滨海湿地生态系统土壤微生物及其影响因素研究综述

土壤微生物是滨海湿地生态系统中不可或缺的关键组分,在土壤发育、物质循环和污染物净化等诸多土壤生态过程中发挥着重要作用,对滨海湿地生态系统的维持与健康具有重大影响。系统梳理了滨海湿地土壤微生物群落结构特征和多样性,综述了土壤理化性质、植被状况、水文因素、生物入侵、全球变化、湿地开垦、石油污染等因素对滨海湿地土壤微生物的影响。在此基础上,对今后的研究重点提出了4个方面的展望:(1)加强全球变化多因子交互作用下滨海湿地土壤微生物的响应机制;(2)强化滨海湿地土壤微生物与环境因子的互作机理;(3)深化滨海湿地水动力条件对土壤微生物的影响机制;(4)开展土壤微生物与滨海湿地生态系统物质循环综合研究。研究以期为滨海湿地生态系统的保护和修复提供参考。     

白洋淀湿地区土壤有机碳密度及储量的空间分布特征

湿地生态系统碳储量是陆地生态系统碳循环的重要组成部分,提供重要的生态系统服务功能。白洋淀湿地是国家重要生态湿地和华北平原最大的淡水湿地,同时是雄安新区的核心水系,湿地区土壤碳储量的估算研究将为湿地生态系统服务评估和湿地生态恢复提供数据支撑。研究通过对白洋淀湿地7种不同地类的105个土壤剖面进行分层取样,揭示了其湿地土壤有机碳密度及储量的空间分布特征,结果表明:(1)白洋淀湿地区土壤有机碳含量整体偏低,在各层土壤中,淹水芦苇湿地的有机碳含量均显著高于其他植被类型,约为其他类型土壤碳含量的3倍左右。(2)在各植被类型中土壤有机碳含量均以表层(0—20 cm)最高,其分配比例均集中在30%左右,随着土壤剖面深度的增加,湿地土壤的有机碳含量逐渐减少。(3)不同植被类型土壤有机碳含量与土壤有机碳密度的差异显著,具体表现为:乔木园地<旱地<常绿针叶林<落叶阔叶林<水田<台田芦苇<淹水芦苇。(4)根据估算,白洋淀湿地区的土壤有机碳储量约为5816.77×10³Mg。随着雄安新区环境治理工作的推进,白洋淀湿地区生态系统固碳将呈现持续向好态势,结...     

长江河口典型湿地碳库动态研究方法

湿地生态系统在维持碳平衡和全球气候调节中起着重要作用。长江河口湿地生态系统是国际公认的生态过程敏感区,选择长江河口典型湿地——崇明东滩作为长期碳循环观测和实验模拟的研究对象,针对长江河口湿地生态系统碳库动态研究具体的科学问题,从"土壤-植被-大气"连续体(SPAC)碳流过程监测、涡度相关法碳通量监测、植物生长控制实验(开顶式气候室,OTC)、"湿地碳循环-气候变化"生态过程模型构建、多方数据源校正等方面,总结了全球气候变化条件下长江河口湿地碳库动态的研究方法。旨在了解长江河口湿地生态系统碳库动态特征,探寻湿地碳平衡的主导控制因子,评估中国东部沿海湿地碳库对全球气候变化的响应。进而为提出长江河口湿地碳储备功能的保育策略提供理论依据。     

国内外湿地生态系统研究进展

湿地生态系统具有重要的生态功能和社会经济价值。由于诸多因素的影响,目前全球范围内相当一部分湿地生态系统已经丧失或正在遭受不同程度的威胁,湿地生态系统已经成为近年来相关领域研究的热点之一。近年来,国内外湿地生态系统的研究主要集中在湿地生态系统生物多样性本底资料的调查、湿地生态系统的动态以及湿地生态系统胁迫因子研究、退化湿地生态系统的重建和管理,以及恢复湿地有效性的评估体系等4个方面。一些新方法、新技术也不断应用于湿地生态系统研究中。除了自然湿地外,人工湿地的构建和评价体系的建立也成为该领域研究的热点方向。影响湿地生态系统的因素涉及到自然、社会经济、文化等多个方面,加之湿地类型多样性,因此开展更为广泛的湿地生态系统结构、功能和动态的研究是十分必要的。同时,对特定区域内的湿地生态系统修复过程中的关键技术(包括物种的选择等)的研究、新方法和新手段的应用研究也应该在湿地生态系统研究中给予特别关注。     

植物功能性状与湿地生态系统土壤碳汇功能

湿地生态系统碳平衡对气候变化极为敏感,是陆地生态系统碳循环响应全球变化的重要环节。然而,湿地生态系统碳汇调节机制仍不十分清楚,并且对影响因子的研究多集中在非生物因子上。综述了植物功能性状和功能性状多样性对湿地生态系统土壤碳汇功能的影响,阐明了生物因子对生态系统碳循环响应全球变化的重要性,介绍了植物功能性状对生态系统碳输入和输出过程的影响,简述了植物功能性状多样性的研究现状及其在指示生态系统碳汇功能现状和预测未来趋势等方面的应用。从优势植物、植物种间关系和植物-微生物种间关系3方面总结了植物功能性状多样性直接和间接影响生态系统碳循环的途径。展望了植物功能性状和功能性状多样性与湿地生态系统土壤碳汇功能的研究前景。     

西藏高原湿地植物和土壤细菌多样性及其影响因素分析

植物和微生物是湿地生态系统的主要组成部分,也是其能量流动和物质循环的重要驱动力。了解湿地植物和土壤微生物的多样性及其关键影响因子,对于维持湿地生态系统的结构和功能有重要意义。本研究对西藏高原26个湿地进行野外调查和实验室分析,以揭示湿地植物与土壤细菌多样性的关系,明确影响植物多样性和土壤细菌多样性的关键因子。结果显示,植物群落特征与土壤细菌多样性显著相关,但驱动土壤细菌多样性变异的主要因素是环境因子而非植物。植物多样性的变异主要受土壤电导率影响,而细菌多样性的变异则与海拔、年降水量、土壤pH值以及植物功能性状（叶片总氮和总碳）相关。     

湿地水生无脊椎动物群落结构及影响因素

湿地是介于陆地和水体系统之间的具有多种功能的特殊地理综合体和生态系统。水生无脊椎动物是湿地生态系统的一个重要类群,是湿地物质循环和能量流动的重要参与者,其群落特征及空间分布能够反映出湿地的许多特征。本文总结了湿地水生无脊椎动物组成特征,系统介绍了不同类型湿地中水生无脊椎动物群落结构,讨论了非生物因子(底质、温度、水文、溶解氧、pH、氮、磷等)、生物因子(植被、竞争和捕食)及人类活动干扰(电站建设、城镇化等)对湿地水生无脊椎动物群落结构的影响,提出了目前湿地水生无脊椎动物研究存在的问题,并对未来研究方向和重点提出了展望。     

寒温带湿地火后植被恢复的影响因子

寒温带湿地在维护区域生态平衡方面发挥着重要作用.火是湿地的重要干扰因子.重度火烧会导致湿地生态功能明显退化.火后植被恢复,特别是火后早期植被的恢复是生态系统功能恢复的前提和基础.本文对火后湿地植被恢复影响因子的国内外研究进展进行了综述.寒温带湿地火后植被恢复受到火强度、火面积、火前植被类型、物种更新特性、立地条件等多因子的制约.寒温带湿地火后恢复的长期监测、植被恢复的关键影响因子、冻土层在植被恢复过程中的作用、植被恢复的理论与技术将是今后研究的重要方向.     

荒漠灌丛土壤动物分布及其生态功能

在干旱、半干旱荒漠生态系统中,灌丛作为一种重要的植被类型,其独特的形态和生理适应特性能够有效促进退化生态系统结构与功能的恢复。土壤动物是荒漠生态系统中不可或缺的重要组成部分,对促进灌丛"肥岛"演变具有重要的生态作用,有利于灌丛生态功能的发挥及退化生态系统的恢复。近年来,国内外学者对荒漠灌丛微生境土壤动物的研究逐步深入,取得大量的研究成果。在此基础上,首先综述荒漠灌丛微生境土壤动物群落分布和生态功能,总结灌丛与土壤动物分布间作用关系的数学模型,针对荒漠灌丛土壤动物研究中存在的问题提出了未来可能的研究方向和建议。     

生源要素有效性及生物因子对湿地土壤碳矿化的影响

湿地土壤是全球碳存储的重要场所,湿地生态系统的碳循环过程对全球变化有重要指示作用。土壤碳矿化是湿地生态系统碳循环的重要环节,对于认知湿地生态系统生物地球化学循环过程具有重要的意义。综述了生源要素及生物因素对湿地土壤碳矿化的内在作用机制。土壤活性有机碳库通过调节土壤能源物质和微生物活性影响土壤碳库的有效性,是表征土壤碳矿化的敏感指标。湿地其它养分如N、P、S等元素的有效性也是影响土壤碳矿化的关键要素。电子受体(NO₃^-、SO₄^2-、Fe³⁺、Mn⁴⁺等)对湿地土壤碳矿化和有机碳转变的影响主要通过电子受体的还原过程完成,在厌氧分解过程中,湿地土壤利用难溶性电子受体可能是土壤C矿化的更重要途径。动物、植物、微生物群落和区系等则是土壤碳矿化的主要驱动因子。土壤动物区系在有机态养分矿化为无机态养分的过程有着独特的功能,能显著增加土壤碳矿化。土壤微生物的活性,决定着土壤中有机碎屑的降解速率,是土壤有机碳分解周转的主要诱导因素。湿地植物则通过影响根系、微生物呼吸底物的供应以及对小气候和土壤因子的调节而影响土壤有机质的分解。湿地生源要素和生物因子还极易与土壤理化性质如温度、水分、pH值和质地等环境因素形成交互和制约,共同影响土壤碳矿化。最后,提出了进一步研究生源要素和生物因素与湿地土壤碳矿化关系需要解决的一些重要问题。     

Ecosystem Development After Mangrove Wetland Creation: Plant–Soil Change Across a 20-Year Chronosequence

Mangrove wetland restoration and creation efforts are increasingly proposed as mechanisms to compensate for mangrove wetland losses. However, ecosystem development and functional equivalence in restored and created mangrove wetlands are poorly understood. We compared a 20-year chronosequence of created tidal wetland sites in Tampa Bay, Florida (USA) to natural reference mangrove wetlands. Across the chronosequence, our sites represent the succession from salt marsh to mangrove forest communities. Our results identify important soil and plant structural differences between the created and natural reference wetland sites; however, they also depict a positive developmental trajectory for the created wetland sites that reflects tightly coupled plant-soil development. Because upland soils and/or dredge spoils were used to create the new mangrove habitats, the soils at younger created sites and at lower depths (10–30?cm) had higher bulk densities, higher sand content, lower soil organic matter (SOM), lower total carbon (TC), and lower total nitrogen (TN) than did natural reference wetland soils. However, in the upper soil layer (0–10?cm), SOM, TC, and TN increased with created wetland site age simultaneously with mangrove forest growth. The rate of created wetland soil C accumulation was comparable to literature values for natural mangrove wetlands. Notably, the time to equivalence for the upper soil layer of created mangrove wetlands appears to be faster than for many other wetland ecosystem types. Collectively, our findings characterize the rate and trajectory of above- and below-ground changes associated with ecosystem development in created mangrove wetlands; this is valuable information for environmental managers planning to sustain existing mangrove wetlands or mitigate for mangrove wetland losses.     

蚯蚓在生态系统中的作用

蚯蚓能够对许多决定土壤肥力的过程产生重要影响, 被称为“生态系统工程师”。它通过取食、消化、排泄和掘穴等活动在其体内外形成众多的反应圈, 从而对生态系统的生物、化学和物理过程产生影响。蚯蚓在生态系统中既是消费者、分解者, 又是调节者, 它在生态系统中的功能具体表现在: (1) 对土壤中有机质分解和养分循环等关键过程的影响; (2) 对土壤理化性质的影响; (3) 与植物、微生物及其他动物的相互作用。蚯蚓活动及其在生态系统中的功能受蚯蚓生态类群、种群大小、植被、母岩、气候、时间尺度以及土地利用历史的综合控制。蚯蚓外来种入侵与生态系统的关系以及蚯蚓对全球变化的响应和影响是两个值得关注的问题。土壤本身的复杂性, 蚯蚓自然历史和生物地理学知识的缺乏, 野外控制蚯蚓群落方法的滞后等都限制了蚯蚓生态学的发展。其他新技术如研究养分循环的碳氮同位素分析和揭示土壤微结构的图像分析等技术的应用是蚯蚓生态功能研究的迫切需要。     

Legacy phosphorus in subtropical wetland soils: Influence of dairy, improved and unimproved pasture land use

Wetlands provide various ecosystem services. One of these services includes nutrient storage in soils. Soils retain and release nutrients such as phosphorus (P). This dynamic can be controlled by soil characteristics, overlying water quality, environmental conditions and historical nutrient loading. Historical nutrient loading contributes to a legacy of P stored in soils and this may influence present day P dynamics between soil and water. We quantified P characteristics of wetland soils and determined the availability and capacity of soils to retain additional P loadings. We sampled surface (0-10) and subsurface (10-30) wetland soils within dairy, improved and unimproved pastures. Surface soils had much greater concentrations of organic and inorganic P. Wetland soils in dairy had greatest concentrations of Ca and Mg, probably due to inputs of inorganic fertilizer. They also had much greater total P, inorganic P, and P sorption capacity; however, these soils were P saturated and had little capacity to retain additional P loading. Improved and unimproved pasture wetland soils had greatest amounts of organic P (>84%) and a capacity to store additional P loadings. Using multivariate statistics, we determined that rather than being different based on land use, wetland soils in improved and unimproved pasture were dissimilar based upon organic matter, organic P fractions, residual P, and soil metal (Fe and Al) content. The legacy of stored P in soils, particularly wetland soils from dairies, combined with best management practices (BMPs) to reduce nutrient loading to these systems, could contribute to a short-term release of soil-stored P to overlying wetland water.     

湿地资源保护经济学分析——以北京野鸭湖湿地为例

湿地资源保护是全球生态保护的核心问题之一。在分析湿地资源保护的经济属性的基础上,以北京市野鸭湖湿地为案例,运用经济学的理论和方法以及清晰的图表重点分析了野鸭湖湿地资源保护过程中的外部性以及资源利用中成本与收益两个问题。研究结果表明:(1)从正外部性分析,个人收益小于社会收益,个人保护的湿地资源小于社会最优量,会造成湿地资源保护的不足;从负外部性分析,个人成本小于社会成本,个人对湿地资源的利用水平大于社会最优利用水平,造成湿地资源的过度利用;(2)根据湿地资源利用的成本收益分析结果,"搭便车"行为会造成湿地资源的退化甚至恶化;(3)明晰产权有利于湿地资源配置效率的提高。研究结果可以为中国湿地保护过程中出现的资源利用矛盾提供有益的借鉴,特别是为保护北京野鸭湖湿地提供理论支撑和政策建议。     

Detecting soil and plant community changes in restored wetlands using a chronosequence approach

Wetland restoration aims to recreate or enhance valuable ecosystem services lost during wetland destruction. Regaining wetland ecosystem services depends on restarting basic wetland functions, like carbon (C) storage, which are unmeasured in many Wetlands Reserve Program (WRP) restoration sites. We collected soil and plant data from 17 WRP sites in western New York that were used for tillage or non-tillage agriculture and then actively restored as isolated depressional wetlands by excavating basins and disabling drainage systems. Sites had been restored for 0–15 years when sampled in August-October 2010. We analyzed data as chronosequences and tested whether soil and vegetation parameters in restored wetlands, over time, (1) departed from pre-restoration baselines, estimated using active agricultural fields paired to each WRP site, and (2) converged towards “natural” benchmarks, estimated from four naturally-occurring wetlands. Restored WRP soils remained similar to agricultural soils in organic matter, density, moisture, and belowground plant biomass across chronosequences, indicating negligible C storage and belowground development for 15 years following restoration. Soil changes were limited in sites restored after both tillage and non-tillage agriculture and throughout the upland meadow, emergent shoreline, and open-water habitat zones that characterize these sites. Many plant metrics like aboveground biomass matched natural wetlands within 15 years, but recovered inconsistently among tilled and untilled sites and across all habitat zones, suggesting land-use history impacts and/or zonation effects. Disparities in recovery times exists between vegetation, which can respond quickly to wetland restoration, and underlying soils, which show limited signs of recovery 15 years after being restored.     

湿地生态系统设计的一些基本问题探讨

湿地生态系统设计是恢复、调整湿地的重要手段,本文3从湿地生态系统设计概念入手,阐述了设计的基本原则。较详细地讨论了设计中的指标（水文指标、化学指标、基质指标和生物指标）要求,根据湿地生态系统设计的用途不同,探讨了3种主要的湿地生态系统设计类型,即作为废水处理湿地的设计,作为调整湿地的系统设计和作为洪水及非点源污染控制的湿地设计。     

Different plant traits affect two pathways of riparian nitrogen removal in a restored freshwater wetland

Background & aims

Plants may have dissimilar effects on ecosystem processes because they possess different attributes. Given increasing biodiversity losses, it is important to understand which plant traits are key drivers of ecosystem functions. To address this question, we studied the response of two ecosystem functions that remove nitrogen (N) from wetland soils, the accumulation of N in plant biomass and denitrification potential (DNP), to variation in plant trait composition.

Methods

Our experiment manipulated plant composition in a riparian wetland. We determined relative importance of plant traits and environmental variables as predictors of each ecosystem function.

Results

We demonstrate that Water Use Efficiency (WUE) had a strong negative effect on biomass N. Root porosity and belowground biomass were negatively correlated with DNP. Trait ordination indicated that WUE was largely orthogonal to traits that maximized DNP.

Conclusions

These results indicate that plant species with different trait values are required to maintain multiple ecosystem functions, and provide a more mechanistic, trait-based link between the recent findings that higher biodiversity is necessary for multi-functionality. While we selected plant traits based on ecological theory, several of the plant traits were not good predictors of each ecosystem function suggesting the ecological theory linking traits to function is incomplete and requires strengthening.     

Differences of ecological functions inside and outside the wetland nature reserves in Sanjiang Plain, China

Conservation effectiveness of wetland nature reserves is determined by both the management intensity inside the reserves and the hydrological status outside the reserves. Therefore, differences of ecological functions inside and outside the reserves are an integrated indictor for assessing conservation effectiveness. Based on the land use map created from Landsat-TM satellite image and 1:50000 Digital Elevation Model (DEM) data in the study area, the catchments that belong to the wetland reserves were determined as their hydrological sensitive zones by SWAT (Soil and Water Assessment Tool) hydrological model. The ecological function indices of wetland reserves and their corresponding hydrological sensitive zones were calculated through expert consultation and value assessment on wetland ecosystem service functions. The results showed that the ecological functions of national wetland reserves were better than those of local reserves in general. However, the wetland ecological functions of hydrological sensitive zones of the former were not always better than those of the latter. Meanwhile, clustering analysis showed that the wetland ecological functions of several adjacent reserves in Nongjiang-Bielahonghe watershed were similar. But correlation analysis found that there existed a remarkable positive correlation between the wetland ecological function indices of local reserves and their hydrological sensitive zones.