丛枝菌根在植物修复重金属污染土壤中的作用

丛枝菌根（Arbuscular mycorrhizae,AM）是自然界中分布最广的一类菌根,AM真菌能与陆地上绝大多数的高等植物共生,常见于包括重金属污染土壤在内的各种生境中。在重金属污染条件下,AM真菌可以减轻重金属对植物的毒害,影响植物对重金属的吸收和转运,在重金属污染土壤的植物修复中显示出极大的应用潜力。重点介绍了AM真菌对植物重金属耐性的影响及其在植物提取和植物稳定中的应用等方面的进展,讨论了未来研究所面临的任务和挑战。     

芦苇在微咸水河口湿地甲烷排放中的作用

本研究以长江口微咸水河口湿地为研究对象,通过模拟潮汐淹没和改进的静态箱法,针对芦苇在不同淹水条件下对甲烷的传输作用进行了研究。结果表明,长期淹没样点割除芦苇前后平均甲烷释放分别为1.60 mgCH4 m-2h-1和0.50 mgCH4 m-2h-1,而短期淹没样点割除芦苇前后平均甲烷释放分别为0.94 mgCH4 m-2h-1和0.55 mgCH4 m-2h-1。芦苇的存在增加了大约41.5%—69%的甲烷释放,割除芦苇导致长期淹没样点甲烷释放显著地减少。从淹水前到淹水后的一个潮周期内,长期淹没样点和短期淹没样点的甲烷释放分别在淹没期达到最小和最大释放(1.21 mgCH4 m-2h-1 vs. 1.18 mgCH4 m-2h-1),说明芦苇对甲烷的传输作用受到潮汐淹没程度的影响。实验室针对芦苇自身产甲烷的可能性进行的离体芦苇茎干和叶片的甲烷释放研究发现,离体茎干释放大约0.7 μL/L和0.2 μL/L甲烷,且下部茎干的甲烷释放量要明显高于上部茎干和叶片,随后均不再增加。结果进一步证实芦苇增加的甲烷排放来自对土壤气体的传输。同时,传输作用主要发生在植株的下部茎干。     

根系分泌物及其在植物修复中的作用

 近年来环境污染日益严重,污染物在土壤植物中的行为引起了人们的高度关注。利用植物去除土壤水体等介质中污染物的植物修复是近10年来兴起的一项安全、廉价的技术,已成为污染生态学和环境生态学的研究热点,它通过植物吸收、根滤、稳定、挥发等方式清除环境中的重金属和有机污染物。国内外有关植物修复的研究报道和概述很多, 但对植物根系分泌物在植物修复中所起的作用及其机理少有述评。 本文从根系分泌物对土壤重金属和土壤有机污染物的去除作用出发,对根系分泌物的种类、数量及其在去除环境污染物中的作用机理和功能地位进行了总结,并借助研究事例对影响植物根系分泌的内外因子,如植物种类、营养胁迫、重金属胁迫、根际环境的理化性质、土壤微生物及其它环境因子进行了讨论。概言之,根系分泌物在修复污染土壤中的重金属途径是多种多样的,主要是通过调节根际pH值、与重金属形成螯合物、络合反应、沉淀、提高土壤微生物数量和活性来改变重金属在根际中的存在形态以及提高重金属的生物有效性,从而减轻它对环境的危害。在清除有机污染物时,根系分泌物中的酶可以对有机污染物进行直接降解,根系分泌物影响下的微生物也可以对有机污染物进行间接降解,且被认为是主要的降解途径。根系分泌物在植物修复过程中确实起着某些重要作用,今后应将这方面的研究重点放在某些特异性根系分泌物植物,尤其是某些重金属超富集植物资源的寻找、筛选上,通过室内实验和野外研究确定其根系分泌物对清除重金属和有机污染物的效率,证实超富集植物根系分泌物的特异性与污染物超富集的内在联系,找到污染土壤生态恢复和治理的有效方法并加以推广应用,如针对性地在被污染地大面积种植此类具特异性根分泌物植物,并辅以营林措施如修剪等,加快生物修复进程,提高修复效率。植物根系分泌物在植物修复过程中所具有的重要生态意义和可能应用前景,为污染生态学和化学生态学之间的联合研究开拓了全新的领域,今后将取得新的突破和重要进展。     

5种湿地植物对土壤重金属的富集转运特征

选择芦苇、水葱、千屈菜、扁秆藨草、长苞香蒲5种湿地植物进行盆栽实验,比较它们对土壤中的5种重金属镉、铬、汞、铅、锌的富集特性,分析重金属在各植物体和土壤中的动态分布,以评价所测植物对土壤中重金属的综合富集能力,为利用植物修复金属污染土壤提供理论依据和技术支持。结果表明:(1)种植湿地植物对土壤重金属的富集效果显著高于无植物对照,且随着处理时间的延长,土壤中重金属镉、铬、汞、铅、锌的含量均呈下降趋势。(2)湿地植物对重金属镉、铬、汞、铅、锌的富集效果差异显著,其中水葱根部对重金属镉的富集系数最大,芦苇根部对重金属铬、汞、铅、锌的富集系数均最大,千屈菜、扁秆藨草和长苞香蒲根部对5种重金属的富集系数均较小;芦苇地上部分对金属镉的富集系数最大,千屈菜地上部分对金属铬、汞、铅的富集系数均最大,水葱地上部分对金属锌的富集系数最大。(3)5种湿地植物对重金属镉、铬、汞、铅、锌的转移系数差异显著,其中扁秆藨草对土壤中镉、铬、铅、锌的转移系数均为最大,对铬和锌的转移系数均大于1,长苞香蒲对铬的转移系数大于1,仅次于扁秆藨草。其他3种植物对5种重金属的转移系数均小于1。研究表明,5种湿地植物对重金属Cd、Cr、Hg、Pb、Zn都有富集和转移的能力,但不同植物对不同重金属的富集效果不同。     

入侵植物加拿大一枝黄花与乡土植物芦苇的相互化感作用

以加拿大一枝黄花和芦苇的共优群落和各自单优群落的种子为化感受体,分析其分别在加拿大一枝黄花和芦苇5个浓度梯度(12.5、25、50、100和200mg·mL-1)浸提液处理下的发芽率和芽长差异,研究2种植物的相互化感作用规律.结果表明:2种植物在共优群落中的千粒重和蒸馏水培养下的发芽率均比单优群落大.加拿大一枝黄花的浸提液对自身种子发芽率在单优和共优群落中均具有在低浓度下(12.5、25 mg·mL-1)轻微促进、中高浓度下(50、100和200mg·mL-1)强烈抑制的作用,其中对共优群落种子的抑制作用尤为显著;而芦苇浸提液对加拿大一枝黄花种子的影响无明显规律.加拿大一枝黄花的种子芽长在单优和共优群落中均随自身浸提液浓度的升高趋于减小,随芦苇浸提液浓度的升高呈波动减小趋势.在芦苇和加拿大一枝黄花浸提液处理下,芦苇种子发芽率在单优群落中均显著大于共优群落(P＜0.05),但2种浸提液处理间无显著差异.     

蚯蚓在重金属污染土壤生物修复中的应用潜力

综述了不同生态类型的蚯蚓的特性及其土壤生态功能;总结了其对土壤重金属富集和有效性的作用及影响重金属活化的机理,并指出目前相关的生物化学机理研究的不足及其未来研究方向.同时,文章针对蚯蚓在农业和环境领域的应用现状,提出其应用于重金属污染土壤的植物提取技术的可能性,在未来工作中应加强真实污染土壤室内模拟和田间试验研究,进一步探索筛选和繁育本地蚯蚓品种以及添加有机物等相关技术.     

植物螯合肽及其在抗重金属胁迫中的作用

植物螯合肽(PCs)广泛存在于植物体中,与植物抗重金属胁迫关系密切。植物螯合肽及其复合物是一类富含半胱氨酸的低分子量化合物。现有研究证明,PCS由谷胱甘肽(GSH)为底物的酶促反应合成,其合成受相关基因的调控,从模式植物拟南芥的突变体中已分离到与PCS合成有关的几个基因。植物螯合肽首先与重金属离子结合形成低分子量(LMW)复合物,以此形态经由细胞质进入液泡后,再与一个分子的植物螯合肽结合,形成对植物组织毒性较小的高分子量(HMW)复合物,从而达到缓解重金属对植物的危害作用。就植物螯合肽及其复合物的结构、生物合成、基因调控及重金属解毒机理等进行了综述,并对今后的研究方向提出了一些看法。     

有机框架材料在多肽富集的应用

生物医药领域近年来发展迅猛,多肽类药物因其生物学活性高、毒性小、生物相容性好等优势,在肿瘤治疗、细胞活性模拟、抗体检测等领域展开广泛应用,多肽的检测分析也成为研究的一大热点。传统的色谱法、溶剂沉淀法、离心超滤法和固相萃取法对多肽能够展现富集效果,但富集的效率往往不够理想。近年来,以有机框架材料为代表的纳米材料,在气体吸附、荧光、传感和催化等领域展开了广泛应用。有机框架材料凭借着独特的结构尺寸,成为了一类理想的生物吸附剂。由于其具有表面可修饰性,能够大大提高对多肽的富集效率。本文着重介绍近5年来金属-有机框架材料（metalorganic frameworks,MOFs）和共价-有机框架（covalent-organic frameworks,COFs）在多肽富集中的应用。     

miRNA在植物重金属胁迫应答中的作用

microRNA （miRNA）是一种新型的长度为20~24 nt的非编码RNA,通过对靶基因的表达调节进而参与调控植物体的多种生理代谢活动。重金属是一类重要的环境污染物,严重危害植物的生长发育,甚至导致植物死亡。植物在长期的进化过程中形成了抵御重金属胁迫的多种机制,如miRNA对特定基因转录后水平的调控就在逆境胁迫应答中发挥重要作用。本文综述了植物中参与重金属胁迫应答miRNA的种类及作用机制,为揭示重金属胁迫条件下基因表达调控机制,以及利用基因工程手段改良植物对重金属的耐受性提供了线索和依据。     

菌根和根分泌物在植物抗重金属中的作用

多年来人们对植物抗重金属的研究一直集中在植物体内的代谢调节和控制上。随着近年来对根际环境的研究,人们发现植物体外的根际环境对植物抗重金属有着重要的影响,目前研究主要集中在对菌根真菌和根系分泌物与植物抗重金属的关系,本文就近年来对菌根真菌和根系分泌物在植物抗重金属毒害中发挥的作用及其可能机理的研究状况作一概述,并对该领域的研究和应用前景作出展望。     

Isoprene emission and primary metabolism in Phragmites australis grown under different phosphorus levels

Aquatic plants are generally used for wastewater purification and phytoremediation, but some of them also emit large amounts of isoprene, the most abundant biogenic volatile organic compound. Since isoprenoid biosynthesis requires high amounts of phosphorylated intermediates, the emission may also be controlled by inorganic phosphorus concentration (Pi) in leaves. We carried out experiments to determine the emission of isoprene from Phragmites australis plants used in reconstructed wetlands to phytoremediate elevated levels of phosphorus contributed by urban wastes. Four groups of plants were grown hydroponically in water containing different levels of KH(2)PO(4). High levels of phosphorus in the water resulted in high Pi in the leaves. High Pi stimulated photosynthesis at intercellular CO(2) concentrations lower and higher than ambient, implying higher ribulose 1,5-bisphosphate carboxylase (Rubisco) activity and higher ribulose 1,5-bisphosphate regeneration rates, respectively. However, isoprene emission was substantially lower at high Pi than at low Pi, and was not associated to photosynthesis rates at high Pi. This surprising result suggests that isoprene is limited by processes other than photosynthetic intermediate availability or by energetic (ATP) requirements under high Pi levels. Irrespective of the mechanism responsible for the observed reduction of isoprene emission, our results show that Phragmites plants may effectively remove phosphorus from water without concurrently increase isoprene emission, at least on a leaf area basis. Thus, Phragmites used in reconstructed wetlands for phytoremediation of urban wastes rich of phosphates will not contribute high loads of hydrocarbons which may influence air quality over urban and peri-urban areas.     

Die-back of Phragmites australis: influence on the distribution and rate of sediment methanogenesis

Methanogenesis was measured during the summer of 1994, in sediment coresand bulk samples from a Phragmites australis wetland in northern Jutland,Denmark. We compared sediment from healthy reed and dying-back reed, andan open lagoon resulting from die-back. Cores revealed variability withdepth and between sites, with the highest rates coinciding with layers oforganic gyttja, and negligible methane production from the underlying sandbase. Methanogenesis rates in the lagoon and die back sites were higher(up to 100–150 nmol h^-1 g^-1dry wt. sediment) than in the healthy reed (50–80 nmolh^-1 g^-1), with the highest rates being recordedfrom May to July. At these times, methanogenesis was markedly temperature-limited; samples incubated at 30 °C anon-limiting temperature, gave rates as high as 200–400nmol h^-1 g^-1 for the lagoon and die-backareas and 150 nmol h^-1 g^-1 for the healthyarea. Addition of 8 mM acetate and H₂/CO₂headspace suggested that both acetate-fermenting andCO₂-reducing bacteria were present. Acetate additions suggested some co-limitation by substrate availability, with acetate limitation occurring in the healthy site during July and in the die-back site during August. Lower rates during August, especially in the healthy area, were associated with low water levels which resulted in more oxidized sediments. The data reveal highly variable methanogenesis in the sediment which, when considered with sediment depths, indicates that sites of Phragmites die-back have significantly greater rates of anaerobic mineralization than surrounding healthy wetland, and may be intense sources of methane.     

Pyrosequencing Reveals Bacterial Diversity in the Rhizosphere of Three Phragmites australis Ecotypes

Here we present the use of high-throughput DNA pyrosequencing to assess bacterial diversity in the rhizosphere of three Phragmites australis ecotypes from the Hexi Corridor, China. In total, 43404 sequences were obtained for the three ecotypes, representing 31 phyla and a small amount of unclassified bacteria. The predominant bacterial groups in the rhizosphere of P. australis were Proteobacteria, Actinobacteria, Bacteroidetes, Chloroflexi, Gemmatimonadetes and Planctomycetes. The bacterial community structure varied with the different degrees of wetland degradation, which were exhibited by the three P. australis ecotypes in the study area. At the phylum level, the Caldiserica, Chlamydiae, Deferribacteres, Lentisphaerae, and candidate division WS3 were only detected in the swamp reed (SR) sample. Then, δ-proteobacteria, Acidobacteria, Cyanobacteria and Fusobacteria decreased, the Actinobacteria increased with the degree of degradation from SR through salt meadow reed (SMR) to dune reed (DR). The functional bacterial genera also varied with wetland degradation. The sulfur and sulfate-reducing, nitrifying and nitrogen-fixing bacteria were more abundant in the rhizosphere of the SR sample. Methane-oxidizing bacteria were abundant in the SR and DR samples but less so in the SMR. In our study, pyrosequencing of different P. australis ecotypes provided insight into the structural variation of the rhizosphere bacterial community. This study gave a database for the use of bacteria in the protection and ecological restoration of wetland.     

Diel methane emission patterns from Scirpus lacustris and Phragmites australis

In mature Phragmites australis and Scirpus lacustris vegetated sediment methane was emitted almost exclusively by plant-mediated transport, whereas in unvegetated, but otherwise identical sediment, methane was emitted almost exclusively by ebullition. Diel variations in methane emission, with highest emission rates at daytime and emission peaks following sunrise, were demonstrated for Phragmites and Scirpus. The diel difference and magnitude of the emission peaks were much smaller for Scirpus than for Phragmites. In contrast to Phragmites, methane concentrations within Scirpus stems did not change significantly over the diel period. These patterns are consistent with a two-way transport mechanism for Phragmites (convective at daytime and diffusive at night-time) and an all day diffusive mechanism for Scirpus. The patterns could not be accounted for by diel variation in air and sediment temperature, plant transpiration, or photosynthetically coupled methane production. Comparison of the experimentally derived ratio of methane emission in helium and nitrogen under light and dark conditions with the theoretical derived ratio (calculated according to the kinetic theory of gases) confirmed the exploitation of the different transport mechanism for Phragmites and Scirpus. Methane emission from Phragmites correlated significantly with incident light, which probably drove the pressure differential associated with thermally induced convection. Decrease of the radial resistance of Scirpus stems for methane transport under light compared to dark conditions, in combination with morphological characteristics of the plant species, suggested that stomatal aperture, regulated by light, controls methane emission from Scirpus. Diel variation in bubble emission from the non-vegetated sediment coincided with sediment temperature changes. The results have important implications for sampling and scaling strategies for estimating methane emission from wetlands.     

Aluminium and phosphate uptake by Phragmites australis: the role of Fe,Mn and Al root plaques

Aluminium, a potentially phytotoxic metal, is an important constituent of many mine water discharges but has largely been neglected in the literature. The behaviour of this element in the rhizosphere of the wetland plant Phragmites australis was investigated in the laboratory in the presence and absence of Mn and Fe root plaques. Electron microscopy and chemical extraction techniques were utilized to determine the physico-chemical properties of the plaques and any association of Al. Both Mn and Fe plaques occurred as amorphous coatings on root surfaces with uneven distributions. Al was not adsorbed onto the surface of either plaque type but formed a separate phosphate deposit closely resembling the Fe and Mn plaques. Phosphorus was also found to be adsorbed to the surface of the Fe plaques (but not the Mn plaques). Both mechanisms were found to immobilize P at the root surface but this did not significantly reduce the concentration of P in aerial plant tissues that was sufficient to ensure adequate growth.     

芦苇收割对宫苍仁蚧密度及其五种寄生蜂共寄生关系的影响

【目的】本文旨在揭示芦苇Phragmites australis(Cav.)Trin.ex Steudel收割对宫苍仁蚧Nipponaclerda biwakoensis Kuwana密度及其5种寄生蜂寄生率和共寄生关系的影响及作用机制。【方法】在上海九段沙湿地上沙的芦苇未收割区和收割区分别设置16个和20个样方,于2011年7月和9月进行重复采样,对未收割区和收割区的蚧虫密度、寄生蜂寄生率、共寄生关系和雌性比率分别进行比较分析。【结果】芦苇收割能够显著降低蚧虫密度(P<0.001);从7月到9月,寄生蜂总寄生率呈增高趋势,但7月芦苇未收割区和收割区间寄生蜂总寄生率差异不显著(P>0.05),而9月芦苇收割区寄生蜂总寄生率则显著高于未收割区(P<0.001);而寄生蜂总寄生率与蚧虫密度相关性并不显著。不同寄生蜂对芦苇收割的响应不同,且存在时间差异性。7月,Aprotocetus sp.的寄生率最高,且在收割区的寄生率显著高于未收割区(P<0.05),而其他寄生蜂寄生率均较低。9月,Aprotocetus sp.的寄生率呈下降趋势,而其余寄生蜂寄生率则呈升高趋势;而且除Encyrtidae sp.外,其他寄生蜂寄生率在未收割区和收割区间存在显著差异(P<0.001)。此外,芦苇收割还显著增加Boucekiella depressa与Astymachus japonicus的共寄生率(P<0.001),并显著减少B.depressa与Aprotocetus sp.的共寄生率(P<0.001)。除Aprotocetus sp.(P<0.05)外,芦苇收割对寄生蜂的雌性比率无显著影响。【结论】不同寄生蜂对芦苇收割的响应,不仅依赖于蚧虫密度,而且还与寄生蜂的扩散能力和竞争能力等生物学特性有关。因此,芦苇收割能通过多种途径影响寄生天敌和宫苍仁蚧的高营养级互作关系,需引起足够的重视。     

敦煌阳关盐沼湿地芦苇种群小尺度空间分布格局

植物种群的空间分布格局是研究连接植物与外界环境关系的重要桥梁,是植物种群稳定性和生活史策略的表现形式。本研究以敦煌阳关盐沼湿地克隆植物芦苇(Phragmites australis)为对象,设置湿生区、轻度盐化区、重度盐化区和荒漠区采样梯度,应用Ripley K(d)函数分析法研究了芦苇种群的小尺度空间分布格局特征及生态适应对策。结果表明:(1)随着从湿生到荒漠区环境梯度的变化,芦苇种群的盖度、密度、高度、地上生物量及种群领地面积都呈现出显著下降的趋势,空斑面积呈现出显著增加的趋势,而种群领地密度则呈现出先增加后下降的趋势;(2)从湿生到荒漠生境,芦苇种群的小尺度空间拓展策略主要表现为由聚集分布为主、非聚集分布(随机分布或均匀分布)为辅,转变为随机分布为主、非随机分布(聚集分布或均匀分布)为辅的特征。研究结果明晰了干旱区内陆河湿地中芦苇种群的空间分布格局特点及其影响因素,为进一步理解克隆植物的生态适应机制提供了案例研究,为科学保护和管理干旱区内陆河湿地生态系统提供了理论依据。     

用芦苇恢复受损河岸生态系统的工程化方法

我国中小河流的护岸工程只考虑工程的耐久性多采用混凝土护岸。忽略了河流的生态功能,破坏了河流的各种生态过程,导致河流污染严重,生态作用越来越小。本研究提出一种用芦苇恢复受损河岸的工程化方法,以解决恢复受损河岸时成本高,破坏了芦苇原生地的生态环境和芦苇不便于运输的问题。其优点在于：在保证能够达到防止河岸崩塌及侵蚀的同时,在河岸工程设计中纳入生态学原理．创造出动植物及微生物能够生存的多孔隙河岸工程生态结构;可以减少对芦苇原生地的破坏。并且能够快速、大量繁殖芦苇幼苗。快速恢复受损河岸的芦苇群落及其生态环境;此方法在减少劳力、时间和成本的基础上,能够更容易恢复浅水带和河岸缓冲带芦苇群落,构建出一个芦苇繁茂的水域。