[1] Orazinska D L, Bardgett R D, Blauw M B, et al. Relationships at the aboveground below ground interface: plants, soil biota, and soil processes[J]. Ecological Monographs,2003,73(3):377-395.
[2] Pablo L P, Vernica G, Pastur G M. Above-and belowground nutrients storage and biomass accumulation in marginal Nothofagus antarctica forests in Southern Patagonia[J]. Forest Ecology and Management,2008,255(7):2502-2511.
[3] 曾德慧,陈广生.生态化学计量学:复杂生命系统奥秘的探索[J]植物生态学报,2005,29(6):1007-1019.
[4] 贺金生,韩兴国.生态化学计量学:探索从个体到生态系统的统一化理论[J].植物生态学报,2010,34(1):2-6.
[5] 王绍强,于贵瑞.生态系统碳氮磷元素的生态化学计量学特征[J].生态学报,2008,28(8):3937-3947.
[6] 杨炳强,李大南.广西雅长细叶云南松分布区土壤的肥力特性[J].广西农学院学报,1988,7(3):27-33.
[7] 黄承标,冯昌林,李保平,等.广西雅长兰科植物分布区土壤理化性质[J].东北林业大学学报,2010(1):56-59.
[8] 张伟,陈洪松,王克林,等.桂西北喀斯特洼地土壤有机碳和速效磷的空间变异[J].生态学报,2007,27(12):5169-5175.
[9] 吴海勇,彭晚霞,宋同清,等.桂西北喀斯特人为干扰区植被自然恢复与土壤养分变化[J].水土保持学报,2008,22(4):143-147.
[10] Elser J J, Sterner R W, Gorokhova E, et al. Biological stoichiometry from genes to ecosystems[J]. Ecology Letters,2000,3(6):540-550.
[11] Elser J J, Acharya K, Kyle M, et al. Growth rate-stoichiometry couplings in diverse biota[J]. Ecology Letters,2003,6:936-943.
[12] Tessier J T, Raynal D J. Use of nitrogen to phosphorus ratios in plant tissue as indicator of nutrient limitation and nitrogen saturation[J]. Journal of Applied Ecology,2003,40:523-534.
[13] 高三平,李俊祥,徐明策,等.天童常绿阔叶林不同演替阶段常见种叶片NP化学计量学特征[J].生态学报,2007,27(3):947-952.
[14] 刘兴诏,周国逸,张德强,等.南亚热带森林不同演替阶段植物与土壤中N、P的化学计量特征[J].植物生态学报,2010,34(1):64-71.
[15] 刘万德,苏建荣,李帅锋,等.云南普洱季风常绿阔叶林演替系列植物和土壤C、N、P化学计量特征[J].生态学报,2010,30(23):6581-6590.
[16] 魏孝荣,邵明安.黄土高原沟壑区小流域坡地土壤养分分布特征[J].生态学报,2007,27(2):603-612.
[17] Chen J, Stark J M. Plant species effects and carbon and nitrogen cycling in a sagebrush crested wheatgrass soil[J]. Soil Biology＆Biochemistry,2000,32(1):47-57.
[18] 陈伏生,曾德慧,何兴元.森林土壤氮素的转化与循环[J].生态学杂志,2004,23(5):126-133.
[19] Cleveland C C, Townsend A R, Schmidt S K. Phosphorus limitation on microbial process in moist tropical forests：evidence from short-term laboratory incubation and field studies[J]. Ecosystems,2002,5(7):680-691.
[20] He Y Q, Zhu Y G, Smith S E, et al. Interactions between soil moisture content and phosphorus supply in spring wheat plants grown in pot culture[J]. Journal of Plant Nutrition,2002,25,913-925.
[21] Nilsson C, Xiong S, Johansson M E, et al. Effects of leaf-litter accumulation on riparian plant diversity across Europe[J]. Ecology,1999,80(5):1770-1775.
[22] Huttl R F, Schaa F W. Nutrient supply of forest soils in relation to management and site history[J]. Plant＆soil,1995,169(1):31-41.
[23] 阎恩荣,王希华,周武.天童常绿阔叶林不同退化群落的凋落物特征及与上壤养分动态的关系[J].植物生态学报,2008,32(1):1-12.
[24] 任书杰,曹明奎,陶波,等.陆地生态系统氮状态对碳循环的限制作用研究进展[J].地理科学进展,2006,25(4):58-67.
[25] Gang W, Jing W, Hong B D, et al. Nutrient cycling in an Alpine tundra ecosystem on Changbai Mountain, Northeast China[J]. Applied Soil Ecology,2006,32(2):199-209.
[26] 王绍强,于贵瑞.生态系统碳氮磷元素的生态化学计量学特征[J].生态学报,2008,28(8):3937-3947.
[27] 王维奇,仝川,曾从盛.不同质地湿地土壤碳、氮、磷计量学及厌氧碳分解特征[J].中国环境科学,2010,30(10):1130-1134.
[28] Aitkenhead J, Mcdowell W. Soil C/N ratio as a predictor of annual riverine DOC flux at local and global scales[J]. Global Biogeochemical Cycles,2000,14(1):127-138.
[29] Sterner R W, Elser J J. Ecological stoichiometry:the biology of elements from molecules to the biosphere[M]. Princeton:Princeton University Press,2002:906-907.
|
