黑龙江省东部森林群落β多样性的研究

以连续带指数和集合环境梯度作为植物群落演替动态和环境质量的定量指标,探讨了黑龙江省东部森林群落β多样性随环境梯度和演替动态的变化规律．结果表明,森林群落中植物种的β多样性βＺ和昆虫种的β多样性βＫ都随环境梯度的增加而升高,即随着环境质量升高群落间物种更替速率降低,且βＫ的变化滞后于βＺ．βＺ和βＫ与连续带指数（ＣＩ）呈非线性相关,在演替初期群落间物种更替速率较高,在演替中后期群落间物种的更替速率最小．βＫ曲线的峰值出现滞后于βＺ曲线,说明森林昆虫群落多样性变化对植物群落多样性变化的依赖性     

黑龙江省东部森林群落β多样性的研究

以连续带指数和集合环境梯度作为植物群落演替动态和环境质量的定量指标,探讨了黑龙江省东部森林群落β多样性随环境梯度和演替动态的变化规律。结果表明,森林群落中植物种的β多样性β_Z和昆虫种的β多样性β_K都随环境梯度的增加而升高,即随着环境质量升高群落间物种更替速率降低,且β_K的变化滞后于β_Z.β_Z和β_K与连续带指数(CI)呈非线性相关,在演替初期群落间物种更替速率较高,在演替中后期群落间物种的更替速率最小。β_K曲线的峰值出现滞后于β_Z曲线,说明森林昆虫群落多样性变化对植物群落多样性变化的依赖性.     

长白山北坡森林群落结构组成及其海拔变化

对长白山北坡海拔700～1900m的13个森林群落进行了群落组成、结构随海拔上升变化情况的研究。结果表明,随着海拔的升高,群落的建群种组成、层次结构等,都表现出由复杂多样逐渐向简单单一过渡的变化趋势,从700m至1700m,针叶树所占的比例随海拔的升高呈明显的增加趋势,阔叶树比例随之减少,到林线时针阔叶树种均急剧减少,沿海拔梯度存在明显的树种更替现象。从群落的平均胸径及胸高断面积和可知。最大值出现于900～1100m及1600m,这2个海拔段正是不同森林群落类型间的过渡区。除海拔1800m的岳桦林之外,其它群落径级结构都呈倒J形分布,即各径级树木中,更新幼苗、幼树在数量上占绝对优势,随着胸径的增大,立木株数逐渐减少,这种径级结构表明,长白山北坡各海拔群落更新良好,群落处于稳定的发展状态。     

历山自然保护区猪尾沟森林群落植物多样性研究

采用丰富度指数、物种多样性指数和均匀度指数对山西历山自然保护区猪尾沟森林群落多样性进行研究。结果表明 :1 )同一群落内 ,多样性指数存在一定的波动范围 ;不同群落间 ,物种多样性也存在差异 ,但其并不一定具有统计学意义。由此表明 ,群落之间存在差异 ,同时也存在着连续性。 2 )海拔高度是决定本区多样性分布格局的主导因子 ,随着群落分布海拔高度的增加 ,多样性呈一致的上升趋势 ,即多样性与海拔呈正相关关系。 3)群落物种多样性对海拔的敏感性由大到小的次序为草本层 >乔木层 >灌木层 ,其中乔木层的丰富度指数、草本层均匀度指数与海拔有着极显著的正相关关系 ,而乔木层的多样性指数、草本层的丰富度指数与海拔有着极显著的负相关关系 ,灌木层的多样性与海拔没有显著的相关性。 4)群落中不同结构、不同层次对群落总体多样性的贡献是不同的 ,两种测定方法所产生的总体多样性之间呈显著相关关系 ,表明给定加权参数的测定方法没有影响客观生态意义的反映 ,同时也更好地反映出群落结构对于群落多样性的功能差异     

幕阜山森林群落结构与物种多样性研究

幕阜山地处中亚热带-北亚热带过渡地带,物种资源丰富.通过对其典型样地的调查,分别采用Shannon-Wiener指数、Simpson指数和Pielou均匀度指数作为测度指标,研究了幕阜山地区森林群落结构及其物种多样性特征.结果表明,该地区主要有21个森林群落类型.其中常绿阔叶林中,物种丰富度指数与多样性指数在群落梯度上的总体趋势均为灌木层相对高于乔木层,乔木层相对高于草本层;在落叶阔叶林中,其丰富度指数的趋势为灌木层＞草本层和乔木层,而在草本层与乔木层间是波动的,多样性指数的趋势为灌木层＞草本层＞乔木层;在针叶林中,物种丰富度、多样性指数表现的总趋势基本一致,即灌木层的丰富度相对较高,其次为草本层,乔木层的相对较小.在其他群落类型中,多样性指数、均匀度指数在乔木层、灌木层和草本层则表现出多样化的趋势;另外,从总体上看,各种指数在海拔梯度上并未表现出明显的规律性.     

地带性森林群落物种多样性的比较研究

在群落调查以及文献收集的基础上,对暖温带地区、暖温带和亚热带过渡地区、亚热带地区以及热带地区的典型地带笥植被不同群落类型群落多样性进行了分析和研究。结果发现这４类地区物种多样性的变化具有一定的规律性,具体表现在热带地区群落乔木层的物种丰富度和多样性为最高,然后依次是亚热带地区、秦蛉地区和东灵山地区;灌木层的物种丰富度和多样性则以亚热带地区为最高,其次是秦岭地区,热带地区的则仍高于东灵山地区;灌木层     

深圳南山区天然森林群落多样性及演替现状

对南山区5个主要天然森林群落(铁榄群落、鼠刺 降真香群落、鸭脚木群落、假苹婆群落、水翁 假苹婆群落)的组成结构及物种多样性进行分析,并与相邻的香港地区地带性森林群落(黄桐群落)作比较。结果表明,依照亚热带及南亚热带森林群落演替规律,南山区天然林处于不同的演替发育阶段：铁榄群落处于演替第3阶段;鼠刺 降真香群落处于第4阶段;其它3个群落处于第5阶段,均未达到稳定的顶极群落阶段。随着铁榄群落、鼠刺 降真香群落、鸭脚木群落、假苹婆群落、水翁 假苹婆群落这个演替序列,物种丰富度的变化规律是：先逐渐上升,到达一个峰值,再缓慢下降。Shannon-Wiener指数和Pielous均匀度指数的变化规律与物种丰富度相同,Simpson指数变化曲线与这些指数相反。但这些指数反映的结果是一致的。综合多个指数分析,鸭脚木群落物种多样性最大,即当群落中阳生性树种与中生性树种优势度相差不大时。群落具有最大的物种多样性。多样性比较结果显示,南山森林群落物种多样性大大低于香港黄桐群落。5个群落的Shannon—Wiener指数在2．04～2．953之间,明显低于黄桐群落,其Shannon—Wiener指数为4．74;Simpson指数0．1～0．268,黄桐群落为0．05;Pielous均匀度指数64．2％～74％,黄桐群落为79％。南山森林群落物种多样性水平低下的状况与长期的人类干扰有关,必须尽快采取“封山育林”等相应措施来促进群落的保护和恢复。     

浙江仙居俞坑森林群落物种多样性研究

分别采用物种丰富度、物种多样性指数和群落均匀度指标对浙江省仙居县俞坑森林群落的物种多样性进行测定和分析。结果表明：本木植物的物种多样性以生境优越的常绿阔叶林为高,木本植物的物种丰富度、物种多样性指数明显大于草本植物。在群落垂直结构中,木本植物等2层的物种丰富度、物种多样性指数均显著大于第1层。物种丰富度以木本第3层最大,草本层最小;而物种多样性指数、群落均匀度则以木本第2层最大、草本层最小。木本植物各层次、草本层的物种多样性各项指标在群落各样地间均有一定的差异。     

闽北地区森林群落物种多样性的测定

采用8个物种多样性指数对闽北地区的8个森林群落类型物种多样性进行测定,并选用4个种一多度关系模型(对数正态分布、Weibull分布、对数级数分布、生态位优先占领模型)分析其物种-多度关系,把多样性指数与对数正态分布、Weibull分布和生态位优先占领模型的有关参数进行线性回归,以分析多度模型参数描述物种多样性的可行性。结果表明：(1)多数物种多样性指数对群落的测度是一致的,(2)对数正态分布、Weibull分布和生态位优先占领模型对8个群落的物种多度拟合效果很好;(3)对数正态分布、Weibull分布和生态位优先占领模型有关模型参数与部分物种多样性指数的线性关系达显著或极显著水平。通过闽北地区8个类型森林群落物种多样性指数测定,使生物多样性较准确地数量化,同时还说明采用改进单纯形法进行非线性分布函数的拟合是简单有效的,可推广应用。     

山西文峪河上中游森林群落多样性

基于山西文峪河上中游森林群落的野外调查数据,选取植物生活型、生活史、固氮类型、传粉途径、种子传播途径等14个植物功能性状,计算丰富度指数(R)、多样性指数(H')、均匀度指数(E)等物种多样性指数和功能丰富度指数(FRic)、功能均匀度指数(FEve)、功能分歧度指数(FDiv)等功能多样性指数,并用TWINSPAN对森林群落进行分类,Spearman秩相关分析多样性指数间及其与环境因子间的相关性,对山西文峪河上中游森林群落多样性进行研究。结果表明:青杄林种数最多(R=27),辽东栎油松林和油松林种数最少(R=16);白桦林的H'和E最大,油松林的H'和E最小。山杨白桦林的FRic值最大,白杄林的FRic值最小;青杄林的FEve值最大,山杨白桦林的FEve值最小;山杨林的FDiv值最大,白桦林的FDiv值最小。文峪河上中游森林群落物种多样性指数与功能多样性指数间相关性不显著(P0.05),仅FDiv与H'呈显著负相关关系(P0.05);物种多样性指数间呈极显著相关关系(P0.01),功能多样性指数间相关性不显著(P0.05),仅FRic与FEve呈显著负相关关系(P0.05);随着海拔增加,物种多样性指数增加(P0.05或P0.01),但功能多样性指数减小(P0.01或P0.05)。     

Latitudinal gradients of associations between beta and gamma diversity of trees in forest communities in the New World

Aims We analyze two continental data sets of forest communities from across the New World to examine the latitudinal gradients of beta diversity after accounting for gamma diversity and the latitudinal gradient of gamma diversity after accounting for beta diversity.Methods Correlation and regression analyses were used to relate beta and gamma diversity to latitude along two latitudinal gradients in the New World (one including 72 forest sites located south of the equator and the other including 79 forest sites located north of the equator).Important findings Beta diversity and gamma diversity were negatively correlated with latitude. Beta diversity was strongly and positively correlated with gamma diversity (Pearson's correlation coefficient: 0.783 for New World North and 0.848 for New World South). When beta diversity was regressed on latitude and gamma diversity, 69.8 and 85.7% of the variation in beta diversity were explained, respectively, for New World North and New World South. When gamma diversity was regressed on latitude and beta diversity, 81.8 and 84.3% of the variation in gamma diversity were explained, respectively, for New World North and New World South. After statistically removing the relationship between beta and gamma diversity, latitude has weak or no relationships with beta and gamma diversity. However, strong positive correlations between beta and gamma diversity may not be considered as evidence of one driving the other along a latitudinal gradient.     

The variation of tree beta diversity across a global network of forest plots

Aims With the aim of understanding why some of the world's forests exhibit higher tree beta diversity values than others, we asked: (1) what is the contribution of environmentally related variation versus pure spatial and local stochastic variation to tree beta diversity assessed at the forest plot scale; (2) at what resolution are these beta‐diversity components more apparent; and (3) what determines the variation in tree beta diversity observed across regions/continents? Location World‐wide. Methods We compiled an unprecedented data set of 10 large‐scale stem‐mapping forest plots differing in latitude, tree species richness and topographic variability. We assessed the tree beta diversity found within each forest plot separately. The non‐directional variation in tree species composition among cells of the plot was our measure of beta diversity. We compared the beta diversity of each plot with the value expected under a null model. We also apportioned the beta diversity into four components: pure topographic, spatially structured topographic, pure spatial and unexplained. We used linear mixed models to interpret the variation of beta diversity values across the plots. Results Total tree beta diversity within a forest plot decreased with increasing cell size, and increased with tree species richness and the amount of topographic variability of the plot. The topography‐related component of beta diversity was correlated with the amount of topographic variability but was unrelated to its species richness. The unexplained variation was correlated with the beta diversity expected under the null model and with species richness. Main conclusions Because different components of beta diversity have different determinants, comparisons of tree beta diversity across regions should quantify not only overall variation in species composition but also its components. Global‐scale patterns in tree beta diversity are largely coupled with changes in gamma richness due to the relationship between the latter and the variation generated by local stochastic assembly processes.     

A latitudinal gradient in large-scale beta diversity for vascular plants in North America

Species turnover, or beta diversity, has been predicted to decrease with increasing latitude, but few studies have tested this relationship. Here, we examined the beta diversity–latitude relationship for vascular plants at a continental scale, based on complete species lists of native vascular plants for entire states or provinces in North America (north of Mexico). We calculated beta diversity as the slope of the relationship between the natural logarithm of the Jaccard index (ln J ) for families, genera or species, and both geographic distance and climate difference within five latitude zones. We found that beta diversity decreased from south to north; within latitude zones, it decreased from species to genera and families. Geographic and climatic distance explained about the same proportion of the variance in ln J in zones south of c. 50°N. North of this latitude, nearly all the explained variance in ln J was attributable to geographic distance. Therefore, decreasing beta diversity from south to north reflects decreasing climate differentiation within more northerly latitude zones, and primarily post-glacial dispersal limitation north of 50°N.     

Latitudinal gradients in Atlantic reef fish communities: trophic structure and spatial use patterns

Trophic strategies and spatial use habits were investigated in reef fish communities. The results supported the hypothesis of differential use of food resources among tropical and higher latitude reef fishes, i.e . the number of species and relative abundance of fishes relying on relatively low‐quality food significantly decreased from tropical to temperate latitudes. The species : genus ratio of low‐quality food consumers increased toward the tropics, and was higher than the overall ratio considering all fishes in the assemblages. This supports the view that higher speciation rates occurred among this guild of fishes in warm waters. It was also demonstrated that density of herbivorous fishes (the dominant group relying on low‐quality food resources) in the western Atlantic decreased from tropical to temperate latitudes. Spatial use and mobility varied with latitude and consequently reef type and complexity. Fishes with small‐size home ranges predominated on tropical coral reefs.     

A latitudinal gradient of beta diversity for exotic vascular plant species in North America

Determining relationships between the ranges of introduced species and geographical and environmental factors is an important step in understanding the mechanisms and processes of the spread of introduced species. In this study, I examined the beta diversity and latitude relationship for all naturalized exotic species of vascular plants in North America at a continental scale. Beta diversity was calculated as the absolute value of the slope of the relationship between the natural logarithm of the Simpson index of similarity (lnS) and spatial distance between pairs of state‐level exotic floras within four latitudinal zones examined. Relative contributions of spatial distance and environmental difference to species turnover between exotic floras were examined. I found that beta diversity decreased monotonically from low to high latitudes: beta diversity for the southernmost zone was shallower than that for the northernmost zone by a factor of 2.6. Regression models of lnS in relation to spatial distance and environmental (climatic and topographical) difference for each latitudinal zone demonstrated that the explanatory power of these variables diminishes monotonically with latitude: the explained variance in lnS is 70.4%, 62.1%, 53.9%, and 33.9%, respectively, for the four latitudinal zones from south to north. For the southernmost zone, 58.3% of the variance in lnS is explained by climate variables and topography, and spatial distance explains only 2.3% of the variance. In contrast, for the northernmost zone, more than half the amount (22.5%) of the explained variance in lnS is attributable to spatial distance, and the remaining (18.9%) of the explained variance is attributable to climate variables and topography.     

The latitudinal gradient of beta diversity in relation to climate and topography for mammals in North America

Aim Spatial turnover of species, or beta diversity, varies in relation to geographical distance and environmental conditions, as well as spatial scale. We evaluated the explanatory power of distance, climate and topography on beta diversity of mammalian faunas of North America in relation to latitude. Location North America north of Mexico. Methods The study area was divided into 313 equal‐area quadrats (241 × 241 km). Faunal data for all continental mammals were compiled for these quadrats, which were divided among five latitudinal zones. These zones were comparable in terms of latitudinal and longitudinal span, climatic gradients and elevational gradients. We used the natural logarithm of the Jaccard index (lnJ) to measure species turnover between pairs of quadrats within each latitudinal zone. The slope of lnJ in relation to distance was compared among latitudinal zones. We used partial regression to partition the variance in lnJ into the components uniquely explained by distance and by environmental differences, as well as jointly by distance and environmental differences. Results Mammalian faunas of North America differ more from each other at lower latitudes than at higher latitudes. Regression models of lnJ in relation to distance, climatic difference and topographic difference for each zone demonstrated that these variables have high explanatory power that diminishes with latitude. Beta diversity is higher for zones with higher mean annual temperature, lower seasonality of temperature and greater topographic complexity. For each latitudinal zone, distance and environmental differences explain a greater proportion of the variance in lnJ than distance, climate or topography does separately. Main conclusions The latitudinal gradient in beta diversity of North American mammals corresponds to a macroclimatic gradient of decreasing mean annual temperature and increasing seasonality of temperature from south to north. Most of the variance in spatial turnover is explained by distance and environmental differences jointly rather than distance, climate or topography separately. The high predictive power of geographical distance, climatic conditions and topography on spatial turnover could result from the direct effects of physical limiting factors or from ecological and evolutionary processes that are also influenced by the geographical template.     

The effect of climatic gradients, topographic variation and species traits on the beta diversity of rain forest trees

Aim  We assessed the rates of turnover of tree species with distance (beta diversity) in wet forests of the Western Ghats (WG) complex of India to see whether climate, topographic variation or species traits influence beta diversity.
Location  The Western Ghats is a chain of mountains about 1600 km in length, running parallel to the western coast of the Indian Peninsula from above 8° N to almost 21° N latitude.
Methods  We used data from 60 small plot inventories concentrated in three regions: the southernmost part of the Western Ghats (SWG) (8°24' to 9°37' N), the Nilgiri Hills (11°12' to 11°14' N), and the central Western Ghats (CWG) (12°32' to 14°51' N). We used Sorensen's index (SI) to estimate the similarity in species composition between two plots and regressed SI against the logarithm of the distance between plots to assess beta diversity. A bootstrapping procedure provided confidence intervals for regression coefficients. To test for the effects of climate, we regressed seasonality differences between plots against SI for low-elevation (< 800 m) plots along the north–south axis, and all plots in the SWG. We assessed the impact of the rainfall gradient in the Kogar region.
Results  Among all three regions, beta diversity was highest along the latitudinal axis, and along the rainfall gradient in the Kogar region. Differences in seasonality between sites were strongly related to beta diversity along the north–south seasonality gradient and within the SWG. Within the three regions, beta diversity was highest in the region with the strongest rainfall gradient and lowest for the topographically heterogeneous SWG. Beta diversity did not differ between forest strata and dispersal modes.
Main conclusions  We conclude that climate, particularly seasonality, is probably the primary driver of beta diversity among rain forest trees of the Western Ghats complex.