[1] Sterner RW, Elser JJ. Ecological Stoichiometry: The Biology of Elements from Molecules to the Biosphere. Princeton: Princeton University Press, 2002 [2] Wang S-Q (王绍强), Yu G-R (于贵瑞). Ecological stoichiometry characteristics of ecosystem carbon, nitrogen and phosphorus element. Acta Ecologica Sinica (生态学报), 2008, 28(8): 3937-3947 (in Chinese) [3] Wright IJ, Reich PB, Westoby M, et al. The worldwide leaf economics spectrum. Nature, 2004, 428: 821-827 [4] McGroddy ME, Daufresne T, Hedin LO. Scaling of C:N:P stoichiometry in forests worldwide: Implications of terrestrial Redfield-type ratios. Ecology, 2004, 85: 2390-2401 [5] Yuan Z, Chen HY, Reich PB. Global-scale latitudinal patterns of plant fine-root nitrogen and phosphorus. Nature Communications, 2011, 2: 344 [6] Xu X, Thornton PE, Post WM. A global analysis of soil microbial biomass carbon, nitrogen and phosphorus in terrestrial ecosystems. Global Ecology and Biogeography, 2013, 22: 737-749 [7] Cleveland CC, Liptzin D. C:N:P stoichiometry in soil: Is there a ‘Redfield ratio’ for the microbial biomass? Biogeochemistry, 2007, 85: 235-252 [8] Ågren GI. Stoichiometry and nutrition of plant growth in natural communities. Annual Review of Ecology, Evolution, and Systematics, 2008, 39: 153-170 [9] Yang Y, Luo Y. Carbon:nitrogen stoichiometry in forest ecosystems during stand development. Global Ecology and Biogeography, 2011, 20: 354-361 [10] Zeng D-P (曾冬萍), Jiang L-L (蒋利玲), Zeng C-S (曾从盛), et al. Reviews on the ecological stoichiome-try characteristics and its applications. Acta Ecologica Sinica (生态学报), 2013, 33(18): 5484-5492 (in Chinese) [11] Ouyang X-J (欧阳学军), Huang Z-L (黄忠良), Zhou G-Y (周国逸), et al. Accumulative effects of forest community succession on soil chemical properties in Dinghushan of tropical China. Journal of Soil and Water Conservation (水土保持学报), 2003, 17(4): 51-54 (in Chinese) [12] Zhou Z-H (周正虎), Wang C-K (王传宽), Zhang Q-Z (张全智). The effect of land use change on soil carbon, nitrogen, and phosphorus contents and their stoichiometry in temperate sapling stands in northeastern China. Acta Ecologica Sinica (生态学报), 2015, 35(20): 6694-6702 (in Chinese) [13] Tischer A, Potthast K, Hamer U. Land-use and soil depth affect resource and microbial stoichiometry in a tropical mountain rainforest region of southern Ecuador. Oecologia, 2014, 175: 375-393 [14] Yang Y, Wang G, Shen H, et al. Dynamics of carbon and nitrogen accumulation and C:N stoichiometry in a deciduous broadleaf forest of deglaciated terrain in the eastern Tibetan Plateau. Forest Ecology and Management, 2014, 312: 10-18 [15] Murty D, Kirschbaum MU, Mcmurtrie RE, et al. Does conversion of forest to agricultural land change soil carbon and nitrogen? A review of the literature. Global Change Biology, 2002, 8: 105-123 [16] Xu X, Li D, Cheng X, et al. Carbon:nitrogen stoichio-metry following afforestation: A global synthesis. Scientific Reports, 2016, 6: 19117 [17] Smith CK, Coyea MR, Munson AD. Soil carbon, nitrogen, and phosphorus stocks and dynamics under disturbed black spruce forests. Ecological Applications, 2000, 10: 775-788 [18] Uhl C, Jordan CF. Succession and nutrient dynamics following forest cutting and burning in Amazonia. Ecology, 1984, 65: 1476-1490 [19] Kaye JP, Binkley D, Rhoades C. Stable soil nitrogen accumulation and flexible organic matter stoichiometry during primary floodplain succession. Biogeochemistry, 2003, 63: 1-22 [20] Knops JM, Tilman D. Dynamics of soil nitrogen and carbon accumulation for 61 years after agricultural abandonment. Ecology, 2000, 81: 88-98 [21] Yang Y, Luo Y, Finzi AC. Carbon and nitrogen dyna-mics during forest stand development: A global synthesis. New Phytologist, 2011, 190: 977-989 [22] Wardle DA, Jonsson M, Bansal S, et al. Linking vegetation change, carbon sequestration and biodiversity: Insights from island ecosystems in a long-term natural experiment. Journal of Ecology, 2012, 100: 16-30 [23] Persson H. The distribution and productivity of fine roots in boreal forests. Plant and Soil, 1983, 71: 87-101 [24] Warton DI, Wright IJ, Falster DS, et al. Bivariate line-fitting methods for allometry. Biological Reviews, 2006, 81: 259-291 [25] Li D, Niu S, Luo Y. Global patterns of the dynamics of soil carbon and nitrogen stocks following afforestation: A meta-analysis. New Phytologist, 2012, 195: 172-181 [26] Liu X-Z (刘兴诏), Zhou G-Y (周国逸), Zhang D-Q (张德强), et al. N and P stoichiometry of plant and soil in lower subtropical forest successional series in southern China. Chinese Journal of Plant Ecology (植物生态学报), 2010, 34(1): 64-71 (in Chinese) [27] Zhang Q-F (张庆费), Song Y-C (宋永昌), Qu W-H (由文辉). Relationship between plant community secondary succession and soil fertility in Tiantong, Zhejiang Province. Acta Ecologica Sinica (生态学报), 1999, 19(2): 174-178 (in Chinese) [28] Li H, Li J, He Y, et al. Changes in carbon, nutrients and stoichiometric relations under different soil depths, plant tissues and ages in black locust plantations. Acta Physiologiae Plantarum, 2013, 35: 2951-2964 [29] Kang B (康 冰), Liu S-R (刘世荣), Cai D-X (蔡道雄), et al. Soil physical and chemical characteristics under different vegetation restoration patterns in China south subtropical area. Chinese Journal of Applied Ecology (应用生态学报), 2010, 21(10): 2479-2486 (in Chinese) [30] Brais S, Camiré C, Paré D. Impacts of whole-tree harvesting and winter windrowing on soil pH and base status of clayey sites of northwestern Quebec. Canadian Journal of Forest Research, 1995, 25: 997-1007 [31] Mao R, Zeng DH, Hu YL, et al. Soil organic carbon and nitrogen stocks in an age-sequence of poplar stands planted on marginal agricultural land in Northeast China. Plant and Soil, 2010, 332: 277-287 [32] Chapin FS, Walker LR, Fastie CL, et al. Mechanisms of primary succession following deglaciation at Glacier Bay, Alaska. Ecological Monographs, 1994, 64: 149-175 [33] Jia GM, Cao J, Wang C, et al. Microbial biomass and nutrients in soil at the different stages of secondary forest succession in Ziwulin, Northwest China. Forest Ecology and Management, 2005, 217: 117-125 [34] Wei Q (魏 强), Ling L (凌 雷), Chai C-S (柴春山), et al. Soil physical and chemical properties in forest succession process in Xinglong Mountain of Gansu. Acta Ecologica Sinica (生态学报), 2012, 32(15): 4700-4713 (in Chinese) [35] Yang Y, Mohammat A, Feng J, et al. Storage, patterns and environmental controls of soil organic carbon in China. Biogeochemistry, 2007, 84: 131-141 [36] Pu X-Y (卜晓燕), Mi W-B (米文宝), Xu H (许浩), et al. Contents and ecological stoichiometry cha-racteristics of soil carbon, nitrogen and phosphorus in wetlands of Ningxia plain. Journal of Zhejiang University (Agriculture & Life Science) (浙江大学学报: 农业与生命科学版), 2016, 42(1): 107-118 (in Chinese) [37] Meng L-H (孟令涵), Zeng H (曾 辉), Xiong Y-M (熊燕梅), et al. Soil carbon, nitrogen and phosphorus contents and fine root biomass under different vegetation types and building densities in Shenzhen City. Acta Scientiarum Naturalium Universitatis Pekinensis (北京大学学报: 自然科学版), 2013, 49(5): 899-907 (in Chinese) [38] Rasse DP, Rumpel C, Dignac MF. Is soil carbon mostly root carbon? Mechanisms for a specific stabilisation. Plant and Soil, 2005, 269: 341-356 [39] Tian H, Chen G, Zhang C, et al. Pattern and variation of C:N:P ratios in China’s soils: A synthesis of observational data. Biogeochemistry, 2010, 98: 139-151 [40] Fan H, Wu J, Liu W, et al. Linkages of plant and soil C:N:P stoichiometry and their relationships to forest growth in subtropical plantations. Plant and Soil, 2015, 392: 127-138 [41] Jobbágy EG, Jackson RB. The distribution of soil nut-rients with depth: Global patterns and the imprint of plants. Biogeochemistry, 2001, 53: 51-77 |