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河口微生物多样性和氮循环沿着沙泥梯度增加,与盐度和距离无关。

Estuarine microbial diversity and nitrogen cycling increase along sand-mud gradients independent of salinity and distance.

作者信息

Boey Jian Sheng, Mortimer Redmond, Couturier Agathe, Worrallo Katie, Handley Kim M

机构信息

School of Biological Sciences, Faculty of Science, University of Auckland, Auckland, New Zealand.

Ecole Supérieure de Biologie Biochimie Biotechnologies, Faculté des Sciences, Université Catholique de Lyon, Lyon, France.

出版信息

Environ Microbiol. 2022 Jan;24(1):50-65. doi: 10.1111/1462-2920.15550. Epub 2021 May 13.

Abstract

Estuaries are depositional environments prone to terrigenous mud sedimentation. While macrofaunal diversity and nitrogen retention are greatly affected by changes in sedimentary mud content, its impact on prokaryotic diversity and nitrogen cycling activity remains understudied. We characterized the composition of estuarine tidal flat prokaryotic communities spanning a habitat range from sandy to muddy sediments, while controlling for salinity and distance. We also determined the diversity, abundance and expression of ammonia oxidizers and N O-reducers within these communities by amoA and clade I nosZ gene and transcript analysis. Results show that prokaryotic communities and nitrogen cycling fractions were sensitive to changes in sedimentary mud content, and that changes in the overall community were driven by a small number of phyla. Significant changes occurred in prokaryotic communities and N O-reducing fractions with only a 3% increase in mud, while thresholds for ammonia oxidizers were less distinct, suggesting other factors are also important for structuring these guilds. Expression of nitrogen cycling genes was substantially higher in muddier sediments, and results indicate that the potential for coupled nitrification-denitrification became increasingly prevalent as mud content increased. Altogether, results demonstrate that mud content is a strong environmental driver of diversity and N-cycling dynamics in estuarine microbial communities.

摘要

河口是易于发生陆源泥质沉积的沉积环境。虽然大型动物多样性和氮保留受沉积泥含量变化的影响很大,但其对原核生物多样性和氮循环活动的影响仍未得到充分研究。我们在控制盐度和距离的同时,对从砂质沉积物到泥质沉积物的河口潮滩原核生物群落组成进行了表征。我们还通过amoA和I类nosZ基因及转录本分析,确定了这些群落中氨氧化菌和N O还原菌的多样性、丰度和表达。结果表明,原核生物群落和氮循环组分对沉积泥含量的变化敏感,且整个群落的变化由少数门类驱动。泥含量仅增加3%时,原核生物群落和N O还原组分就发生了显著变化,而氨氧化菌的阈值则不太明显,这表明其他因素对构建这些类群也很重要。氮循环基因的表达在泥质含量更高的沉积物中显著更高,结果表明,随着泥含量的增加,耦合硝化-反硝化的潜力变得越来越普遍。总之,结果表明泥含量是河口微生物群落多样性和氮循环动态的一个强大环境驱动因素。

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