized that cells inside the aggregates are protected against the toxicity of nitrous acid. Nitrification by aggregated chemolithoautotrophic bacteria may be the dominating process of nitrate formation in many acid soils as it does not appear to depend on the existence of microsites of high pH (acid-sensitive autotrophic nitrification) or on the availability of organic carbon (heterotrophic nitrification).

摘要

进行了一项研究,以深入了解耐酸、化能自养硝化的机制。从两个荷兰酸性土壤中富集了能够在 pH 值 4 下进行硝化的微生物。由于以下两个原因,富集培养物中的硝酸盐生成被认为具有化能自养性质:(i)在低至 1 mumol/l 浓度的乙炔存在下完全被抑制;(ii)在二氧化碳限制条件下受到强烈抑制。富集培养物的电子显微镜观察显示存在形态上类似于已知化能自养硝化属的细菌。许多富集细菌,特别是那些被鉴定为铵氧化菌的细菌,聚集在一起。过滤实验表明,聚集的细胞能够在低 pH 值下进行硝化,而单个细胞则不能。因此推测,聚集物内部的细胞受到保护,免受亚硝酸的毒性影响。在许多酸性土壤中,由聚集的化能自养细菌进行的硝化作用可能是硝酸盐形成的主要过程,因为它似乎不依赖于高 pH 值微区(对酸敏感的自养硝化)的存在或有机碳的可用性(异养硝化)。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa8a/184019/e01571021b7a/aem00065-0213-a.jpg

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