[1] 中国科学院中国植物志编辑委员会.中国植物志[M].北京:科学出版社,1999:120.
[2] 刘迎春,刘琪璟,汪宏清,等.芒萁生物量分布特征[J].生态学杂志,2008,27(5):705-706.
[3] 李小飞,陈志彪,陈志强,等.南方红壤侵蚀区芒萁生长特征及其对环境因子的响应[J].水土保持通报,2013,33(3):33-37.
[4] 邓恢,林沁文,滕华卿,等.强度水土流失区芒萁生长规律分析[J].福建林学院学报,2004,24(3):262-26.
[5] 陈建.不同环境条件下芒萁群落生物量动态规律的研究[J].生态学杂志,1991,10(4):18-22.
[6] 管东生.香港草地、芒萁、灌木群落植物养分浓度和养分利用效率[J].中山大学学报:自然科学版,1998,37(2):167-171.
[7] 管东生.香港草地、芒萁、灌木群落的C素动态[J].生态学报,2001,21(3):440-445.
[8] 汪振立,魏正贵,陶冶,等.岩石-土壤-铁芒萁系统中稀土元素的分布、迁移和累积[J].地质通报,2002,21(2):881-889.
[9] Agren G I.The CNP stoichiometry of autotrophs-theory and observations[J].Ecology,2004(7):85-191.
[10] Wassen M J,Olde Venterink H G M,Swart Evalyne O A M.Nutrient concentrations in mire vegetation as a measure of nutrient limitation in mire ecosystems[J].Journal of Vegetation Science,1995,6(1):5-16.
[11] Harpole S W,Ngai J T,Cleland E E,et al.Nutrient co-limitation of primary producer communities[J].Ecology Letters,2011,14(9):852-862.
[12] Richardson S J,Allen R B,Docherty J E.Shifts in leaf N:P ratio during resorption reflect soil P in temperate rainforest[J].Functional Ecolory,2008,22(4):738-745.
[13] 平川,王传宽,全先奎.环境变化对兴安落叶松氮磷化学计量特征的影响[J].生态学报,2014,34(8),1965-1974.
[14] 洪江涛,吴建波,王小丹.全球气候变化对陆地植物碳氮磷生态化学计量学特征的影响[J].应用生态学报,2013,24(9):2658-2665.
[15] 任书杰,于贵瑞,陶波,等.中国东部南北样带654种植物叶片氮和磷的化学计量学特征研究[J]. 环境科学,2007,28(12):2666-2668.
[16] Wright I J,Reich P B,Westoby M,et al.The worldwide leaf economics spectrum[J].Nature,2004,428:821-827.
[17] Mason N W H,Richardson S J,Peltzer D A,et al.Changes in coexistence mechanisms along a long-term soil chronosequence revealed by functional trait diversity[J].Journal of Ecology,2012,100(3):678-689.
[18] 吴统贵,吴明,刘丽,等.杭州湾滨海湿地3种草本植物叶片N、P化学计量学的季节变化[J].植物生态学报,2010,34(1):23-28.
[19] Elser J J,Dobberfuhl D,Mackay N A,et al.Organism size,life history and N:P cycle[J].Biogeochemistry,1996,46(9):237-252.
[20] Kerkhoff A J,Fagan W F,Elser J J,et al.Phylogenetic and growth form variation in the scaling of nitrogen and phosphorus in the seed plants[J].American Naturalist,2006,168(4):E103-E122.
[21] Koerselman W,Meuleman A F M.The vegetation N:P ratio:a new tool to detect the nature of nutrient limitation[J].Journal of Applied Ecology,1996,33(6):1441-1450.
[22] 吴波波,郭建芬,吴君君,等.采伐剩余物对林地表层土壤生化特性和酶活性的影响[J].生态学报,2014,34(7):1645-1653.
[23] 庾强.内蒙古草原植物化学计量生态学研究[D].北京:中国科学院研究生院,2009.
[24] 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.
[25] Koerselman W,Meuleman A F M.The vegetation N:P ratio:a new tool to detect the nature of nutrient limitation[J].Journal of Applied Ecology,1996,33(6):1441-1450.
[26] 陈嘉茜,张玲玲,李炯,等.蕨类植物碳氮磷化学计量特征及其与土壤养分的关系[J].热带亚热带植物学报,2014,22(6):567-575.
[27] 丁凡,廉培勇,曾德慧.松嫩平原草甸三种植物叶片N、P化学计量特征及其与土壤N、P浓度的关系[J].生态学杂志,2011,30(1):77-81.
[28] Vitousek P M.Foliar and litter nutrients,nutrient resorption and decomposition in Hawaiian Metrosideros polymorpha[J].Ecosystems,1998,1(4):401-407.
[29] 陈建,钟章成.芒萁群落中营养元素的循环特点[J].生态学报,1991,11(4):299-306.
[30] Schreeg L A,Santiago L S,Wright S J,et al.Stem,root,and older leaf N:P ratios are more responsive indicators of soil nutrient availability than new foliage[J].Ecology,2014,95(8),2062-2068.