海拔梯度上高寒草甸土壤细菌功能多样性与环境因子的关系

doi:10.7523/j.issn.2095-6134.2013.05.008

中国科学院大学学报 ›› 2013, Vol. 30 ›› Issue (5): 620-627.DOI: 10.7523/j.issn.2095-6134.2013.05.008

海拔梯度上高寒草甸土壤细菌功能多样性与环境因子的关系

邓永翠¹, 吴静¹, 吴伊波², 杜岩功³, 张妍⁴, 崔骁勇¹

1. 中国科学院大学, 北京 100049;
2. 宁波大学, 浙江宁波 315211;
3. 中国科学院西北高原生物研究所, 西宁 810008;
4. 中国科学院地理科学与资源研究所, 北京 100101

收稿日期:2012-11-13 修回日期:2013-03-04 发布日期:2013-09-15
基金资助:
Supported by National Natural Science Foundation of China (11079053,31200367)

Soil bacterial diversity in relation to change in altitudinal environment in alpine meadow

DENG Yong-Cui¹, WU Jing¹, WU Yi-Bo², DU Yan-Gong³, ZHANG Yan⁴, CUI Xiao-Yong¹

1. University of Chinese Academy of Sciences, Beijing 100049, China;
2. Ningbo University, Ningbo 315211, Zhejiang, China;
3. Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Xining 810008, China;
4. Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China

Received:2012-11-13 Revised:2013-03-04 Published:2013-09-15
Contact: 崔骁勇,E-mail:cuixy@ucas.ac.cn
Supported by:
Supported by National Natural Science Foundation of China (11079053,31200367)

摘要/Abstract

摘要： 在青藏高原3200~3800 m的海拔梯度上,利用BIOLOG和冗余分析的方法,对细菌功能多样性和环境因子的关系进行了研究. 结果表明,碳氮磷等土壤的基本性质可以解释46.6%的细菌群落功能多样性的变化. 土壤中有效磷的贡献最大,它可能是青藏高原上限制土壤细菌功能多样性的一个重要因子. 由于海拔梯度变化而引起的土壤温度的变化,对细菌群落的功能多样性也有显著的影响.

关键词: 高寒草甸, BIOLOG, 冗余分析, 海拔, 有效磷

Abstract: Along an elevation gradient(3200 m to 3800 m) on Qinghai-Tibetan plateau, BIOLOG GN2 plates were used to analyze the elevation patterns of bacterial community functional diversity. The redundancy analysis (RDA) method was further used to analyze the relationship between bacterial profiles and the environmental variables. The results indicate that soil variables explain 46.6% of the variation in bacterial community functional diversity. Among the soil variables, soil available phosphorus explains the largest part, which suggests that it might be an important limiting factor for soil bacterial community functional diversity in this area. The soil temperature, which changes with the altitute, also has a profound effect on bacterial community functional diversity.

Key words: alpine meadow, BIOLOG, RDA, elevation, available phosphorus

中图分类号:

S714.3

邓永翠, 吴静, 吴伊波, 杜岩功, 张妍, 崔骁勇. 海拔梯度上高寒草甸土壤细菌功能多样性与环境因子的关系[J]. 中国科学院大学学报, 2013, 30(5): 620-627.

DENG Yong-Cui, WU Jing, WU Yi-Bo, DU Yan-Gong, ZHANG Yan, CUI Xiao-Yong. Soil bacterial diversity in relation to change in altitudinal environment in alpine meadow[J]. , 2013, 30(5): 620-627.

参考文献

[1] Cramer W, Bondeau A, Woodward F I, et al. Global response of terrestrial ecosystem structure and function to CO₂ and climate change: results from six dynamic global vegetation models[J]. Global Change Biology,2001, 7(4):357-373.
[2] Weltzin J F, Bridgham S D, Pastor J, et al. Potential effects of warming and drying on peatland plant community composition[J]. Global Change Biology,2003, 9(2):141-151.
[3] Hu Y, Chang X, Lin X, et al. Effects of warming and grazing on N₂O fluxes in an alpine meadow ecosystem on the Tibetan plateau[J]. Soil Biology & Biochemistry,2010, 42:944-952.
[4] Zhang W, Parker K M, Luo Y, et al. Soil microbial responses to experimental warming and clipping in a tallgrass prairie[J]. Global Change Biology,2005, 11(2):266-277.
[5] Butler S M, Melillo J M, Johnson J E, et al. Soil warming alters nitrogen cycling in a New England forest: implications for ecosystem function and structure[J]. Oecologia, 2012, 168(3):819-828.
[6] Rinnan R, Stark S, Tolvanen A. Responses of vegetation and soil microbial communities to warming and simulated herbivory in a subarctic heath[J]. Journal of Ecology, 2009, 97(4):788-800.
[7] Fierer N, McCain C M, Meir P, et al. Microbes do not follow the elevational diversity patterns of plants and animals[J]. Ecology, 2011, 92(4):797-804.
[8] Liu Z, Fu B, Zheng X, et al. Plant biomass, soil water content and soil N:P ratio regulating soil microbial functional diversity in a temperate steppe: A regional scale study[J]. Soil Biology & Biochemistry,2010, 42(3):445-450.
[9] Sundqvist M K, Giesler R, Graae B J, et al. Interactive effects of vegetation type and elevation on aboveground and belowground properties in a subarctic tundra[J]. Oikos, 2011, 120(1):128-142.
[10] Dunne J A, Saleska S R, Fischer M L, et al. Integrating experimental and gradient methods in ecological climate change research[J]. Ecology, 2004, 85(4):904-916.
[11] Hu Q W, Cao G M, Wu Q, et al. Comparative study on CO₂ emissions from different types of alpine meadows during grass exuberance period[J]. Journal of Geographical Sciences,2004, 14(2):167-176.
[12] Garland J L, Mills A L. Classification and characterization of heterotrophic microbial communities on the basis of patterns of community-level sole-carbon-source utilization[J]. Applied and Environmental Microbiology, 1991, 57(8):2351-2359.
[13] Preston-Mafham J, Boddy L, Randerson P F. Analysis of microbial community functional diversity using sole-carbon-source utilisation profiles-a critique[J]. FEMS Microbiology Ecology,2002, 42(1):1-14.
[14] Kaufmann K, Christophersen M, Buttler A, et al. Microbial community response to petroleum hydrocarbon contamination in the unsaturated zone at the experimental field site Vœrlψse, Denmark[J]. FEMS Microbiology Ecology, 2004, 48(3):387-399.
[15] Bryant J A, Lamanna C, Morlon H, et al. Microbes on mountainsides: contrasting elevational patterns of bacterial and plant diversity[J]. PNAS, 2008, 105:11505.
[16] Singh D, Takahashi K, Kim M, et al. A Hump-backed trend in bacterial diversity with elevation on mount Fuji, Japan[J]. Microbial Ecology, 2012, 63(2):429-437.
[17] Körner C. The use of 'altitude’ in ecological research[J]. Trends in Ecology & Evolution, 2007, 22(11):569-574.
[18] Rowe R J, Lidgard S. Elevational gradients and species richness: do methods change pattern perception[J]? Global Ecology and Biogeography, 2009, 18(2):163-177.
[19] Baudoin E, Benizri E, Guckert A. Impact of artificial root exudates on the bacterial community structure in bulk soil and maize rhizosphere[J]. Soil Biology & Biochemistry,2003, 35(9):1183-1192.
[20] Wu Y, Tan H, Deng Y, et al. Partitioning pattern of carbon flux in a Kobresia grassland on the Qinghai-Tibetan Plateau revealed by field 13C pulse-labeling[J]. Global Change Biology,2010, 16(8):2322-2333.
[21] Jackson R B, Canadell J, Ehleringer J R, et al. A global analysis of root distributions for terrestrial biomes[J]. Oecologia,1996, 108(3):389-411.
[22] Hirota M, Zhang P, Gu S, et al. Altitudinal variation of ecosystem CO₂ fluxes in an alpine grassland from 3600 to 4200 m[J]. Journal of Plant Ecology, 2009, 2(4):197-205.
[23] Schindlbacher A, Rodler A, Kuffner M, et al. Experimental warming effects on the microbial community of a temperate mountain forest soil[J]. Soil Biology & Biochemistry,2011, 43(7):1417-1425.
[24] Zhou J Z, Xue K, Xie J P, et al. Microbial mediation of carbon-cycle feedbacks to climate warming[J]. Nature Climate Change, 2012, 2(2):106-110.
[25] Sowerby A, Emmett B, Beier C, et al. Microbial community changes in heathland soil communities along a geographical gradient: interaction with climate change manipulations[J]. Soil Biology & Biochemistry,2005, 37(10):1805-1813.
[26] Blankinship J C, Niklaus P A, Hungate B A. A meta-analysis of responses of soil biota to global change[J]. Oecologia, 2011, 165(3):553-565.
[27] Ma X, Chen T, Zhang G, et al. Microbial community structure along an altitude gradient in three different localities[J]. Folia Microbiologica,2004, 49(2):105-111.
[28] Chen M M, Zhu Y G, Su Y H, et al. Effects of soil moisture and plant interactions on the soil microbial community structure[J]. European Journal of Soil Biology, 2006, 43(2007):31-38.
[29] Williams M A, Rice C W. Seven years of enhanced water availability influences the physiological, structural, and functional attributes of a soil microbial community[J]. Applied Soil Ecology,2007, 35(3):535-545.
[30] Fierer N, Jackson R B. The diversity and biogeography of soil bacterial communities[J]. PNAS,2006, 103(3):626-631.
[31] Wardle D A, Walker L R, Bardgett R D. Ecosystem properties and forest decline in contrasting long-term chronosequences[J]. Science, 2004, 305(5683):509-513.
[32] Chapin III F S. Effects of multiple environmental stresses on nutrient availability and use. In: Response of plants to multiple stresses[M]. San Diego: Academic Press, 1991:67-88.
[33] Elser J J, Bracken M E S, Cleland E E, et al. Global analysis of nitrogen and phosphorus limitation of primary producers in freshwater, marine and terrestrial ecosystems[J]. Ecology Letter,2007, 10(12):1135-1142.
[34] [ZK(]Cao G M, Zhang J X, Bao X K, et al. The phosphorus cycling in an alpine meadow ecosystem[J]. Acta Ecologica Sinica, 1999, 19(4):514-518(in Chinese).曹广民,张金霞,鲍新奎,等. 高寒草甸生态系统磷素循环[J]. 生态学报, 1999, 19(4):514-518.[ZK)]
[35] Sundareshwar P, Morris J, Koepfler E, et al. Phosphorus limitation of coastal ecosystem processes[J]. Science, 2003, 299(5606):563-565.
[36] Cleveland C C, Townsend A R, Schmidt S K. Phosphorus limitation of microbial processes in moist tropical forests: evidence from short-term laboratory incubations and field studies[J]. Ecosystems, 2002, 5(7):680-691.

海拔梯度上高寒草甸土壤细菌功能多样性与环境因子的关系

Soil bacterial diversity in relation to change in altitudinal environment in alpine meadow

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 4

编辑推荐

Metrics

本文评价

访问统计

联系我们

[1]	崔骁勇, 杨以宁. “梯度”在中国生态学中的使用考辨[J]. 中国科学院大学学报, 2019, 36(6): 760-765.
[2]	李框宇, 周梅, 陈玖英, 潘苗苗, 李传荣, 唐伶俐. 一种适用于气温空间插值的改进梯度距离平方反比法[J]. 中国科学院大学学报, 2019, 36(4): 491-497.
[3]	何海勇, 齐鑫, 石元亮. 水热条件下磷矿粉活化条件的筛选[J]. 中国科学院大学学报, 2013, 30(6): 845-850.
[4]	易现峰. 两个不同海拔地区珠芽蓼抗氧化系统的比较研究(英文)[J]. 中国科学院大学学报, 2003, 20(2): 172-176.