三江平原毛果苔草湿地光辐射能的利用与分配

毛果苔草湿地的物理过程观测设在中国科学院三江平原沼泽湿地生态实验站内,用美国CID公司出品的光合仪对典型湿地中几种优势植物的光合能力进行测定;在80℃干燥的植物样品(含各种不同的构件),粉碎后,分别称量约1g左右,用美国公司Parr型氧弹式热量计测定;研究发现毛果苔草湿地建群种中毛果苔草的净光合速率最大,为47．41μmol／m／s。以太阳总辐射能和生长季内光合有效辐射为基础计算出各器官的能量利用效率计,极大值是细根,分别为1．3945％和3．1879％,极小值是穗,分别为0．0020％和0．0046％,毛果苔草种群的能量利用率为2．54％。湿地不同植物群落地下部分的能量含量分布中毛果苔草群落的地下部分能量含量的平均值最大。这说明毛果苔草种群具有较高的能量转化效率,并将大部分能量储存在地下部分。在不同层次的能量含量分配中,随着土壤深度的增加,地下部分的能量含量趋于递减。     

鄱阳湖苔草湿地非淹水期CO2释放特征

2009年9月至2010年4月非淹水期,在鄱阳湖南矶湿地国家级自然保护区,选择以灰化苔草为建群种的洲滩湿地,设置土壤-植物系统(TC)、剪除植物地上部分(TJ)2个试验处理(分别代表生态系统和土壤呼吸),利用密闭箱-气相色谱法测定了非淹水期鄱阳湖苔草湿地CO,释放通量.结果表明:苔草湿地生态系统呼吸与土壤呼吸均具有明显的季节变化模式,释放速率变化范围分别为89.57～1243.99和75.30～960.94 mg CO2·m-2·h-1,土壤呼吸占生态系统呼吸的比例为64%(39%～84%);土壤温度是苔草湿地CO2通量的主要控制因子,可以解释呼吸速率80%以上的变异;生态系统呼吸与土壤呼吸的温度敏感性指数(Q10)分别为3.31和2.75,且冬季的Q10值明显高于春秋季节;土壤水分与CO2释放速率之间未达到显著相关;非淹水期,鄱阳湖苔草湿地是大气CO2的汇,其强度为1717.72 g C·m-2.     

鄱阳湖湿地灰化苔草生长季氮磷含量与储量的变化

湿地植物在营养元素生物地球化学循环过程中起着重要作用,研究植物氮磷元素的吸收、分配和积累特征对于正确理解氮磷循环关键过程及其生态作用具有重要意义。基于野外实地观测和室内实验分析,研究了鄱阳湖淡水湿地灰化苔草春草生长季内不同部位生物量、氮磷含量及氮磷储量的动态变化。结果表明:在生长季内,灰化苔草各部位生物量随时间推移而增加,地上部分生物量在各生长期均高于地下部分,地下部分生物量积累速率相对稳定,而地上部分和总体平均积累速率表现为生长前期高于生长后期;各部位氮磷含量经历了先减少再增加的变化过程,其中地上部分氮元素在灰化苔草生长的中后期显著高于地下部分,而磷元素在中前期两者差异更为显著;生物量与氮磷储量均呈显著正相关,是灰化苔草氮磷储量动态变化的主导因子,氮磷元素主要储存在灰化苔草的地上部分;研究期间灰化苔草平均氮磷比介于3.32—3.83之间,按营养限制理论进行判断,氮元素可能是灰化苔草生长的限制性营养因子。     

羊草草地植被—土壤系统氮循环研究

研究表明,0－30cm土层7月氮（N）总储量为479．2g.m^-2,其中主要为有机N,占总N量的98．5％,土壤中的无机N年度变化很大,在2．55－11．3g.m^-2之间,7月无机N储量为7．3g.m^-2,与其它类型草地不同。该类型草地土壤铵态N与硝态N含量有些季节相差不大,有些季节硝态N的含量超过铵态N的含量,铵态N的峰值出现的时间早于硝态N。植物根系吸收利用的无机N约为3.48g.m^-2.a^-1,植物根系向地上每年输送的N量为2．97g.m^-2.a^-1,地上活体向地下转移的N量为1.54g.m^-2.a^-1,植物地上部分每年转为立估凋落物的N量为1.43g.m^-2.a^-1,由立枯凋落物转为土壤有机N的量大于1.08g.m^-2.a^-1,植物根系每年转为土壤有机N的量为1.51g.m^-2.a^-1。     

三江平原草甸湿地土壤呼吸和枯落物分解的CO2释放

利用静态箱-碱液吸收法研究了三江平原草甸湿地土壤呼吸和枯落物分解的CO2释放速率,讨论了影响CO2释放的环境因素,估算了枯落物分解的CO2释放对于总释放的贡献.结果表明,生长季,小叶章沼泽化草甸和小叶章湿草甸各部分CO2释放均具有明显的时间变化特征,温度和水分是重要制约因素.两类草甸湿地的平均土壤呼吸速率分别为4.33g·m-2·d-1和6.15g·m-2·d-1,枯落物分解的CO2平均释放速率分别为1.76g·m-2·d-1和3.10g·m-2·d-1,枯落物分解的CO2释放占总释放量的31%和35%,说明在碳素由地上植物碳库转移到地下土壤碳库的过程中,湿地枯落物是一个不可忽略的碳损失源.     

高寒草原不同植物群落地上-地下生物量碳分布格局

高寒草原具有独特的自然生境和生物资源,对高寒草原开展系统研究对于减缓气候变化与草原恢复具有重要实践意义。以往研究主要针对高寒草原生物量碳开展整体评估,缺乏对不同群落类型间的定量比较。本文分析了高寒草原10种主要典型植物群落地上-地下生物量碳分布格局以及对总生物量碳的贡献差异。结果表明:高寒草原面积为167.33×10^6hm^2,总生物量碳为1.53 Pg(1 Pg=1015g),其中地上生物量碳0.19 Pg,地下生物量碳1.34 Pg;紫花针茅、青藏苔草和紫花针茅-小蒿草群落面积大,生物量碳密度高,为高寒草原贡献了69.3%的生物量碳。高寒草原平均生物量碳密度为690.80 g C·m^-2,其中紫花针茅群落(196.14 g C·m^-2)和蔷薇群落(177.93 g C·m^-2)具有最高的地上生物量碳密度(AGC);蔷薇(1491.18 g C·m^-2)和紫花针茅-小蒿草群落(1306.51 g C·m^-2)则具有最高的地下生物量碳密度(BGC),且显著高于其他群落类型(P<0.05)。不同群落的BGC在土壤中的垂直分布格局存在较大差异,驼绒藜、盐爪爪、金露梅、紫花针茅、青藏苔草、紫花针茅-小蒿草、蔷薇、固沙草、砂生槐等群落的BGC主要集中在表层土壤(0~10 cm),分布曲线呈指数函数,而华扁穗草群落的BGC则集中在40~60 cm土壤层,分布曲线呈二次函数关系。对草原植物群落的地上-地下生物量碳开展评估,可以提高生物量碳的估算精度,为草原生态管理提供更有力的数据支持。     

三江平原土地利用方式改变对湿地汞含量的影响

通过测定三江平原小叶章湿地、水稻田、玉米地土壤以及小叶章、乌拉苔草、毛果苔草、杨树叶及苔藓中的汞含量,探讨了湿地土壤和植物汞来源及分布特征,研究了土地利用方式变化对土壤汞含量的影响.结果表明,三江平原土壤汞含量0.006～0.208mg·kg-1,平均为0.053 mg·kg-1,高于黑龙江省土壤汞背景值含量.由表层至底层,小叶章湿地土壤中汞含量变化不大,水稻田及玉米地中汞含量变化较大.植物中汞含量表现为苔藓＞乌拉苔草＞小叶章＞毛果苔草>杨＞树叶,其中苔藓中汞含量高达0.132 mg·kg-1.相关分析表明,土壤中汞含量与可溶性有机碳含量呈显著正相关(r=0.269,P＜0.05).干湿沉降及植物对大气中汞的吸收可能是本地区土壤中汞的主要来源.湿地开垦为农田后,土壤中汞含量降低了45.6%,而旱田改为水田后,土壤中汞含量则增加了18.3%.     

三江平原小叶樟、毛果苔草枯落物中氮素变化分析

以三江平原沼泽湿地主要优势植物小叶樟(Deyeuxiaangustifolia)和毛果苔草(Carexlasiocarpa)枯落物为例,探讨了N素在枯落物中的季节变化、含量特征以及对维持生态系统物质平衡的作用．结果表明,枯落物N含量随气温升高和地上生物量增大而减少;枯落物失重率随时间延长而增大;小叶樟年累积失重率为32．2％,毛果苔草为27．7％;小叶樟群落N素年累积输入量为1478mg     

植物物种丰富度对水培微宇宙中硝态氮去除的影响

在沙基质的人工湿地中植物多样性能够提高污水去除效果,但无基质水生系统中植物多样性对除氮效应的影响还未知.本研究在45个水培微宇宙(53 cm×37.5 cm×18.5cm)中配置了4个物种丰富度梯度(1、2、3和4),并定期供给硝氮为唯一氮形态的模拟污水,氮载荷率为548.5 gN· m-2 ·a-1.结果表明:物种丰富度对出水中氮去除有显著效应,4个种系统出水总无机氮浓度(54.3 mg·L-1)明显低于单种系统(129.0 mg·L-1);物种丰富度显著提高群落生物量,4个种微宇宙系统群落总生物量为1621.6 g·m-2,高于单种群落的1032.7 g·m-2.水培微宇宙的氮平均移除速率为466.8 g N·m-2·a-1,不低于已有报道的全尺度人工湿地的去除能力,同时,4个种的系统比单种系统约高13％,因而可以通过物种多样性配置提高人工湿地效能.     

养分添加对三江平原沼泽化草甸植物群落组成和地上生物量的影响

三江平原是人类农业开垦活动最为强烈的区域之一,农业施肥已经显著增加了该地区自然沼泽湿地氮和磷的输入量,这将会深刻影响到湿地生态系统的结构和功能。通过3年的氮和磷添加试验,研究了养分富集对三江平原沼泽化草甸植物群落物种组成、多样性和地上生物量的影响。结果表明:与对照相比,氮添加(N,6 g N·m~(-2)·a~(-1))显著增加了禾本科植物的优势度,降低莎草科植物的优势度,导致物种多样性下降,但提高了植物群落地上生物量;而磷添加(P,1.2 g P·m~(-2)·a~(-1))降低了禾本科植物的优势度,增加了莎草科植物的优势度,但对植物群落物种多样性和地上生物量均没有造成显著的影响;氮、磷同时添加(N+P)虽然对植物多样性和地上生物量的影响没有产生显著的交互作用,但增强了小叶章在群落中的优势地位,降低了植物群落的物种多样性,提高了植物地上生物量。本研究表明,在三江平原沼泽化草甸中,养分富集将显著改变植物群落组成和地上净初级生产力,而且氮素和磷素富集影响并不一致。     

内蒙古高原湖滨湿地优势植物功能性状特征及其适应性

受人类活动和气候变化的影响,湖泊湖滨带退化速度显著加快。植物功能性状的方法可以量化植物特征,预测植物对外界环境干扰的反应,有助于理解退化湖滨带湿地植物应对环境变化所表现出的适应机制,对湖泊湖滨湿地生态系统植被的恢复与重建具有重要意义。在内蒙古高原典型湖泊湖滨湿地选取芦苇（Phragmites australis）、赖草（Leymus secalinus）、毛茛（Ranunculus japonicus）、鹅绒委陵菜（Potentilla anserina）、碱蓬（Suaeda glauca）、盐角草（Salicornia europaea）和拂子茅（Calamagrostis epigeios）7种优势植物的叶片和根系作为研究对象,对不同湿地植物的11种功能性状变化规律及其与环境因子的关系进行研究。旨在探究环境变化影响下湖滨带湿地植物的物种分布和功能性状的差异,以及湿地植物在不同湖滨带湿地生境下的适应策略。在评估植物功能性状差异基础上,采用环境矩阵连接性状矩阵（RLQ）结合第四角分析（Fourth-Corner）的方法分析环境因子对植物功能性状的影响。结果表明,内蒙古湖滨带湿地中7种优势植物为了适应不同的环境的影响,植物的功能性状均产生不同程度的种间与种内变异,在湖滨带湿地中植物的植株高度、叶片碳含量、叶片氮含量、叶片碳氮比、比根长、根组织密度、根氮含量对环境变化的响应比较敏感,土壤pH与叶片干物质含量呈显著负相关;土壤盐分与植株高度、叶片碳含量和叶碳氮比显著负相关,与叶片氮含量、根组织密度显著正相关;土壤的总氮含量与植株高度显著正相关,与比根长显著负相关;土壤碳氮比与植株高度和叶片碳含量显著负相关,与植物比根长显著正相关;土壤容重与根氮含量显著负相关。研究表明内蒙古高原湖滨带湿地植物的功能性状受环境的作用强烈,植物采取了不同的性状策略来适应环境。     

天津汉沽农田土壤－植物系统中汞的分布、迁移和积累

本文研究了受汞污染的农田土壤—植物系统中汞的分布,迁移和积累的规律。土壤中的汞在离污染源3公里的范围内含量最高;主要集中在0一20厘米的土壤上层,几乎不往下迁移。植物可以从土壤和大气中吸收、积累汞。在汉沽区没有发现由于汞污染所造成的植物受害症状。植物中的汞含量与土壤中的汞含量成正相关。土壤汞含量与水稻茎叶汞含量的相关系数为0.836(N=7),与糙米汞含量的相关系数为0.898(N=7)。植物不同部位的汞含量根>叶>茎>种子。不同作物种子比较,糙米>高粱>小麦。在大气中汞含量高的地段,植物地上部分汞含量高于根。土壤、植物中的汞不断地向大气扩散,而大气中的汞随着降雨、降尘等又不断地沉降到土壤和植物的气生表面,并可被植物吸收。汞向其邻近地区扩散的能力较小。     

若尔盖高原湿地土壤-植物系统有机碳的分布与流动

 湿地碳素变化对全球气候变化的影响一直是国内外湿地研究的热点。国内对沼泽湿地碳循环的研究主要集中在三江平原,其它地区则鲜见报道。若尔盖高原位于全球气候变化最敏感的区域之一——青藏高原的东北部,冷湿的气候条件下沼泽十分发育,泥炭贮量丰富,沼泽面积和泥炭资源贮量均居中国首位。为了评估该区湿地在全球气候变化中的作用,作者以该区分布最为广泛的3种沼泽植物群落——木里苔草（Carex muliensis）群落、乌拉苔草（Carex meyeriana）群落和藏嵩草（Kobresia tibetica）群落以及最为典型的3种湿地土壤——泥炭土、泥炭沼泽土和草甸沼泽土为对象,采用田间腐解试验方法,系统研究了高原湿地植物——土壤系统中有机碳的分布与流动,其目的在于：1)探明该区湿地土壤有机碳的数量与分布状况;2)了解植物碳在向土壤流动过程中的消失与残留情况。结果表明,若尔盖高原湿地土壤的有机碳含量一般较高且随土层加深而降低;在植物由活体—立枯—残落物的不同阶段,植物不同化学组分中碳的消失率各异,其中易分解组分碳的消失率最大（3种群落分别为61.37%、69.59%和66.34%）,木质素碳的消失率（44.53%～52.98%）略大于纤维素碳的消失率（38.23%～43.86%）,3种群落植物碳的总消失率分别为53.8%、60.03%和55.18%;3种群落的植物残落物在土壤中分解一年和两年后的残留碳量分别为30 g·m﹣2和25.5 g·m﹣2,而植物残根的相应数值则分别高达179～223 g·m﹣2和161～208 g·m﹣2,说明若尔盖高原湿地生态系统中植物残根是形成土壤有机碳的主要来源。由于该区湿地的生物量较高,有机碳的流动量也相应较大。     

Alleviation of Mercury Toxicity in Wheat by the Interaction of Mercury-Tolerant Plant Growth-Promoting Rhizobacteria

Heavy metal contamination of agricultural soils has increased along with industrialization. Mercury is a toxic heavy metal and a widespread pollutant in the ecosystem. Mercury-tolerant and plant growth-promoting rhizobacteria (PGPR) HG 1, HG 2, and HG 3 were isolated from the rhizosphere of plants growing in a mercury-contaminated site. These isolates were able to grow in the presence of mercury ranging from 10 to 200 µM in minimal medium and 25 to 500 µM in LB medium. The strains were characterized by morphological, biochemical, and plant growth-promoting traits. In the present study, these PGPR strains were analyzed for their involvement in metal stress tolerance in Triticum aestivum (wheat). Two bacterial strains, namely, Enterobacter ludwigii (HG 2) and Klebsiella pneumoniae (HG 3), showed better growth promotion of T. aestivum seedlings under metal stress. Different growth parameters like, water content and biochemical properties were analyzed in the PGPR-inoculated wheat plants under 75 µM HgCl₂. Shoot length, root length, shoot dry weight, root dry weight and relative water content (RWC) were significantly higher in inoculated plants compared to uninoculated plants under stress condition. Proline content, electrolyte leakage, and malondialdehyde content (shoots and roots) were significantly lower in inoculated plants with respect to uninoculated plants under mercury stress. Therefore, it could be assumed that all these parameters collectively improve plant growth under mercury stress conditions in the presence of PGPR. Hence, these PGPRs can serve as promising candidates for increasing plant growth and also have immense potential for bioremediation of mercury-contaminated soils.     

Does the different photosynthetic pathway of plants affect soil respiration in a subtropical wetland?

Plants with different photosynthetic pathways could produce different amounts and types of root exudates and debris which may affect soil respiration rates. Therefore, wetland vegetation succession between plants with different photosynthetic pathways may ultimately influence the wetland carbon budget. The middle and lower reaches of the Yangtze River has the largest floodplain wetland group in China. Tian'e Zhou wetland reserve (29°48'N, 112°33′E) is located in Shishou city, Hubei province and covers about 77.5 square kilometers. Hemathria altissima (C4) was found gradually being replaced by Carex argyi (C3) for several years in this place. An in situ experiment was conducted in Tian'e Zhou wetland to determine the change of soil respiration as the succession proceeds. Soil respiration, substrate‐induced respiration, and bacterial respiration of the C4 species was greater than those of the C3 species, but below‐ground biomass and fungal respiration of the C4 species was less than that of the C3 species. There were no significant differences in above‐ground biomass between the two species. Due to the higher photosynthesis capability, higher soil respiration and lower total plant biomass, we inferred that the C4 species, H. altissima, may transport more photosynthate below‐ground as a substrate for respiration. The photosynthetic pathway of plants might therefore play an important role in regulating soil respiration. As C. argyi replaces H. altissima, the larger plant biomass and lower soil respiration would indicate that the wetland in this area could fix more carbon in the soil than before.     

芦竹修复镉汞污染湿地的研究

以湿土盆栽方法研究了芦竹在Cd和Hg污染模拟湿地中的富集能力及其在植株中的分布.结果表明,芦竹在101mg·kg^-1Hg污染环境中生长8个月后,对Hg的富集量是根系>茎>叶片,植物地上部分对Hg富集量为200±20mg·kg^-1DW;而在115mg·kg^-1Cd污染环境中生长8个月后,其对Cd的富集量是叶片>根系>茎,芦竹叶片对Cd的富集量在160±26mg·kg^-1DW.重金属在芦竹各器官内的含量随种植时间的延长而增加,8个月生长期富集量比4个月生长期富集量高30%～50%.芦竹生物富集系数(Bio concentrationfactorBCF)随土壤中重金属含量增加而减小.在污染土壤中,芦竹叶、茎对Hg的BCF为1.9和2.1、对Cd为1.5和0.3;在未受污染的空白对照湿土中(含Hg6.8mg·kg^-1,Cd8.5mg·kg^-1),芦竹叶、茎对Hg的BCF为6.8和12.2,对Cd为7.0和2.7,表明芦竹具有生物量大、根系发达、适应性强等特点,对Cd、Hg有较大富集量和较好的耐受性.     

Mercury toxicity in plants

Mercury poisoning has become a problem of current interest as a result of environmental pollution on a global scale. Natural emissions of mercury form two-thirds of the input; manmade releases form about one-third. Considerable amounts of mercury may be added to agricultural land with sludge, fertilizers, lime, and manures. The most important sources of contaminating agricultural soil have been the use of organic mercurials as a seed-coat dressing to prevent fungal diseases in seeds. In general, the effect of treatment on germination is favorable when recommended dosages are used. Injury to the seed increases in direct proportion to increasing rates of application. The availability of soil mercury to plants is low, and there is a tendency for mercury to accumulate in roots, indicating that the roots serve as a barrier to mercury uptake. Mercury concentration in aboveground parts of plants appears to depend largely on foliar uptake of Hg⁰ volatilized from the soil. Uptake of mercury has been found to be plant specific in bryophytes, lichens, wetland plants, woody plants, and crop plants. Factors affecting plant uptake include soil or sediment organic content, carbon exchange capacity, oxide and carbonate content, redox potential, formulation used, and total metal content. In general, mercury uptake in plants could be related to pollution level. With lower levels of mercury pollution, the amounts in crops are below the permissible levels. Aquatic plants have shown to be bioaccumulators of mercury. Mercury concentrations in the plants (stems and leaves) are always greater when the metal is introduced in organic form. In freshwater aquatic vascular plants, differences in uptake rate depend on the species of plant, seasonal growthrate changes, and the metal ion being absorbed. Some of the mercury emitted from the source into the atmosphere is absorbed by plant leaves and migrates to humus through fallen leaves. Mercury-vapor uptake by leaves of the C₃ speciesoats, barley, and wheat is five times greater than that by leaves of the C₄ species corn, sorghum, and crabgrass. Such differential uptake by C₃ and C₄ species is largely attributable to internal resistance to mercury-vapor binding. Airborne mercury thus seems to contribute significantly to the mercury content of crops and thereby to its intake by humans as food. Accumulation, toxicity response, and mercury distribution differ between plants exposed through shoots or through roots, even when internal mercury concentrations in the treated plants are similar. Throughfall and litterfall play a significant role in the cycling and deposition of mercury. The possible causal mechanisms of mercury toxicity are changes in the permeability of the cell membrane, reactions of sulphydryl (-SH) groups with cations, affinity for reacting with phosphate groups and active groups of ADP or ATP, and replacement of essential ions, mainly major cations. In general, inorganic forms are thought to be more available to plants than are organic ones. Plants can be exposed to mercurials either by direct administration as antifungal agents, mainly to crop plants through seed treatment or foliar spray, or by accident. The end points screened are seed germination, seedling growth, relative growth of roots and shoots, and, in some case, studies of leaf-area index, internode development, and other anatomical characters. Accidental exposures occur through soil, water, and air pollution. The level of toxicity is usually tested under laboratory conditions using a wide range of concentrations and different periods of exposure. Additional parameters include biochemical assays and genetical studies. The absorption of organic and inorganic mercury from soil by plants is low, and there is a barrier to mercury translocation from plant roots to tops. Thus, large increases in mercury levels in soil produce only modest increases in mercury levels in plants by direct uptake from soil. Injuries to cereal seeds caused by organic mercurials has been characterized by abnormal germination and hypertrophy of the roots and coleoptile. Mercury affects both light and dark reactions of photosynthesis. Substitution of the central atom of chlorophyll, magnesium, by mercury in vivo prevents photosynthetic light harvesting in the affected chlorophyll molecules, resulting in a breakdown of photosynthesis. The reaction varies with light intensity. A concentration and time-dependent protective effect of GSH seems to be mediated by the restricted uptake of the metal involving cytoplasmic protein synthesis. Plant cells contain aquaporins, proteins that facilitate the transport of water, in the vacuolar membrane (tonoplast) and the plasma membrane. Many aquaporins are mercury sensitive, and in AQP1 a mercury-sensitive cysteine residue (Cys-189) is present adjacent to a conserved Asn-Pro-Ala motif. At low concentrations mercury has a toxic effect on the degrading capabilities of microorganisms. Sensitivity to the metal can be enhanced by a reduction in pH, and tolerance of mercury by microorganisms has been found to be in the order: total population > nitrogen fixers > nitrifiers. Numerous experiments have been carried out to study the genetic effects of mercury compounds in experimental test systems using a variety of genetic endpoints. The most noticeable and consistent effect is the induction of c-mitosis through disturbance of the spindle activity, resulting in the formation of polyploid and aneuploid cells and c-tumors. Organomercurials have been reported to be 200 times more potent than inorganic mercury. Exposure to inorganic mercury reduces mitotic index in the root-tip cells and increases the frequency of chromosomal aberrations in degrees directly proportional to the concentrations used and to the duration of exposure. The period of recovery after removal of mercury is inversely related to the concentration and duration of exposure. Bacterial plasmids encode resistance systems for toxic metal ions, including Hg²⁺, functioning by energy-dependent efflux of toxic ions through ATPases and chemiosmotic cationproton antiporters. The inducible mercury resistance (mer) operon encodes both a mercuric ion uptake and detoxification enzymes. In gram-negative bacteria a periplasmic protein,MerP, an inner-membrane transport protein,MerT, and a cytoplasmic enzyme, mercuric reductase, theMerA protein, are responsible for the transport of mercuric ions into cells and their reduction to elemental mercury, Hg(II). InThiobacillus ferrooxidans, an acidophilic chemoautotrophic bacterium sensitive to mercury ions, a group of mercury-resistant strains, which volatilize mercury, has been isolated. The entire coding sequence of the mercury-ion resistance gene has been located in a 2.3 kb fragment of chromosomal DNA (encoding 56,000 and 16,000 molecular-weight proteins) from strain E-l 5 ofEscherichia coli. Higher plants andSchizosaccharomyces pombe respond to heavy-metal stress of mercury by synthesizing phytochelatins (PCs) that act as chelators. The strength of Hg(II) binding to glutathione and phytochelatins follows the order: γGlu-Cys-Gly(γGlu-Cys)₂Gly(γGlu-Cys)₃Gly(γGlu-Cys)₄Gly. Suspension cultures of haploid tobacco,Nicotiana tabacum, cells were subjected to ethyl methane sulfonate to raise mercury-tolerant plantlets. HgCl₂-tolerant variants were selected from nitrosoguanidine (NTG)-treated suspension cell cultures of cow pea,Vigna unguiculata, initiated from hypocotyl callus and incubated with 18 ⧎g/ml HgCl₂. Experiments have been carried out to develop mercury-tolerant plants ofHordeum vulgare through previous exposure to low doses of mercury and subsequent planting of the next generation in mercury-contaminated soil. Phytoremediation involves the use of plants to extract, detoxify, and/or sequester environmental pollutants from soil and water. Transgenic plants cleave mercury ions from methylmercury complexes, reduce mercury ions to the metallic form, take up metallic mercury through their roots, and evolve less toxic elemental mercury. Genetically engineered plants contain modified forms of bacterial genes that break down methyl mercury and reduce mercury ions. The first gene successfully inserted into plants wasmerA, which codes for a mercuric ion reductase enzyme, reducing ionic mercury to the less toxic elemental form.MerB codes for an organomercurial lyase protein that cleaves mercury ions from highly toxic methyl mercury compounds. Plants with themerB gene have been shown to detoxify methyl mercury in soil and water. Both genes have been successfully expressed inArabidopsis thaliana, Brassica (mustard),Nicotiana tabacum (tobacco), andLiriodendron tulipifera (tulip poplar). Plants currently being transformed include cattails, wild rice, andSpartina, another wetland plant. The problem of mercury contamination can be reduced appreciably by combining the standard methods of phytoremediation—removal of mercury from polluted areas through scavenger plants—with raising such plants both by routine mutagenesis and by genetic engineering. The different transgenics raised utilizing the two genesmerA andmerB are very hopeful prospects.     

华南地区8种常见园林地被植物抗旱性比较研究

以华南地区8种常见园林地被植物为研究对象,在温室内设置盆栽控水试验,分组测定各参试植物的永久萎蔫率,叶片失水率、相对含水量、相对电导率、可溶性糖、脯氨酸以及丙二醛含量等生理生化指标,并用隶属函数法对其抗旱性进行综合评价。结果表明:(1)植物的永久萎蔫率和叶片失水率以鹅掌藤、白蝴蝶相对较低,其植株表现出较强的抗旱性。(2)随着持续干旱时间的延长,8种地被植物的叶片相对含水量呈不同程度下降趋势;叶片相对电导率、MDA含量均有不同程度升高;叶片可溶性糖和脯氨酸含量的变化趋势不一。(3)3种木本植物的抗旱性强弱依次为鹅掌藤>红花龙船花>红背桂,5种草本植物依次为水鬼蕉>蚌兰>白蝴蝶>葱兰>大叶红草。研究表明,植物的永久萎蔫率、叶片失水率、相对含水量、相对电导率、丙二醛含量与其实际抗旱性密切相关,可作为评价园林地被植物抗旱性的有效指标。     

Thiosulphate-induced mercury accumulation by plants: metal uptake and transformation of mercury fractionation in soil - results from a field study

Aims

The thiosulphate induced accumulation of mercury by the three plants Brassica juncea var.LDZY, Brassica juncea var.ASKYC and Brassica napus var. ZYYC and the transformation of mercury fractionation in the rhizosphere of each plant was investigated in the field.

Methods

Experimental farmland was divided into control and thiosulphate plots. Each plot was divided into three subplots with each planted with one of the plants. After harvesting, the mercury concentration in plants, mercury fractionation in rhizosphere soil before and after phytoextraction, and the vertical distribution of bioavailable mercury in bulk soil profiles was analyzed.

Results

The cultivar B. juncea var.LDZY accumulated a higher amount of mercury in shoots than the other two plants. Thiosulphate treatment promoted an increase in the concentration of metal in plants and a transformation of Fe/Mn oxide-bound and organic-bound mercury (potential bioavailable fractions) into soluble and exchangeable and specifically-sorbed fractions in the rhizosphere. The observed increase in bioavailable rhizosphere mercury concentration was restricted to the root zone; mercury did not move down the soil profile as a function of thiosulphate application to soil.

Conclusions

Thiosulphate-induced phytoextraction has the potential to manage environmental risk of mercury in soil by decreasing the concentration of mercury associated with potential bioavailable fraction that can be accumulated by crop plants.     

4种不同生活型湿地植物对富营养化水体的净化效果

选择4种湿地植物菖蒲、香蒲、浮萍和金鱼藻,研究单一及组合湿地植物对高浓度污水(污水处理厂进水)、低浓度污水(污水处理厂出水)中营养物质的去除效果.结果表明: 水体中总氮(TN)、总磷(TP)、化学需氧量(COD)浓度呈现试验前期快速下降,后期缓慢下降的趋势,表明湿地植物能有效净化污水中的TN、TP、COD,但不同湿地植物及湿地植物组合的净化效果存在差异.多种湿地植物组合比单种湿地植物对TN的净化作用强,其中香蒲＋浮萍＋金鱼藻对TN的净化效果最佳;高浓度污水中,单种挺水植物对TP的净化效果较好,低浓度污水中,则是多种湿地植物组合对TP的去除率较高;高浓度污水中,湿地植物对COD的去除率为85.1%～96.0%,其中菖蒲、香蒲去除效果最佳,低浓度污水中,湿地植物对COD去除率为76.9%～94.8%,以菖蒲＋浮萍＋金鱼藻去除效果最好.总体看来,湿地植物对高浓度污水中TN、TP、COD的净化效果好于低浓度污水,两种水体的pH都得到改善.