海南俄贤岭石灰岩山地海南大戟灌丛群落研究

根据样方调查,对海南俄贤岭自然保护区海南大戟灌丛群落的种类组成、外貌、结构特征和物种多样性进行分析。结果表明,在700m2样地中,有维管植物77种,隶属于47科70属。群落中乔木的个体数量很少,主要由灌木和草本组成,灌木层主要优势种为海南大戟等。群落外貌常绿,生活型以小高位芽为主,占22.08%;按照Raunkiaer的频度等级定律,属于B级的种类最多,频度值为43.42。整个群落的物种丰富度Magarlef指数为8.56,Shannon-Wiener指数为1.38,Simposon为0.90,均匀度指数为0.32。群落各层次的丰富度格局表现为灌木层>草本层>乔木层>藤本植物,多样性格局为灌木层>乔木层>草本层<(>)藤本植物,均匀度格局为乔木层>藤本植物>灌木层>草本层。     

浙江天童灌丛群落的种类组成、结构及外貌特征

根据野外调查的样地资料 ,分析了浙江天童地区灌丛的群落特征。结果表明 ,该区灌丛共有维管束植物94种 ,隶属于 45科 ,76属。地理成分分析表明 ,该区灌丛具有次生、退化的性质。生活型和叶的性质的分析表明 ,该区灌丛群落的外貌主要由小型和中型草质落叶及常绿革质的、非全缘单叶高位芽植物所决定。在分析灌丛群落特征的基础上 ,还对其生态恢复进行了探讨。     

澳门青洲山翻白叶树群落特征及物种多样性研究

根据样方调查结果,对澳门青洲山翻白叶树(Pterospermum heterophyllum)群落的种类组成、外貌、结构特征与动态及物种多样性进行分析.结果表明:(1)在1 600 m2样地中,有维管束植物47种,隶属于29科44属;对乔木层和灌木层主要物种的重要值以及频度分析结果显示,该群落是以翻白叶树为主的单优种群落,群落种类组成多样性和水平分布不均匀,其外貌终年常绿;对优势种种群的年龄结构分析显示,该种群处于增长状态;(2)整个群落的物种丰富度Margalef指数为13.72,Shannon-Wiener指数为1.15,Simpson指数为0.875,均匀度指数为0.34,该群落的层次格局为:灌木层>藤本层>乔木层>草本层;(3) 与其他5个不同类型地区森林群的物种多样性比较结果显示,澳门翻白叶树群落的物种多样性明显低于其他5个森林群落.     

不同处理措施下浙江天童灌丛群落组成结构的变化

采用物种丰富度,Simpson指数,Shannon-Wiener指数,群落均匀度指数研究浙江天童灌丛群落在人工处理下群落的α多样性动态特征,采用β多样性指数和相似性系数测定该区灌丛群落在处理后群落间多样性的变化,此外,还分析了实验样地及对照样地在处理前后的种类组成及其重要值的变化。结果表明,除对照样地外,各实验样地的种类组成及其重要都有不同程度的改变;与处理前相比,实验样地灌木层的物种多样性有所减少,但生态优势度及群落均匀度有所提高,β多样性的研究结果同样表明在实验处理措施下各实验样地的种类组成已经发生了一定的变化。     

广东古兜山自然保护区蕨类植物群落的特征

通过对广东新会古兜山自然保护区中108个5m ×5m的蕨类植物样方调查,初步分析了样方中蕨类植物的种类组成和区系特点及种群的多度、频度、重要值、蕨类的生长型、叶的性质和群落的外貌、季相等群落学特征。结果表明:(1)古兜山自然保护区的蕨类植物种类具有典型的南亚热带植物区系特点,热带亚洲植物区系成分对古兜山蕨类植物区系有强烈影响;(2)由于蕨类植物种群的随机分布和环境因子的异质性,种群的多度和重要值分布表现出明显的正态分布规律;(3)样方中蕨类植物的形态外貌、叶的性质及其群落的外貌和季相均表现出典型的南亚热带蕨类植物群落特征;古兜山自然保护区的蕨类植物可划分为花篮状蕨类、树蕨类、匍匐类、攀援类、附生类5种生长型类型。     

广东石门台自然保护区粘木—甜锥群落特征研究

根据样方调查的结果 ,分析了广东石门台自然保护区粘木—甜锥群落的种类组成 ,区系成分 ,外貌特征和年龄结构。结果表明 ,在 5 0 0m2 样方中 ,有维管束植物 78种 ,分别隶属 46科、64属 ;优势科为樟科、山茶科、壳斗科、茜草科等。热带 -亚热带区系成分在群落中占明显优势 ,具有南亚热带向中亚热带过渡的特点。群落的生活型以高位芽为主 ,群落外貌主要由革质、单叶和中、小型叶为主的常绿阔叶林高位芽植物决定。群落成层现象明显 ,可分为乔木层、灌木层、草本层 ,乔木层可再划分为 2～ 3个亚层。种群的立木结构表明 ,粘木种群已处于衰退状态 ,将来有被其他种群替代的可能。对粘木的保护应采取采种育苗 ,扩大其种植面积的保护措施。     

峨眉山峨眉栲、华木荷群落研究

 峨眉栲、华木荷群落是我国西南部亚热带山地常绿阔叶林群落的主要代表类型。本文从群落分布区域自然环境、群落植物组成特点、群落外貌和结构特征以及主要种群的结构及动态趋势等方面对该群落进行了较全面的探讨,并将其与我国部分同类或类似群落作了系统的比较分析,阐明了该群落的性质、特征和演变趋势。1．尽管该群落分布于我国中亚热带,但区域性环境独特,使该群落保存了较强的热带残遗性和亚热带雨林特征。2．样地调查统计有维管植物61科116属171种,区系组成复杂,地理成分以热带分布类型居多,物种多样性指数较高。3．群落外貌是由中小型叶、革质与厚革叶、单叶的常绿高位芽植物所决定。群落垂直结构较复杂,地上成层较明显,优势种显著。4．主要种群及其苗木的分布格局多呈集群分布,体现出中亚热带湿性常绿阔叶林种群个体的水平空间配置及分布特点。5．群落主要种群的年龄结构均处于增长和相对稳定状态,各年龄级的分布具有较高的生态结构水平,但仍存在种间竞争替代现象,表明群落尚处于进展演替阶段。6．各样地间种类相似性较高,群落内种类分布相对一致。乔木种间联结性具有一定规律,反映了环境梯度变化和群落种类分布关系。     

澳门青洲山白楸+假苹婆+破布叶群落特征研究

采用样方调查法对澳门青洲山白楸（Mallotus paniculatus）＋假苹婆（Sterculia lanceolata）＋破布叶（Microcos paniculata）群落的种类组成、外貌、结构特征、区系和物种多样性进行了分析,结果表明,1700m2样方中有维管植物70种,隶属于42科65属,其中热带性分布属占90.32%,群落属于南亚热带常绿阔叶林植被类型。群落外貌常绿,生活型以藤本高位芽为主（占22.86%）。群落的物种丰富度Magarlef指数为8.78,Shannon-Wienner指数为2.22,Simpson指数为0.98,均匀度Pielou指数为0.52。群落各层次的丰富度、Simpson指数以及Shannon-Wienner指数均表现为下木层〉乔木层〉藤本植物〉草本层,均匀度表现为藤本植物〉乔木层〉下木层〉草本层,表明下木层中组成的种类较乔木层多,优势树种较乔木层明显。     

河北衡水湖国家级自然保护区水鸟群落特征及其季节性变化

2020年5月—2021年4月,对河北衡水湖国家级自然保护区进行了水鸟调查,共记录水鸟82种,隶属于7目14科。其中,鹬科、鹭科和鸭科鸟类共同组成了该区域水鸟群落的优势类群,涉禽种类多、种群规模小,游禽种类少、种群规模大。豆雁、苍鹭、灰翅浮鸥等为自然保护区内水鸟群落的优势种。不同月份水鸟群落的物种丰富度、种群数量、物种多样性指数差异较大,其最大值分别出现在3—4、1和5月。总体上,衡水湖自然保护区水鸟物种丰富度维持较高水平,迁徙期水鸟物种丰富度和Shannon多样性指数更高,越冬期水鸟种群数量更大,7月水鸟物种丰富度最低、Pielou均匀度指数最高。迁徙期的水鸟群落相似度普遍较高,春季迁徙期鸻鹬类种数占比高,秋季迁徙期和越冬期雁鸭类种数占比高、种群数量大。此外,本次调查共记录国家重点保护水鸟18种,集中出现在越冬期及早春和晚秋。     

太岳林区连翘灌丛群落特征的研究

根据野外调查的样地资料,本文分析了分布于山西太岳山林区的连翘灌丛群落的种类组成、区系成分、外貌特征、垂直结构等基本生态学特征,并将连翘样方以及上层无乔木覆盖灌木为建群层的连翘样方归为9个群系,对连翘群落的特征以及连翘株高随海拔梯度的变化作出相应分析．结果表明：该群落种类组成丰富,区系成分以北温带分布为主,生活型以高位芽占优势。垂直分化明显,一般分为乔木层、灌木层、草本层3层,9个群系由于地理位置不同、生境特点各异,因而种类组成不同,连翘在群系中的地位也不同,各群系中主要灌木种群的分布格局一般为集群型,少数随机型,随着海拔的逐渐上升,连翘平均株高先升后降。     

Bacterial and fungal community structure in Arctic tundra tussock and shrub soils

Fungal and bacterial community structure in tussock, intertussock and shrub organic and mineral soils at Toolik Lake, Alaska were evaluated. Community structure was examined by constructing clone libraries of partial 16S and 18S rRNA genes. The soil communities were sampled at the end of the growing season in August 2004 and just after the soils thawed in June 2005. The communities differed greatly between vegetation types, although tussock and intertussock soil communities were very similar at the phyla level. The communities were relatively stable between sample dates at the phyla and subphyla levels, but differed significantly at finer phylogenetic scales. Tussock and intertussock bacterial communities were dominated by Acidobacteria, while shrub soils were dominated by Proteobacteria. These results appear consistent with previous work demonstrating that shrub soils contain an active, bioavailable C fraction, while tussock soils are dominated by more recalcitrant substrates. Tussock fungi communities had higher proportions of Ascomycota than shrub soils, while Zygomycota were more abundant in shrub soils. Recent documentation of increasing shrub abundance in the Arctic suggests that soil microbial communities and their functioning are likely to be altered by climate change.     

百花山植物群落物种多样性研究

基于百花山50个样方的调查资料，从不同类型群落的物种多样性及其与海拔的关系等方面对百花山植被进行了分析，并且用DCA排序和海拔高程排序对物种多样性在环境梯度上的分布格局进行了初步研究。结果表明：群落内不同生长型的物种丰富度指数在森林群落中大小顺序为草本层＞灌木层＞乔木层，灌丛群落主要表现为草本层﹥灌木层，只有荆条灌丛表现为灌木层＞草本层；Shannon-Wiener指数在山杨—华北落叶松群落中表现为灌木层＞草本层＞乔木层,其他森林群落为草本层＞灌木层＞乔木层，在灌丛群落中主要表现为草本层＞灌木层，只有荆条灌丛表现为灌木层＞草本层；均匀度指数在灌丛群落中表现为灌木层＞草本层，在辽东栎林和山杨—华北落叶松林中表现为灌木层＞乔木层＞草本层,而其他森林群落表现为乔木层＞灌木层＞草本层。物种多样性在DCA第一轴排序和海拔高程梯度上都表现出单峰曲线变化趋势，但拟和效果的显著程度不同：丰富度和均匀度指数在海拔高程上曲线的拟和效果优于DCA环境梯度排序效果；而多样性指数则相反。     

浑善达克沙地小叶锦鸡儿灌丛的空间异质性

豆科锦鸡儿属(C arag ana)植物因其可以生物固氮而在草原生态系统中具有特殊的地位。定量分析小叶锦鸡儿(C arag anam icrophy lla)灌丛在浑善达克沙地不同生境条件下的分布格局,有助于理解植被与土壤养分循环之间的关系和合理制定退化沙地的恢复对策。采用地统计学中的半方差分析和分形分析两种方法研究了浑善达克沙地小叶锦鸡儿灌丛的空间分布格局,分析了不同生境中小叶锦鸡儿灌丛的植被、土壤水分和养分间的相关性。结果表明:(1)小叶锦鸡儿灌丛在3种生境条件下(滩地、固定沙丘和半固定沙丘)的盖度、土壤有机质和全氮的空间分布符合球状模型,空间自相关显著;(2)土壤pH值在滩地和固定沙丘的空间分布符合球状模型且空间自相关显著,但在半固定沙丘空间自相关不显著;(3)土壤水分在3种生境中的空间分布都符合线性模型,空间自相关显著。(4)植被的变异尺度(变程)小于各个土壤要素的变异尺度。植被(小叶锦鸡儿灌丛)的分布和形成过程决定了土壤养分的分布和形成过程。当地的小叶锦鸡儿灌丛在养分“沃岛”现象的形成中起了重要作用,合理的利用和布局当地的小叶锦鸡儿灌丛的分布,可以更加有效地补充草地生态系统的养分,从而有利于加快生态系统的恢复进程。     

Examining differences in phylogenetic composition enhances understanding of the phylogenetic structure of the shrub community in the northeastern Qinghai‐Tibetan Plateau

Periodic climatic oscillations and species dispersal during the postglacial period are two important causes of plant assemblage and distribution on the Qinghai‐Tibet Plateau (QTP). To improve our understanding of the bio‐geological histories of shrub communities on the QTP, we tested two hypotheses. First, the intensity of climatic oscillations played a filtering role during community structuring. Second, species dispersal during the postglacial period contributed to the recovery of species and phylogenetic diversity and the emergence of phylogenetic overdispersion. To test these hypotheses, we investigated and compared the shrub communities in the alpine and desert habitats of the northeastern QTP. Notably, we observed higher levels of species and phylogenetic diversity in the alpine habitat than in the desert habitat, leading to phylogenetic overdispersion in the alpine shrub communities versus phylogenetic clustering in the desert shrub communities. This phylogenetic overdispersion increased with greater climate anomalies. These results suggest that (a) although climate anomalies strongly affect shrub communities, these phenomena do not act as a filter for shrub community structuring, and (b) species dispersal increases phylogenetic diversity and overdispersion in a community. Moreover, our investigation of the phylogenetic community composition revealed a larger number of plant clades in the alpine shrub communities than in the desert shrub communities, which provided insights into plant clade‐level differences in the phylogenetic structures of alpine and desert shrub communities in the northeastern QTP.     

基于茎流-蒸渗仪法的荒漠草原带人工灌丛群落蒸散特征

中国西北地区通过大量种植中间锦鸡儿(Caragana liouana)进行生态治理, 在荒漠草原带上形成人工灌丛景观, 改变了生态系统的结构和功能, 影响到地-气水汽循环过程, 研究该人工灌丛群落的蒸散特征, 对揭示其生态水文效应和指导地方生态治理实践具有重要意义。该文以宁夏盐池荒漠草原带上的人工灌丛群落为例, 利用茎流-蒸渗仪法测定了2018年5-8月的灌木蒸腾和丛下蒸散, 并分析了环境因子对人工灌丛群落蒸散的影响。结果表明: (1)茎流-蒸渗仪法所测的群落蒸散与水量平衡法、涡度相关法得到的群落蒸散有较好的一致性, 茎流-蒸渗仪法能适用于荒漠草原带人工灌丛群落蒸散及其组分结构的测定; (2)观测期内晴天的灌木蒸腾速率和丛下蒸散速率日变化趋势相近, 均为单峰曲线, 群落蒸散主要发生在日间, 但灌丛最大蒸腾速率的出现时间比丛下蒸散最大速率的出现时间晚1 h; (3) 5-8月间灌木累积蒸腾为83.6 mm, 日平均蒸腾量为0.7 mm·d^-1, 季节变化呈抛物线状; 同期丛下累积蒸散为182.5 mm, 日平均蒸散量为1.5 mm·d^-1; 丛下蒸散明显大于灌木蒸腾; (4)观测期间人工灌丛群落累积蒸散266.1 mm, 而同期的降水量为222.6 mm, 陆面水分收支处于亏缺状态; (5)净辐射是影响蒸散最主要、最直接的驱动因素, 且能够影响其他因子进而对人工灌丛群落蒸散产生作用。综上, 人工灌丛引发荒漠草原地带陆面水分收支亏缺的现象, 在生态恢复与重建中须引起注意。     

Characteristics of evapotranspiration in planted shrub communities in desert steppe zone based on sap flow and lysimeter methods

中国西北地区通过大量种植中间锦鸡儿(Caragana liouana)进行生态治理, 在荒漠草原带上形成人工灌丛景观, 改变了生态系统的结构和功能, 影响到地-气水汽循环过程, 研究该人工灌丛群落的蒸散特征, 对揭示其生态水文效应和指导地方生态治理实践具有重要意义。该文以宁夏盐池荒漠草原带上的人工灌丛群落为例, 利用茎流-蒸渗仪法测定了2018年5-8月的灌木蒸腾和丛下蒸散, 并分析了环境因子对人工灌丛群落蒸散的影响。结果表明: (1)茎流-蒸渗仪法所测的群落蒸散与水量平衡法、涡度相关法得到的群落蒸散有较好的一致性, 茎流-蒸渗仪法能适用于荒漠草原带人工灌丛群落蒸散及其组分结构的测定; (2)观测期内晴天的灌木蒸腾速率和丛下蒸散速率日变化趋势相近, 均为单峰曲线, 群落蒸散主要发生在日间, 但灌丛最大蒸腾速率的出现时间比丛下蒸散最大速率的出现时间晚1 h; (3) 5-8月间灌木累积蒸腾为83.6 mm, 日平均蒸腾量为0.7 mm·d^-1, 季节变化呈抛物线状; 同期丛下累积蒸散为182.5 mm, 日平均蒸散量为1.5 mm·d^-1; 丛下蒸散明显大于灌木蒸腾; (4)观测期间人工灌丛群落累积蒸散266.1 mm, 而同期的降水量为222.6 mm, 陆面水分收支处于亏缺状态; (5)净辐射是影响蒸散最主要、最直接的驱动因素, 且能够影响其他因子进而对人工灌丛群落蒸散产生作用。综上, 人工灌丛引发荒漠草原地带陆面水分收支亏缺的现象, 在生态恢复与重建中须引起注意。     

阿拉善荒漠灌丛群落谱系结构及其影响因子

为探究阿拉善荒漠灌丛群落的构建机制,该研究选取净亲缘关系指数(NRI)作为谱系结构指数,在对阿拉善荒漠灌丛群落野外调查的基础上,以群落物种组成为基础数据,计算各样地群落的NRI,并分析NRI在经纬度梯度上的变化趋势及其与土壤因子和水热因子的关系。结果表明:(1)阿拉善荒漠灌丛群落谱系结构在阿拉善高原东南部以发散状态为主,在阿拉善高原西部和北部地区以聚集状态为主。(2)阿拉善荒漠灌丛群落的NRI随经度的升高而减小,随纬度的升高而增大。(3)阿拉善荒漠土壤质地、土壤容重、土壤pH值和土壤有机碳含量与其群落谱系结构均无显著相关性;在降水因子和温度因子中,与群落谱系结构相关系数最大的分别为年降水量和年温度变化范围(最暖月最高温与最冷月最低温的差值),其中:年降水量与NRI呈显著负相关关系,年温度变化范围与NRI呈显著正相关关系,且最暖月最高温和最冷月最低温与NRI均有显著相关性,推测年温度变化范围对阿拉善灌丛群落谱系结构的影响是通过最暖月最高温和最冷月最低温起作用的。研究发现,阿拉善高原东南部区域的荒漠灌丛群落构成主要受竞争排斥的作用,其西部和北部地区的群落构成主要受环境过滤的影响;阿拉善荒漠灌丛群落的谱系结构主要受年降水量和极端温度的影响。     

A new ecological-wind erosion model to simulate the impacts of aeolian transport on dryland vegetation patterns

Drylands cover more than 40% of the land surface of the Earth and are characterized by patchy vegetation and that permits erosion of the surface. Vegetation-aeolian transport is an important feedback in drylands, particularly those undergoing shrub encroachment. Although one side of the feedback, the influence of vegetation loss on aeolian transport, has been well studied, the other, the influence of aeolian transport on existing vegetation, has been never studied in detail. In this study, a new ecological-wind erosion model (ECO-WEMO) that contains an aeolian transport component was created to simulate how aeolian transport impacts vegetation pattern and causes the state change. Two modeling scenarios were investigated: 1) stable grass and shrub communities without/with aeolian transport and 2) unstable shrub and grass communities without/with aeolian transport disturbed by different drought conditions. The first scenario focuses on the simulation of the influence of aeolian transport on vegetation communities and the second scenario focuses on the simulation of the state change of vegetation communities. The results from the first scenario show that: First, the mean biomasses of grass and shrub become consistent in the case of no wind in both shrub-dominated and grass-dominated communities. Second, the mean biomass of shrub becomes higher than the grass in the case of wind in shrub-dominated communities and the mean biomass of grass becomes higher than the shrub in the case of wind in grass-dominated communities. Third, the dust flux of shrub-dominated communities is higher than the grass-dominated communities. Fourth, the net change in surface height in shrub-dominated communities has a considerably higher range than in grass-dominated communities. Fifth, the spatial pattern of shrub-dominated communities is sparser than the spatial pattern of grass in the vegetation communities in the case of wind. The results from the second scenario show that: First, the state change only took place from grass-dominated communities to shrub-dominated communities in the condition of drought. Second, the state change only took place in the case of wind. Third, the state change didn't take place after the slight and moderate droughts but only took place after the drought. Fourth, large vegetation biomass reduction only took place in the case of wind after the severe drought. Our results confirm, in a modeling context, the important role that aeolian transport can play in vegetation dynamics and state change in deserts.     

Phylogenetic structure and formation mechanism of shrub communities in arid and semiarid areas of the Mongolian Plateau

The mechanisms of species coexistence within a community have always been the focus in ecological research. Community phylogenetic structure reflects the relationship of historical processes, regional environments, and interactions between species, and studying it is imperative to understand the formation and maintenance mechanisms of community composition and biodiversity. We studied the phylogenetic structure of the shrub communities in arid and semiarid areas of the Mongolian Plateau. First, the phylogenetic signals of four plant traits (height, canopy, leaf length, and leaf width) of shrubs and subshrubs were measured to determine the phylogenetic conservation of these traits. Then, the net relatedness index (NRI) of shrub communities was calculated to characterize their phylogenetic structure. Finally, the relationship between the NRI and current climate and paleoclimate (since the Last Glacial Maximum, LGM) factors was analyzed to understand the formation and maintenance mechanisms of these plant communities. We found that desert shrub communities showed a trend toward phylogenetic overdispersion; that is, limiting similarity was predominant in arid and semiarid areas of the Mongolian Plateau despite the phylogenetic structure and formation mechanisms differing across habitats. The typical desert and sandy shrub communities showed a significant phylogenetic overdispersion, while the steppified desert shrub communities showed a weak phylogenetic clustering. It was found that mean winter temperature (i.e., in the driest quarter) was the major factor limiting steppified desert shrub phylogeny distribution. Both cold and drought (despite having opposite consequences) differentiated the typical desert to steppified desert shrub communities. The increase in temperature since the LGM is conducive to the invasion of shrub plants into steppe grassland, and this process may be intensified by global warming.