漓江水陆交错带土壤理化性质及其分布特征

水陆交错带是水生生态系统与陆地生态系统之间的过渡带,是一种典型的生态交错区,承载着能量流动、物质循环和信息交换的重要作用。土壤作为水陆交错带系统的重要组成部分,是水陆交错带功能实现的基础之一。鉴于此,以桂林漓江水陆交错带纵向梯度(上游、中游、下游)不同植被覆盖条件下的土壤为研究对象,采用野外取样调查、实验分析与统计检验相结合,系统的分析了土壤理化性质及其分布特征,旨在为该区域退化生态系统恢复与重建提供依据。结果表明:11个土壤理化性质,其中5个指标(土壤含水量、全氮、全磷、速效氮和速效钾)在上游、中游和下游均差异性显著。不同梯度下的土壤理化性质的相关性及相关性大小也不尽相同,但在总体上存在一些较相似的变化规律,如上游、中游和下游的土壤容重和孔隙度均呈现显著负相关,土壤全磷和有机质与多数土壤化学性质呈显著正相关;土壤含水量在下游与多数土壤化学性质均显著相关,但在上游仅与土壤全磷显著负相关。PCA主成分分析表明,土壤容重、土壤孔隙度和土壤全磷含量的贡献均大于其他环境因子的平均贡献率,体现了它们是影响漓江水陆交错带土壤理化性质的重要环境因子。     

Seasonal variation in the diversity and species richness of phytoplankton in a tropical eutrophic reservoir

The water chemistry, structure of sediment grain size, algal biomass, and patterns of nine bacteria physiological groups were studied monthly from May to October 1991 in an adjacent stream, ecotone, and reservoir zones (southern Poland). The distribution of five particulate organic carbon fractions was significantly different among the zones. Biomass of benthic algae demonstrated a maximum in the ecotone (22.74 g C m^–2). Most of the bacterial groups were more numerous in the stream sediments where aerobic heterotrophs prevailed (1.2–6.5 × 10¹¹ cells m^–2). The significant differences in density were found for anaerobic heterotrophs, anaerobic nitrogen fixing, amylolytic, and cellulolytic bacteria among the zones. The small density of bacteria in the ecotone was probably an effect of the rapid water fluctuations, accompanied by movement of fine sediments or/and an inhibitory effect of compounds secreted by the periphyton. The principal component analysis showed that the ecotone zone was more similar to the reservoir open water than to the stream.     

Toward Conceptual Cohesiveness: a Historical Analysis of the Theory and Utility of Ecological Boundaries and Transition Zones

Ecological transition zones are increasingly recognized as systems that play a critical role in controlling or modifying flows of organisms, materials, and energy across landscapes. Many concepts describing transitional areas have been proposed over the years, such as the prevalent and durable ecotone concept. Confusion among ecologists and land managers about transition zone concepts and the isolation of studies that use only one transition concept can hinder unified progress in understanding these key systems. Currently, a movement toward conceptual synthesis under the umbrella concept of ‘ecological boundary’ is underway. Here we examine the history and theoretical baggage of the ecotone, riparian zone, and several other concepts. Subsequently, we present a conceptual cluster analysis, which facilitates a better understanding of the similarities and differences between boundary and transition concepts. We emphasize the hierarchical nature of these concepts: higher-level synthetic concepts can be used in the development of theory, whereas lower-level concepts allow more specificity and the formulation of operational definitions. Finally, we look briefly at the utility and future use of boundary and transition zone concepts.     

Interannual variations of the fish assemblage in the transitional zone of the Three Gorges Reservoir: persistence and stability

The construction of dams may lead to dramatic changes in fish assemblages due to the loss of lotic habitat caused by impoundment, which have been well documented. However, knowledge of the temporal variation of fish assemblages in the transitional zone, which is an ecotone between lotic and lentic environments of the reservoir, is still very rare. In the present study, fishes in the transitional zone of the Three Gorges Reservoir were sampled from 1997 to 2002 and from 2006 to 2009 to investigate interannual variations of fish assemblages. The results showed that 9 families, composed of 77 species, were found in the transitional zone with Cyprinidae as the dominant group. By cluster analysis (CLUSTER) and non-metric multidimensional scaling analysis (MDS), assemblages were separated into two groups at a Bray-Curtis similarity value of 77.26%, representing the pre-impoundment period and post-impoundment period. Following analysis of similarity percentages of species contributions (SIMPER), shifts in abundances of Coreius guichenoti, Rhinogobio cylindricus and Coreius heterodon, etc. contributed most to the difference between the two groups. Surprisingly, contrasting to the drastic changes in lacustrine region, the fish assemblage in the transitional zone appeared to be relatively stable, since the ten core species caught were consistently recorded every year, and no significant species replacement occurred during our study period. Besides, the moderate index of persistence indicated persistence of the fish assemblage as well, in spite of the shift of some species. Based on the results of ordination and time-lag analysis, the fish assemblage in the transitional zone showed no directional change. We conclude that fish assemblage in the transitional zone of the Three Gorges Reservoir was stable across the surveyed years. Based on our results, we propose that maintenance of dynamic transitional zones in reservoirs will be useful for the preservation of fishes, particularly for the endemic species inhabiting the upper Yangtze.     

华北农牧交错带农田-草地界面土壤水分影响域分析

在华北农牧交错区,选择线状边界的农田与草地典型区进行调查与土壤水分测定,采用移动窗口法,对农田-草地景观界面表层（0～20 cm）土壤水分影响域进行研究.结果表明：界面水分的影响域为草地6 m到农田4 m,总宽度10 m,属急变型界面;将农田-草地景观界面划分为3个功能区：农田功能区、草地功能区和农田-草地复合功能区.其中农田-草地复合功能区的土壤含水量变化剧烈,而草地功能区与农田功能区内土壤水分基本呈线性分布;草地生态系统土壤平均含水量比农田高约1 g·g^-1,这主要是由于草地开垦为农田后风蚀等作用而引起的土壤毛管持水力下降所致.作为植被覆盖不同的两个生态系统,不同的植物蒸腾和地表蒸发,可使不同功能区的土壤含水量产生明显差异,从而使土壤水势发生变化,使水分跨生态系统运移成为可能.     

生态交错带及其研究进展

生态交错带研究对探索自然生态规律和保护环境有重要意义。近30a来,有关生态交错带的论文数平均年增57%,显示其得到了愈来愈广泛的关注。回顾了生态交错带概念的产生与发展,区分了它与边缘、生态边界层与生态过渡带等概念的异同;简述了其7个基本属性,即高生物多样性、丰富的特有种、大量外来种、频繁的物质流动、敏感的时空动态性、结构的异质性和脆弱性;总结提炼了生态交错带的基本原理和假说;综述了生态交错带的生物多样性产生机制、对全球变化的响应与反馈、生态设计与管理以及生态交错带模型发展和整合的研究进展。提出今后需要大力发展理论研究、多尺度模型转化和多因子综合分析,以完善生态交错带理论并支持生态学机理的探索。     

大兴安岭次生林白桦对林下日阴菅及其它主要草本植物的影响

探讨了白桦树冠投影面积对林下日阴菅密度的影响,发现日阴菅密度随白桦树冠投影面积呈双峰型变化。海拔高度、坡向、坡度对于日阴菅随白桦树冠投影面积的变化也有一定程度的影响。白桦荫蔽度、日阴菅地上部生物量和土壤水分含量三者具有较为一致的格局规模,这表明白桦通过改变林下的光照和地表水分而影响了日阴菅的生长。日阴菅在中等尺度上与土壤有机质的格局规模一致。溪荪个体数量与土壤pH值在大、中尺度上均显示一致的格局规模,说明溪荪受pH值的影响。     

Variation in phytoplankton composition and limnological features in a water–water ecotone of the Lower Paraná Basin (Argentina)

1. Structure and dynamics of phytoplankton were studied at six sites in a reach of the Lower Paraná River floodplain, from the main course to a marginal shallow lake, connected through a stream. This system is defined as a water–water ecotone and thus, the aim of this work is to analyse the spatial changes of phytoplankton along the transitional system.
2. Temporal fluctuations in number of species and phytoplankton density were more pronounced in the river than in the shallow lake. Even though most species were ubiquitous, there was a clear segregation of the most abundant populations across the ecotone. Aulacoseira granulata var. granulata and other centric diatoms decreased towards the lentic system.
3. Transparency varied according to river discharge, being higher in the lake during high water phases, while the opposite behaviour was observed during dry periods. These fluctuations were related to precipitation and resuspension processes.
4. Nitrate concentration diminished towards the lake while soluble reactive phosphorus remained fairly homogeneous across the ecotone.     

川西亚高山林线过渡带及邻近植被土壤性质

研究了川西亚高山林线过渡带及邻近植被上缘流石滩草甸与下缘冷杉林残积母质土壤物理、化学和生物学特性.结果表明:从流石滩草甸→林线过渡带→冷杉林,土层逐渐增厚,表层土壤(0～30 cm)粉粒、粘粒、物理性粘粒含量、团聚度、结构系数和自然含水量逐渐增高,砂粒含量逐渐降低,阳离子交换量(CEC)、交换性盐基含量、盐基饱和度以及水解性酸含量逐渐增高,pH值逐渐降低,有机质及养分库全P、全K、有效N、有效P和速效K含量逐渐增高,土壤物理结构和化学性质逐步有所改善,但亚高山林线过渡带区域残积母质土壤成土过程缓慢.林线过渡带表层土壤细菌、真菌、放线菌及微生物总量,土壤脲酶、蔗糖酶、酸性磷酸酶、中性磷酸酶、多酚氧化酶及过氧化氢酶活性高于邻近植被上缘流石滩草甸与下缘冷杉林,体现了作为生态交错带,林线过渡带比邻近植被土壤具有相对较强的生物学活性.     

The role of water exchange between a stream channel and its hyporheic zone in nitrogen cycling at the terrestrial-aquatic interface

The subsurface riparian zone was examined as an ecotone with two interfaces. Inland is a terrestrial boundary, where transport of water and dissolved solutes is toward the channel and controlled by watershed hydrology. Streamside is an aquatic boundary, where exchange of surface water and dissolved solutes is bi-directional and flux is strongly influenced by channel hydraulics. Streamside, bi-directional exchange of water was qualitatively defined using biologically conservative tracers in a third order stream. In several experiments, penetration of surface water extended 18 m inland. Travel time of water from the channel to bankside sediments was highly variable. Subsurface chemical gradients were indirectly related to the travel time. Sites with long travel times tended to be low in nitrate and DO (dissolved oxygen) but high in ammonium and DOC (dissolved organic carbon). Sites with short travel times tended to be high in nitrate and DO but low in ammonium and DOC. Ammonium concentration of interstitial water also was influenced by sorption-desorption processes that involved clay minerals in hyporheic sediments. Denitrification potential in subsurface sediments increased with distance from the channel, and was limited by nitrate at inland sites and by DO in the channel sediments. Conversely, nitrification potential decreased with distance from the channel, and was limited by DO at inland sites and by ammonium at channel locations. Advection of water and dissolved oxygen away from the channel resulted in an oxidized subsurface habitat equivalent to that previously defined as the hyporheic zone. The hyporheic zone is viewed as stream habitat because of its high proportion of surface water and the occurrence of channel organisms. Beyond the channel's hydrologic exchange zone, interstitial water is often chemically reduced. Interstitial water that has not previously entered the channel, groundwater, is viewed as a terrestrial component of the riparian ecotone. Thus, surface water habitats may extend under riparian vegetation, and terrestrial groundwater habitats may be found beneath the stream channel.     

Communities of hydrobionts and the physical-chemical characteristics of the estuary area of inflow of a flat water basin

The transitive and stable sites in the zone of changeable backup waters of inflow in the Ribinsk reservoir are determined on their physical-chemical parameters. The distribution of bacterioplankton and zooplankton and the density of the fish population are described. The similarities and distinctions of hydrobionts in the river, reservoir, and the zone of their water contact are shown. The zone of changeable backup waters (CBWs) is determined as ecotone according to its number of typical features.     

孔雀河下游断流河道的环境特征及物种间关系

基于孔雀河下游断流河道的环境因子和植被样地数据,采用聚类与CCA排序法,分析了生境的退化特征以及物种间的相互关系,结果表明:1)断流河道退化生境分为绿洲-荒漠过渡类型、轻度荒漠化类型和盐土荒漠化类型。绿洲-荒漠过渡类型地下水位低、盐分含量相对较低,植被盖度相对较高,土壤维持着原砂质壤土,为潜在退化型;轻度荒漠化类型地下水位、土壤质地与含盐量与前者基本相同,土壤未明显退化,但植被盖度低于10%,植物种类与个体数目都较低,属于轻度退化型;盐土荒漠化类型地下水位高、盐分含量高,土壤机械组成中砂粒比重较大、无建群种幸存,属于重度退化型。2)绿洲-荒漠过渡类型总体联结性为显著正联结,正负联结比小于1,生态系统表现为建群种维系物种关系的不稳定状态;轻度荒漠化类型总体联结性为不显著负联结,正负联结比小于1,表现出生态系统进入退化演替的阶段;盐土荒漠化类型总体联结性为显著正联结,正负联结比大于1,表现出重度退化群落的种间平衡状态,物种间以达到稳定共存,其中,真盐生植物对这种平衡的维持起着重要的作用。3)CCA排序表明,绿洲-荒漠过渡类型形成以胡杨为中心的种间正联结,幸存于盐分适中、水分养分相对较高的生境;轻度荒漠化类型,形成以多枝柽柳与刚毛柽柳相互依存的不显著负联结,幸存于土壤养分、水分相对较低的生境;盐土荒漠化类型形成以盐爪爪、盐节木、盐穗木等真盐生植物维系的显著正联结,幸存于土壤贫瘠、地下水位浅、盐分含量高、沙化严重的生境。     

Environmental filtering of species with different functional traits into plant assemblages across a tropical coniferous-broadleaved forest ecotone

Background and aims

Ecotones between coniferous and broadleaved forests in tropical regions are poorly understood. Our aim was to understand community assembly across the ecotones by integrating changes in both plant functional traits and environmental factors.

Methods

The coniferous, ecotone, and broadleaved zones along each of the 15 investigation transects were discerned and surveyed. We measured eight functional traits of 174 woody species and 10 environmental factors along transects across the ecotones. We assessed between-site differences by using ANOVA, and correlations between functional traits and the environmental factors by RDA ordination.

Results

With the variation of vegetation zones from coniferous through the ecotone to broadleaved, the functional traits of plants at the community level changed in accordance with the changes in soil and light regimes. The low soil nutrients and low soil water in the coniferous zone were the major constraints for most lowland rain forest species with acquisitive traits, while high soil nutrients, high soil water and low light in the broadleaved zone had strong filtering effects on the conifer and tropical monsoon rainforest species with conservative traits.

Conclusions

The soil and light conditions were the major determinants for the functional community structure of the vegetation types across the tropical coniferous and broadleaved forest ecotone.     

河北省塞罕坝地区种子植物区系的过渡性分析

河北省塞罕坝地处森林区向草原区的过渡区域,植物种类丰富,共有种子植物75科318属713种或变种。塞罕坝植物区系的地理成分以北温带分布为主,占全区种子植物属数的47．65％。其次是世界分布和旧世界温带分布,分别占全区种子植物属数的15．41％和14．38％,其它分布的植物属较少。植物生活型以地面芽植物为主,高位芽植物、地上芽植物、地面芽植物、地下芽植物和一年生植物分别占全区种子植物的16．27％、1．54％、40．95％、25．39％和15．85％。通过与周围5个地区的主分量分析,塞罕坝植物区系处在森林区植物区系与草原区植物区系之间,具有明显的过渡性。塞罕坝植物区系与草原区锡林河流域和森林区松山植物区系的关系比较密切。     

Spatial patterns of total and available N and P at alpine treeline

Background and aims

Vegetation can have direct and indirect effects on soil nutrients. To test the effects of trees on soils, we examined the patterns of soil nutrients and nutrient ratios at two spatial scales: at sites spanning the alpine tundra/subalpine forest ecotone (ecotone scale), and beneath and beyond individual tree canopies within the transitional krummholz zone (tree scale).

Methods

Soils were collected and analyzed for total carbon (C), nitrogen (N), and phosphorus (P) as well as available N and P on Niwot Ridge in the Colorado Rocky Mountains.

Results

Total C, N, and P were higher in the krummholz zone than the forest or tundra. Available P was also greatest in the krummholz zone while available N increased from the forest to the tundra. Throughout the krummholz zone, total soil nutrients and available P were higher downwind compared to upwind of trees.

Conclusions

The krummholz zone in general, and downwind of krummholz trees in particular, are zones of nutrient accumulation. This pattern indicates that the indirect effects of trees on soils are more important than the direct effects. The higher N:P ratios in the tundra suggest nutrient dynamics differ from the lower elevation sites. We propose that evaluating soil N and P simultaneously in soils may provide a robust assay of ecosystem nutrient limitation.     

Comparative water relations of adjacent california shrub and grassland communities

Summary Much of the coastal mountains and foothills of central and southern California are covered by a mosaic of grassland, coastal sage scrub, and evergreen sclerophyllous shrubs (chaparral). In many cases, the borders between adjacent plant communities are stable. The cause of this stability is unknown. The purpose of our study was to examine the water use patterns of representative grasses, herbs, and shrubs across a grassland/chaparrel ecotone and determine the extent to which patterns of water use contribute to ecotone stability. In addition, we examined the effects of seed dispersal and animal herbivory. We found during spring months, when water was not limited, grassland species had a much higher leaf conductance to water vapor diffusion than chaparral plants. As the summer drought progressed, grassland species depleted available soil moisture first, bare zone plants second, and chaparral third, with one chaparral species (Quercus durata) showing no evidence of water stress. Soil moisture depletion patterns with depth and time corresponded to plant water status and root depth. Rabbit herbivory was highest in the chaparral and bare zone as indicated by high densities of rabbit pellets. Dispersal of grassland seeds into the chaparral and bare zone was low. Our results support the hypothesis that grassland species deplete soil moisture in the upper soil horizon early in the drought, preventing the establishment of chaparral seedlings or bare zone herbs. Also, grassland plants are prevented from invading the chaparral because of low seed dispersability and high animal herbivory in these regions.     

Properties of ecotones: Evidence from five ecotones objectively determined from a coastal vegetation gradient

Abstract. Several properties have been suggested to be characteristic of ecotones, but their prevalence has rarely been tested. We sampled five ecotones to seek evidence on seven generalizations that are commonly made about ecotones: vegetational sharpness, physiognomic change, occurrence of a spatial community mosaic, many exotic species, ecotonal species, spatial mass effect, and species richness higher or lower than either side of the ecotone. The ecotones were in a sequence from scattered mangroves, through salt marsh, rush‐marsh, scrub, woodland, to pasture. We developed a method to objectively define, by rapid vegetational change, the position and depth of an ecotone, identifying five ecotones. Their positions were consistent across three sampling schemes and two spatial grain sizes. One ecotone is a switch ecotone, produced by positive feedback between community and environment. Another is anthropogenic, due to clearing for agriculture. Two others are probably environmental in cause, and one may be largely a relict environmental ecotone. Sharp changes in species composition occurred. Three ecotones were associated with a change in plant physiognomy. In two, the ecotone was located just outside a woodland canopy, in the zone influenced by the canopy. Community mosaicity was evident at only one ecotone. There were few strictly ecotonal species; many species occurred more frequently within ecotones than in adjacent vegetation, but there were never significantly more ecotonal species than expected at random. There was little evidence for the spatial mass effect reducing ecotonal sharpness, or leading to higher species richness within ecotones. Species richness was higher than in the adjacent habitat in only one ecotone. It seems that supposedly characteristic ecotone features depend on the particular ecological situation, and the ecology of the species present, rather than being intrinsic properties of ecotones.     

河北北部和内蒙古东部森林-草原交错带森林景观格局初步研究

河北北部、内蒙古东部森林 草原交错带的森林景观主要有白桦林、山杨林、云杉林、蒙古栎林和榆树疏林。森林斑块的数量在森林 草原交错带的森林草甸区最多 ,其次是森林带 ,再次是森林 草原交错带的草甸草原区 ,草原带没有森林斑块。从森林带到森林 草原交错带 ,森林斑块变小、森林景观破碎化程度提高。森林 草原交错带森林景观的形成是气候变化和现代气候、地形、火灾和人为活动综合作用的结果     

Functioning of land-water ecotones in relation to nutrient cycling

Preliminary results of the study on the functioning of the littoral zone of the Gooimeer, The Netherlands, are presented. The results comprise data on the chemical composition of the open water and the aquatic littoral zone, the composition of phytoplankton, metaphyton and epiphyton. On the basis of these data, the Gooimeer littoral zone is characterized as an eutrophic land-water ecotone dominated by a few species of primary producers. Some data on characteristic processes concerning the decomposition of organic matter in rooted littoral sediments are also discussed. Enzyme activities, relevant to mineralization of macrophytic polymers, appear to be highly stimulated in the reed belt of the littoral zone. A first impression of the distribution and the efflux of oxygen in the rhizosphere of reed is given.     

The role of seed predation in the maintenance of the Cross Timbers ecotone of Oklahoma,USA

I investigated how seed predation differed among tree species and among microhabitats across the Cross Timbers and what that variation may tell us about how this ecotone is maintained. The ecotone is located in Oklahoma, USA, between the eastern deciduous forest and tallgrass prairie where seeds of eight common tree species were placed in three microhabitats (oak forest, tallgrass prairie, and sumac shrub/small-tree/grass mix). After nine days in the field, percent seeds remaining were scored for each of the 120 (8 species×3 microhabitats×5 replicates) dishes. I found for both wind-dispersed tree species, (ash, elm) there was significantly more predation in the prairie microsite, with similar small predation levels in the shrub and forest. For two of the three bird-dispersed species (dogwood, hackberry), there was significantly more predation in the prairie and shrub microsites compared to the forest. Red cedar, however, was not taken by predators very much anywhere. Finally, all three mammal-dispersed tree species (two oaks, pecan) showed significantly more predation in the shrub and forest microsites compared to the prairie. Whereas wind- and bird-dispersed species suffered less predation as microsites became more woody and dark, the dominant oaks showed the opposite trend. Consequently, seed predators are not preventing oaks from advancing across this ecotone, but yearly fluctuations in predator population density, especially in the shrub transitional zone, could be helping to maintain it.