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1.
倒木是森林生态系统维持健康和更新的重要组成部分, 在倒木不同腐解阶段, 倒木上定植的苔藓植物组合的差异尚不清楚。为深入探讨倒木上苔藓植物组合变化规律及其影响因素, 该文对西藏色季拉山同一地点不同腐解程度的4株华山松(Pinus armandii)倒木上的苔藓植物进行了样方调查和数据分析。结果表明: 4株倒木上40个样方共有苔藓植物22科52种, 其中藓类13科38种, 苔类9科14种; 以恒有优势种为特征进行划分, 共得到14个物种组合。随着倒木腐解程度加大以及周围环境的不断改变, 生长其上的苔藓植物物种多样性逐渐增加, 但组合数量和苔藓总盖度却呈现先增大后减小的趋势。苔藓物种由耐旱性强的丛生型藓类, 如木灵藓科、白发藓科, 逐渐演替为喜阴湿环境、快速生长的垫状或毯状藓类, 如提灯藓科、羽藓科和青藓科。倒木苔藓植物组合空间结构复杂程度逐渐增大。倒木是多种苔藓植物选择的重要生长基质, 其上苔藓植物受倒木的腐解程度、水分和光照等条件的影响而发生相应的物种组合变化。 相似文献
2.
《植物生态学报》2018,42(5):562
性状变异反映了植物的生活史对策。该研究以贵州普定县天龙山10种木本植物为对象, 通过分析枝叶和根系9个功能性状的种间与种内变异, 揭示植物对喀斯特生境的适应策略。结果表明: (1) 9个性状变异程度不同, 细根组织密度的种间和种内变异系数最大, 分别达96.47%和51.44%, 小枝干物质含量的种间与种内变异最小, 分别为11.67%和6.83%。(2)种间水平的细根组织密度在不同物种中没有显著的差异, 比根长、叶厚度、叶面积、比叶面积、叶干物质含量、叶组织密度、小枝干物质含量和小枝组织密度均表现出显著的差异。在种内, 比叶面积差异显著, 其他性状差异不显著。(3)绝大多数叶和枝性状间显著相关, 比根长与比叶面积显著负相关, 其他根系性状与枝叶性状相关性不显著。总之, 与同纬度非喀斯特地区植物相比, 普定喀斯特地区植物具有较小的叶面积和比根长度, 较大的叶干物质含量、叶组织密度等一系列有利于减小蒸腾和储存养分的功能性状组合, 这可能是其适应干旱贫瘠的喀斯特环境的主要生态策略。 相似文献
3.
《植物生态学报》2017,41(10):1069
Aims The stoichiometric characteristics of carbon (C), nitrogen (N) and phosphorus (P) in plant organism is vital to understand plant adaptation to environment. In particular, the correlations of elemental stoichiometric characteristics between leaf and fine root could provide insights into the interaction and balance among the plant elements, nutrient use strategies and plant response to global change.Methods We measured C, N, P contents and C:N, C:P, N:P in leaves and fine roots of 60 dominant plants in Horqin sandy land. The 60 plant species were classified into five life forms and two categories such as perennial forb, annual forb, perennial grass, annual grass, shrub, legume, and non-legume. We statistically analyzed the differences and correlations of C, N and P stoichiometry either between fine root and leaf or among five life forms.Important findings The average C, N and P concentrations in leaves of 60 plant species in Horqin sandy land are 424.20 mg·g-1, 25.60 mg·g-1 and 2.10 mg·g-1, respectively. In fine roots, the corresponding element concentrations are 434.03 mg·g-1, 13.54 mg·g-1, 1.13 mg·g-1. N and P concentrations in leaf are approximately twice as high as averages in fine root. Furthermore, similar N:P between leaf and fine root indicates conservative characteristic of elemental stoichiometry in plant organism, suggesting that nutrients distribution is proportional between aboveground and underground of plants. There are significant difference of C, N, P, C:N, C:P and N:P in leaf and root among five life forms. N and P in forb and C:N and C:P in grass are averagely higher than those in other life forms. N:P in annual forb and grass, however, are lower than those in other life forms. C, N in legume are higher than those in non-legume, while C:N in legume is lower than in non-legume. These results imply that nutrient use strategies are significantly different among plant life forms. Correlations analysis showed that N and P in leaf or fine root positively correlated, but C and N, C and P in fine root negatively correlated, suggesting coupling relationship among C, N and P in leaf and fine root. Subsequently, we detected positively significant correlations in C, N, P and their ratios between leaf and fine root, suggesting proportional distribution of photosynthate and nutrient between aboveground and underground during plant growth. Generally, these results supplied fundamental data to understand mass turnover and nutrients cycling of leaves and roots in sand land. 相似文献
4.
叶片性状-环境关系对于预测气候变化对植物的影响至关重要。该研究以青藏高原东缘常见阔叶木本植物为研究对象, 从47个样点采集了332个物种共666个种群的叶片, 测量了15个叶片性状, 调查了该区域木本植物叶片性状的变异程度, 并从种内和种间水平探讨了叶片性状对环境的响应及适应策略。结果表明, 反眏叶片大小的性状均具有较高的变异, 其中, 叶片面积是变异程度最大的性状。除气孔密度外, 大多数叶片性状与海拔显著相关。气候是叶片性状变异的重要驱动因素, 3.3%-29.5%的叶片性状变异由气候因子组合解释。其中, 气温对叶片性状变异解释度最高, 日照时间能解释大部分叶片性状的变异, 而降水量对叶片性状变异的解释度相对较小。与环境(海拔和气候因子)显著相关的叶片性状在种内明显少于种间水平, 可能是植物性状之间的协同变化与权衡使种内性状变异比较小, 从而减弱了种内叶片性状与环境因子的相关性。研究结果总体表明,叶片性状与木本植物对环境的适应策略密切相关, 植物通过选择小而厚的叶片和较短的叶柄以适应高海拔的 环境。 相似文献
6.
《植物生态学报》2017,41(1):31
Aims Understanding the changes in N and P concentration in plant organs along the environmental gradients can provide meaningful information to reveal the underline mechanisms for the geochemical cycles and adaptation strategies of plants to the changing environment. In this paper, we aimed to answer: (1) How did the N and P concentration in leaves of evergreen and deciduous woody plants change along the environmental gradients? (2) What were the main factors regulating the N and P concentration in leaves of woody plants in the shrublands across southern China?
Methods Using a stratified random sampling method, we sampled 193 dominant woody plants in 462 sites of 12 provinces in southern China. Leaf samples of dominant woody plants, including 91 evergreen and 102 deciduous shrubs, and soil samples at each site were collected. N and P concentration of the leaves and soils were measured after lapping and sieving. Kruskal-Wallis and Nemenyi tests were applied to quantify the difference among the organs and life-forms. For each life-form, the binary linear regression was used to estimate the relationships between leaf log [N] and log [P] concentration and mean annual air temperature (MAT), mean annual precipitation (MAP) and log soil total [N], [P]. The effects of climate, soil and plant life-form on leaf chemical traits were modeled through the general linear models (GLMs) and F-tests.
Important findings 1) The geometric means of leaf N and P concentrations of the dominant woody plants were 16.57 mg·g-1 and 1.02 mg·g-1, respectively. The N and P concentration in leaves (17.91 mg·g-1, 1.14 mg·g-1) of deciduous woody plants was higher than those of evergreen woody plants (15.19 mg·g-1, 0.89 mg·g-1). The dependent of leaf P concentration on environmental (climate and soil) appeared more variable than N concentration. 2) Leaf N and P in evergreen woody plants decreased with MAT and but increased with MAP, whereas those in deciduous woody plants showed opposite trends. With increase in MAP, leaf P concentration decreased for both evergreen and deciduous woody plants. 3) Soil N concentration had no significant effect on both evergreen and deciduous woody plants. However, leaf P concentration of the tow increased significantly with soil P concentration. (4) GLMs showed that plant growth form explained 7.6% and 14.4% of variation in leaf N and P, respectively. MAP and soil P concentration contributed 0.8% and 16.4% of the variation in leaf P, respectively. These results suggested that leaf N was mainly influenced by plant growth form, while leaf P concentration was driven by soil, plant life-form, and climate at our study sites. 相似文献
Methods Using a stratified random sampling method, we sampled 193 dominant woody plants in 462 sites of 12 provinces in southern China. Leaf samples of dominant woody plants, including 91 evergreen and 102 deciduous shrubs, and soil samples at each site were collected. N and P concentration of the leaves and soils were measured after lapping and sieving. Kruskal-Wallis and Nemenyi tests were applied to quantify the difference among the organs and life-forms. For each life-form, the binary linear regression was used to estimate the relationships between leaf log [N] and log [P] concentration and mean annual air temperature (MAT), mean annual precipitation (MAP) and log soil total [N], [P]. The effects of climate, soil and plant life-form on leaf chemical traits were modeled through the general linear models (GLMs) and F-tests.
Important findings 1) The geometric means of leaf N and P concentrations of the dominant woody plants were 16.57 mg·g-1 and 1.02 mg·g-1, respectively. The N and P concentration in leaves (17.91 mg·g-1, 1.14 mg·g-1) of deciduous woody plants was higher than those of evergreen woody plants (15.19 mg·g-1, 0.89 mg·g-1). The dependent of leaf P concentration on environmental (climate and soil) appeared more variable than N concentration. 2) Leaf N and P in evergreen woody plants decreased with MAT and but increased with MAP, whereas those in deciduous woody plants showed opposite trends. With increase in MAP, leaf P concentration decreased for both evergreen and deciduous woody plants. 3) Soil N concentration had no significant effect on both evergreen and deciduous woody plants. However, leaf P concentration of the tow increased significantly with soil P concentration. (4) GLMs showed that plant growth form explained 7.6% and 14.4% of variation in leaf N and P, respectively. MAP and soil P concentration contributed 0.8% and 16.4% of the variation in leaf P, respectively. These results suggested that leaf N was mainly influenced by plant growth form, while leaf P concentration was driven by soil, plant life-form, and climate at our study sites. 相似文献
7.
《植物生态学报》2014,38(5):477
人工林目前存在结构单一、土壤退化、生物多样性降低等人类普遍关注的生态问题。马尾松(Pinus massoniana)是长江上游低山丘陵区退耕还林的主要人工林树种。研究采伐林窗对植物物种组成和更新的影响, 对马尾松低效人工林的改造, 提升其生态服务功能具有重要的意义。该文以采伐39年生的马尾松人工林形成的7种不同大小的林窗为研究对象, 分析了不同季节林窗内的植物生活型组成及多样性变化。结果表明: 1)马尾松人工林林下植物以高位芽植物居多, 其次是地面、地下芽植物, 一年生植物较少而缺少地上芽植物。在林窗形成初期, 林窗的高位芽植物比例明显低于林下, 大林窗的高位芽植物比例稍高于小林窗, 地下芽和一年生植物的比例低于小林窗。2)林下的物种丰富度和物种多样性指数显著低于大林窗。不同林窗下植物的丰富度指数、优势度指数、多样性指数也存在显著差异。3)夏季林窗下植物多样性最高, 其次是秋季, 春季多样性最低。1225-1600 m2的大林窗能够促进马尾松人工林植物多样性恢复和植被更新。 相似文献
8.
新疆三工河流域苔藓植物生活型分析 总被引：1，自引：0，他引：1
研究将新疆三工河流域苔藓植物的生活型划分为：漂浮型、石生固着型、附生固着型、水生根着型、中生根着型和旱生根着型等类型。其中,中生根着型种类最多,占该流域苔藓植物种数的89．81％,主要分布于森林带;其次为旱生根着型,占该流域苔藓植物种数的11．57％;漂浮型种类最少,只占该流域苔藓植物种数的1．38％,且分布范围十分有限。从分析结果还可知,新疆三工河流域苔藓植物的种类和生活型类型是比较丰富的,反映出该流域独特而复杂的苔藓植物多样性特点。 相似文献
9.
以贵州大学喀斯特山地校园为对象,调查其苔藓植物物种多样性及其生境特征,探讨苔藓植物生长与环境的关系。结果表明,研究区域内苔藓植物共12科27属51种。优势科是丛藓科(Pottiaceae)、青藓科(Brachytheciaceae)和灰藓科(Hypnaceae);主要生活型为丛集型、交织型和垫型;不同功能区域的苔藓植物生物多样性从高到低依次为行政办公区、休闲游憩区、教学科研区、体育运动区、宿舍休息区;不同生境物种丰富度从高到低依次是疏林草坪、林下、草坪环境、灌丛花池、道路;人为干扰程度与光照、湿度是影响苔藓植物多样性组成的重要因子。研究区域内苔藓植物多样性较低,多为土生藓类。在苔藓生长的微生境中,人为干扰低、空气湿度大的林地、疏林草坪更利于苔藓生长。 相似文献
10.
磷(P)是地球生态系统中重要的生命元素。全球变化背景下, 科学地探究森林土壤磷储量现状及其影响因子, 对陆地生态系统的稳定以及磷的可持续利用具有重要意义。因此, 该研究利用青海省240个森林标准样地土壤实测数据, 并结合青海省森林资源清查资料估算出了青海省森林土壤磷储量, 揭示了其分布格局, 并讨论了土壤磷储量与环境因子的关系。结果表明: (1)青海省森林土壤磷储量为1.74 Tg, 全省1 m深土壤平均磷密度为4.65 Mg·hm -2, 土壤磷密度总体上呈地带性分布。(2)土壤磷密度在中低海拔(2 200-3 000 m)区域随海拔的升高显著减小, 在高海拔(3 300-3 900 m)区域随海拔高度的增加而显著变大。山地灰褐色森林土的磷密度最大且显著大于山地棕色暗针叶林土和山地暗褐土。(3)土壤磷含量随海拔升高显著减小, 山地棕色暗针叶林土各土层磷含量相对较大, 山地暗褐土的磷含量最小, 且土壤磷含量随着土层的加深而减小。(4)海拔、温度、土壤类型以及土壤含水量均对土壤磷含量有直接影响, 且影响较大, 其中海拔和温度是影响土壤磷含量变化的关键因子; 土壤磷密度对土壤容重、土壤磷含量、土壤含水量、海拔、土壤类型的变化响应较为明显, 而土壤容重可能是限制土壤磷密度变化的主导因素。 相似文献
11.
在新疆阿尔泰山中段的红山嘴地区选取一条沿海拔745-2 413 m的不同植被带群落样方进行调查, 对应采集37个表土样品进行孢粉统计和排序分析, 初步探究了红山嘴地区的植被与表土孢粉之间的对应关系, 并将之与新疆阿尔泰西部的喀纳斯西坡孢粉垂直带进行对比。结果表明, 红山嘴地区表土孢粉谱依照海拔高度自上而下划分为4个孢粉组合类型, 分别对应亚高山草甸、山地森林、灌丛草原和荒漠草原。乔木植物中云杉属(Picea)和松属(Pinus)花粉, 灌木植物中麻黄属(Ephedra)及草本植物中的苋科和蒿属(Artemisia)因受到自然风力、水流及人为活动的影响, 表现出明显的超代表性; 乔木植物中的落叶松属(Larix)花粉, 草本植物中的禾本科及莎草科花粉, 却在其自身为优势种的群落中呈现低代表性; 蒿属与苋科花粉百分含量的比值(Ar/Am)能较好地反映该区气候垂直带的干湿状况, 灌丛草原带的Ar/Am低, 在一定程度上反映了人类活动对草原灌丛化的影响。与新疆阿尔泰西部的喀纳斯西坡孢粉垂直带相比, 红山嘴垂直带的孢粉类型偏少, 同时相似的孢粉带在该区的分布高度比喀纳斯西坡高。此外, 排序分析(RDA)结果表明, 年降水量是影响该区表土孢粉组合的主要环境因子。 相似文献
12.
灌木层作为森林生态系统的重要组成部分, 了解其生态化学计量特征将有助于揭示森林生态系统物质周转和养分循环等生态功能。该研究选取青海省7种主要优势林分——白桦(Betula platyphylla)林、毛白杨(Populus tomentosa)林、红桦(Betula albosinensis)林、青扦(Picea wilsonii)林、山杨(Populus davidiana)林、圆柏(Sabina chinensis)林、云杉(Picea asperata)林为研究对象, 采用野外取样和室内实验分析相结合的方法, 研究了不同林分林下灌木层不同器官(叶、枝干、根)及其表层(0-10 cm)土壤的碳(C)、氮(N)、磷(P)含量及其相关性。结果表明: 7种林分间灌木(叶、枝干、根) P含量、C:P均没有明显差异性; 山杨林、圆柏林、云杉林的林下灌木(叶、枝干、根) N含量、N:P高于白桦林、毛白杨林、红桦林和青扦林, C:N则相反。圆柏林的林下灌木生长受P限制, 其余6种林分的林下灌木生长受N限制。7种林分间土壤有机碳(SOC)和总氮(TN)含量呈现出明显差异性, 而总磷(TP)含量则差异不明显。相关性分析表明, 林下灌木(叶、枝干、根) N含量、C:N、N:P与土壤TN含量、C:N、N:P呈极显著相关性, 而P含量、C:P与土壤TP含量呈显著相关性。冗余分析表明, 林下灌木层植被C、N、P含量及生态化学计量特征受到土壤化学计量特征及各环境因子的共同影响, 其中土壤C:N、海拔、年平均气温、年降水量为主要影响因子。 相似文献
13.
冷杉天然林下地表主要苔藓斑块生物量及其影响因素 总被引：2，自引：0，他引：2
调查分析了大渡河上游藓类-冷杉天然林下5种主要地表苔藓斑块（锦丝藓、赤茎藓、大羽藓、塔藓及锦丝-大羽藓）的生物量,同时测定了各斑块相关环境因子（斑块表面气温、空气湿度、光照强度及基质湿度等）。对苔藓生物量和相关环境因子进行综合分析表明,不同苔藓斑块的生物量有差异,且不同斑块环境因子也表现出一定的差异性。对斑块生物量与环境因子进行相关分析显示,苔藓斑块生物量与环境因子之间相关性较显著,苔藓生物量特征受空气温度、空气湿度、光照强度、灌木层盖度及草本层盖度等因素影响较大。但不同环境因子对不同斑块苔藓生物量的影响水平有差异。 相似文献
14.
为查明长湖浮游植物群落特征及其水环境影响因子, 并确定水体富营养化程度, 于2012年夏季对长湖浮游植物及相关环境因子进行调查检测分析, 运用藻类生物学法和综合营养状态指数法, 对长湖水体营养状态进行综合评定, 同时利用典范对应分析法(CCA)对浮游植物与环境因子的关系进行了分析。结果表明, 2012年夏季长湖浮游植物共有53种(含变种、变型), 隶属于7门41属, 其中以绿藻最多(24种, 占总数量的38.9%), 其次为蓝藻(15种, 占总数量的36.0%)和硅藻(7种, 占总数量的14.1%)。优势种(优势度指数大于0.02)共10种, 其中两栖颤藻(Oscillatoria amphibia)是4个区域的共有优势种, 最高优势度达0.72。浮游植物丰度为12.03 × 10 6- 62.13 × 10 6cell·L -1, 平均值为27.71 × 10 6cell·L -1。浮游植物丰度的平面分布呈现圆心湖、海子湖、马洪台、庙湖依次降低的特点。浮游植物多样性指数变化范围为0.89-3.24, 均匀度指数变化范围为0.23-0.83。选取叶绿素a、总磷、总氮、透明度和化学需氧量5项参数计算得出综合营养化指数。通过藻类生物学法和综合营养状态指数法进行综合评价发现: 2012年夏季长湖处于中度富营养化到富营养化程度。典范对应分析表明: 浮游植物空间分布主要受总氮、总悬浮物、总磷、溶氧以及亚硝酸氮等环境因子的影响。针状蓝纤维藻(Dactylococcopsis acicularis)、两栖颤藻、席藻属(Phormidium)、鱼腥藻属(Anabeana)等蓝藻对总氮的需求较大。长湖各站点由于在不同程度上受到地形、人为干扰以及水动力条件的影响, 它们与环境因子的典范对应分析表现出明显的区域性。 相似文献
15.
《植物生态学报》2018,42(3):265
分析不同草地类型生物量与碳密度空间分布特征及其影响因素, 揭示草地植物碳库的变化规律, 对于了解我国草地生态系统碳汇具有重要意义。2011-2013年以河北省天然草地为研究对象, 调查了不同草地类型的地上活体生物量、凋落物生物量和根系生物量以及各组分的碳密度。结果表明: 温性草原、温性草甸、温性山地草甸、低地盐化草甸、暖性草丛和暖性灌草丛6种草地类型的总生物量差异显著, 其中低地盐化草甸总生物量最高, 为2 770.2 g·m -2, 而温性草原最低, 为747.6 g·m -2, 前者约为后者的3.7倍; 地上活体生物量最大的是低地盐化草甸, 其次是暖性灌草丛和温性山地草甸, 最小的是温性草原, 分别为285.0、235.1、203.1和110.6 g·m -2; 凋落物生物量也是低地盐化草甸最大, 其次是温性山地草甸和温性草甸, 分别为584.0、187.9和91.0 g·m -2。6种草地类型的根系生物量均大于地上生物量, 是地上生物量的1.9-4.3倍, 不同草地类型根冠比的平均值为3.1; 低地盐化草甸的根系生物量最高, 为1901.3 g·m -2, 温性草原的根系生物量最低, 只有低地盐化草甸的1/3。在各类草地生物量碳密度方面, 低地盐化草甸的地上活体碳密度、凋落物碳密度与根系碳密度均为最大, 分别为132.7、81.2和705.9 g C·m -2。草地地上生物量、凋落物生物量和根系生物量以及总生物量均随海拔的升高先减少而后增加(p < 0.05); 草地生态系统总生物量和根系生物量随大于10 ℃积温的增加先降低而后升高(p < 0.01)。该研究中暖性灌草丛多分布在石质山区, 土层很薄, 植物地上生物量和根系生物量都比土层较厚的草甸草原低。可见, 在较大区域比较不同草地类型生物量时, 应综合考虑气候、土壤、地理等因素。 相似文献
16.
《植物生态学报》2016,40(9):893
AimsStreams are widely distributed in alpine forests, and litter decomposition in which is an important component of material cycling across the forest landscape. The leaching and fragmenting effects as well as the unique environmental factors in streams may have significant impacts on lignin degradation during litter decomposition, but studies on this are lacking.
Methods Using litterbag methods, we investigated the dynamics of lignin mass remaining and concentration (percent litter mass, %) during the decomposition of four foliar litters, which varied significantly in the initial litter chemical traits, from the dominant species of Salix paraplesia, Rhododendron lapponicum, Sabina saltuaria, and Larix mastersiana under different habitats (forest floor, stream, and riparian zone) in the upper reaches of the Minjiang River.
Important findings After two year’s incubation, litter lignin mass remaining for a specific litter species varied significantly (p < 0.05) among habitats, with an order of stream < riparian zone < forest floor. Lignin was degraded substantially in the early stage of litter decomposition process, and the lignin concentration first decreased and then increased with the proceeding of litter decomposition, but varied significantly (p < 0.05) among different litter species. Lignin mass showed a general trend of decrease across the 2-year decomposition course. In addition, habitat type, decomposition period and microenvironmental factors (e.g., temperature, pH value and nutrient availability) showed substantial influences on lignin degradation rate. These results suggest that the traditional view that lignin was relatively recalcitrant with an increase of concentration in the early stage of litter decomposition is challenged, but the loss of lignin in the early phrase is in line with recent findings about the fate of lignin during litter decomposition. Moreover, the significant differences of lignin degradation rates among different decomposition period and habitat types indicated that local-scale environmental factors can play a significant role in litter decomposition and lignin degradation processes. 相似文献
Methods Using litterbag methods, we investigated the dynamics of lignin mass remaining and concentration (percent litter mass, %) during the decomposition of four foliar litters, which varied significantly in the initial litter chemical traits, from the dominant species of Salix paraplesia, Rhododendron lapponicum, Sabina saltuaria, and Larix mastersiana under different habitats (forest floor, stream, and riparian zone) in the upper reaches of the Minjiang River.
Important findings After two year’s incubation, litter lignin mass remaining for a specific litter species varied significantly (p < 0.05) among habitats, with an order of stream < riparian zone < forest floor. Lignin was degraded substantially in the early stage of litter decomposition process, and the lignin concentration first decreased and then increased with the proceeding of litter decomposition, but varied significantly (p < 0.05) among different litter species. Lignin mass showed a general trend of decrease across the 2-year decomposition course. In addition, habitat type, decomposition period and microenvironmental factors (e.g., temperature, pH value and nutrient availability) showed substantial influences on lignin degradation rate. These results suggest that the traditional view that lignin was relatively recalcitrant with an increase of concentration in the early stage of litter decomposition is challenged, but the loss of lignin in the early phrase is in line with recent findings about the fate of lignin during litter decomposition. Moreover, the significant differences of lignin degradation rates among different decomposition period and habitat types indicated that local-scale environmental factors can play a significant role in litter decomposition and lignin degradation processes. 相似文献
17.
《植物生态学报》2018,42(12):1179
精确模拟冠层气孔导度(GS)对于评估区域蒸散具有重要意义。该研究选择两种常见的人工阔叶树种尾叶桉(Eucalyptus urophylla, 外来种)和木荷(Schima superba, 本地种)作为研究对象, 利用K?stner法和修订的Penman-Monteith公式计算冠层平均气孔导度(分别定义为GS1和GS2)。研究还分析了环境因子对冠层脱耦联系数(Ω)的影响, 并用其来评价两种方法模拟的冠层气孔导度的合理性。结果表明, 两个树种冠层气孔导度均与气象条件耦合较好(尾叶桉: Ω = 0.10 ± 0.03, 木荷: Ω = 0.17 ± 0.03)。主成分分析显示, 光合有效辐射(PAR)以及水汽压亏缺(D)显著影响Ω的大小, 而风速(u)的影响较小。单因素分析则发现各环境因子与Ω之间的相关性并不显著。边界线分析表明D和PAR的增加使得Ω最终趋向于一个与树种有关的稳定值(木荷≈ 0.20, 尾叶桉≈ 0.05), 而Ω随u的增加呈幂指数下降。与木荷相比, 尾叶桉具有更高的气孔导度(尾叶桉和木荷的GS2年平均值分别为(33.42 ± 9.37) mmol·m -2·s -1和(23.40 ± 2.03) mmol·m -2·s -1), 并且尾叶桉和木荷的GS1与GS2的线性拟合斜率分别为0.92 (R 2 ≈ 0.70)和0.98 (R 2 ≈ 0.76) , 表明GS1比GS2高估了冠层气孔导度。另外, GS1和GS2对水汽压亏缺的敏感性与参比气孔导度(GSiref, D = 1 kPa时的气孔导度)的比值Pi与Ω紧密相关。根据统计, 尾叶桉和木荷的GS1估计值在Ω = 0.05-0.15 (83.1%的数据)和0.10-0.20 (47.8%的数据)之间时是相对可靠的。 相似文献
18.
《植物生态学报》2017,41(8):914
Mesophyll conductance (gm) represents the CO2 diffusion facility from sub-stomatal internal cavities to carboxylation sites in chloroplasts, and the variation of gm across genotypes as well as environmental conditions is expected to be related to the anatomical structures and biochemical properties of leaves. In recent years, the variation of gm has attracted wide attention. The limiting factors in photosynthetic rate are no longer divided simply into stomatal limitation and non-stomatal limitation, but splitted in stomatal limitation, mesophyll limitation and carboxylation limitation. In this review, we summarize the potential influences of cell wall, cell membrane, cytoplasm, chloroplast envelope and stroma on gm, and indicate that cell wall thickness and the surface area of chloroplast exposed to intercellular air space (Sc) are the most important factors influencing the gm. We also analyze the probable effects of biochemical process related with aquaporins and carbonic anhydrase on gm. Meanwhile, the regulation mechanisms of long- and short-term environment changes (including temperature, light intensity, drought, and nutrients) on gm are also summarized. The relationship between gm and hydraulic conductance (Kleaf) is debated. Finally, we discuss the scientific problems related with gm. 相似文献
19.
《植物生态学报》1958,44(5):515
作为地球表层重要的组成部分, 陆地生态系统是人类生存和发展的重要场所。进入21世纪以来, 气候变化导致干旱事件发生的强度、频度和持续时间显著增加, 对陆地生态系统带来深远的影响, 严重制约甚至威胁人类社会的可持续发展。因此, 开展极端干旱对陆地生态系统影响的研究并评估其生态风险效应, 是当前全球变化领域研究的重点问题。该文从植物生理生态过程、生物地球化学循环、生物多样性以及生态系统结构和功能4个方面综述了极端干旱对陆地生态系统的影响, 并对当前的研究热点进行探讨, 深度剖析当前研究中存在的难点问题和未来可能的发展方向, 以期为未来开展干旱对陆地生态系统影响的观测与预测研究提供参考, 为在未来干旱影响下加强陆地生态系统风险评估和管理提供新思路。 相似文献
20.
《植物生态学报》1958,44(5):475
Due to huge consumption of fossil fuels and chemical fertilizers, substantial amount of anthropogenic reactive nitrogen (N) has been released into the environment. Therefore, N deposition has gradually increased worldwide and become one of the most important issues of global change. China has been a N deposition hotspot, and N deposition is projected to last long duration, which poses serious threats to ecosystem stability and functionality. In this synthesis paper, we summarized the impacts of N deposition on aboveground vegetation, soil microorganisms and biogeochemical cycling of major elements (carbon, N and phosphorus) in terrestrial ecosystems by outlining the progresses in the research field during the past 40 years. Results indicate that the accumulation of reactive N compounds induced by N deposition alters the soil environment, ecological stoichiometric balance and species co-occurrence patterns, thereby changing biodiversity and ecosystem functions. The rates, forms and duration of N deposition and the homeostasis of biosystem together with abiotic environments determine the direction and extent of the ecosystem response to N deposition. Through analysing local and foreign studies in this research area, we explore the weaknesses of relevant research that are being conducted in China. To advance the basic research on and risk management of N deposition, we propose the establishment of a N deposition monitoring and research network across the country with consideration of different ecosystems to promote regional and global risk assessments. Future research should highlight the combined multiple factors with N deposition and conduct direct and in-depth mechanism studies. 相似文献