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在中国东北白浆土中,由大豆田转为水稻田后氨氧化古菌和细菌的群落结构和丰度变化。

Community structure and abundance of ammonia-oxidizing archaea and bacteria after conversion from soybean to rice paddy in albic soils of Northeast China.

机构信息

School of Marine Science and Engineering, Tianjin University of Science and Technology, Tianjin, 300457, People's Republic of China.

出版信息

Appl Microbiol Biotechnol. 2014 Mar;98(6):2765-78. doi: 10.1007/s00253-013-5213-2. Epub 2013 Oct 5.

DOI:10.1007/s00253-013-5213-2
PMID:24092004
Abstract

Community composition of ammonia-oxidizing archaea (AOA) and ammonia-oxidizing bacteria (AOB) in the albic soil grown with soybean and rice for different years was investigated by construction of clone libraries, denaturing gradient gel electrophoresis (DGGE), and quantitative polymerase chain reaction (q-PCR) by PCR amplification of the ammonia monooxygenase subunit A (amoA) gene. Soil samples were collected at two layers (0-5 and 20-25 cm) from a soybean field and four rice paddy fields with 1, 5, 9, and 17 years of continuous rice cultivation. Both the community structures and abundances of AOA and AOB showed detectable changes after conversion from soybean to rice paddy judged by clone library, DGGE, and q-PCR analyses. In general, the archaeal amoA gene abundance increased after conversion to rice cultivation, while bacterial amoA gene abundance decreased. The abundances of both AOA and AOB were higher in the surface layer than the bottom one in the soybean field, but a reverse trend was observed for AOB in all paddy samples regardless of the duration of paddy cultivation. Phylogenetic analysis identified nine subclusters of AOA and seven subclusters of AOB. Community composition of both AOA and AOB was correlated with available ammonium and increased pH value caused by flooding in multiple variance analysis. Community shift of AOB was also observed in different paddy fields, but the two layers did not show any detectable changes in DGGE analysis. Conversion from soybean to rice cultivation changed the community structure and abundance of AOA and AOB in albic agricultural soil, which requires that necessary cultivation practice be followed to manage the N utilization more effectively.

摘要

采用克隆文库、变性梯度凝胶电泳(DGGE)和实时定量 PCR(q-PCR)技术,对种植大豆和水稻不同年限的白浆土中氨氧化古菌(AOA)和氨氧化细菌(AOB)的群落组成进行了研究。通过扩增氨单加氧酶亚基 A(amoA)基因,对土壤样本进行了采集。从大豆田的两个土层(0-5 和 20-25 cm)和连续种植水稻 1、5、9 和 17 年的四个稻田采集了土壤样本。通过克隆文库、DGGE 和 q-PCR 分析,发现 AOA 和 AOB 的群落结构和丰度在从大豆田转为水稻田后发生了可检测的变化。总的来说,在转为水稻种植后,古菌 amoA 基因丰度增加,而细菌 amoA 基因丰度减少。在大豆田中,AOA 和 AOB 的丰度均在表层高于底层,但在所有稻田样本中,无论水稻种植年限如何,AOB 的丰度均呈相反趋势。系统发育分析确定了 9 个 AOA 亚群和 7 个 AOB 亚群。在多元方差分析中,AOA 和 AOB 的群落组成与有效铵和因淹水而升高的 pH 值相关。在不同的稻田中也观察到了 AOB 的群落变化,但在 DGGE 分析中,两个土层均未显示出任何可检测的变化。从大豆田转为水稻种植改变了白浆土中 AOA 和 AOB 的群落结构和丰度,这需要遵循必要的种植实践,以更有效地管理氮素利用。

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