黄山松年轮硫及重金属元素含量动态特征

对黄山松80年的年轮序列中S及重金属元素Mn、Fe、Zn、Cu和Pb含量分析结果表明,年轮中S浓度可划分为3个等级:58.5%年轮段,S浓度<2mg·kg^-1;24.4%年轮段,S浓度3.65～6.0mg·kg^-1;17.1%年轮段,S浓度>11mg·kg^-1.年轮序列中S的积累有较大幅度的波动,可分为波动型(1917～1960年)、相对稳定型(1961～1980年)和持续增长型(1981年以后)3种类型;在1935～1938年、1959～1960年以及最近10年的年轮中,S含量均>11mg·kg^-1,表明该时段大气中S的浓度较高.统计分析表明,近18年来,旅游人数的增加与年轮中S含量呈显著相关性,一些景点较集中的燃料消耗可能造成局部大气污染,从而影响到树木.年轮序列中Pb的积累浓度低于土壤背景值;Mn、Fe、Zn和Cu在年轮中的积累均有明显的波动性;统计上无显著的相关性,表明这4种元素在年轮中的积累是独立的;Zn和Cu在年轮序列中积累的波动与树龄无关;Mn在年轮序列中的浓度随树龄增加而降低,在最新的几个年轮段又略有增加,Fe则相反.     

南京城市土壤重金属含量及其影响因素

研究了南京城市土壤重金属含量、来源及其与土壤性质的关系。结果表明,南京城市土壤中,Fe、Ni、Co、V污染不明显,但受到了不同程度的Mn、Cr、Cu、Zn、Pb污染,其中：Pb污染非常严重;重金属在土壤剖面分布没有规律性;Fe、Ni、Co、V元素主要来源于原土壤物质,Cu、Zn、Pb、Cr元素主要来源于人为输入,Mn可能在不同的土壤中来源不同;Fe、Cr、Ni、Co、V元素含量之间均呈极显著正相关,Cu、Zn、Pb、Cr元素含量之间均呈极显著正相关。Fe、Co、V、Ni含量与粘粒含量、CEC呈极显著正相关;Cu、Zn、Pb含量与粘粒含量呈极显著负相关;Cu、Zn、Pb、Cr含量与有机碳呈极显著正相关,Pb含量与pH呈极显著正相关。     

天山土壤微量(类)重金属的来源解析及潜在生态危害评估

从天山山地3个区段(巴里坤-伊吾、乌鲁木齐-阿克苏、昭苏-特克斯)采集土壤样品,测定了其中(类)重金属Pb、Ni、Cd、Co、Hg、Cu、Mn、Zn、Cr和As的含量.运用经典统计学与多元统计方法分析了这些(类)重金属的来源;同时采用污染指数法与潜在生态风险指数法,并结合天山及新疆土壤背景值、国家土壤质量标准开展了区域土壤微量(类)重金属生态风险的评价.结果表明： 所测10种(类)重金属的平均含量均高于天山或新疆土壤背景值.从变异系数来看,均为中等变异.总体上看,天山山地土壤中10种(类)重金属的含量均较低;主成分分析显示,10种元素可以辨识出 2 个主成分,主成分1(PC1,包括Cd、Pb、Hg、Mn和Zn)为人为源因子,主成分2(PC2,包括Cu、Ni、Cr、Co和As)为自然源因子.Mn 和As在PC1和PC2上均有较大载荷,主要受人为源和自然地质背景的共同控制;污染评价表明, 重金属Hg、Cd在天山中部的乌鲁木齐-阿克苏区段、As在天山西部的昭苏-特克斯区段的单因子污染指数(P_i)属于警戒等级,其他均属于安全等级和清洁水平.从综合污染(P_z)指数来看,天山中部乌鲁木齐 阿克苏区段土壤中10种(类)重金属元素的综合污染程度均属于轻度污染,其他两个区段均属于清洁水平;生态风险评估表明,重金属Hg、Cd在天山中部乌鲁木齐 阿克苏区段,As在天山西部昭苏 特克斯区段的潜在生态风险系数(E_i^r)和生态危害指数(RI)相对较高.     

包头南海子湿地三种鹭鸟羽毛与环境中重金属含量的关系

于2016年7至10月采用电感耦合等离子体发射光谱法(ICP-OES),测定了内蒙古包头南海子湿地繁殖期过后的白琵鹭(Platalea leucorodia)、苍鹭(Ardea cinerea)和夜鹭(Nycticorax nycticorax)3种鹭鸟初级飞羽及环境因子(水、土壤、食物)中As、Cd、Cr、Cu、Ni、Pb、Zn、Fe、Mn、Hg 10种重金属的含量,采用单因素方差分析方法比较了不同鹭鸟种类羽毛重金属含量差异,并通过生物富集系数及Pearson相关性检验分析了羽毛与环境因子间重金属含量之间的关系,以揭示包头南海子湿地环境中重金属污染现状及生物富集特征。结果表明:(1)被检测的10种重金属中,As、Cd、Cr、Cu、Pb、Zn、Hg 7种元素在湿地环境中均已超标,尤其土壤中Fe、Zn、Cu已达到重度污染的程度。(2)不同重金属元素在鹭鸟羽毛中的含量存在差异,其中Fe元素在白琵鹭羽毛中的含量水平最高(388.77 mg/kg),Cd元素在夜鹭羽毛中的含量最低(0.12 mg/kg)。在鹭鸟羽毛中重金属含量由高至低的顺序分别为,白琵鹭Fe、Zn、Mn、Cu、Hg、Cr、Ni、Pb、As、Cd,苍鹭Zn、Fe、Cu、Cr、Ni、As、Mn、Hg、Pb、Cd,夜鹭Zn、Fe、Mn、Cu、Ni、Pb、Hg、Cr、As、Cd。除Pb和Cd元素外,其他8种元素含量在3种鹭鸟羽毛中的含量种间差异显著。(3)相关分析表明,鹭鸟羽毛中的重金属含量与环境因子中的重金属含量显著相关且呈现富集特征,为此可作为监测当地环境污染的指示性材料。     

福州酸雨区次生林中台湾相思与银合欢叶片的12种元素含量

在酸雨区,研究叶片元素浓度变化规律对于理解树种选择与重建亚热带森林具有重要意义。在中亚热带丘陵次生林的酸雨区内,测定两个优势树种——台湾相思树(Acacia confusa)、银合欢(Leucaena glauca)的叶片元素(N、P、S、K、Ca、Na、Mg、Fe、Mn、Cu、Zn和Al)含量,并探讨其可能遭受酸雨的影响。结果表明,两树种叶片营养元素含量均表现为N > K > Ca > S > P > Mg > Na,重金属元素表现为Fe > Al > Cu。两树种叶片的P、Ca、Mg、Na、Mn和Cu含量差异极显著,Zn含量差异显著。受频繁酸雨影响,台湾相思(3.42 g/kg)和银合欢(2.70 g/kg)的S含量明显高于中国陆生被子植物叶片的平均值((1.66±3.06) g/kg),Na含量低于S含量,也明显低于中国陆生被子植物叶片Na含量的平均值((2.48±5.45)g/kg),表明研究区域植物叶片的Na元素的特异性,酸雨加速土壤酸化导致土壤Na含量低可能是一个原因。由N/P、Ca/Al摩尔比值的大小可得出,台湾相思为P制约型树种,虽然其Al含量并未超出正常范围值,但其Ca/Al摩尔比值小于12.5,表明存在Al的危害风险;而银合欢属N制约型树种,并未受到Al的危害,更适应研究区生长环境。若仅从叶片元素含量分析,该区域的台湾相思和银合欢受到Fe危害风险,且存在更大的Cu和Zn危害风险,银合欢的Zn、Cu元素累积量大于台湾相思,所以可以认为银合欢的抗性强于台湾相思,可能更适应于酸雨区域生长。     

有色稻米Fe、Zn、Cu和Mn含量及与种皮颜色相关分析

用AAS方法测定了弥勒县相同生态条件下种植的27份有色稻和34份普通稻糙米4种矿质元素含量,并对有色米和普通米Fe、Zn、Cu和Mn含量进行了比较研究。结果表明,有色稻米4种矿质元素含量明显高于无色稻米,其差异均达显著水平,其含量高低依次为Zn>Fe>Cu>Mn;对黑、褐、红、黄、绿5种不同种皮颜色的稻米4种矿质元素含量进行比较研究,发现稻米Fe含量(mg/kg)依次为黑>绿>褐>红>黄,Zn含量(mg/kg)依次为绿>红>黑>褐>黄,Cu含量(mg/kg)依次为黑>褐>红>黄>绿,Mn含量(mg/kg)依次为褐>黑>红>黄>绿;并且Fe和Mn含量在不同颜色稻米间差异均达显著水平,与有色米种皮颜色密切相关,而Zn和Cu差异不显著,与有色米种皮颜色关系不大。黑米和褐米富Fe、Zn、Cu和Mn,绿米富Fe和Zn,红米富Zn和Cu,黄米4种矿质元素含量较低,Fe、Cu和Mn均低于普通稻米。     

珠江口桂山岛表层沉积物中重金属的分布特征及潜在生态危害评价

于2011年8月采集了珠江口桂山岛海域12个站点的表层沉积物, 对沉积物中重金属的含量进行了测定。结果表明, 桂山岛沉积物中重金属含量与国内外港湾相比属于中等水平, Pb、Cr、Ni、Cu、Zn、Mn平均含量分别为40.06、31.29、14.17、30.67、100.18、599.76 mg/kg。富集系数法和 Hakanson潜在生态风险指数法评价表明:桂山岛沉积物各重金属元素的富集顺序为Cu﹥Pb﹥Zn﹥Mn﹥Cr﹥Ni, 其中Cu、Pb、Zn和Mn富集系数大于1;该海域重金属潜在生态风险总体上处于低水平, 从空间上看, S11危害最为严重。进一步通过主成分分析研究沉积物中重金属的来源, 发现前2个主成分贡献率分别为44.38%、42.61%, 表明重金属主要有2个来源:工业和生活污水排放、岩石的自然风化与侵蚀过程。     

沈阳市住宅区小区与街道灰尘重金属污染评价

城市住宅区是人类活动的重要场所,与居民的日常生活紧密相关。为了解沈阳市住宅区小区与街道灰尘中重金属污染的空间分布,采集了不同住宅区小区与街道的灰尘样品,分析了灰尘中重金属的含量,并使用富集因子和地累积指数评估了其污染程度。结果表明,沈阳市灰尘中重金属Cr、Cd、Cu、Pb和Zn的平均含量均超过辽宁省表层土壤元素背景值。单因素方差分析表明,街道灰尘中重金属Cu、Fe、Mn和Zn的空间分布具有显著性差异,而小区灰尘中重金属Cd、Cr、Fe、Mn和Pb在空间上具有显著性差异。重金属Cd、Zn和Pb的平均污染水平较高,其中小区内Cd和Zn的污染程度高于街道。沈阳市不同方位住宅区灰尘中重金属的污染水平介于轻度污染至中度污染之间。     

刺楸年轮中重金属含量动态变化及富集特性

为探索刺楸对受污染土壤重金属的富集和修复效应, 以南京栖霞山的乡土树种刺楸及其根际周边土壤为研究对象, 截取其根基部年轮盘及根际土壤样本, 采用ICP-AES法测定年轮及土壤样本中重金属(Cu、Cd、Cr、Mn、Ni、Pb、Zn)元素含量。结果表明: 栖霞山样地中的土壤受Mn、Pb和Zn污染最为严重, 存在Cu、Cd、Mn、Pb、Zn元素的高度复合污染, Cd、Cr、Cu、Ni、Zn在土壤和年轮中存在相关性, Mn和Pb则没有表现出明显的相关性; 刺楸修复受Cd、Mn、Pb、Zn污染的土壤效果并不显著, 更适用于Cr、Cu、Ni污染的土壤修复; 鉴于Cu元素含量变化特征, 刺楸也可以作为反映当地污染历史的记录载体; 刺楸年轮中的重金属元素之间存在交互作用, 其中Cd与Zn元素含量高度相关(r=0.984, p<0.01), 在刺楸年轮吸收重金属元素的过程中, Cu与Cd、Cr、Mn、Zn元素具有协同作用, Mn元素对其他元素有一定的拮抗作用。     

防城港临时性海洋倾倒区沉积物重金属污染现状及其生态风险评价

对防城港临时性海洋倾倒区表层沉积物重金属的含量和分布进行了对比分析,并采用污染指数法和Hakanson潜在生态风险指数法对其重金属的污染特征及潜在生态风险程度进行了评价。结果表明,倾倒区沉积物Hg、Pb、As和Zn的含量显著性升高;总体污染程度为中等污染,各重金属元素的污染程度由高到低排序依次为As(3.59)>Hg(2.19)>Pb(1.42)>Zn(1.20)>Cu(1.05)>Cd(0.91),其中As是主要污染因子;该海域表层沉积物重金属总体潜在生态风险程度为中等,各重金属元素的潜在生态风险程度由高到低排序依次为Hg(87.74)>As(35.89)>Cd(27.27)>Pb(7.08)>Cu(5.23)>Zn(1.20),其中Hg为主要潜在生态风险因子。     

Adsorption of Cu and Zn onto Mn/Fe Oxides and Organic Materials in the Extractable Fractions of River Surficial Sediments

The roles of the extractable components (Mn oxides, Fe oxides, and organic materials) of surficial sediments in controlling metals adsorption were investigated. Cu and Zn adsorptions were conducted before and after the surficial sediments extracted with hydroxylamine hydrochloride, an oxalate solution, and H ₂ O ₂ , respectively. The extraction removed target components with extraction efficiencies from 63 to 98%. Nonlinear regression analyses of Cu and Zn adsorptions based on the assumption of additive Langmuir adsorption isotherm were employed to estimate the relative contributions of sediment components to Cu and Zn adsorptions. The results indicate that the greatest contribution to total Cu and Zn adsorption to the surficial sediments on a molar basis was from Mn oxides in the extractable fractions. Both Cu and Zn adsorption capacities of Mn oxides exceeded those of Fe oxides by approximately one order of magnitude, fewer roles were attributed to the adsorption of organic material (OM), and the estimated contribution of the residual fraction to total Cu and Zn adsorption was insignificant. These information implied that the roles of metal oxides (Fe and Mn oxides) in the extractable form of the surficial sediments, especially Mn oxides, was the most important component in controlling heavy metal transportation in aquatic environments.     

Comparison of the toxicity of heavy metals to cabbage growth

Summary Cabbage plants were grown for 55 days with a nutrient solution containing 1 and 10 ppm of V, Cr(III), Cr(VI), Mn, Fe, Co, Ni, Cu, Zn, Cd, Hg(I), orHg(II). A comparison of the plant growth and chemical analysis revealed that Cr(VI), Cu, Cd, and Hg(II) in the solution are most toxic to the plant growth (hence detrimental to the cabbage-head formation) and Mn, Fe, and Zn are less toxic than other heavy metals, and that Mn, Zn, Co, Ni, and Cd and translocated into all the plant organs while V, Cr(III), Cr(VI), Fe, Cu, Hg(I), and Hg(II) are accumulated in the roots.     

运用油松年轮提示承德市硫及重金属污染的历史

本文利用油松年轮研究了承德市自1800年以来大气污染的历史过程,结果表明：避暑山庄油松年轮内S含量自本世纪初开始升高,比19世纪初增加1—2倍,至70—80年代达3—5倍,而在最近8—10年则达到10倍以上。 其中碧峰门古松木质部年轮内S含量由40—50μg·g-1达到目前的572.9μg·g-1,从而指示出承德市大气SO2浓度由城市化初期的<0.1 mg·m-3增加到目前的30mg·m-3,这一历史过程主要与城市化过程尤其是近50年来工业化的出现并加剧有密切的关系。随着1927—1945年大庙铁矿的开采,年轮内Fe明显增高。Mn在整个历史时期表现为增加趋势,由1840—1850年的4.1μg·g-1增加到1980—1990年的10.4μg·g-1。Pb在1980年前的含量增加不明显,但在最近10年内形成的木质部中,Pb含量明显增加,超过1920—1930年的560%。Cu、Zn、Ni含量的变化不表现线性增加,除个别点的某些时期变化较大外,基本上很平缓。19世纪初油松年轮内S及重金属含量最低,可视为油松内元素自然背景值,与该值比较,1980—1990年这10年内年轮S含量增加了10倍,Fe,2.4倍;Pb,1.8倍;Mn,1.5倍;Ni,1.0倍;Zn,0.8倍。 日益加剧的大气污染尤其是SO2的污染,造成承德市大气质量严重下降,同时危及古松的生存,造成古松大量死亡,必须引起高度重视。     

Incidence of heavy metals in the mangrove flora and sediments in Kerala, India

The mangroves of Kerala on the south-west coast of India are fast disappearing due to land reclamation and other anthropogenic disturbances. There are very few ecosystem level studies made in these much threatened biotopes in Kerala. The present study involves the measurement of heavy metals in the mangrove flora and sediments of three mangrove habitats along the Kerala coast. Sampling was carried out for a period of one year at bi-monthly intervals, with concentrations of Fe, Mn, Cu,Zn,Pb and Co analysed using atomic absorption spectrophotometry. An appreciable variation was observed in metal concentrations indifferent mangrove species. Cu, Zn and Pb were found to be in higher concentrations in Avicennia officinalis whereas higher levels of Fe, Mn and Co were observed in the species Barringtonia racemosa. The analysis of heavy metals indicated a high level of metal pollutants such as Fe, Cu, Zn and Pb in the mangrove habitats of Quilon and Veli compared to the relatively uncontaminated areas of Kumarakom. This revised version was published online in August 2006 with corrections to the Cover Date.     

Bioaccumulation and translocation of heavy metals by nine native plant species grown at a sewage sludge dump site

In the present study, nine native plant species were collected to determine their potential to clean up nine heavy metals from soil of a sewage sludge dump site. Almost all nine plant species grown at sewage sludge dump site showed multifold higher concentrations of heavy metals as compared to plants grown at the reference site. All the investigated species were characterized by a bioaccumulation factor (BF) > 1.0 for some heavy metals. BF was generally higher for Cd, followed by Pb, Co, Cr, Cu, Ni, Mn, Zn, and Fe. The translocation factor (TF) varied among plant species, and among heavy metals. For most studied heavy metals, TFs were <1.0. The present study proved that the concentrations of all heavy metals (except Cd, Co, and Pb) in most studied species were positively correlated with those in soil. Such correlations indicate that these species reflect the cumulative effects of environmental pollution from soil, and thereby suggesting their potential use in the biomonitoring of most heavy metals examined. In conclusion, all tissues of nine plant species could act as bioindicators, biomonitors, and remediates of most examined heavy metals. Moreover, Bassia indica, Solanum nigrum, and Pluchea dioscoridis are considered hyperaccumulators of Fe; Amaranthus viridis and Bassia indica are considered hyperaccumulators of Pb; and Portulaca oleracea is considered hyperaccumulator of Mn.     

Binding of manganese in human and rat plasma

Albumin, transferrin and 'transmanganin' have all been proposed as the major Mn-binding ligand in plasma. The present investigations were initiated in order to resolve these discrepancies. Compared to other metals tested (109 Cd2+, 65Zn2+, 59Fe3+), 54Mn2+ bound poorly to purified albumin. The addition of exogenous albumin to plasma did not result in an increased 54Mn radioactivity associated with this protein. Also, incubation of 65Zn-albumin in the presence of excess Mn2+ (1 mM) did not result in the displacement of Zn from albumin or Mn binding. In contrast to these results, 54Mn was bound to purified transferrin, not as readily as Fe3+, but better than Zn2+ or Cd2+. Saturation of transferrin with Fe3+ (1.6 micrograms Fe/mg) prevented the binding of 54Mn indicating that Mn probably binds to Fe-binding sites on the protein. Polyacrylamide gel electrophoresis further demonstrated the association of 54Mn with transferrin rather than with albumin in both human and rat plasma. The amount of 54Mn radioactivity recovered with transferrin increased as incubation time was increased, probably due to oxidation of Mn2+ to Mn3+. Mn binding to transferrin reached a maximum within 5 and 12 h of incubation. About 50% of 54Mn migrated with transferrin, whereas only 5% was associated with albumin. A significant portion (20-55%) of the 54Mn radioactivity migrated with electrophoretically slow plasma components whose identity was not determined. Possibilities include alpha 2-macroglobulin, heavy gamma-globulins and/or heavy lipoproteins.     

Blocking of electron donation by Mn(II) to Y(Z*) following incubation of Mn-depleted photosystem II membranes with Fe(II) in the light

The donation of electrons by Mn(II) and Fe(II) to Y(Z*) through the high-affinity (HA(Z)) site in Mn-depleted photosystem II (PSII) membranes has been studied by flash-probe fluorescence yield measurements. Mn(II) and Fe(II) donate electrons to Y(Z*) with about the same efficiency, saturating this reaction at the same concentration (ca. 5 microM). However, following a short incubation of the membranes with 5 microM Fe(II), but not with Mn(II) in room light, added Mn(II) or Fe(II) can no longer be photooxidized by Y(Z)(*). This blocking effect is caused by specifically bound, photooxidized Fe [> or =Fe(III)] and is accompanied by a delay in the fluorescence yield decay kinetics attributed to the slowing down of the charge recombination rate between Q(a-) and Y(Z*). Exogenously added Fe(III), on the other hand, does not donate electrons to Y(Z*), does not block the donation of electrons by added Mn(II) and Fe(II), and does not change the kinetics of the decay of the fluorescence yield. These results demonstrate that the light-dependent oxidation of Fe(II) by Y(Z*) creates an Fe species that binds at the HA(Z) site and causes the blocking effect. The pH dependence of Mn(II) electron donation to Y(Z*) via the HA(Z) site and of the Fe-blocking effect is different. These results, together with sequence homologies between the C-terminal ends of the D1 and D2 polypeptides of the PSII reaction center and several diiron-oxo enzymes, suggest the involvement of two or perhaps more (to an upper limit of four to five) bound iron cations per reaction center of PSII in the blocking effect. Similarities in the interaction of Fe(II) and Mn(II) with the HA(Z) Mn site of PSII during the initial steps of the photoactivation process are discussed. The Fe-blocking effect was also used to investigate the relationship between the HA(Z) Mn site and the HA sites on PSII for diphenylcarbazide (DPC) and NH2OH oxidation. Blocking of the HA(Z) site with specifically bound Fe leads to the total inhibition of electron donation to Y(Z*) by DPC. Since DPC and Mn(II) donation to PSII is noncompetitive [Preston, C., and Seibert, M. (1991) Biochemistry 30, 9615-9624], the Fe bound to the HA(Z) site can also block the DPC donation site. On the other hand, electron donation by NH2OH to PSII still occurs in Fe-blocked membranes. Since hydroxylamine does not reduce the Fe [> or =Fe(III)] specifically bound to the HA(Z) site, NH2OH must donate to Y(Z*) through its own site or directly to P680+.     

Field-based investigation on phytoremediation potentials of Lemna minor and Azolla filiculoides in tropical,semiarid regions: Case of Ethiopia

This study investigated the concurrent accumulation of eight heavy metals by two floating aquatic macrophytes (Lemna minor and Azolla filiculoides) cultivated in ambient media and blended wastewaters in the semiarid regions of Ethiopia. Both species accumulated heavy metals in varying degrees with a significant concentration gradient within the immediate water media. Highest bioconcentration factor (BCF) was determined for Mn and Fe in both plants. Results revealed that L. minor was high phytoaccumulator for Fe, Mn, Zn, and Co but moderate for Cd, Cu, Ni, and Cr. On the other hand, A. filiculoides was a high accumulator for Fe, Mn, Zn, and Cu, but its potency was moderate for Co, Cr, and Ni, but lower for Cd. Both species exhibited significant difference in accumulating Co, Zn, and Mn (p < 0.05). In general, the BCFs for both plants were comparable within the same treatment. In this study, stronger associations between the heavy metal concentrations in the plant tissues and in the grown water media were observed for A. filiculoides.     

Biochemical characterization of the structural Zn2+ site in the Bacillus subtilis peroxide sensor PerR

In Bacillus subtilis most peroxide-inducible oxidative stress genes are regulated by a metal-dependent repressor, PerR. PerR is a dimeric, Zn2+-containing metalloprotein with a regulatory metal-binding site that binds Fe2+ (PerR:Zn,Fe) or Mn2+ (PerR: Zn,Mn). Reaction of PerR:Zn,Fe with low levels of hydrogen peroxide (H2O2) leads to oxidation of two His residues thereby leading to derepression. When bound to Mn2+, the resulting PerR:Zn,Mn is much less sensitive to oxidative inactivation. Here we demonstrate that the structural Zn2+ is coordinated in a highly stable, intrasubunit Cys4:Zn2+ site. Oxidation of this Cys4:Zn2+ site by H2O2 leads to the formation of intrasubunit disulfide bonds. The rate of oxidation is too slow to account for induction of the peroxide stress response by micromolar levels of H2O2 but could contribute to induction under severe oxidative stress conditions. In vivo studies demonstrated that inactivation of PerR:Zn,Mn required 10 mM H2O2, a level at least 1000 times greater than that needed for inactivation of PerR:Zn,Fe. Surprisingly even under these severe oxidation conditions there was little if any detectable oxidation of cysteine residues in vivo: derepression was correlated with oxidation of the regulatory site. Because oxidation at this site required bound Fe2+ in vitro, we suggest that treatment of cells with 10 mM H2O2 released sufficient Fe2+ into the cytosol to effect a transition of PerR from the PerR:Zn,Mn form to the peroxide-sensitive PerR: Zn,Fe form. This model is supported by metal ion affinity measurements demonstrating that PerR bound Fe2+ with higher affinity than Mn2+.