模拟氮沉降对中亚热带杉木幼树根系生物量的影响

植物根系是全球陆地生态系统碳储量的重要组成部分,在全球生态系统碳循环中起着重要作用,日益加剧的氮沉降会影响根系生物量在空间和不同径级的分配,进而影响森林生态系统的生产力和土壤养分循环。以杉木幼树为研究对象,通过野外氮沉降模拟实验,研究氮沉降四年后对不同土层、不同径级根系生物量的影响。结果发现：（1）低氮和高氮处理总细根生物量较对照均无显著差异（P > 0.05）,高氮处理粗根生物量及总根系生物量较对照分别增加45%和40%（P < 0.05）;（2）与对照相比,施氮处理显著增加20-40 cm与40-60 cm土层细根和粗根生物量,且在低氮处理下,20-40 cm土层细根、粗根在总土层细根与粗根生物量的占比显著提高。（3）与对照相比,高氮处理显著增加了2-5 mm、5-10 mm及10-20 mm径级的根系生物量,低氮处理显著增加2-5 mm、5-10 mm径级根系生物量,且显著降低20-50 mm径级根系生物量。综上所述表明：氮沉降后杉木幼树通过增加较粗径级根系来增加对养分及水分的输送,同时通过增加深层根系生物量及其比例的策略来维持杉木幼树的快速生长;而根系生物量的增加,在一定程度上会增加根系碳源的输入,影响土壤碳循环过程。     

模拟氮沉降对低磷胁迫下马尾松不同家系根系分泌和磷效率的影响

近年来大气氮(N)沉降的增加, 导致森林土壤中有效N含量增加、N:P发生改变, 研究N沉降对低磷(P)胁迫下林木根系分泌和P效率的影响具有重要意义。该文以马尾松(Pinus massoniana)家系作为试验材料, 设置模拟N沉降与同质低P (介质表层与深层均缺P)、异质低P (介质表层P丰富、深层缺P)耦合的二年生盆栽实验, 系统研究了模拟N沉降对低P胁迫下马尾松根系分泌性酸性磷酸酶(APase)活性、有机酸分泌以及P效率的影响。结果表明: (1)同质低P和异质低P下, 模拟N沉降均显著提高了植株N:P化学计量比、增加了P素的相对匮乏程度, 从而诱导根系增加了APase和有机酸的分泌, 而同质低P比异质低P下增加幅度更大, 其中有机酸分泌均与马尾松生长呈正相关关系, 而APase活性与P效率相关性较小; (2)同质低P下, N沉降虽然增加了根系分泌, 但未提高马尾松P素吸收和生长量, 其原因在于, 同质低P下植株N:P过高, 因而植株对N沉降敏感性低; 在异质低P下, 植株表现为N、P共同限制, 因而对N敏感性较高, N沉降增加了根系分泌, 同时提高了N和P吸收效率、增加了生物量; (3)马尾松根系分泌对模拟N沉降的响应存在较大的家系差异。同质低P下, 家系71×20的有机酸分泌和生物量对N沉降的响应幅度较大; 异质低P下, 家系36×29、71×20和73×23对N沉降的响应幅度较大。     

低磷胁迫下不同种源马尾松的根构型与磷效率

以浙江淳安、福建武平、广西岑溪和广东信宜4个代表性的马尾松种源为试材,设置异质低磷胁迫、同质低磷胁迫等不同磷素处理,研究马尾松种源感知不同类型低磷胁迫的根构型及磷效率变异规律.结果表明:无论在异质低磷还是同质低磷胁迫下,参试种源马尾松的主要生长性状和磷效率指标均存在极显著的种源间变异.异质低磷胁迫下,广东信宜、福建武平种源马尾松表现出较高的磷效率和干物质积累量,根构型发生适应性变化,富磷表层介质中的根系参数显著高于低磷效率的广西岑溪和浙江淳安种源.这是磷高效种源具有较高的磷素吸收效率和磷效率的重要机制.不同种源的表层富磷介质根系参数与其整株干物质积累量相关系数在0.95以上.同质低磷胁迫下,高磷效率种源马尾松的磷吸收率显著高于低磷效率种源,但表层介质中的根系参数和整株根系参数与整株干物质积累量的相关性较低.不同种源马尾松适应同质低磷胁迫和异质低磷胁迫的生物学机制有所差异,应有针对性地选择不同土壤磷素的森林立地并推广磷营养高效的马尾松种源.     

模拟氮沉降对华西雨屏区苦竹林细根特性和土壤呼吸的影响

细根在森林生态系统地下碳循环过程中具有核心地位.2007年11月-2009年11月,对华西雨屏区苦竹人工林进行了模拟氮沉降试验.氮沉降水平分别为对照(CK,0 g N·m^-2·a^-1)、低氮(5 g N·m^-2·a^-1)、中氮(15 g N·m^-2·a^-1)和高氮(30 g N·m^-2·a^-1)处理,研究氮沉降对苦竹人工林细根和土壤根际呼吸的影响.结果表明：不同处理氮沉降下,<1 mm和1～2 mm细根特性差异较大,与< 1 mm细根相比,1～2 mm细根的木质素、磷和镁含量更高,而纤维素、钙含量更低;氮沉降显著增加了<2 mm细根生物量,对照、低氮、中氮和高氮处理的细根生物量分别为(533±89)、(630±140)、(632±168)和(820±161) g·m^-2,氮、钾、镁元素含量也明显增加;苦竹林各处理年均土壤呼吸速率分别为(5.85±0.43)、(6.48±0.71)、(6.84±0.57)和(7.62±0.55) t C·hm^-2·a^-1,氮沉降对土壤呼吸有明显的促进作用;苦竹林的年均土壤呼吸速率与<2 mm细根生物量和细根N含量呈极显著线性相关.氮沉降使细根生物量和代谢强度增加,并通过增加微生物活性促进了根际土壤呼吸.     

施氮对木荷3个种源幼苗根系发育和氮磷效率的影响

以浙北、闽北和赣南3个木荷有代表性的种源作为试验材料,通过人工控制施氮来研究氮沉降对林地贫瘠土壤上木荷幼苗生长和氮磷效率的影响.实验分为4个处理组,分别人工喷施NH4NO3溶液0、50、100和200 kg N hm-2·a-1.结果表明:氮沉降对木荷幼苗生长产生了不同程度的促进作用.木荷幼苗根系干物质重、总长、平均直径、根总表面积和总体积增加了33％-73％,其中＞0.5mm直径的根系生长最为显著,根系呈粗壮舒张型.随氮水平的提高,氮磷吸收效率与根系总长、根系体积、根系平均直径和总表面积相关性增强.在中氮水平下,木荷幼苗根系氮吸收效率受＞0.5mm根长的作用显著,而磷吸收效率与≤0.5mm,0.5-1.0mm和≥1.0mm 3种直径根系根长均显著相关.木荷种源间差异显著,福建建瓯种源根系发达,氮磷的利用效率更高,低氮水平对其根系生长促进作用显著;浙江杭州种源在低氮水平下,地上部分生长促进作用显著,苗高和地径较对照分别增长34％和26％,而根系生长发育迟缓,对氮素响应迟钝;低氮促进江西信丰种源整体增长,但随氮水平提高,地下部生长抑制加强.     

局部供氮对低磷胁迫下马尾松不同家系生长及根系参数的影响

土壤资源有效性在空间分布上的差异会对植物的生长发育产生重要影响。该文选择马尾松(Pinus massoniana)二代育种亲本育成的5个全同胞家系(1、25、49、52、57)为材料,进行一个生长季的局部供氮苗木盆栽实验。实验在同质低磷和异质低磷两种低磷环境下分别设置4个供氮处理:均匀供氮(HHH)、表层和中间层供氮(HHL)、底层供氮(LLH)和底层半侧供氮(LLH/L),研究了模拟异质养分环境对马尾松不同家系苗木生长及根系发育的影响。结果表明:1)与同质低磷相比,异质低磷促进了马尾松的生长和根系发育,其根长和根表面积分别为同质低磷下的1.95倍和2.11倍。2)局部供氮对马尾松生长的影响受土壤磷素环境影响较大,与HHH相比,局部供氮(HHL、LLH和LLH/L)对同质低磷下苗木的株高、地径和干物质积累量有明显的促进作用,但在异质低磷下,仅LLH和LLH/L处理有利于苗木地上部分的生长,HHL处理反而有抑制效应。3)在两种低磷环境下,LLH/L和LLH处理对马尾松苗木根系生长发育的促进作用显著,尤其在异质低磷环境下的促进作用较强(LLH/L处理下根长和根表面积较HHH处理高出29.2%和32.3%),但HHL对根长和根表面积有一定的抑制作用。4)马尾松不同家系间对不同供氮处理的响应差异显著。家系49、52和57主要通过增加根系在土壤中的分布来响应局部氮素分布的变化,促进整株干物质量的积累;家系25地上部分的生长随氮、磷含量的增大而增加,但根系的增生发育对其整株生长的贡献较小;家系1生长发育迟缓,对局部供氮的响应较为迟钝。研究结果显示,局部供氮较均匀供氮更有利于马尾松苗木生长,且土壤深层施肥的促进作用更强。     

模拟氮沉降对低磷胁迫下马尾松生长和磷效率的影响

近年来大气N沉降日趋严重,导致森林土壤有效N含量增加,N/P发生改变,将会影响低P胁迫下林木的生长发育和P效率.本文以马尾松家系为研究对象,设置模拟N沉降与同质低P(介质表层与深层均缺P)、异质低P(介质表层P丰富、深层缺P)耦合的盆栽试验,研究N沉降对马尾松生长性状以及P吸收和利用效率的影响.结果表明： 同质低P下,模拟N沉降对马尾松生长性状和P效率影响较小,但存在显著的N×家系互作效应,家系40×44和71×20在N沉降后生物量增加,家系36×29和73×23生物量降低;异质低P下,模拟N沉降显著增加了马尾松苗高、生物量以及P吸收效率等,其原因是促进了根系生长和表层土壤中根系分布比例的增加.不同P环境下模拟N沉降对马尾松生长的影响,还与植株N/P有关.同质低P环境下,马尾松植株N/P为13.8,植株对N敏感性低,酸性磷酸酶活性增加,但未改善马尾松生长状况.在异质低P环境中,植株N/P为9.7,模拟N沉降显著增加了苗木生物量和P吸收效率,但未显著改变酸性磷酸酶活性.     

不同分类系统下油松幼苗根系特征的差异与联系

植物根序和径级不仅反映细根的形态结构, 而且能反映根系的一些生理特征, 如细根寿命和周转等。该文以二年生油松(Pinus tabulaeformis)幼苗根系为研究对象, 系统比较了根序分类方法和径级分类方法在描述根系特征上的优缺点, 探索了两者之间的内在联系。结果表明: 二年生油松幼苗最多可包括6级根序, 直径的变化范围为0.169-3.877 mm。按根序划分, I-VI级根序的总根长和总根表面积主要集中在前3级根序, 这3级根序的根占总根长的78.77%和总根表面积的62.72%。前3级根序的比根长是后3级根序比根长的1.3-3.0倍, 比根面积是后3级比根面积的1.0-1.5倍。按常用的径级(以0.5、1.0、1.5和2.0 mm为阈值)划分方法, 油松幼苗大部分根系直径≤1.5 mm, 此区间细根的根长和根表面积占总根长的93.76%和总根表面积的84.35%。直径≤1.5 mm的细根平均比根长是>1.5 mm细根比根长的3-7倍, 比根面积的1.5-3.0倍。由于油松根序和径级之间有显著的指数关系, 依据径级最大程度反映根序的原则, 提出了新的径级划分方法, 即以0.4、0.8、1.3和2.0 mm为阈值对油松幼苗根系径级重新进行划分。此时, 上述区间可分别包括I级、II级、III级、IV级、V级根序中根尖数的93.22%、86.37%、75.96%、70.47%和76.67%。同时也可分别涵盖各径级根长的89.34%-70.83%、根面积的86.01%-76.12%以及体积的87.73%-76.12%。此时, 根系不同径级与根序之间可以建立起良好的对应关系。这些结果表明, 通过合理划分径级区间可以较好地反映根序 特征。     

增温下土壤资源异质分布对杉木幼苗生长的影响

在福建三明森林生态系统与全球变化研究站陈大观测点开展大气温度控制、土壤温度控制和土壤资源分布3因子试验,探讨土壤资源异质分布和增温对杉木幼苗地下和地上生长的影响,以及增温是否能改变杉木幼苗细根对土壤资源异质分布的识别度,以明确杉木人工林在全球变暖背景下对土壤资源异质分布的响应.结果表明:杉木对土壤资源异质分布的识别度主要体现在吸收根(0~1 mm径级)上,而1~2 mm径级细根则不具有识别度.除了单独大气增温处理对杉木1~2 mm径级细根的避贫系数具有显著影响外,不同增温处理均未对杉木幼树细根的贫富比、趋富系数和避贫系数产生显著影响.与土壤资源均质分布相比,土壤资源异质分布增加了0~1 mm径级细根生物量,降低了树高.与无大气增温相比,大气增温降低了0~1和0~2 mm径级细根生物量,增加了树高.与无土壤增温相比,土壤增温降低了1~2 mm径级细根生物量,但增加了树高和侧枝长度.大气增温控制、土壤增温控制和土壤资源异质分布对杉木地下、地上生长都无显著交互作用.杉木幼苗吸收根本身对土壤资源异质分布具有识别度,但增温并不会改变杉木幼苗细根对土壤资源异质分布的识别度.     

不同林龄杨树细根生物量分配及其对氮沉降的响应

氮沉降已经成为全球变化背景下的热点问题,并呈现逐渐加重趋势,了解森林生态系统对这种持续氮增长和快速氮循环的响应模式及反馈机制,对于维护森林生态系统健康具有重要的理论意义。本研究选择不同林龄杨树人工林作为试验样地,设置N0(0 g N·m-2·a-1)、N1(5 g N·m-2·a-1)、N2(10 g N·m-2·a-1)、N3(15 g N·m-2·a-1)、N4(30 g N·m-2·a-1)5个不同浓度,进行氮沉降野外模拟实验,探讨不同林龄杨树人工林细根生物量的垂直分布及对模拟氮沉降的响应。结果表明:(1)70%~80%细根生物量分配在0~20 cm土层,呈现表层富集特征;外源氮增加后,幼龄林(4年生)中,0~10 cm土层细根生物量所占比例有所增加,而中龄林(8年生)和成熟林(15年生)则不同程度的减少;(2)细根生物量主要分布在0~0.5和0.5~1.0 mm径级,其中0~0.5 mm径级细根约占总细根(2.0 mm)生物量的50%,外源氮输入增加极小径级(0~0.5 mm)的根系生物量,特别是幼龄林;(3)30~40 cm土层中,成熟林0~0.5 mm细根生物量分配量远大于幼龄林和中龄林,表明随着林龄的增加,小直径细根有向下分配趋势;(4)林龄、土层、径级以及施氮浓度4个因素的综合效应能够解释细根生物量66.3%的变异,其中林龄、土层、径级3个因素各自对细根生物量的影响极显著(P0.01),分别能解释细根生物量17.6%、16.1%、10.4%的变异,而增氮处理仅能解释细根生物量0.24%的变异,影响效应不显著(P0.05)。     

Effects of simulated nitrogen deposition on fine root morphology,nitrogen and phosphorus efficiency of Pinus massoniana clone under phosphorus deficiency

Aims In forest ecosystems with phosphorus (P) deficiency, the impact of atmospheric nitrogen (N) deposition on nutritional traits related to N and P uptake potentially affect plant growth and vegetation productivity. The objective of this study was to explore the effects of simulated N deposition on fine root morphological characteristics and effiency of N and P absorption in Pinus massoniana under under low P stress.
Methods Two clones of P. massoniana seedling with different P efficiency (high P efficiency 19-5 vs. low P efficiency 21-3) were used. A two-year pot experiment was applyed with treatments of two P conditions, (i.e. homogeneous low P availability vs. heterogeneous low P availability) and three N deposition levels (0, 30 and 120 kg N·hm^-2·a^-1; i.e., N0, N30, or N120, respectively) .
Important findings 1) The growth of P. massoniana seedling was interactively affected the three factors: simulated N deposition, P condition and genotypes. Simulated N deposition increased the seedling height and dry mass under heterogeneous P deficiency, but did not significantly affect those traits under homogeneous P deficiency. Under heterogeneous P deficiency and N120 treatment, the seedling height and dry mass of clone 19-5 were 1.1 times and 1.6 times higher than that of clone 21-3, respectively. 2) Fine root length and surface area decreased as root diameter increased. N deposition significantly stimulated proliferation of fine root with diameter ≤1.5 mm, while roots with diameters ranged from 1.5 to 2.0 mm and over 2.0 mm were not influenced. The length of fine root ≤1.5 mm in diameter accounted for 90.4%-92.8% of the total root length and was not affected by N deposition. 3) Under the heterogeneous low P condition, clone 19-5 was found to respond to the simulated N deposition with increased root length and surface area in fine-root diameter class of ≤1.5 mm. Additionally, in compared with control, its N and P absorption efficiency were significantly enhanced 93.3% and 148.4%, respectively under N120 treatment. However, the N and P absorption efficiency of clone 21-3 was less affected by the simulated N deposition. The N and P use efficiency had no notable variation. Finally, we found that the proliferation of fine-root ≤1.5 mm in diameter and high N (P) absorption efficiency maybe the adaptive mechanisms of P. massoniana responding to atmospheric N deposition under P deficiency.     

Effects of localized nitrogen supply treatments on growth and root parameters in Pinus massoniana families under phosphorus deficiency

Aims A heterogeneous spatially distribution of nutrients in natural soil may affect plant growth. The objective of this study was to determine the effects of localized nitrogen (N) supply treatments on growth traits and root parameters among different families in Pinus massoniana.Methods Five families of P. massoniana seedlings from full-sib progenies were used as test materials (1, 25, 49, 52, and 57). This study included two conditions, (i.e. homogeneous phosphorus (P) deficiency vs. heterogeneous P efficiency) among soil layers in combination with four N supply treatments in a one-year pot experiment. These N supply treatments were: (1) Homogeneously high N along the soil profile (HHH); (2) high N-high N-low N (HHL); (3) low N-low N-high N (LLH); (4) low N-low N-on side with N addition and the other side without N supply (LLH/L).Important findings This study indicated that localized N supply treatment did enhance the growth of P. massoniana, and this enhancement mainly happened in the pattern of N applied to deep soil. The results showed: 1) Compared to the homogeneous low P condition, there were increase in the growth traits and root parameters of P. massoniana under heterogeneous low P condition. Particularly, the root length and root surface area under the heterogeneous P deficiency condition were 1.95 times and 2.11 times higher than that subjected to the homogeneous P deficiency. 2) Localized N supply treatment affected seedling growth, and there was a significant interaction among N supply pattern and P condition. In compared with homogeneous N supply treatment, the height, basal diameter and dry weight of seedlings increased significantly by localized N supply treatments (LLH and/or LLH/L) under both two P deficiency conditions. But when the seedlings parameters were enhanced under homogeneous P deficiency, they were inhibited under heterogeneous P deficiency subjected to HHL. 3) Within the two P conditions, LLH and LLH/L stimulated root proliferation significantly, and root parameters were significantly enhanced under the heterogeneous P deficiency condition. Specifically, the root length and root surface area subjected to LLH/L rather than HHH were significantly enhanced by 29.2% and 32.3%, respectively. However, the length and surface area of the roots were suppressed by HHL treatment. 4). There were significant differences in response to different N supply treatments among P. massoniana families Seedlings in the families of 49, 52, and 57 responded to the localized N supply treatments with increased root proliferation, which enhanced seedling dry mass. On the other hand, the seedling growth in the family of 25 were stimulated by N and (or) P concentration, while the response of seedlings in the family of 1 to local nitrogen supply was relatively slow and exhibited growth retardation.     

Edge effects of forest gap in Pinus massoniana plantations on the ecological stoichiometry of Cinnamomum longepaniculatum

Aims Pinus massoniana is one of the major plantation tree species in the low hilly lands along the upper reaches of the Yangtze River Valley in China’s “Grain for Green” project. The objective of this study was to explore the edge effects of forest gap on the ecological stoichiometry of dominant tree species in a P. massoniana plantation forest.Methods We collected Cinnamomum longepaniculatum leaves in a 39-year-old P. massoniana plantation forest with seven forest gap sizes (G1: 100 m²; G2: 225 m²; G3: 400 m²; G4: 625 m²; G5: 900 m²; G6: 1 225 m²; G7: 1 600 m², and the control: closed canopy) located in Gao County, south Sichuan Province during different seasons. The contents of C, N and P in leaves were measured, and the effects of edges, seasons and their interaction on leaf C, N and P contents and C:N:P stoichiometry were evaluated.Important findings The leaf C content, C:N and C:P of C. longepaniculatum at the edge of forest gaps in different seasons were all significantly higher than those of understory plants in P. massoniana plantation. With increasing size of forest gaps, leaf C content and C:N ratio, C:P and N:P of C. longepaniculatum increased initially and then decreased with the maximum at medium size (400-900 m²). From spring to winter, leaf N and P contents of C. longepaniculatum increased after an obvious decrease; and the C:N and C:P increased first but then decreased. However, the inflection point all appeared in the summer. The nutrient utilization of C. longepaniculatum at the edge of forest gaps was more efficient in summer and autumn than in spring and winter, indicating significant edge effects. The results of principal component analysis (PCA) suggested that gap size, relative light intensity and monthly average air temperature were the main environmental factors affecting the stoichiometry of C. longepaniculatum at the different edge of forest gaps in the P. massoniana plantation. These results indicated that forest gap with size 625 m² had the highest organic matter storage and nutrient utilization efficiency in the edge areas in all seasons, and therefore had the most significant edge effect on leaf element stoichiometry.     

Interactive effects of soil warming and nitrogen addition on fine root production of Chinese fir seedlings

Aims There have been a large number of studies on the independent separate responses of fine roots to warming and nitrogen deposition, but with contradictory reporting. Fine root production plays a critical role in ecosystem carbon, nutrient and water cycling, yet how it responds to the interactive warming and nitrogen addition is not well understood. In the present study, we aimed to examine the interactive effects of soil warming and nitrogen addition on fine root growth of 1-year-old Chinese fir (Cunninghamia lanceolata) seedlings in subtropical China.
Methods A mesocosm experiment, with a factorial design of soil warming (ambient, +5 °C) and nitrogen addition (ambient, ambient + 40 kg·hm^-2·a^-1, ambient + 80 kg·hm^-2·a^-1), was carried out in the Chenda State-owned Forest Farm in Sanming City, Fujian Province, China. Fine root production (indexed by the number of fine roots emerged per tube of one year) was measured biweekly using minirhizotrons from March of 2014 to February of 2015.
Important findings (1) The two-way ANOVA showed that soil warming had a significant effect on fine root production, while nitrogen addition and soil warming × nitrogen addition had no effect. (2) The three-way ANOVA (soil warming, nitrogen addition and diameter class) showed that soil warming, diameter class and soil warming × diameter class had significant effects on fine root production, especially for the number of fine roots in 0-1 mm diameter class that had been significantly increased by soil warming. Compared with the 1-2 mm roots, the 0-1 mm roots seemed more flexible. (3) Repeated measures of ANOVA (soil warming, nitrogen addition and season) showed that soil warming, season, soil warming × season, and soil warming × nitrogen addition × season had significant effects on fine root production. In spring, the number of fine roots was significantly increased both by soil warming and soil warming × season, while soil warming, nitrogen addition, soil warming × nitrogen addition significantly decreased fine root production in the summer. (4) Soil warming, soil layer, soil warming × soil layer had significant effects on fine root production. The number of in-growth fine roots was significantly increased by soil warming at the 20-30 cm depth only. It seemed that warming forced fine roots to grow deeper in the soil. In conclusion, soil warming significantly increased fine root production, but they had different responses and were dependent of different diameter classes, seasons and soil layers. Nitrogen addition had no effect on fine root production. Only in spring and summer, soil warming and nitrogen addition had significant interactive effects.     

Stoichiometric characteristics of carbon,nitrogen and phosphorus of Sibiraea angustata shrub on the eastern Qinghai-Xizang Plateau

Aims Little is known about the stoichiometric characteristics of carbon (C), nitrogen (N) and phosphorus (P) in plateau shrubs across China. Sibiraea angustata is a typical and representative shrub species on the eastern Qinghai- Xizang Plateau, and exploring its C, N and P distribution patterns and stoichiometric properties in different organs (including root, shoot, leaf, twig and fruit) would help us better understand the mechanisms of C, N and P cycling and balance in the S. angustata dominated shrub ecosystem.
Methods Sixteen sampling sites were selected on the eastern Qinghai-Xizang Plateau by the stratified sampling method. The height and coverage of the dominant shrubs, latitude, longitude and altitude of the sites were recorded. Three 5 m × 5 m plots were selected at each site. At least 128 biological samples of plant organs of S. angustata were collected and measured, respectively. The C and N concentrations of plant samples were analyzed using an elemental analyzer (2400 II CHNS). The P concentration was analyzed using the molydate/ascorbic acid method after H₂SO₄-H₂O₂ digestion.
Important findings The C, N and P concentrations of different organs followed the order of: shoot (495.07 g·kg^-1) > twig (483.37 g·kg^-1) > fruit (480.35 g·kg^-1) > root (468.47 g·kg^-1) > leaf (466.33 g·kg^-1); leaf (22.27 g·kg^-1) > fruit (19.74 g·kg^-1) > twig (7.98 g·kg^-1) > shoot (4.54 g·kg^-1) > root (4.00 g·kg^-1) and fruit (2.85 g·kg^-1) > leaf (1.92 g·kg^-1) > twig (0.96 g·kg^-1) > root (0.52 g·kg^-1) > shoot (0.45 g·kg^-1), respectively. The ranges of the coefficient of variation (CV) for C, N and P concentrations were 1.71%-4.44%, 14.49%-25.50% and 11.46%-46.15%, respectively. Specifically, the C concentration was relatively high and stable, and the maximum CV values for N and P were found in roots. The N:P value of different organs varied from 7.12-12.41 and the minimum CV for N:P was found in twig, which indicated that N:P in twig had higher internal stability. In addition, correlation analysis indicated that the C concentration was significantly negatively correlated with N and P concentrations and correlation coefficients were -0.407 and -0.342, respectively. However, N concentration had dramatically positive correlation with P concentration and the correlation coefficient was 0.814. These results also could indicate that the C, N and P stoichiometric characteristics in the S. angustata shrub accorded with the homeostatic mechanism and growth rate hypothesis to some extent, the distributions of C, N and P concentrations were closely related to the function of the organs and it should be prudent to use ecological stoichiometric ratios to judge the condition of nutrient limitation at the species level.     

Carbon,nitrogen and phosphorus stoichiometry of Myrica nana in Yunnan,China

Aims Carbon (C), nitrogen (N) and phosphorus (P) play important roles in plant growth and physiological functions. We aimed at exploring the intrinsic relationships of C, N and P in Myrica nana—a common shrub in Yunnan Province—as well as their relationships with pant biomass and soil nutrients.
Methods We measured the concentration of C, N and P of M. nana from 29 sites for their magnitudes and correlations with soil nutrients.
Important findings 1) The arithmetic mean value of C, N and P concentration in the roots, stems and leaves of M. nana was 45.94%, 0.54%, 0.03%, and 46.32%, 0.58%, 0.03%, and 49.05%, 1.70%, 0.06%, respectively. C, N and P concentrations in the leaves were significantly higher than those in the roots and the stems. The C:N:P in roots, stems and leaves was 1531:18:1, 1544:19:1, and 818:10:1, respectively. 2) The C concentration and N:P in leaves of M. nana decreased with the increase of biomass of M. nana; the leaf C concentration was significantly correlated with biomass (p < 0.01), while the correlation between N:P and biomass was not significant (p > 0.05). The leaf N increased with the increase of plant biomass, the P was significantly correlated with biomass (p < 0.05), but the correlation between N concentration and biomass was not significant (p > 0.05). N:P in leaves was 34.2, suggesting that plant growth was limited by P. 3) C, N and P concentration in the roots were significantly correlated with soil P (p < 0.05), with N, P concentrations correlated with soil P positively (p < 0.01) and C negatively (p < 0.05). C concentration in the stems was significantly and negatively correlated with soil C, N, with significant correlation with C, N, and P concentration (p < 0.01). P concentration in the stems was significantly and positively correlated with soil P concentration (p < 0.01), while leaf P significantly and positively correlated with soil C, N and P (p < 0.01); leaf C concentration was significantly and negatively correlated with soil P (p < 0.01).     

Impacts of nitrogen addition on foliar nitrogen and phosphorus stoichiometry in a subtropical evergreen broad-leaved forest in Mount Wuyi

Aims Our purpose was to explore the effects of nitrogen addition on foliar nitrogen (N), phosphorus (P) and N:P stoichiometry and to assess their differences among different species and functional groups.
Methods N addition experiment has been conducted in a subtropical evergreen broad-leaved forest in Mount Wuyi, Fujian Province since 2011. Foliar concentrations of nitrogen and phosphorus were measured and foliar stoichiometry was estimated in tree, shrub, herb, fern and moss species following the N addition treatments from 2013 to 2015.
Important findings Generally, foliar N increased for almost all species and herbaceous plants are much more sensitive than trees and shrubs under N addition. Foliar N of Castanopsis carlesii, Amomum villosum, Woodwardia japonica increased significantly under N addition. Foliar P for most species was sensitive to the N addition. Foliar P of herbaceous plants increased significantly but foliar P of Leucobryum chlorophyllosum decreased significantly. The results showed the subtropical evergreen forest in Mount Wuyi was mainly limited by P and mean foliar N:P ratios enhanced from 18.67 to 19.72 under N addition, indicating that the strength of P limitation was enhanced by N addition. N:P ratios of the dominant arboreal species in the communities tended to be stable, while N:P ratios of herbaceous plants and shrubs increased. The changes in N:P ratios were mainly determined by P dynamics instead of N dynamics under N addition, and our results confirmed that increasing N availability can affect P cycling.     

Foliar nitrogen and phosphorus stoichiometry of alien invasive plants and co-occurring natives in Xishuangbanna

Aims How alien invasive plants and co-occurring native plants utilize nutrients is one of major issues in invasion ecology. Foliar nitrogen (N) and phosphorus (P) contents and stoichiometry can elucidate the uptake ability and limitation status of nutrients in plants, which provides basic knowledge for understanding the invading ability and co-occurrence or disappearance of plants.
Methods Based on typical alien invasive plants (Chromolaena odorata, Ageratina adenophora) and native plants in southwestern China, this study focused on strategies of N and P utilization among invasive plants and native plants under different invasion conditions. The species compositions, aboveground biomass, leaf N and P contents and leaf N:P were investigated for plants in plots with no invasion and with different invasion extents (estimated by the plot-based percentage of invaders’ biomass in total community) at Mt. Kongming in Xishuangbanna region, Yunnan Province, China.
Important findings The species number decreased significantly with the invasion extent of both C. odorata and A. adenophora, although the aboveground biomass was greatly enhanced. Leaf N and P contents did not differ between the two studied invaders, but they showed significantly higher N and P levels than both co-occurring and only native species (p < 0.05). Besides, leaf N and P contents of invaders increased with the invasion extent, and leaf N of native plants also showed an increasing trend with the invasion extent. When the influence of invasion was checked for the same species, leaf P contents decreased, whereas leaf N and N:P increased for most native plants under invasion. Based on the absolute foliar N and P contents, N:P values, we inferred that native plants were still limited by N, although N availability might be enhanced by invasion. Both invasive plants had leaf N:P values lower than 10, suggesting a higher P uptake relative to N uptake. All above results highlighted a higher N and P uptake of typical alien invasive plants in southwestern China.     

氮添加对武夷山亚热带常绿阔叶林植物叶片氮磷化学计量特征的影响

该文以福建武夷山亚热带常绿阔叶林为研究对象, 通过设置3个氮(N)添加梯度的野外实验, 研究了群落内乔木植物、灌木植物、草本植物、蕨类植物和苔藓植物叶片N、磷(P)化学计量特征对N沉降的响应, 以及不同功能群和物种化学计量特征对N沉降响应的差异。在已开展5年人工N添加的样地内, 3年的监测结果表明: N添加整体上提高了植物叶片N含量, 草本层植物叶片N含量对N添加的响应比乔木层和灌木层植物更加敏感, 优势种米槠(Castanopsis carlesii)、草本植物砂仁(Amomum villosum)、蕨类植物狗脊(Woodwardia japonica)的叶片N含量显著增加。N添加整体上增加了植物叶片P含量, 乔木层植物和灌木层植物叶片P含量没有显著变化, 草本层植物叶片P含量显著增加, 而苔藓植物叶片P含量显著减少。N添加促使武夷山亚热带常绿阔叶林植物叶片N:P由18.67上升至19.72, 加剧了植物生长的P限制; 乔木物种N:P的变化较灌木和草本物种更加稳定。N添加条件下, 植物叶片N:P的变化主要受到叶片P含量而非N含量变化的影响, N添加对生态系统P循环的影响显著。