River beads as a conceptual framework for building carbon storage and resilience to extreme climate events into river management

River beads refer to retention zones within a river network that typically occur within wider, lower gradient segments of the river valley. In lowland, floodplain rivers that have been channelized and leveed, beads can also be segments of the river in which engineering has not reduced lateral channel mobility and channel-floodplain connectivity. Decades of channel engineering and flow regulation have reduced the spatial heterogeneity and associated ecosystem functions of beads occurring throughout river networks from headwaters to large, lowland rivers. We discuss the processes that create and maintain spatial heterogeneity within river beads, including examples of beads along mountain streams of the Southern Rockies in which large wood and beaver dams are primary drivers of heterogeneity. We illustrate how spatial heterogeneity of channels and floodplains within beads facilitates storage of organic carbon; retention of water, solutes, sediment, and particulate organic matter; nutrient uptake; biomass and biodiversity; and resilience to disturbance. We conclude by discussing the implications of river beads for understanding solute and particulate organic matter dynamics within river networks and the implications for river management. We also highlight gaps in current understanding of river form and function related to river beads. River beads provide an example of how geomorphic understanding of river corridor form and process can be used to restore retention and resilience within human-altered river networks.     

Extreme weather events threaten biodiversity and functions of river ecosystems: evidence from a meta-analysis

Both gradual and extreme weather changes trigger complex ecological responses in river ecosystems. It is still unclear to what extent trend or event effects alter biodiversity and functioning in river ecosystems, adding considerable uncertainty to predictions of their future dynamics. Using a comprehensive database of 71 published studies, we show that event – but not trend – effects associated with extreme changes in water flow and temperature substantially reduce species richness. Furthermore, event effects – particularly those affecting hydrological dynamics – on biodiversity and primary productivity were twice as high as impacts due to gradual changes. The synthesis of the available evidence reveals that event effects induce regime shifts in river ecosystems, particularly affecting organisms such as invertebrates. Among extreme weather events, dryness associated with flow interruption caused the largest effects on biota and ecosystem functions in rivers. Effects on ecosystem functions (primary production, organic matter decomposition and respiration) were asymmetric, with only primary production exhibiting a negative response to extreme weather events. Our meta-analysis highlights the disproportionate impact of event effects on river biodiversity and ecosystem functions, with implications for the long-term conservation and management of river ecosystems. However, few studies were available from tropical areas, and our conclusions therefore remain largely limited to temperate river systems. Further efforts need to be directed to assemble evidence of extreme events on river biodiversity and functioning.     

西江大型底栖动物群落特征研究

河流担负着水源供给、食物生产、旅游、航运等功能。近年来, 人类活动的加剧导致河流生态系统受到威胁。底栖动物常被作为环境指示生物, 研究其群落特征为河流保护及管理有着重要意义。为了航运需求,西江开展了航道整治工程, 由此引起河道生物栖息生境条件的改变, 从而影响河流的生态健康。为了西江的保护和管理, 研究于2009 年枯水期和2010 年丰水期对西江的底栖动物开展了系统调查。调查期间共鉴定底栖动物70 种, 隶属于30 科59 属。其中环节动物7 科12 属16 种, 软体动物11 科14 属21 种, 节肢动物11科32 属32 种, 其他动物1 科1 属1 种。底栖动物的密度和生物量分别为140 ind/m2、0.23 g dry weight/m2。统计分析表明河床底质在底栖动物丰度和分布上起着尤为重要的作用。稳定性越高的底质越有利于底栖动物生存。软泥底质以直接收集者(主要包括颤蚓科寡毛类和摇蚊亚科昆虫)占优, 而各类石质底质则以刮食者(主要是短沟蜷Semisulcospira spp.)或过滤收集者(主要是淡水壳菜Limnoperna lacustris)占优。西江航道整治工程的开展降低了生境条件质量甚至使得原有生物栖息地丧失, 由此会对底栖动物的生存产生不利影响。       

Characterization of hydraulic habitat and retention across different channel types; introducing a new field-based technique

Understanding the interactions between physical habitat and aquatic biodiversity has become a key research objective in river management. River research and management practitioners are increasingly seeking new methodologies and techniques for characterizing physical habitat heterogeneity. The physical biotope has been widely employed as the standard mesoscale unit in river surveys. However, few surveys have quantified the combined physical heterogeneity at the meso- and microscale scale via a single technique. This paper describes a new field methodology for assessing variations in hydraulic habitat and retention across different channel types (e.g. step-pool, bedrock, plane-bed and pool-riffle). Hydraulic habitat and retention was measured by timing 100 flow tracers across a 100-m stream length, and recording the types of trapping structures. The pattern of flow tracers and retention varied significantly between channel types and structures. Rocks (boulders and cobbles) were more important retentive structures than eddies and snags (woody material and vegetation). The results indicate the importance of a diverse hydraulic environment, woody material and channel substrate character in increasing physical heterogeneity within a stream reach. The findings suggest that the field methodology may be an effective tool to assess differences in physical heterogeneity pre and post river restoration activities.     

Have grass carp driven declines in macrophyte occurrence and diversity in the Vaal River,South Africa?

The Vaal River, South Africa, historically had a rich diversity of native submerged macrophytes with at least 13 species from 5 families recorded. Over the past 10 years there has been a noticeable reduction in the occurrence and diversity of submerged macrophytes in the river. It is possible that this is linked to the recent increase in the populations of invasive alien grass carp Ctenopharyngodon idella Cuvier & Valenciennes (Cyprinidae) in the river, where populations have been a concern since 2005. Grass carp invasions worldwide have been shown to have severe impacts on macrophyte biodiversity and ecosystem functioning. This fish is an aggressive feeder on submerged macrophytes, as well as being an ecosystem engineer that can change water and sediment chemistry.     

A national approach for mapping and quantifying habitat-based biodiversity metrics across multiple spatial scales

Ecosystem services, i.e., services provided to humans from ecological systems have become a key issue of this century in resource management, conservation planning, and environmental decision analysis. Mapping and quantifying ecosystem services have become strategic national interests for integrating ecology with economics to help understand the effects of human policies and actions and their subsequent impacts on both ecosystem function and human well-being. Some aspects of biodiversity are valued by humans in varied ways, and thus are important to include in any assessment that seeks to identify and quantify the benefits of ecosystems to humans. Some biodiversity metrics clearly reflect ecosystem services (e.g., abundance and diversity of harvestable species), whereas others may reflect indirect and difficult to quantify relationships to services (e.g., relevance of species diversity to ecosystem resilience, cultural value of native species). Wildlife habitat has been modeled at broad spatial scales and can be used to map a number of biodiversity metrics. In the present study, we present an approach that (1) identifies mappable biodiversity metrics that are related to ecosystem services or other stakeholder concerns, (2) maps these metrics throughout a large multi-state region, and (3) compares the metric values obtained for selected watersheds within the regional context. The broader focus is to design a flexible approach for mapping metrics to produce a national-scale product. We map 20 biodiversity metrics reflecting ecosystem services or other aspects of biodiversity for all vertebrate species except fish. Metrics include species richness for all vertebrates, specific taxon groups, harvestable species (i.e., upland game, waterfowl, furbearers, small game, and big game), threatened and endangered species, and state-designated species of greatest conservation need, and also a metric for ecosystem (i.e., land cover) diversity. The project is being conducted at multiple scales in a phased approach, starting with place-based studies, then multi-state regional areas, culminating into a national-level atlas. As an example of this incremental approach, we provide results for the southwestern United States (i.e., states of Arizona, New Mexico, Nevada, Utah, and Colorado) and portions of two watersheds within this region: the San Pedro River (Arizona) and Rio Grande River (New Mexico). Geographic patterns differed considerably among metrics across the southwestern study area, but metric values for the two watershed study areas were generally greater than those for the southwestern region as a whole.     

Large wood and fluvial processes

1. Large wood forms an important component of woodland river ecosystems. The relationship between large wood and the physical characteristics of river systems varies greatly with changes in the tree species of the marginal woodland, the climatic and hydrological regime, the fluvial geomorphological setting and the river and woodland management context. 2. Research on large wood and fluvial processes over the last 25 years has focussed on three main themes: the effects of wood on flow hydraulics; on the transfer of mineral and organic sediment; and on the geomorphology of river channels. 3. Analogies between wood and mineral sediment transfer processes (supply, mobility and river characteristics that affect retention) are found useful as a framework for synthesising current knowledge on large wood in rivers. 4. An important property of wood is its size when scaled to the size of the river channel. ′Small′ channels are defined as those whose width is less than the majority of wood pieces (e.g. width < median wood piece length). `Medium' channels have widths greater than the size of most wood pieces (e.g. width < upper quartile wood piece length), and `Large' channels are wider than the length of all of the wood pieces delivered to them. 5. A conceptual framework defined here for evaluating the storage and dynamics of wood in rivers ranks the relative importance of hydrological characteristics (flow regime, sediment transport regime), wood characteristics (piece size, buoyancy, morphological complexity) and geomorphological characteristics (channel width, geomorphological style) in `Small', `Medium' and `Large' rivers. 6. Wood pieces are large in comparison with river size in `small' rivers, therefore they tend to remain close to where they are delivered to the river and provide important structures in the stream, controlling rather than responding to the hydrological and sediment transfer characteristics of the river. 7. For `Medium' rivers, the combination of wood length and form becomes critical to the stability of wood within the channel. Wood accumulations form as a result of smaller or more mobile wood pieces accumulating behind key pieces. Wood transport is governed mainly by the flow regime and the buoyancy of the wood. Even quite large wood pieces may require partial burial to give them stability, so enhancing the importance of the sediment transport regime. 8. Wood dynamics in `Large' rivers vary with the geometry of the channel (slope and channel pattern), which controls the delivery, mobility and breakage of wood, and also the characteristics of the riparian zone, from where the greatest volume of wood is introduced. Wood retention depends on the channel pattern and the distribution of flow velocity. A large amount is stored at the channel margins. The greater the contact between the active channel and the forested floodplain and islands, the greater the quantity of wood that is stored.     

Linking biodiversity indicators,ecosystem functioning,provision of services and human well-being in estuarine systems: Application of a conceptual framework

Assuming that human well-being strongly relies on the services provided by well-functioning ecosystems, changes in the ecological functioning of any system can have direct and indirect effects on human welfare. Intensive land use and tourism have expanded in recent decades along coastal ecosystems, together with increasing demands for water, food and energy; all of these factors intensify the exploitation of natural resources. Many of the interrelations between ecosystem functioning and the provision of ecosystem services (ES) still require quantification in estuarine systems. A conceptual framework to assess such links in a spatially and temporally explicit manner is proposed and applied to the Mondego estuary (Portugal). This framework relies on three consecutive steps and discriminates among biodiversity structural components, ecosystem functioning and stability and the services provided by the ecosystem.Disturbances in abiotic factors were found to have a direct effect on biodiversity, ecosystem functioning and the provision of ES. The observed changes in the species composition of communities had a positive effect on the ecosystem's productivity and stability. Moreover, the observed changes in the estuarine ES provision are likely to arise from changing structural and abiotic factors and in the present case from the loss or decline of locally abundant species. This study also indicates that linear relationships between biodiversity, ecosystem functioning and services provision are unlikely to occur in estuarine systems. Instead, cumulative and complex relations are observed between factors on both temporal and spatial scales. In this context, the results suggest several additional conclusions: (1) biodiversity and ecosystem functioning interaction with human well-being need to be incorporated into decision-making processes aimed at the conservative management of systems; (2) the institutional use of research results must be part of the design and implementation of sustainable management activities; and (3) more integrative tools/studies are required to account for the interactions of estuarine ecosystems with surrounding socio-economic activities. Therefore, when performing integrated assessments of ecosystem dynamics, it becomes essential to consider not only the effects of biodiversity and ecosystem functioning on services provision but also the effects that human well-being and ES provision may have on estuarine biodiversity and ecosystem functioning.The proposed framework implies taking into account both the functional and the commodities points of view upon natural ecosystems and by this representing a line of thought which will deserve further research to explore more in detail the conceptual links between biodiversity–ecosystem functioning–services provided.     

Interactive effects of global change drivers as determinants of the link between soil biodiversity and ecosystem functioning

Biodiversity, both aboveground and belowground, is negatively affected by global changes such as drought or warming. This loss of biodiversity impacts Earth's ecosystems, as there is a positive relationship between biodiversity and ecosystem functioning (BEF). Even though soils host a large fraction of biodiversity that underlies major ecosystem functions, studies exploring the relationship between soil biodiversity and ecosystem functioning (sBEF) as influenced by global change drivers (GCDs) remain scarce. Here we highlight the need to decipher sBEF relationships under the effect of interactive GCDs that are intimately connected in a changing world. We first state that sBEF relationships depend on the type of function (e.g., C cycling or decomposition) and biodiversity facet (e.g., abundance, species richness, or biomass) considered. Then, we shed light on the impact of single and interactive GCDs on soil biodiversity and sBEF and show that results from scarce studies studying interactive effects range from antagonistic to additive to synergistic when two individual GCDs cooccur. This indicates the need for studies quantitatively accounting for the impacts of interactive GCDs on sBEF relationships. Finally, we provide guidelines for optimized methodological and experimental approaches to study sBEF in a changing world that will provide more valuable information on the real impact of (interactive) GCDs on sBEF. Together, we highlight the need to decipher the sBEF relationship in soils to better understand soil functioning under ongoing global changes, as changes in sBEF are of immediate importance for ecosystem functioning.     

黄河流域内蒙古段植被时空变化特征及条带状分布成因

监测干旱、半干旱地区植被覆盖度的动态变化,评估大尺度区域地质背景,尤其是活动构造在植被变化过程中发挥的作用对植被时空格局的认识具有重要意义。黄河流域内蒙古段地处干旱半干旱区,植被多依赖于地下水;且该地区活动构造较发育,是认识植被非地带性特征的理想区域。基于中分辨率成像光谱仪（MODIS）、归一化植被指数（NDVI）、气象与土地利用数据,对2000-2018年黄河流域内蒙古段植被覆盖度（FVC）的时空变化及稳定性进行分析,在此基础上针对河套段植被条带状特征及其成因进行讨论。结果表明,近20年研究区的FVC总体表现为增加趋势。降雨增加是大黑河流域、浑河流域及十大孔兑区域FVC增加的主要原因,沙漠地区FVC的增加得益于三北防护林工程建设。大黑河与浑河流域水分条件较好,物种多样性丰富,植被覆盖度高,能较好的抵御气候变化;而十大孔兑区域和沙漠地区FVC较低,生态系统脆弱,对气候波动的响应较大。河套灌区受人类活动主导,对气候变化的敏感性较低。河套段山前植被赋存环境为条带状地下水溢出带,在地下水储量增多条件下呈条带状增加趋势;而在山前过渡带,新构造运动及其造成的较大地表高差使得土壤层薄且储水能力较差,表现为FVC的高波动。现今黄河干流沿岸植被受土地利用转变影响整体减少;且在河流摆动、河道变迁扰动下,稳定性较差。河套盆地与鄂尔多斯台地边界处,受隐伏断裂和地震活动影响,地下水易沿带状透水断裂下渗,难以维持浅表水分和稳定的补给条件,使得FVC呈线状显著降低,且稳定性较差。研究从宏观水文地质条件和地表过程的角度,更加深入认识了植被空间分布的非地带性特征,为相似地区的研究提供了较好的科学依据。     

近60年挠力河流域生态系统服务价值时空变化

根据1950-2005年挠力河流域土地利用数据,利用中国陆地生态系统单位面积生态服务价值当量表,对近60年挠力河流域生态系统服务价值的时空变化进行研究.结果表明,自1950年至2005年,挠力河流域生态系统服务价值逐渐减少,由749.84亿元降低至308.82亿元,损失约58.82％;价值空间格局由以高价值区为主导的状态逐渐转化为以低价值区为主导的状态,且价值质心由北向南发生转移;挠力河流域生态系统服务价值的全局自相关指数逐渐减小,高-高自相关类型沿河流主干道逐渐萎缩,且呈现破碎化趋势,低-低自相关类型呈先减少后增加的“V”趋势,呈现不显著连片化趋势.人为垦殖活动是该流域生态系统服务价值时空动态变化的主要驱动因素.     

生物多样性与生态系统功能:最新的进展与动向

生物多样性与生态系统功能的关系及其内在机制是当前生态学领域的重大科学问题。 2 0 0 2年以来人们不再过多地纠缠于“抽样 -互补之争” ,对这一世纪课题的认识又有了新的进展。 (1)人们开始运用已有的知识揭示更大时间和空间尺度上的物种多样性 -生态系统功能关系。多样性作用机制可能存在着动态变化———“抽样向互补转型” :群落建立初期 ,抽样效应是主要的多样性作用机制 ;随时间推移 ,生态位互补成为主要机制。理论研究则预测 :局域尺度上生态系统功能与物种多样性呈现单峰曲线关系 ,在区域尺度上为单调上升关系 ;(2 )非生物因素与多样性 -生产力的交互关系吸引了许多实验研究。人们发现 :物种多样性 -生产力关系可能会受到资源供给率和环境扰动的修正 ,环境因素可能是多样性 -生产力关系的幕后操纵者 ;(3)人们开始重视营养级相互作用对于多样性 -生态系统功能关系的影响 ,生态位互补和抽样假说开始被扩展运用到消费者营养级上 ;(4 )人们开始认真思考物种共存机制在多样性 -生态系统功能关系的形成中所扮演的角色。理论模型研究表明 ,不同的物种共存机制会导致不同的多样性 -生产力关系     

石羊河流域生态系统服务权衡与协同关系研究

生态系统服务权衡与协同研究是国际生态学、地理学等学科研究的热点。以石羊河流域为研究区,借助In VEST模型,对流域2005、2010和2015年的水源涵养、土壤保持、水质净化、碳储存和生物多样性五项服务进行精准测度,分析服务的时空格局及演变特征,并利用相关系数法逐像元定量计算5种服务之间的权衡与协同关系,从不同尺度分析权衡与协同关系的空间格局特征。结果表明:(1)各项服务具有空间异质性:水源涵养、土壤保持、碳储存、生物多样性呈"西南高-东北低"的空间格局,且水质净化、碳储存服务的高值区沿河流分布。(2) 10年期间,水源涵养、水质净化、碳储存、生物多样性服务呈现"整体增加-局部减少"的变化趋势,而土壤保持呈"整体减少-局部增加"的变化特征。(3)多种服务之间权衡与协同关系具有区域依赖特征:水源涵养与土壤保持、水源涵养与水质净化、水质净化与碳储存、水质净化与生物多样性、土壤保持与碳储存、土壤保持与生物多样性以权衡关系为主;水源涵养与碳储存、水源涵养与生物多样性、土壤保持与水质净化、碳储存与生物多样性以协同关系为主。定量可视化评估生态系统服务及权衡关系,为制定区域发展与生态保护双赢政策提供依据,同时也为其他流域的相关研究提供可靠参考。     

黄河三角洲潮间带及近岸浅海大型底栖动物物种组成及长周期变化

黄河三角洲湿地是渤海重要的生态功能区, 在生物多样性保护与生态功能恢复方面发挥着重要作用。为系统研究该区域内大型底栖动物群落物种组成及时空分布, 作者在该区域典型潮间带和近岸浅海(5 m以浅水域)布设11个断面, 分别于2016年8月和11月, 2017年5月、8月和11月进行3个季节取样。结果显示: 黄河三角洲潮间带和邻近海域共发现大型底栖动物187种。其中, 潮间带分布119种, 近岸浅海分布99种。黄河三角洲潮间带和近海大型底栖动物物种组成均具有明显的时空差异。与历史资料相比, 黄河三角洲潮间带和近岸浅海大型底栖动物物种组成发生了明显变化, 动物个体呈小型化趋势。总体表现为自20世纪90年代末至今, 个体大的甲壳动物和软体动物经济类群逐渐被个体小且经济价值较低的多毛类、双壳类和甲壳动物取代。引起上述变化的原因复杂, 主要驱动力包括黄河来水量与输沙量的减少、人类活动(过度捕捞、开发力度加大)和互花米草(Spartina alterniflora)入侵。     

Channel response to multiple damming in a meandering river, middle and lower Aragón River (Spain)

Small hydropower plants (SHP) affect river flow and sediment transport and thus impact river morphology. Eight hydropower schemes were studied along the meandering middle and lower reaches of Aragón River (Spain) to assess their effects on channel morphology and sediment dynamics from 1927 to 2010. GIS tools were used to measure changes in fluvial surfaces, channel planform and lateral and vertical dynamics. Three periods (early, middle and late twentieth century) were analysed to discern the effects of the main pressures, such as changes in land use, large reservoirs upstream and SHPs. Results were combined with field and topographical measurements and hydrological analysis. Active channel width and channel migration suffered a clear reduction in the whole period. They started as a consequence of land cover changes in the drainage basin, but their speed increased after a large reservoir was built upstream. More recent changes occurred since most of the SHPs were put into operation in the 1990s, especially in their short-circuited reaches and in the four more downstream ones. These changes are interpreted as a consequence of reduced discharge, transitory sediment trapping and reactivation of sediment transport after weirs became filled as well as by the impact of flood hydrology.     

Bioturbating space enhances the effects of non‐additive interactions among benthic ecosystem engineers on cross‐habitat nutrient regeneration

Understanding the mechanisms that drive complementary interactions among species is key to the progress of the debate over the role of biodiversity in ecosystem functioning. In addition, interspecific interactions among physical ecosystem engineers have rarely been framed in the context of biodiversity experiments. Here, we provide an empirical test of how the physical niche space of species influences the effects of the biodiversity of bioturbators on cross‐habitat nutrient fluxes in benthic sediments. In the laboratory, we orthogonally manipulated the number and composition of three benthic invertebrate bioturbator species that differ in the dimensions of their bioturbating space niche; i.e. their vertical distribution in the sediment over a gradient of sediment depth and volume. The ammonium (NH₄‐N) flux from the sediment to the water was positively related to bioturbator species richness only in the sediments with the deepest depth and greatest volume. The non‐additive effects of bioturbator species richness on the benthic–pelagic NH₄‐N flux increased linearly with sediment depth and volume, but only in the three‐species mixtures. Furthermore, no individual species dominated the rates of H₄‐N fluxes, indicating that biodiversity effects were mainly driven by complementarity. These results suggest that sediment bioturbating space mediates the magnitude of non‐additive effects among the three invertebrate species and sheds light on the importance of physical niche space in modulating the positive effects of biodiversity on ecosystem functioning.     

青藏高原高寒草地地下生物多样性: 进展、问题与展望

栖息于土壤中的微生物和微型动物种类繁多、数量巨大, 在对地上生物多样性的调控和在生态系统功能与服务的维系中, 具有举足轻重的作用。虽然对土壤微生物以及土壤动物已经开展了广泛的调查, 但是整体上对于地下生物多样性的分布格局、驱动机制及其对全球变化的响应与适应过程, 仍缺乏深刻的认识。青藏高原是全球变化的敏感区域, 其中高寒草地是高原最主要的植被类型, 占高原面积的60%左右, 在高寒生态系统生物多样性维持中具有重要意义。近年来, 已有大量研究关注于高寒草地地下生物多样性, 但是缺乏系统的总结与论述。基于此, 本文从细菌、真菌、古菌、线虫、节肢动物五大土壤生物类群出发, 阐述了青藏高原高寒草地的地下物种丰富度、分布格局及其影响因素, 重点探讨了它们对气候变化和人类活动的响应, 并就未来高寒草地地下生物多样性亟需关注的关键问题进行了展望, 包括: (1)地下各个生物类群的分布格局、各类群之间的联系及驱动机制; (2)地上与地下生物多样性耦联的机制; (3)地下生物多样性对生态系统功能和健康的影响; (4)地下生物多样性的调控实验研究。     

The role of geomorphology in evaluating remediation options for floodplain wetlands: the case of Ramsar-listed Seekoeivlei,eastern South Africa

The range of benefits bestowed by wetlands is today increasingly recognized, and remediation of degraded wetlands is being carried out around the world. Many degraded wetlands are associated with river floodplains, and an essential requirement for their remediation planning is a comprehensive knowledge of the geomorphological functioning of the river channel and floodplain. Here, we review previous geomorphological investigations of the Ramsar-listed Seekoeivlei floodplain wetlands, Free State Province, South Africa, and demonstrate how the knowledge gained is playing a key role in evaluating remediation options that are needed following more than a century of direct and indirect human impacts. Faunal and floral changes, coupled with channel modifications, have altered the flow and sediment regime and initiated major changes to erosional and depositional patterns, including promoting rapid headward growth of a new channel and abandonment of a former channel. These changes have led to further management interventions, including installation of weirs and erosion control structures. In an ideal world, remediation would strive to return a wetland to its natural, pre-impact state but, in reality, other management goals have to be taken into consideration. In the case of Seekoeivlei, these include maintaining current habitat and biodiversity (this has the added advantage of promoting local tourism, especially bird watching), and using the wetlands for water quality enhancement. Attempts to return the wetlands to their pre-impact state (e.g. by removing exotic trees and erosion control structures) would in fact further reduce habitat and biodiversity, permanently in the case of some avian species, and for centuries in the case of some aquatic species, because of the very slow natural rates of channel and floodplain change. Alternative options will all require ongoing intervention, albeit of variable intensity, but in effect will mean that the wetland will never return to its pre-impact state. Remediation will thus create an essentially ‘artificial’ wetland complex that restores some of the ecological and hydrological functions but that is likely to remain very far from its natural geomorphic condition.     

青藏高原沙柳河流域自然径流驱动的流域生物信息流量化特征——以环境微生物为指标

物质流、能量流、信息流是生态系统过程研究中的三大主题。然而,在流域生态学研究中,有关信息流的研究一直缺位。为了推动流域信息流研究,从生物信息流切入,提出"流域生物信息流"概念,将其定义为"生物信息依托于流域生态系统过程在不同空间和系统之间进行传递、交流、作用、反馈的路径、过程与控制",并将其研究内容拟定为主要关注于水陆间、干支流间、上下游间、不同生态斑块间的流域生物信息流及其周期性节律和趋势性变迁,以及地貌、水文、人类活动等对这些生物信息流的影响等。然后,以青藏高原上青海湖重要入湖河流--沙柳河的河流水体微生物和岸带土壤微生物为研究对象,利用环境DNA技术,对沙柳河流域的自然径流驱动的流域生物信息流进行量化研究。结果表明（1）岸带土壤到水体的流域生物信息流主要由地表表面流、地下潜流等驱动,并受环境过滤效应影响,其输移效率降雨天约为62.76%、晴天约为44.16%,其中输移能力降雨天约为68.49%、晴天约为56.82%,环境过滤效应降雨天约为8.38%、晴天约为22.28%;（2）水体上游到下游的流域生物信息流主要由河川径流驱动,并受衰减效应影响,其基础综合输移效率约为97.41%/km,其中径流输移能力约为99.42%/km,无效流域生物信息流占比约为43.46%,无效流域生物信息流的半衰距离约为14.52 km;（3）降雨通过增加地表表面流等的冲蚀搬运能力并削弱环境过滤效应,促使岸带土壤到水体的流域生物信息流输移能力和输移效率增大;（4）流域生物信息流的输入在一定程度上增加了输入地的可检出生物多样性,但这种增加对于流水生态系统来讲是非累积的。     

流域库坝工程开发的生物多样性敏感度分区

流域生态敏感性是流域生态系统遇到干扰时产生生态失衡与生态环境问题的难易程度和可能性大小,生物多样性是其影响最为重要的生态因子。主要考虑物种丰富度、珍稀程度、濒危程度、保护等级和生态系统类型等生物多样性敏感因子,借助GIS强大的空间数据采集和建模分析能力,在专家打分求取敏感因子权重基础上,通过空间模型计算生物多样性敏感度综合得分。基于二级流域综合得分最大值,采用ARCGIS自然间断点法实现敏感度分区,结果表明:极敏感区域主要分布在长江区的岷沱江、金沙江石鼓以下、金沙江石鼓以上、宜宾至宜昌、嘉陵江流域,珠江区的郁江、红柳河和西江流域,西南诸河区的澜沧江、红河和怒江及伊洛瓦底江流域,黄河区的龙羊峡以上流域等,这些区域水生生物特有种和受威胁物种丰度大,国家级自然保护区密集,是陆地生物多样性最丰富的地区。不敏感区域主要分布在松花江区除第二松花江以外流域,西北诸河区的塔里木盆地荒漠、古尔班通古特荒漠、中亚西亚内陆河、塔里木河干流等荒漠区,松花江区低温高寒,具有大森林、大草原、大湿地、大农田和大水域的特点,库坝工程对其生物多样性产生影响的可能性较小,西北诸河的荒漠区生境严酷,生物多样性贫乏,也不具备修建大型水库的条件,生物多样性敏感度也较低。其它区域介于二者之间,因其所处的生态系统类型、物种丰富度、珍稀程度、濒危程度和保护等级不一样,生物多样性敏感度各异。对流域库坝工程产生的生物多样性敏感度进行辨识,可为未来流域水资源合理和适度开发提供科学依据。