Effects of microclimate on soil bacterial communities across two contrasting timberline ecotones in southeast Tibet | |
Yuan, Y. L.1; Si, G. C.1,2; Wang, J.1,3; Han, C. H.1,3; Zhang, G. X.1 | |
刊名 | EUROPEAN JOURNAL OF SOIL SCIENCE |
2015-11-01 | |
卷号 | 66期号:6页码:1033-1043 |
DOI | 10.1111/ejss.12292 |
文献子类 | Article |
英文摘要 | The Sergyemla Mountains have unique timberline patterns. Abies georgei var. smithii (Viguie & Gaussen) and Juniperus saltuaria (Rehder & E. H. Wilson) dominate the north-facing and south-facing slopes of a U-shaped valley, respectively. Although these two timberlines represent the world's highest natural tree lines, little is known about the structure of their soil bacterial communities and the factors that control them. To characterize and compare the soil bacterial communities of two timberline ecotones with different spatial orientations, we investigated their structures by terminal restriction fragment length polymorphism analysis and sequencing methods. We found that the structures of the soil bacterial communities differed significantly between the two opposite slopes, and the difference between the bacterial communities correlated primarily with soil carbon:nitrogen ratios. This probably relates to differences in the microclimate (mean soil temperature) between the two aspects in the world's highest timberline ecotones. In addition, the structures of soil bacterial communities also differed significantly with soil depth, and total nitrogen content had the greatest effect on the bacterial communities. In this region, soil temperature rather than mean annual precipitation has a major effect on the structures of soil bacterial communities. Microclimate differences (mainly differences in soil temperature) between the two opposite slopes might indicate that an amplitude increase of 2 degrees C in soil temperature could change the structures of soil bacterial communities by changing the status of soil carbon and nitrogen in these timberline ecotones. |
WOS关键词 | SERGYEMLA MOUNTAINS ; CLIMATE-CHANGE ; GLOBAL CHANGE ; DIVERSITY ; DEPTH ; TEMPERATURE ; PREDICTORS ; LANDSCAPE ; RESPONSES ; ARCHAEAL |
WOS研究方向 | Agriculture |
语种 | 英语 |
WOS记录号 | WOS:000364312500008 |
资助机构 | 973 Project from Science & Technology Department of China(2013CB956002) ; 973 Project from Science & Technology Department of China(2013CB956002) ; Knowledge Innovation Program of the Chinese Academy of Sciences(KZCX2-EW-112) ; Knowledge Innovation Program of the Chinese Academy of Sciences(KZCX2-EW-112) ; Natural Science Foundation of China(41471055) ; Natural Science Foundation of China(41471055) ; 973 Project from Science & Technology Department of China(2013CB956002) ; 973 Project from Science & Technology Department of China(2013CB956002) ; Knowledge Innovation Program of the Chinese Academy of Sciences(KZCX2-EW-112) ; Knowledge Innovation Program of the Chinese Academy of Sciences(KZCX2-EW-112) ; Natural Science Foundation of China(41471055) ; Natural Science Foundation of China(41471055) |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/62172] |
专题 | 地质与地球物理研究所_兰州油气中心 |
作者单位 | 1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Alpine Ecol & Biodivers, Beijing 100101, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources, Gansu Prov Key Lab Petr Resources Res, Lanzhou 730000, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
推荐引用方式 GB/T 7714 | Yuan, Y. L.,Si, G. C.,Wang, J.,et al. Effects of microclimate on soil bacterial communities across two contrasting timberline ecotones in southeast Tibet[J]. EUROPEAN JOURNAL OF SOIL SCIENCE,2015,66(6):1033-1043. |
APA | Yuan, Y. L.,Si, G. C.,Wang, J.,Han, C. H.,&Zhang, G. X..(2015).Effects of microclimate on soil bacterial communities across two contrasting timberline ecotones in southeast Tibet.EUROPEAN JOURNAL OF SOIL SCIENCE,66(6),1033-1043. |
MLA | Yuan, Y. L.,et al."Effects of microclimate on soil bacterial communities across two contrasting timberline ecotones in southeast Tibet".EUROPEAN JOURNAL OF SOIL SCIENCE 66.6(2015):1033-1043. |
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