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热带港湾氨氧化微生物的月分布。

Monthly distribution of ammonia-oxidizing microbes in a tropical bay.

机构信息

School of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang, 524088, P. R. China.

State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai, 200062, P. R. China.

出版信息

J Microbiol. 2021 Jan;59(1):10-19. doi: 10.1007/s12275-021-0287-5. Epub 2020 Nov 17.

DOI:10.1007/s12275-021-0287-5
PMID:33201437
Abstract

Ammonia oxidation, performed by ammonia-oxidizing archaea (AOA) and bacteria (AOB), plays a critical role in the cycle of nitrogen in the ocean. For now, environmental variables controlling distribution of ammonia-oxidizing microbes are still largely unknown in oceanic environments. In this study, we used real-time quantitative PCR and high-throughput sequencing methods to investigate the abundance and diversity of AOA and AOB from sediment and water in Zhanjiang Bay. Phylogenic analysis revealed that the majority of AOA amoA sequences in water and sediment were affiliated with the genus Nitrosopumilus, whereas the Nitrosotalea cluster was only detected with low abundance in water. Nitrosomonas and Nitrosospira dominated AOB amoA sequences in water and sediment, respectively. The amoA copy numbers of both AOA and AOB varied significantly with month for both sediment and water. When water and sediment temperature dropped to 17-20°C in December and February, respectively, the copy number of AOB amoA genes increased markedly and was much higher than for AOA amoA genes. Also, AOA abundance in water peaked in December when water temperature was lowest (17-20°C). Stepwise multiple regression analyses revealed that temperature was the most key factor driving monthly changes of AOA or AOB abundance. It is inferred that low water temperature may inhibit growth of phytoplankton and other microbes and so reduce competition for a common substrate, ammonium.

摘要

氨氧化作用由氨氧化古菌(AOA)和细菌(AOB)完成,在海洋氮循环中起着关键作用。目前,海洋环境中控制氨氧化微生物分布的环境变量在很大程度上仍然未知。在这项研究中,我们使用实时定量 PCR 和高通量测序方法调查了湛江湾沉积物和水中 AOA 和 AOB 的丰度和多样性。系统发育分析表明,水中和沉积物中的大多数 AOA amoA 序列与 Nitrosopumilus 属有关,而 Nitrosotalea 群仅在水中以低丰度检测到。在水中和沉积物中,Nitrosomonas 和 Nitrosospira 分别占 AOB amoA 序列的优势。无论是沉积物还是水,AOA 和 AOB 的 amoA 拷贝数都随月份有显著变化。当 12 月和 2 月水温分别降至 17-20°C 时,AOB amoA 基因的拷贝数显著增加,远高于 AOA amoA 基因。此外,当水温最低(17-20°C)时,水中 AOA 的丰度在 12 月达到峰值。逐步多元回归分析表明,温度是驱动 AOA 或 AOB 丰度月度变化的最关键因素。可以推断,低水温可能会抑制浮游植物和其他微生物的生长,从而减少对共同基质铵的竞争。

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本文引用的文献

1
Responses of Active Ammonia Oxidizers and Nitrification Activity in Eutrophic Lake Sediments to Nitrogen and Temperature.富营养化湖泊沉积物中活性氨氧化菌和硝化活性对氮和温度的响应。
Appl Environ Microbiol. 2019 Aug 29;85(18). doi: 10.1128/AEM.00258-19. Print 2019 Sep 15.
2
Light and temperature control the seasonal distribution of thaumarchaeota in the South Atlantic bight.光照和温度控制着南大西洋湾中泉古菌的季节性分布。
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Distinct distribution patterns of ammonia-oxidizing archaea and bacteria in sediment and water column of the Yellow River estuary.
黄河口沉积物和水柱中氨氧化古菌和细菌的分布模式明显不同。
Sci Rep. 2018 Jan 25;8(1):1584. doi: 10.1038/s41598-018-20044-6.
4
Difference of nitrogen-cycling microbes between shallow bay and deep-sea sediments in the South China Sea.南海浅海和深海沉积物中氮循环微生物的差异。
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Population and diversity of ammonia-oxidizing archaea and bacteria in a pollutants' receiving area in Hangzhou Bay.杭州湾污染物接收区氨氧化古菌和细菌的种群多样性。
Appl Microbiol Biotechnol. 2016 Jul;100(13):6035-45. doi: 10.1007/s00253-016-7421-z. Epub 2016 Mar 10.
7
Diversity, Abundance, and Niche Differentiation of Ammonia-Oxidizing Prokaryotes in Mud Deposits of the Eastern China Marginal Seas.中国东部边缘海泥质沉积物中氨氧化原核生物的多样性、丰度及生态位分化
Front Microbiol. 2016 Feb 12;7:137. doi: 10.3389/fmicb.2016.00137. eCollection 2016.
8
Complete nitrification by a single microorganism.单一微生物实现完全硝化作用。
Nature. 2015 Dec 24;528(7583):555-9. doi: 10.1038/nature16459. Epub 2015 Nov 26.
9
Complete nitrification by Nitrospira bacteria.硝化螺菌属细菌实现完全硝化作用。
Nature. 2015 Dec 24;528(7583):504-9. doi: 10.1038/nature16461. Epub 2015 Nov 26.
10
Species, Abundance and Function of Ammonia-oxidizing Archaea in Inland Waters across China.中国内陆水体中氨氧化古菌的种类、丰度及功能
Sci Rep. 2015 Nov 2;5:15969. doi: 10.1038/srep15969.