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贫氧微区可能是氮限制有氧海洋水中微生物固氮的场所。

Oxygen-poor microzones as potential sites of microbial n(2) fixation in nitrogen-depleted aerobic marine waters.

机构信息

Institute of Marine Sciences, University of North Carolina, Morehead City, North Carolina 28557.

出版信息

Appl Environ Microbiol. 1987 May;53(5):1078-87. doi: 10.1128/aem.53.5.1078-1087.1987.

DOI:10.1128/aem.53.5.1078-1087.1987
PMID:16347337
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC203813/
Abstract

The nitrogen-deficient coastal waters of North Carolina contain suspended bacteria potentially able to fix N(2). Bioassays aimed at identifying environmental factors controlling the development and proliferation of N(2) fixation showed that dissolved organic carbon (as simple sugars and sugar alcohols) and particulate organic carbon (derived from Spartina alterniflora) additions elicited and enhanced N(2) fixation (nitrogenase activity) in these waters. Nitrogenase activity occurred in samples containing flocculent, mucilage-covered bacterial aggregates. Cyanobacterium-bacterium aggregates also revealed N(2) fixation. In all cases bacterial N(2) fixation occurred in association with surficial microenvironments or microzones. Since nitrogenase is oxygen labile, we hypothesized that the aggregates themselves protected their constituent microbes from O(2). Microelectrode O(2) profiles revealed that aggregates had lower internal O(2) tensions than surrounding waters. Tetrazolium salt (2,3,5-triphenyl-3-tetrazolium chloride) reduction revealed that patchy zones existed both within microbes and extracellularly in the mucilage surrounding microbes where free O(2) was excluded. Triphenyltetrazolium chloride reduction also strongly inhibited nitrogenase activity. These findings suggest that N(2) fixation is mediated by the availability of the appropriate types of reduced microzones. Organic carbon enrichment appears to serve as an energy and structural source for aggregate formation, both of which were required for eliciting N(2) fixation responses of these waters.

摘要

北卡罗来纳州氮缺乏的沿海水域含有悬浮细菌,这些细菌可能具有固氮能力。旨在确定控制氮固定发展和增殖的环境因素的生物测定表明,溶解有机碳(如简单糖和糖醇)和颗粒有机碳(源自互花米草)的添加引发并增强了这些水域中的氮固定(固氮酶活性)。固氮酶活性发生在含有絮状、粘液覆盖的细菌聚集体的样品中。蓝细菌-细菌聚集体也显示出氮固定。在所有情况下,细菌的氮固定都与表面微环境或微区有关。由于固氮酶对氧气敏感,我们假设聚集体本身可以保护其组成微生物免受氧气的影响。微电极氧气剖面显示,聚集体的内部氧气张力低于周围水体。四唑盐(2,3,5-三苯基-3-四唑氯化物)还原表明,微生物内部和微生物周围粘液中的细胞外存在斑驳区域,其中排除了游离氧气。三苯基四唑氯化物还原也强烈抑制固氮酶活性。这些发现表明,氮固定是由适当类型的还原微区的可用性介导的。有机碳富集似乎是聚集体形成的能量和结构来源,这两者都是引发这些水域氮固定反应所必需的。

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本文引用的文献

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