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微生物介导的热带珊瑚氮循环。

Microbially facilitated nitrogen cycling in tropical corals.

机构信息

Centre for Coastal Biogeochemistry Research, School of Environment Science and Engineering, Southern Cross University, Lismore, NSW, Australia.

Department of Environmental and Biological Sciences, University of Eastern Finland, Kuopio, Finland.

出版信息

ISME J. 2022 Jan;16(1):68-77. doi: 10.1038/s41396-021-01038-1. Epub 2021 Jul 5.

Abstract

Tropical scleractinian corals support a diverse assemblage of microbial symbionts. This 'microbiome' possesses the requisite functional diversity to conduct a range of nitrogen (N) transformations including denitrification, nitrification, nitrogen fixation and dissimilatory nitrate reduction to ammonium (DNRA). Very little direct evidence has been presented to date verifying that these processes are active within tropical corals. Here we use a combination of stable isotope techniques, nutrient uptake calculations and captured metagenomics to quantify rates of nitrogen cycling processes in a selection of tropical scleractinian corals. Denitrification activity was detected in all species, albeit with very low rates, signifying limited importance in holobiont N removal. Relatively greater nitrogen fixation activity confirms that corals are net N importers to reef systems. Low net nitrification activity suggests limited N regeneration capacity; however substantial gross nitrification activity may be concealed through nitrate consumption. Based on nrfA gene abundance and measured inorganic N fluxes, we calculated significant DNRA activity in the studied corals, which has important implications for coral reef N cycling and warrants more targeted investigation. Through the quantification and characterisation of all relevant N-cycling processes, this study provides clarity on the subject of tropical coral-associated biogeochemical N-cycling.

摘要

热带造礁石珊瑚支持着多种多样的微生物共生体。这些“微生物组”具有进行一系列氮(N)转化的必需功能多样性,包括反硝化、硝化、固氮和异化硝酸盐还原为铵(DNRA)。迄今为止,几乎没有直接证据证明这些过程在热带珊瑚中是活跃的。在这里,我们使用稳定同位素技术、养分吸收计算和捕获宏基因组学的组合,定量了一系列热带石珊瑚中氮循环过程的速率。所有物种都检测到了反硝化活性,尽管速率非常低,这表明在整个共生体 N 去除中意义有限。相对较高的固氮活性证实珊瑚是珊瑚礁系统的净氮进口。净硝化活性较低表明氮再生能力有限;然而,大量的总硝化活性可能通过硝酸盐消耗而被掩盖。基于 nrfA 基因丰度和测量的无机 N 通量,我们计算出研究珊瑚中有显著的 DNRA 活性,这对珊瑚礁氮循环有重要意义,并值得更有针对性的研究。通过对所有相关氮循环过程的定量和特征描述,本研究阐明了热带珊瑚相关生物地球化学氮循环的主题。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5c99/8692614/abe4b2ff18be/41396_2021_1038_Fig1_HTML.jpg

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