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.     

阿拉善荒漠典型植物叶片碳、氮、磷化学计量特征

荒漠植物在水分限制、营养元素相对匮缺的条件下,经过长期的进化适应形成了自身独特的生理生态和生态化学计量特征。在阿拉善荒漠选择52个典型群落类型,分析和研究了54种荒漠植物叶片的碳、氮和磷的化学计量特征。结果表明:荒漠植物叶片的碳(C mg/g)、氮(N mg/g)和磷(P mg/g)含量变幅较大,分别为(379.01±55.42)mg/g、(10.65±7.91)mg/g和(1.04±0.81)mg/g,变异系数分别为0.15、0.74和0.78;C/N、C/P、和N/P分别为66.70±60.81、683.16±561.94、11.53±5.06。元素间相关性分析表明,叶片的C和N不相关(P0.05),C与P显著正相关(P0.05),N和P极显著正相关(P0.01)。从植物功能型的角度分析发现,灌木和1年生草本植物对C的存储能力较低;占整体67%的灌木叶片的N、P含量最低,导致总体N、P含量较低;多年生草本和1年生草本植物叶N含量与灌木植物叶片和整体N含量无差别,而P含量明显高于灌木植物叶片和整体P含量且N/P明显低于灌木植物叶片和总体N/P,导致总体N/P较低。该研究结果与全球和中国尺度的研究相比发现,荒漠植物叶片C、N、P含量和N/P明显偏低,N/P14说明阿拉善荒漠植物在受N、P共同作用的同时更易受N限制。     

危害严重外来入侵植物—紫茎泽兰

我国地处亚洲东南部 ,地域辽阔 ,具有丰富的物种多样性 (biological diversity) ,但因其所跨越的地理带自然条件较好 ,在适宜本地植物 (native species)生长的同时 ,也为外来物种 (alien species)的传播和扩散提供了条件。如紫茎泽兰 (Eupatorium adenophorum)、飞机草(Eupatorium odoratum)、薇甘菊 (Mikania micrantha)、凤眼莲 (Eichhornia crassipes)、大米草 (Spartinaanglica)和三裂叶豚草 (Ambrosia trifida)等 ,近年来因自然或人为因素引进后 ,现已在我国一些地方形成单优势种群 ,对我国的农业、林业、牧业、生物多样性和自然生…     

我国对3种外来入侵植物的利用

主要介绍了我国在防治生物入侵时,对水葫芦、紫茎泽兰、互花米草等入侵植物的综合利用.     

松嫩草地80种草本植物叶片氮磷化学计量特征

以松嫩草地常见草本植物为研究对象, 分析了各生活型和功能群叶片氮磷化学计量特征。结果显示: 松嫩草地80种草本植物的叶片氮、磷质量浓度分别为(24.2 ± 0.96) mg·g ^-1和(2.0 ± 0.10) mg·g ^-1, 面积浓度分别为(13.0 ± 0.54) mg·cm ^-2和(1.0 ± 0.05) mg·cm ^-2, 氮磷比为13.0 ± 0.39, 氮磷比与叶片磷质量浓度、叶片氮、磷面积浓度有显著相关关系; 松嫩草地植物生长受到氮限制。一年生植物叶片氮、磷质量浓度和变异系数高于其他生活型, 各生活型之间氮面积浓度和氮磷比差异不显著。豆科植物叶片氮的质量浓度、面积浓度和氮磷比高于其他功能群。在不同生活型或功能群之间, 植物叶片磷的面积浓度差异不显著, 都在1.0 mg·cm ^-2左右; 适当地增加群落中豆科植物的比例, 可能有助于提高松嫩草地产量和质量。     

外来入侵植物紫茎泽兰不同组织RNA提取方法

从植物组织中提取高质量的RNA是进行cDNA文库构建等分子生物学研究的前提。在苯酚法的基础上,改进并得到了一种适合紫茎泽兰根、茎、叶总RNA快速提取的方法,消除了蛋白质、DNA、多糖等的污染。该方法提取的紫茎泽兰不同组织总RNA纯度高、完整性好,可用于RT-PCR、cDNA文库构建、Northern杂交等分子生物学实验,而且简单、经济、重复性好,适合于多种植物组织总RNA的提取。Northern杂交表明F3’H基因在紫茎泽兰的根、茎、叶等组织中广泛存在,但在叶中的表达量最高,在根中的表达量最低。     

外来入侵植物成灾的机制及防除对策

外来入侵植物是指自然或人为地由原生态系统中引入到新生境的植物 ,会给新生境或其中的物种带来威胁。紫茎泽兰从缅甸自然进入云南 ,其原产地是墨西哥 ;水葫芦从墨西哥引进用作饲料 ,而大米草是从英国南海岸引入用于促淤护堤。 3种外来入侵植物给我国当地的生产、生活等带来了极大的威胁 ,破坏了生态系统 ,影响了生物的多样性。对它们的治理费用昂贵。其繁殖力、适应性和抗逆性极强 ,竞争力也极强或本身拥有化感特性或特殊器官 ,同时又耐瘠、耐污 ,并且在本地还缺乏有力的竞争生物和天敌 ,是 3种外来入侵植物势不可挡 ,扩散蔓延的成灾机制。致力于外来入侵植物的国家能力建设和综合治理是 3种外来入侵植物的防除对策     

两种入侵植物与三种本地植物根系特征的比较研究

以菊科2种入侵植物飞机草(Chromolaena odorata (L.)R. M. King & H. Rob)和紫茎泽兰( Eupatorium adenophorum Speng)以及生活型相似的3种本地植物异叶泽兰(Eupatorium heterophyllum DC.)、佩兰(Eupa-torium for...     

不同入侵程度紫茎泽兰碳氮磷生态化学计量特征研究

紫茎泽兰(Ageratina adenophora)是一种生态危害性较大的入侵植物。为探讨不同入侵程度下紫茎泽兰的化学计量特征,进一步揭示其营养策略与入侵机制,该研究以紫茎泽兰及其本土伴生种条叶猪屎豆(Crotalaria linifolia)为对象,测定研究了轻度入侵、中度入侵和重度入侵下紫茎泽兰根、茎、叶中碳(C)、氮(N)、磷(P)化学计量特征与其入侵地土壤养分状况,并进一步比较了紫茎泽兰和条叶猪屎豆的C、N、P化学计量特征。结果表明：(1)3种入侵程度下,紫茎泽兰叶N、P含量均显著大于根和茎N、P含量,将更多的N和P分配至叶,增加资源获取,以利快速生长。(2)3种入侵程度下,紫茎泽兰茎N∶P<根N∶P<叶N∶P,且茎N∶P在中度入侵下显著大于轻度入侵,在入侵过程中其茎呈现出较高的生长速率,可促进其获取更多环境资源,增强生长竞争优势。(3)与本土种条叶猪屎豆相比,紫茎泽兰具有更高的根P、茎P含量,根和茎C∶P、N∶P均显著小于条叶猪屎豆,各器官C∶N均显著大于条叶猪屎豆,显示出较高的养分利用效率及较低的资源需求量。(4)紫茎泽兰茎C和叶C、茎N和叶N均呈显著正相关,茎...     

入侵植物紫茎泽兰化感作用及其途径研究

紫茎泽兰广泛入侵中国西南地区,研究结果表明化感作用是其入侵的重要武器,但其化感作用的途径并不十分清楚。本研究中,我们发现紫茎泽兰可以通过多种途径对两种栽培植物大麦和玉米的生长产生化感作用,这些途径包括了叶挥发物、叶淋溶物以及根分泌物。并且在紫茎泽兰幼苗早期就可以检测到这些化感作用。然而,没有实验证据表明紫茎泽兰落叶的微生物降解物对两种测试植物具有化感作用。     

Allocation strategies for nitrogen and phosphorus in forest plants

The allocation of limiting elements, such as nitrogen (N) and phosphorus (P), in plants is an important basis for structural stability and functional optimization in natural plant communities. However, because of the lack of systematic investigation data, the mechanisms of optimal nutrient allocation in plants in natural forests are still unclear. Using consistent measurements of N and P contents in 930 plant species, we explored the allocation strategies for N and P in different plant organs and plant functional groups (PFGs) in natural communities. The N and P contents and N:P ratio were the highest in the leaf (the most active organ) at the organ level. At the PFG level, the N and P contents were higher in herbs than in woody plants, but the trend was opposite for the N:P ratio. The elemental plasticity of root was higher than that of leaf. Furthermore, at the large scale, the allometric exponents of N and P were less than 1 and showed no difference, indicating strong conservatism of the scaling relationship in plants. In summary, higher element content in more active organs, higher element plasticity in underground organs, and conservative allometric allocation among different organs and among different PFGs jointly constitute the optimal strategies for the allocation of limiting elements.     

入侵物种飞机草和紫茎泽兰的核型研究

报道了菊科（Asteraceae）原泽兰属（Eupatorium）2种植物的核型,飞机草(Chromolaena odorata (L.) R. M. King &; H. Robinson）2n=60,核型公式为2n=60=32 m+28 sm,核型属于“2A”型,紫茎泽兰(Ageratina adenophora (Sprengel) R. King &; H. Robinson）2n=51,核型公式为2n=51=30 m+21 sm,核型属于“2B”型。飞机草的染色体数目变化较大,紫茎泽兰染色体数目较稳定。紫茎泽兰不能产生正常的花粉。飞机草有性生殖产生的种子发芽率低,紫茎泽兰无融合生殖产生的种子发芽率高,但2种植物入侵能力都很强,种子数量与2种植物的入侵性关系不大。     

Changes of the relationships between soil and microbes in carbon,nitrogen and phosphorus stoichiometry during ecosystem succession

AimsThe carbon (C), nitrogen (N) and phosphorus (P) stoichiometry (C:N:P) of soil profoundly influences the growth, community structure, biomass C:N:P stoichiometry, and metabolism in microbes. However, the relationships between soil and microbes in the C:N:P stoichiometry and their temporal dynamics during ecosystem succession are poorly understood. The aim of this study was to determine the temporal patterns of soil and microbial C:N:P stoichiometry and their relationships during ecosystem succession.MethodsAn extensive literature search was conducted and data were compiled for 19 age sequences of successional ecosystems, including 13 forest ecosystems and 6 grassland ecosystems, from 18 studies published up to May 2016. Meta-analyses were performed to examine the sequential changes in 18 variables that were associated with soil and microbial C, N and P contents and the stoichiometry. Important findings (1) There was no consistent temporal pattern in soil C:N along the successional stages, whereas the soil C:P and N:P increased with succession; the slopes of the linear relationships between soil C:N:P stoichiometry and successional age were negatively correlated with the initial content of the soil organic C within given chronosequence. (2) There was no consistent temporal pattern in microbial C:N:P stoichiometry along the successional stages. (3) The fraction of microbial biomass C in soil organic C (qMBC), the fraction of microbial biomass N in soil total N, and the fraction of microbial biomass P in soil total P all increased significantly with succession, in consistency with the theory of succession that ecosystem biomass per unit resource increases with succession. (4) The qMBC decreased with increases in the values of soil C:N, C:P, or N:P, as well as the stoichiometric imbalances in C:N, C:P, and N:P between soil and microbes (i.e., ratios of soil C:N, C:P, and N:P to microbial biomass C:N, C:P, and N:P, respectively). The C:N, C:P, and N:P stoichiometric imbalances explained 37%-57% variations in the qMBC, about 7-17 times more than that explainable by the successional age, illustrating the importance of soil-microbial C:N:P stoichiometry in shaping the successional dynamics in qMBC. In summary, our study highlights the importance of the theories of ecosystem succession and stoichiometry in soil microbial studies, and suggests that appropriately applying macro-ecological theories in microbial studies may improve our understanding on microbial ecological processes.     

氮磷施肥对拟南芥叶片碳氮磷化学计量特征的影响

研究植物碳(C)氮(N)磷(P)化学计量特征, 有助于了解C、N、P元素的分配规律和确定限制植物生长的元素类型, 理解生长速率调控的内在机制。该研究基于盆栽施肥试验, 测定不同N、P供应水平下拟南芥(Arabidopsis thaliana)叶片的生物量和C、N、P含量, 分析拟南芥的限制元素类型、验证生长速率假说、探讨N、P的内稳性差异和C、N、P元素间的异速生长关系。主要结果如下: 盆栽试验基质中限制元素是P, 施N过多可能引起毒害作用; 拟南芥的生长符合生长速率假说, 即随着叶片N:P和C:P的增加, 比生长速率显著减小; 叶片P含量存在显著的调整系数(3.5), 但叶片N含量与基质N含量之间无显著相关; 叶片N和P含量具有显著的异速生长关系, 但不符合N-P^3/4关系, 施P肥导致表征N、P异速生长关系的幂指数(0.209)显著低于施N肥处理(0.466)。该研究首次基于温室培养实验分析了拟南芥C、N、P的化学计量特征及其对N、P添加的响应, 研究结果将为野外研究不同物种、群落或生态系统的化学计量特征提供参考。     

中温-暖温带表土碳氮磷生态化学计量特征的空间变异性——以河北省为例

解析区域土壤碳氮磷元素的生态化学计量特征的空间分异格局有助于土壤养分的综合管理与利用。运用传统统计学和地统计学分析方法,以河北省为例分析了中温-暖温带表土(0—30cm)碳氮磷元素的生态化学计量特征的空间变异性及影响因素。结果显示:(1)土壤有机碳(SOC)、全氮(TSN)、全磷(TSP)其摩尔比率的变异系数均介于0.1—1之间,表明其在空间上存在中等程度的变异性。此外,C∶N的变异系数较小,表明C∶N较稳定。(2)表土TSP和C∶N具有小范围、强烈的空间自相关性,SOC、TSN、C∶P和N∶P具有较大范围、中等程度的空间自相关性,结构性因素是土壤碳氮磷含量及其摩尔比率空间变异的主要影响因素。从空间分布规律来看,表土碳氮磷含量及其摩尔比率均没有呈现明显的递增或递减的变化规律,SOC、TSN、C∶P和N∶P具有相同的空间分布趋势,高值区主要分布在冀北地区,分布面积较小,低值区分布范围较广;C∶N的高值区零星分布在冀北地区,TSP的高值区和低值区呈现斑块状分布。(3)土壤C∶N、C∶P和N∶P受到土壤理化性状、土地利用方式、人类扰动、气候及地形等因素的调控。此外,不同气候带的C∶N、C∶P和N∶P也存在一定的差异,研究区土壤C∶N与高寒带较接近,同时与其他气候带没有显著的差异;C∶P和N∶P与温带沙漠区较接近,与其余气候带存在显著的差异性,说明不同气候带之间的C∶N较C∶P和N∶P稳定。     

生态系统演替过程中土壤与微生物碳氮磷化学计量关系的变化

土壤碳(C)、氮(N)、磷(P)化学计量特征会显著影响微生物的生长、群落结构、生物量C:N:P化学计量及其代谢活动。然而生态系统演替过程中土壤-微生物C:N:P化学计量的时间格局及其协调关系还不明确。为此, 该研究收集了2016年5月以前发表的文献中19个生态系统演替序列(包括13个森林、6个草地生态系统)的土壤-微生物生物量C:N:P研究结果, 整合分析了其中土壤-微生物生态化学计量的时间动态, 结果表明: (1)生态系统演替过程中土壤C:N没有一致的时间格局, 而土壤C:P和N:P均随演替进程显著增加, 其中土壤C:N:P与演替时间之间线性关系的斜率与相应演替序列的初始土壤有机C含量呈负相关关系。(2)演替进程中土壤-微生物生物量C:N:P没有一致的时间格局。(3)微生物生物量C占土壤有机C百分比(qMBC)、微生物生物量N占土壤全N百分比、微生物生物量P占土壤全P百分比均随着演替进程而显著增加, 即单位资源所能支持的微生物生物量随着演替进程而增加, 这与宏观生态系统演替理论相符。(4) qMBC随着土壤C:N、C:P和N:P以及C:N、C:P和N:P化学计量不平衡性(即土壤C:N、C:P和N:P分别除以微生物生物量C:N、C:P和N:P)的增加而减小; 其中, C:N、C:P和N:P化学计量不平衡性解释了qMBC变异性的37%-57%, 是演替时间解释率的7-17倍, 表明土壤-微生物生态化学计量关系对qMBC演替动态有重要影响。该研究强调了生态化学计量学理论和生态系统演替理论在土壤微生物时间动态研究中的重要作用, 表明适当地融合生态学宏观理论于土壤微生物研究可以加深对土壤-微生物生态过程的认识。