Emergence and disruption of cooperativity in a denitrifying microbial community

Alex V Carr, Anne E Otwell, Kristopher A Hunt, Yan Chen, James Wilson, José P Faria, Filipe Liu, Janaka N Edirisinghe, Jacob J Valenzuela, Serdar Turkarslan, Lauren M Lui, Torben N Nielsen, Adam P Arkin, Christopher S Henry, Christopher J Petzold, David A Stahl, Nitin S Baliga
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Abstract

Anthropogenic perturbations to the nitrogen cycle, primarily through use of synthetic fertilizers, is driving an unprecedented increase in the emission of nitrous oxide (N2O), a potent greenhouse gas and an ozone depleting substance, causing urgency in identifying the sources and sinks of N2O. Microbial denitrification is a primary contributor to biotic production of N2O in anoxic regions of soil, marine systems, and wastewater treatment facilities. Here, through comprehensive genome analysis, we show that pathway partitioning is a ubiquitous mechanism of complete denitrification within microbial communities. We have investigated mechanisms and consequences of process partitioning of denitrification through detailed physiological characterization and kinetic modeling of a synthetic community of Rhodanobacter thiooxydans FW510-R12 and Acidovorax sp. GW101-3H11. We have discovered that these two bacterial isolates, from a heavily nitrate (NO3−) contaminated superfund site, complete denitrification through the exchange of nitrite (NO2−) and nitric oxide (NO). The process partitioning of denitrification and other processes, including amino acid metabolism, contribute to increased cooperativity within this denitrifying community. We demonstrate that certain contexts, such as high NO3−, cause unbalanced growth of community members, due to differences in their substrate utilization kinetics. The altered growth characteristics of community members drives accumulation of toxic NO2−, which disrupts denitrification causing N2O off gassing.
反硝化微生物群落中协同作用的出现和破坏
人为对氮循环的干扰(主要是通过使用合成肥料)正在推动一氧化二氮(N2O)排放的空前增加,N2O是一种强效温室气体和消耗臭氧的物质,因此迫切需要确定N2O的来源和汇。微生物反硝化作用是土壤、海洋系统和废水处理设施缺氧区域生物生产N2O的主要贡献者。在这里,通过全面的基因组分析,我们表明途径分配是微生物群落中普遍存在的完全反硝化机制。我们通过对合成的Rhodanobacter thiooxydans FW510-R12和Acidovorax sp. GW101-3H11进行详细的生理表征和动力学建模,研究了反硝化过程分配的机制和后果。我们发现,这两种细菌分离自重硝酸盐(NO3−)污染的超级基金场地,通过交换亚硝酸盐(NO2−)和一氧化氮(NO)完成反硝化。反硝化过程的分配和其他过程,包括氨基酸代谢,有助于增加这个反硝化群落的合作。我们证明了某些环境,如高NO3−,由于其底物利用动力学的差异,导致群落成员的生长不平衡。群落成员生长特性的改变驱动有毒NO2−的积累,这破坏了反硝化作用,导致N2O排放。
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