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氨氧化古菌——生理、生态与进化。

Ammonia-oxidising archaea--physiology, ecology and evolution.

机构信息

Department of Genetics in Ecology, University of Vienna, Vienna, Austria.

出版信息

Adv Microb Physiol. 2010;57:1-41. doi: 10.1016/B978-0-12-381045-8.00001-1.

Abstract

Nitrification is a microbially mediated process that plays a central role in the global cycling of nitrogen and is also of economic importance in agriculture and wastewater treatment. The first step in nitrification is performed by ammonia-oxidising microorganisms, which convert ammonia into nitrite ions. Ammonia-oxidising bacteria (AOB) have been known for more than 100 years. However, metagenomic studies and subsequent cultivation efforts have recently demonstrated that microorganisms of the domain archaea are also capable of performing this process. Astonishingly, members of this group of ammonia-oxidising archaea (AOA), which was overlooked for so long, are present in almost every environment on Earth and typically outnumber the known bacterial ammonia oxidisers by orders of magnitudes in common environments such as the marine plankton, soils, sediments and estuaries. Molecular studies indicate that AOA are amongst the most abundant organisms on this planet, adapted to the most common environments, but are also present in those considered extreme, such as hot springs. The ecological distribution and community dynamics of these archaea are currently the subject of intensive study by many research groups who are attempting to understand the physiological diversity and the ecosystem function of these organisms. The cultivation of a single marine isolate and two enrichments from hot terrestrial environments has demonstrated a chemolithoautotrophic mode of growth. Both pure culture-based and environmental studies indicate that at least some AOA have a high substrate affinity for ammonia and are able to grow under extremely oligotrophic conditions. Information from the first available genomes of AOA indicate that their metabolism is fundamentally different from that of their bacterial counterparts, involving a highly copper-dependent system for ammonia oxidation and electron transport, as well as a novel carbon fixation pathway that has recently been discovered in hyperthermophilic archaea. A distinct set of informational processing genes of AOA indicates that they are members of a distinct and novel phylum within the archaea, the 'Thaumarchaeota', which may even be a more ancient lineage than the established Cren- and Euryarchaeota lineages, raising questions about the evolutionary origins of archaea and the origins of ammonia-oxidising metabolism.

摘要

硝化作用是一种微生物介导的过程,在全球氮循环中起着核心作用,在农业和废水处理中也具有经济重要性。硝化作用的第一步是由氨氧化微生物完成的,它们将氨转化为亚硝酸盐离子。氨氧化细菌(AOB)已经被人们认识了 100 多年。然而,宏基因组学研究和随后的培养工作最近表明,古菌域的微生物也能够进行这一过程。令人惊讶的是,长期以来被忽视的氨氧化古菌(AOA)的成员在地球上几乎每一种环境中都存在,并且在海洋浮游生物、土壤、沉积物和河口等常见环境中,其数量通常比已知的细菌氨氧化菌多几个数量级。分子研究表明,AOA 是地球上最丰富的生物之一,适应于最常见的环境,但也存在于那些被认为是极端的环境中,如温泉。这些古菌的生态分布和群落动态是目前许多研究小组正在研究的课题,他们试图了解这些生物体的生理多样性和生态系统功能。对来自海洋的单一分离株和两个来自热陆地环境的富集物的培养已经证明了它们是化能自养生长模式。基于纯培养和环境研究都表明,至少一些 AOA 对氨有很高的亲和力,并且能够在极其贫营养的条件下生长。来自 AOA 的第一个可用基因组的信息表明,它们的代谢与细菌截然不同,涉及一个高度依赖铜的氨氧化和电子传递系统,以及一个最近在高温古菌中发现的新型碳固定途径。AOA 独特的信息处理基因集表明,它们是古菌中一个独特的新型门——“泉古菌门”的成员,甚至可能比已建立的广古菌门和泉古菌门更早出现,这引发了关于古菌的进化起源和氨氧化代谢起源的问题。

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