Phylogenetic Analysis of Ammonia Monooxygenase (amoa) Genes From Desert Caves

Kenyan Pius Phlieger, Katelyn Green, Daniel S. Jones
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Abstract

Nitrification is the process by which ammonia is oxidized to nitrate, and is an important biogeochemical reaction in the global nitrogen cycle. This process is catalyzed by ammonia monooxygenase (AMO), which is encoded by the amoA gene. Both bacteria (ammonia-oxidizing bacteria, or AOB) and archaea (ammonia-oxidizing archaea, or AOA) are capable of carrying out ammonia oxidation. This project focuses on the phylogenetic analysis of novel amoA genes from microorganisms found in caves. Through this project, amoA genes from two new metagenomes from Lehman Caves in Nevada and Lechuguilla Cave in New Mexico are being analyzed. Other amoA sequences used for phylogenetic comparison are being compiled from the scientific literature, including amoA studies that go back more than 23 years, as well as from metagenomes from other cave systems. At least one bacterial and one archaeal amoA have been identified so far, and preliminary BLAST analysis showed that these likely originated from close relatives of known ammonia oxidizers, including Nitrosomonas spp., and an unknown archaea. Detailed phylogenetic analysis shows that the amoA from the ammonia-oxidizing bacterium is most closely related to Nitrosomonas spp. and to amoA recovered from other caves, as well as several pmoA sequences, indicating potential use of trace methane. We are now performing additional phylogenetic analyses to further classify these new amoA sequences and explore the evolution of ammonia-oxidizing microorganisms in caves, as well as to further explore the potential use of trace methane as an energy resource in desert caves. The work from this project will be used in future research aimed at uncovering new ammonia-oxidizing cave microorganisms and exploring their role in the subterranean nitrogen cycle.
荒漠洞穴中氨单加氧酶基因的系统发育分析
硝化作用是氨氧化为硝酸盐的过程,是全球氮循环中重要的生物地球化学反应。该过程由氨单加氧酶(AMO)催化,该酶由amoA基因编码。细菌(氨氧化细菌或AOB)和古细菌(氨氧化古细菌或AOA)都能够进行氨氧化。本项目的重点是对洞穴中发现的微生物的新型amoA基因进行系统发育分析。通过该项目,对来自内华达州雷曼洞穴和新墨西哥州勒丘吉拉洞穴的两个新宏基因组的amoA基因进行了分析。其他用于系统发育比较的amoA序列正在从科学文献中编译,包括超过23年前的amoA研究,以及来自其他洞穴系统的宏基因组。到目前为止,已经鉴定出至少一种细菌和一种古细菌amoA,初步BLAST分析表明,这些细菌可能来自已知氨氧化剂的近亲,包括亚硝化单胞菌和一种未知的古细菌。详细的系统发育分析表明,该氨氧化菌的amoA与亚硝化单胞菌(Nitrosomonas sp .)和其他洞穴中发现的amoA以及多个pmoA序列关系最为密切,表明其可能利用微量甲烷。我们目前正在进行进一步的系统发育分析,以进一步对这些新的amoA序列进行分类,并探索洞穴中氨氧化微生物的进化,以及进一步探索微量甲烷作为沙漠洞穴能源的潜在用途。该项目的工作将用于未来的研究,旨在发现新的氨氧化洞穴微生物,并探索它们在地下氮循环中的作用。
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