文献类型：期刊文献

英文题名：Archaeal communities in the sediments of different mangrove stands at Dongzhaigang, China

作者：Li, Wei[1,2,3] Guan, Wei[4] Chen, Huai[1,2,3] Liao, Baowen[4] Hu, Ji[1,2,3] Peng, Changhui[5,6] Rui, Junpeng[1,2] Tian, Jianqing[7] Zhu, Dan[1,2,3] He, Yixin[1,2,3]

第一作者：Li, Wei

通信作者：Chen, H[1];Chen, H[2];Chen, H[3]

机构：[1]Chinese Acad Sci, Chengdu Inst Biol, Key Lab Mt Ecol Restorat & Bioresource Utilizat, Chengdu 610041, Peoples R China;[2]Chinese Acad Sci, Chengdu Inst Biol, Ecol Restorat Biodivers Conservat Key Lab Sichuan, Chengdu 610041, Peoples R China;[3]Chinese Acad Sci, Zoige Peatland & Global Change Res Stn, Hongyuan 624400, Peoples R China;[4]Chinese Acad Forestry, Res Inst Trop Forestry, Guangzhou 510520, Guangdong, Peoples R China;[5]Northwest A&F Univ, Lab Ecol Forecasting & Global Change, Yangling 712100, Peoples R China;[6]Univ Quebec, Inst Sci Environm, 201 President Kennedy, Montreal, PQ H2X 3Y4, Canada;[7]Chinese Acad Sci, Inst Microbiol, Beijing 100101, Peoples R China

年份：2016

卷号：16

期号：7

起止页码：1995-2004

外文期刊名：JOURNAL OF SOILS AND SEDIMENTS

收录：;Scopus(收录号：2-s2.0-84963771539);WOS:【SCI-EXPANDED(收录号:WOS:000378551000014)】；

基金：This study was supported by the 100 Talents Program of The Chinese Academy of Sciences, the External Cooperation Program of BIC, Chinese Academy of Sciences (No. 151751KYSB20130027), and the 1000 Talents Program of Sichuan Province of China and National Natural Science Foundation Item (31570480). The authors give special thanks to Ms. Wan Xiong for her editing and valuable comments on the manuscript.

语种：英文

外文关键词：Archaeal communities; Dongzhaigang mangrove; Miseq sequencing; Sediment

摘要：Purpose Knowledge of archaeal communities is essential for understanding of the mechanism of carbon and nitrogen cycle in the mangrove sediment ecosystem. Presently, little is known about archaeal communities in the Dongzhaigang mangrove sediments. This study aimed to characterize the archaeal communities in sediments of different mangrove stands and to find out the correlations between archaeal communities and the environmental factors of sediments. Materials and methods Sediment samples were collected from the Dongzhaigang mangrove forest for analysis of soil properties and archaeal communities, by national standard methods and Illumina Miseq archaeal 16S ribosomal RNA (rRNA) gene sequencing, respectively. Results and discussion The archaeal community in the Dongzhaigang mangrove forest was constituted by some phyla from "TACK" and "DPANN" supergroups, and dominated by Euryarchaeota. Among sediments of the four mangroves in Dongzhaigang, principal coordinates analysis (PCoA) scatter plot showed a trend of difference in the archaeal community structure in the Bruguiera gymnoihiza and Kandelia candel stands from that in the Laguncularia racemosa and Sonneratia apetala stands. The abundance of the order Methanosarcinales was the highest in the sediments of K. candel mangroves, whereas the order of Methanobacteriales dominated in B. gymnoihiza sediments. The highest richness and diversity values of Archaea occurred in K. candel sediments, while the lowest in B. gymnoihiza. Pearson correlation showed the significant relationships between sediment properties and some dominant genera, with a positive and significant correlation between sediment properties and genus Methanobacterium, coinciding with the maximum values of sediment properties and abundance of Methanobacterium in the sediment of B. gymnoihiza. Such results indicated that the difference of archaeal community structure among mangrove sediments may be caused by the different sediment characteristics. Methanogenic communities in the Dongzhaigang mangrove forest sediments were, at the order level, constituted by Methanobacteriales, Methanomicrobiales, Methanosarcinales, and Methanomassiliicoccales. Conclusions The investigation indicated that the Dongzhaigang mangrove sediment ecosystems support diverse archaeal communities and methanogenic communities, and that there was a general trend of difference in the archaeal community structure in the B. gymnoihiza and K. candel mangrove sediments from that in the L. racemosa and S. apetala sediments. Such difference may be caused by the difference in sediment characteristics.