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[湿润后风干森林土壤中微生物氨氧化菌的恢复]

[Restoration of microbial ammonia oxidizers in air-dried forest soils upon wetting].

作者信息

Zhou Xue, Huang Rong, Song Ge, Pan Xianzhang, Jia Zhongjun

出版信息

Wei Sheng Wu Xue Bao. 2014 Nov 4;54(11):1311-22.

Abstract

OBJECTIVE

This study was aimed to investigate the abundance and community shift of ammonia-oxidizing archaea (AOA) and bacteria (AOB) in air-dried forest soils in response to water addition, to explore the applicability of air-dried soil for microbial ecology study, and to elucidate whether AOA within the marine group 1. 1a dominate ammonia oxidizers communities in the acidic forest soils in China.

METHODS

Soil samples were collected from 10 forest sites of the China Ecosystem Research Network (CERN) and kept under air-drying conditions in 2010. In 2013 the air-dried soil samples were adjusted to 60% of soil maximum water holding capacity for a 28-day incubation at 28 degrees C in darkness. DGGE fingerprinting, clone library construction, pyrosequencing and quantitative PCR of amoA genes were performed to assess community change of ammonia oxidizers in air-dried and re-wetted soils.

RESULTS

After incubation for 28 days, the abundance of bacteria and archaea increased significantly, up to 3,230 and 568 times, respectively. AOA increased significantly in 8 samples, and AOB increased significantly in 5 of 10 samples. However, pyrosequencing of amoA genes reveals insignificant changes in composition of AOA and AOB communities. Phylogenetic analysis of amoA genes indicates that archaeal ammonia oxidizers were predominated by AOA within the soil group 1. 1b lineage, while the Nitrosospira-like AOB dominate bacteria ammonia oxidizer communities. There was a significantly positive correlation between AOA/AOB ratio and total nitrogen (r2 = 0.54, P < 0.05), implying that soil ammonia oxidation might be dominated by AOA in association with ammonium released from soil mineralization.

CONCLUSION

Phylogenetic analysis suggest that AOA members within the soil group 1. 1b lineage were not restricted to non-acidic soils as previously thought. The abundance rather than composition of AOA and AOB changed in response to water addition. This indicates that air-dried soil could be of help for microbial biogeography study.

摘要

目的

本研究旨在调查风干森林土壤中氨氧化古菌(AOA)和细菌(AOB)的丰度及群落变化对加水的响应,探讨风干土壤在微生物生态学研究中的适用性,并阐明海洋类群1.1a中的AOA是否在中国酸性森林土壤的氨氧化菌群落中占主导地位。

方法

从中国生态系统研究网络(CERN)的10个森林站点采集土壤样本,并于2010年保持在风干条件下。2013年,将风干的土壤样本调节至土壤最大持水量的60%,在28℃黑暗条件下培养28天。采用变性梯度凝胶电泳(DGGE)指纹图谱、克隆文库构建、焦磷酸测序和amoA基因定量PCR技术,评估风干和再湿润土壤中氨氧化菌的群落变化。

结果

培养28天后,细菌和古菌的丰度显著增加,分别高达3230倍和568倍。8个样本中的AOA显著增加,10个样本中有5个样本中的AOB显著增加。然而,amoA基因的焦磷酸测序显示AOA和AOB群落组成变化不显著。amoA基因的系统发育分析表明,土壤类群1.1b谱系中的AOA在古菌氨氧化菌中占主导地位,而类硝化螺菌属的AOB在细菌氨氧化菌群落中占主导地位。AOA/AOB比值与总氮之间存在显著正相关(r2 = 0.54,P < ),这意味着土壤氨氧化可能由与土壤矿化释放的铵相关的AOA主导。

结论

系统发育分析表明,土壤类群1.1b谱系中的AOA成员并不像之前认为的那样局限于非酸性土壤。AOA和AOB的丰度而非组成因加水而发生变化。这表明风干土壤有助于微生物生物地理学研究。

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