峰丛洼地恢复演替系列优势种光合生理生态特征日变化研究——以广西马山弄拉峰丛洼地为例

运用LI-6400便携式光合测定系统,测定弄拉峰丛洼地不同演替阶段优势种白茅、黄荆、红背山麻杆、黄杞和青冈的光合生理生态特性,并比较它们的净光合作用速率、蒸腾作用速率、气孔导度、水分利用效率、表观量子效率等生理生态指标及其生境中对应的光合有效辐射、大气CO2浓度、气温、相对湿度的日变化。结果表明,峰丛洼地生态环境因子日变化复杂,黄杞有明显的"午休"现象,先锋种黄荆、红背山麻杆的净光合作用速率、蒸腾速率和气孔导度较大,先锋种中C4植物白茅水分利用效率最高,演替后期优势种青冈和黄杞的表观光量子效率、利用岩溶区水分的效率和适应性更强。对净光合作用速率与生理生态影响因子进行相关性分析,表明生理和生态因子共同影响植物的光合作用,不同演替优势种的影响因子有差异。以逐步回归方式建立净光合作用速率和影响因子之间的回归方程模型,5个方程均有显著性意义和良好的预测性。     

陕西子午岭生态因素对植物群落的影响

为探讨生境对植被格局分布的影响,对黄土高原马栏林区60块样地进行植被学调查的基础上,采用17个环境指标刻画植物群落的空间位置、地形和土壤特征;利用双向指示种分析(TWINSPAN)划分了该区不同演替阶段的植物群落类型;利用前向选择法(forward selection)及Monte Carlo检验对不同演替阶段植物群落物种组成影响显著(p＜0.05)的环境因子进行筛选;利用去势典范对应分析(DCCA)排序方法分析不同演替阶段植物群落分布格局与环境的关系;利用偏典范对应分析(partial CCA)定量分离环境、空间及其交互作用对植被格局总体变异的影响.结果表明:(1)马栏林区的植物群落可划分为13个类型,分别属于4个不同的演替阶段;(2)对演替初期阶段群落影响显著的环境因子是土壤含盐量和碱解氮,对演替过渡阶段群落影响显著的环境因子是海拔和腐殖质厚度,对演替亚顶级阶段群落影响显著的因子是海拔、坡向、枯落物厚度、腐殖质厚度和pH值,而对演替顶级阶段群落分异影响显著的因子是海拔、坡向、pH值和速效磷;(3)不同演替阶段群落的生态学特性和分布规律与环境空间的生态梯度格局吻合较好;(4)随着演替的进行,环境因子单独对植物群落的影响越来越大,而样地位置单独作用和样地位置与环境因子的交互作用之和越来越小.     

古浪县北部荒漠植被主要植物种的生态位特征

利用Shannon-Wiener生态位宽度公式和Pianka生态位重叠公式,计测分析了甘肃省古浪县北部荒漠植被主要植物种在不同植被演替阶段的生态位宽度和生态位重叠。结果表明:在流动沙地上花棒的生态位宽度最大,其次是沙蒿;在半固定沙地上白刺的生态位宽度最大;在固定沙地上,不论是封育植被还是未封育植被中均是花棒的生态位最宽。同一植物种的生态位随着植被演替阶段的变化而发生变化,这种变化反映了不同演替阶段下的植被恢复效果。优势种的生态位重叠大,生态位宽的物种对重叠值也大,相同物种对在不同演替阶段的生态位重叠不一致。有些物种生态位宽度窄,但重叠值大,是由荒漠植被区物种分布存在生境斑块现象造成的。     

上海新江湾地区废弃地低干扰植物群落优势树种的光合生理生态特征

以上海市杨浦区原废弃地(新江湾地区)半自然群落的主要优势树种为对象,测定不同生活型植株在夏季不同生境下叶片的光合特性,从光合生理生态角度分析低干扰条件下上海城市废弃地的植物群落次生演替过程的特点,并结合环境因子分析并预测植物群落结构的动态变化。结果表明:(1)冠层树种光合作用日变化曲线呈双峰型,林窗树种呈单峰型,而林下树种呈不规则变化,体现出亚热带地区植物在夏季典型气候下的"光合午休"现象,而生境特点同时也影响植物光利用对策。(2)冠层成年树以落叶树种刺槐和朴树的日均净光合速率最高,且具有较高的光饱和点;在林下生境中,以强耐阴灌木植物胡颓子的日均净光合速率最高,其次为常绿树种香樟和女贞的幼树和幼苗,而林下落叶树种日均净光合速率均较低。(3)影响冠层树种的净光合速率因子中,生态因子是第一主成分,而对于林窗树种,第一主成分则是生理因子。(4)由于阳性落叶树种具有更高效的光合效率,能迅速占领上层空间,新江湾区域人为低干扰植物群落的演替早期均以扩散能力较强的先锋性树种为主;乔木群落形成后,林下更新苗则以光适应范围较宽的香樟、女贞为主,同时,上层落叶树种大规模自然衰退使得香樟和女贞逐步替代落叶树种。     

公路碾压干扰下群落植物多样性——以藏北矮嵩草草甸为例

运用时空替换法,以空间变换替代时间变换,对公路碾压干扰下藏北矮嵩草草甸恢复演替中不同阶段群落植物多样性进行研究.结果表明：各草地群落样方中共出现高等植物33种,其中菊、豆、禾本科和蔷薇科合计16种,占48.48﹪,在其自然恢复演替所起的作用最大;莎草科植物作为顶级群落的建群种具有重要作用.物种构成具有明显的阶段性特征：演替前期以1年生和2年生植物为主;中期多年生草本植物逐渐占据优势;后期矮嵩草成为单优势种;菊叶萎陵菜和二裂萎陵菜几乎贯穿始终.物种积聚主要是在演替前期和中期完成,其积聚过程符合二次曲线.演替后期群落植物多样性程度最高,多样性随演替进程表现为逻辑斯谛增长规律：前期群落物种丰富度较低,均匀度较高,生态优势度？也比较高,但综合多样性较低;中期群落的均匀度下降,生态优势度也同时下降,综合多样性高;后期矮嵩草成为群落的单优势种,群落的均匀度和生态优势度均下降,综合多样性仍然增加.     

毛乌素沙地油蒿和牛心朴子生理生态学研究

 作为毛乌素沙地植被主要建群种的油蒿(Artemisia ordosica)在一些地方出现了不同程度的退化,而萝摩科的一种多年生草本植物牛心朴子(Cynanchum komarovii)却出现了繁茂的生长。它们之间存在着一定的演替关系。本文通过对油蒿和牛心朴子的生理生态学特性和生殖生物学特性的研究及对其生境各要素的分析,说明了油蒿具有变水植物的特点,牛心朴子具有恒水植物的特点。在不同立地条件下,两种植物的光合、蒸腾及气孔行为都不相同。即便是在相同立地条件下,牛心朴子的水分利用效率亦显著高于油蒿;并且,牛心朴子只受轻微水分胁迫或不受水分胁迫,而油蒿则始终处于水分胁迫之下,说明牛心朴子在竞争中比油蒿占有相对的优势。在生态诸因子中,土壤水分状况是演替的外因,两种植物的水分生理生态特性和生殖生物学特征的差异是演替的内因。     

长江口湿地三个演替阶段大型底栖动物群落特征

2001—2005年对长江口新生沙洲九段沙(上沙、中沙、下沙)盐沼演替序列不同阶段[盐渍藻类阶段(SA)、海三棱草(Scirpusmariqueter)—草(Scirpustriqueter)阶段(MT)、芦苇(Phragmitesaus-tralis)—互花米草(Spartinaalterniflora)阶段(AA)]的大型底栖动物群落特征进行了分析研究。大型底栖动物群落的物种数、Shannon-Wiener多样性指数、Pielou均匀度指数、密度及生物量都是MT>AA>SA。SA、AA优势种的生活型分别是底内型、穴居型;MT优势种的生活型是底上附着型和穴居型。不同沙洲相同盐沼演替阶段大型底栖动物群落结构都较为相似,盐渍藻类阶段的相似性最高;不同演替阶段间差别明显,SA和AA间差别最大。不同盐沼演替阶段大型底栖动物群落特征的明显差异,既反映了环境沿盐沼演替序列的梯度变化,也体现了不同盐沼对底栖动物群落作用的差别,同时也显示了大型底栖动物对不同盐沼演替阶段生境的适应。     

黄土高原先锋种猪毛蒿叶片形态解剖与生理特征对立地的适应性

为了揭示黄土丘陵沟壑区撂荒地植被演替前期优势种猪毛蒿(Artemisia scoparia)对该区立地环境的适应性,探讨猪毛蒿演替生态位的变化,研究了陕北黄土丘陵沟壑区3种立地环境下(阳峁坡、峁顶、阴峁坡)猪毛蒿叶片形态解剖和生理特征的变化,以及这些变化与生态因子之间的相互关系。结果表明:(1)猪毛蒿叶片具有适应该区半干旱环境的形态及解剖结构:叶片针形化、具表皮毛、环栅型叶肉组织、海绵组织特化为贮水组织、维管束退化、具裂生分泌腔,C3植物呈现类似CAM植物的叶片特性;(2)在土壤、空气湿度相对干燥和强光生境的阳峁坡与峁顶,猪毛蒿具有较小的叶面积、发达的栅栏组织、致密的表皮毛和紧密的细胞间隙,而在生境条件较好的阴峁坡则呈相反趋势;(3)阳峁坡猪毛蒿叶片相对含水量和叶绿素含量较小,超氧阴离子自由基增加,但植物体内超氧化物歧化酶和抗坏血酸含量增加以清除植物体内产生的活性氧;(4)冗余及相关性分析表明,猪毛蒿叶片形态、解剖和生理指标的可塑性对立地光照强度、土壤水分和有机质含量较为敏感,同时其形态解剖与生理可塑性可共同调节来适应生境。综合分析,猪毛蒿对陕北黄土丘陵沟壑区撂荒初期光照强度大、土壤贫瘠但土层干化现象尚未出现的立地环境有较好的适应性,使其成为黄土高原植被自然演替过程中的先锋物种。     

海南鹿回头岸礁造礁石珊瑚群落结构动态Ⅱ.物种多样性

根据石珊瑚物种的总数、石珊瑚覆盖的百分率、物种多样性和均匀度,对鹿回头岸礁造礁石珊瑚群落结构类型所处在演替阶段的时间状态和生境的空间状态进行分析。在中等和深水区物种多样性的时间变异,随演替的发展而有所下降;浅水区不随演替而变化。在不同生境区珊瑚生长的聚群上,与时间的发展无关;每个演替时期,物种多样性的类型与生境的变化有关。     

大明山常绿阔叶林演替序列种群生态位动态特征

以广西大明山自然保护区常绿阔叶林的4个演替序列（15、30、60、160年）的群落为对象,分析了演替进程中优势种群重要值、生态位宽度与生态位重叠的动态特征。结果表明：杉木（Cunninghamia lanceolata）、罗浮栲（Castanopsis fabri）、云贵山茉莉（Huodendron biaristatum）、广东琼楠(Beilschmiedia fordii)分别是4个演替序列群落的优势种群,这些优势种群的作用明显,具有最大的生态位宽度。每个序列中较大生态位宽度的物种之间以及与其他物种之间的生态位重叠程度也较高。较小重要值的物种具有较宽生态位的现象暗示了该物种有可能成为下一演替序列的优势物种,较小生态位宽度的物种与其他物种之间的生态位重叠值较大的现象是生境破碎化和空间异质性的结果。整个演替序列中种群生态位宽度与生态位重叠平均值共同呈现了逐渐下降并在最后阶段稍有上升的曲线特征,说明随着演替时间的增加,竞争以及环境资源的变化导致各物种出现了一定程度的生态位分化,种间生态位重叠程度降低,逐渐形成一个结构稳定的群落。     

Arbuscular mycorrhizal fungal communities change among three stages of primary sand dune succession but do not alter plant growth

Plant interactions with soil biota could have a significant impact on plant successional trajectory by benefiting plants in a particular successional stage over others. The influence of soil mutualists such as mycorrhizal fungi is thought to be an important feedback component, yet they have shown benefits to both early and late successional plants that could either retard or accelerate succession. Here we first determine if arbuscular mycorrhizal (AM) fungi differ among three stages of primary sand dune succession and then if they alter growth of plants from particular successional stages. We isolated AM fungal inoculum from early, intermediate or late stages of a primary dune succession and compared them using cloning and sequencing. We then grew eight plant species that dominate within each of these successional stages with each AM fungal inoculum. We measured fungal growth to assess potential AM functional differences and plant growth to determine if AM fungi positively or negatively affect plants. AM fungi isolated from early succession were more phylogenetically diverse relative to intermediate and late succession while late successional fungi consistently produced more soil hyphae and arbuscules. Despite these differences, inocula from different successional stages had similar effects on the growth of all plant species. Host plant biomass was not affected by mycorrhizal inoculation relative to un‐inoculated controls. Although mycorrhizal communities differ among primary dune successional stages and formed different fungal structures, these differences did not directly affect the growth of plants from different dune successional stages in our experiment and therefore may be less likely to directly contribute to plant succession in sand dunes.     

Can Establishment Characteristics Explain the Poor Colonization Success of Late Successional Grassland Species on Ex‐Arable Land?

Abstract Many grassland restoration projects on former arable land face problems because early successional grassland species establish vigorously and persistently but late successional grassland species fail to establish. Differences in establishment characteristics of early and late successional species might provide an explanation for the failure of many late successional species to colonize grasslands on ex‐arable land. I examined whether early and late successional species had different establishment rates in the initial years of a grassland succession, whether a specific establishment stage (seedling emergence, mortality or growth) could be identified as the key process controlling establishment, and what management would enhance the establishment of late successional grassland species. Seeds of three early and three late successional species were sown separately in ex‐arable plots with bare soil, 1‐year‐old vegetation, and 2‐year‐old vegetation. Emergence, mortality, and seedling growth were monitored for 1 year. Early successional species established successfully in the bare soil plots but failed to establish in plots with 1‐ and 2‐year‐old vegetation. Late successional species showed either lower establishment rates in the younger succession stages or decreased establishment with succession that nevertheless resulted in significant establishment in the oldest plots. Seedling emergence proved to be the key factor determining the establishment pattern of early and late successional species. In absolute numbers, emergence of late successional species was, however, similar or higher than that of early successional species, even in the earliest succession stage. The poor establishment of late successional species on former arable land could therefore not be explained solely by differences in establishment characteristics between early and late successional grassland species. Competitive processes between early and late successional species later in the life cycle probably play an important role. The results do point out that establishment of late successional species can be promoted by creating vegetative cover from the start of the restoration effort.     

Amino acid uptake in deciduous and coniferous taiga ecosystems

We measured in situ uptake of amino acids and ammonium across deciduous and coniferous taiga forest ecosystems in interior Alaska to examine the idea that late successional (coniferous) forests rely more heavily on dissolved organic nitrogen (DON), than do early successional (deciduous) ecosystems. We traced ¹⁵N-NH₄⁺ and ¹³C-¹⁵N-amino acids from the soil solution into plant roots and soil pools over a 24 h period in stands of early successional willow and late successional black spruce. Late successional soils have much higher concentrations of amino acid in soil solution and a greater ratio of DON to dissolved inorganic N (DIN) (ammonium plus nitrate) than do early successional soils. Moreover, late successional coniferous forests exhibit higher rates of soil proteolytic activity, but lower rates of inorganic N turnover. Differences in ammonium and amino acid uptake by early successional willow stands were insignificant. By contrast, the in situ uptake of amino acid by late successional black spruce forests were approximately 4-fold greater than ammonium uptake. The relative difference in uptake of ammonium and amino acids in these forests was approximately proportional to the relative difference of these N forms in the soil solution. Thus, we suggest that differences in uptake of different N forms across succession in these boreal forests largely reflect edaphic variation in available soil N (composition), rather than any apparent physiological specialization to absorb particular forms of N. These finding are relevant to our understanding of how taiga ecosystems may respond to increases in temperature, fire frequency, N deposition, and other potential consequences of global change.     

Environmental Heterogeneity Influences Successional Trajectories in Colombian Seasonally Dry Tropical Forests

Environmental characteristics have a major effect on the species composition of seasonally dry tropical forest. However, this effect has been little considered when describing secondary succession of this ecosystem. We tested the hypothesis that local environmental heterogeneity influences successional trajectories when high species richness is available. Changes in species composition and structure were described in 126 vegetation plots differing in successional stage and located along a topographical and soil nutrient gradient. Variation in community composition was partitioned between successional stage, environmental characteristics, and spatial structure using redundancy analyses. In addition, relationships between plot distance matrices for these factors were analysed by means of Mantel tests. High species turnover was observed during succession and species composition similarity was higher among late successional forest than among early and intermediate forests. A higher portion of variation in species composition was explained by environmental characteristics compared to successional stage, whereas the spatial structure of the data was weak. Our results suggest that in the region of study, variation in the successional trajectories is occurring owing to environmental heterogeneity, as well as to human disturbance and other unmeasured processes.     

Rate of succession in restored wetlands and the role of site context

Question: Are changes in plant species composition, functional group composition and rates of species turnover consistent among early successional wetlands, and what is the role of landscape context in determining the rate of succession? Location: Twenty‐four restored wetlands in Illinois, USA. Methods: We use 4 years of vegetation sampling data from each site to describe successional trends and rates of species turnover in wetlands. We quantify: (1) the rate at which composition changes from early‐successional to late‐successional species and functional groups, as indicated by site movement in ordination space over time, and (2) the rate of change in the colonization and local extinction of individual species. We correlate the pace of succession to site area, isolation and surrounding land cover. Results: Some commonalities in successional trends were evident among sites. Annual species were replaced by clonal perennials, and colonization rates declined over time. However, differences among sites outweighed site age in determining species composition, and the pace of succession was influenced by a site's landscape setting. Rates of species turnover were higher in smaller wetlands. In addition, wetlands in agricultural landscapes underwent succession more rapidly, as indicated by a rapid increase in dominance by late‐successional plants. Conclusions: Although the outcome of plant community succession in restored wetlands was somewhat predictable, species composition and the pace of succession varied among sites. The ability of restoration practitioners to accelerate succession through active manipulation may be contingent upon landscape context.     

The role of plant resources in forest succession: changes in radiation, water and nutrient fluxes, and plant productivity over a 300-yr-long chronosequence in NW-Germany

In the past insufficient attention has been paid to quantitative measurements of resource fluxes in ecosystems that undergo successional change. In this study, simultaneous changes in seven plant resources (photosynthetically active radiation (PAR), water, nitrogen, phosphorus, calcium, magnesium and potassium) are quantified by a chronosequence approach for a 300-yr-long secondary succession on poor soil from Calluna vulgaris heathland to Fagus sylvatica-Quercus petraea late-successional forest (heathland-to-forest succession).Above-ground net primary production increases sevenfold, and total above-ground phytomass about fortyfold during heathland-to-forest succession. Plant organs that capture resources increase much more slowly (leaf area index: threefold; fine root biomass: 1.3-fold). The increase in productivity is based both on higher absorptivity and conversion efficiency of PAR by the canopies of the successional plants.Accumulation of organic material on the forest floor significantly improves soil water availability. Evapotranspiration losses increase early in succession as the growing vegetation increases in both height and leaf area but tend to decrease again in the late-successional community. Drainage losses are at their minimum at the conifer-dominated pioneer forest stage.Accumulation of available nutrients in the soil is a key process in heathland-to-forest succession that significantly improves plant nutrient availability but leads to only minor changes in carbon/nutrient ratios and humus quality. Litter decomposition rates increase and result in a more rapid nutrient turnover in late successional stages. External nutrient inputs (from the atmosphere and soil weathering) significantly contribute to plant nutrient supply early in succession, whereas the internal cycling of nutrients through litter fall and nutrient mineralisation by far exceeds external inputs at the late stages.Vitousek & Reiners' (1975) ecosystem nutrient loss hypothesis is supported by the heathland-to-forest succession data. Odum's (1969) hypotheses on how nutrient cycles change during the course of succession is, in one part, rejected, in part supported. Tilman's (1988) hypothesis on nutrient limitation early, and light limitation late in primary succession is rejected.     

Multiple successional pathways of boreal forest stands in central Canada

Predicting forest composition change through time is a key challenge in forest management. While multiple successional pathways are theorized for boreal forests, empirical evidence is lacking, largely because succession has been inferred from chronosequence and dendrochronological methods. We tested the hypotheses that stands of compositionally similar overstory may follow multiple successional pathways depending on time since last stand‐replacing fire (TSF), edaphic conditions, and presence of intermediate disturbances. We used repeated measurements from combining sequential aerial photography and ground surveys for 361 boreal stands in central Canada. Stands were measured in 8–15 yr intervals over a ~ 60 yr period, covering a wide range of initial stand conditions. Multinomial logistic regression was used to analyze stand type transitions. With increasing TSF, stands dominated by shade‐intolerant Pinus banksiana, Populus sp., and Betula papyrifera demonstrated multiple pathways to stands dominated by shade‐tolerant Picea sp., Abies balsamea, and Thuja occidentalis. Their pathways seemed largely explained by neighborhood effects. Succession of stands dominated by shade‐tolerant species, with an exception of stands dominated by Picea sp., was not related to TSF, but rather dependent on edaphic conditions and presence of intermediate disturbances. Varying edaphic conditions caused divergent pathways with resource limited sites being dominated by nutrient‐poor tolerant species, and richer sites permitting invasion of early successional species and promoting species mixtures during succession. Intermediate disturbances promoted deciduous persistence and species diversity in A. balsamea and mixed‐conifer stands, but no evidence was detected to support “disturbance accelerated succession”. Our results demonstrate that in the prolonged absence of stand‐replacing disturbance boreal forest stands undergo multiple succession pathways. These pathways are regulated by neighborhood effects, resource availability, and presence of intermediate disturbance, but the relative importance of these regulators depends on initial stand type. The observed divergence of successional pathways supports the resource‐ratio hypothesis of plant succession.     

茂兰喀斯特森林不同演替阶段植物叶片功能性状与土壤因子的关系

植物如何改变功能性状来适应环境一直是生态学的研究征点。为探究茂兰喀斯特森林不同演替阶段植物叶片的适应策略，该文以茂兰自然保护区5个不同演替阶段(草本、灌木、灌乔、乔木和顶极群落阶段)优势种为研究对象，测定不同演替阶段的优势植物叶片功能性状与土壤理化性质。结果表明：(1)随着植被正向演替的进行，土壤全氮(STN)含量、土壤有机质(SOM)含量、土壤含水量(SWC)逐渐增加，土壤全磷(STP)含量和土壤全钾(STK)含量先增加后减少，土壤pH值整体呈减小的趋势。(2)随着植被演替的进行，叶面积(LA)、叶干物质含量(LDMC)、叶厚度(LT)和叶片碳含量(LCC)逐渐上升，比叶面积(SLA)与叶片钾含量(LKC)则与之相反，叶片氮含量(LNC)呈先升后降的趋势，叶片磷含量(LPC)呈先降后升的趋势。(3)冗余分析表明，演替初期植物主要分布在土壤pH值高而STK、STP、SWC、SOM、STN相对低的环境中，群落内植物叶片采取高SLA、LNC、LPC,低LA、LDMC、LT、LWC的性状组合，演替晚期植物主要分布在土壤水分和养分含量较高的环境，LDMC、LT、LA、LWC与演替初期相比呈上升...     

Conifer seedling recruitment in a southeastern Canadian boreal forest: the importance of substrate

Abstract. In order to explain conifer species recruitment in Canada's southeastern boreal forest, we characterized conifer regeneration microsites and determined how these microsites vary in abundance during succession. Microsite abundance was evaluated in deciduous, mixed and coniferous stands along a 234-yr postfire chronosequence. Conifers were most often found in relatively well-illuminated microsites, devoid of litter, especially broad-leaf litter, and with a reduced cover of lower vegetation (< 50 cm tall). Although associated with moss-rich forest floor substrates, Abies balsamea was the most ubiquitously distributed species. Picea glauca and especially Thuja occidentalis seedlings were frequently found on rotten logs. Light measurements did not show differences among seedling species nor between stand types. The percentage cover of broad-leaf litter decreased significantly during succession. Also, rotten logs covered with moss occupied a significantly larger area in the mid-successionnal stands than in early successional deciduous or late successional coniferous stands. The results suggest that the presence of specific forest floor substrate types is a factor explaining low conifer recruitment under deciduous stands, conifer codominance in the mid-successional stage, and delayed Thuja recolonization after fire. Results also suggest that some facilitation mechanism is responsible for the observed directional succession.     

Microbial community composition but not diversity changes along succession in arctic sand dunes

The generality of increasing diversity of fungi and bacteria across arctic sand dune succession was tested. Microbial communities were examined by high‐throughput sequencing of 16S rRNA genes (bacteria) and internal transcribed spacer (ITS) regions (fungi). We studied four microbial compartments (inside leaf, inside root, rhizosphere and bulk soil) and characterized microbes associated with a single plant species (Deschampsia flexuosa) across two sand dune successional stages (early and late). Bacterial richness increased across succession in bulk soil and leaf endosphere. In contrast, soil fungal richness remained constant while root endosphere fungal richness increased across succession. There was, however, no significant difference in Shannon diversity indices between early and late successional stage in any compartment. There was a significant difference in the composition of microbial communities between early and late successional stage in all compartments, although the major microbial OTUs were shared between early and late successional stage. Co‐occurrence network analysis revealed successional stage‐specific microbial groups. There were more co‐occurring modules in early successional stage than in late stage. Altogether, these results emphasize that succession strongly affects distribution of microbial species, but not microbial diversity in arctic sand dune ecosystem and that fungi and bacteria may not follow the same successional trajectories.