Low micromolar zinc accelerates

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Anomalously Metal-Rich Fluids Form Hydrothermal Ore Deposit

Anomalously Metal-Rich Fluids Form Hydrothermal Ore Deposit

33.The price for multiwall carbon nanotubes has droppedfrom a few hundred U.S.dollars per gram in the1990s to about100U.S.dollars per kilogram.See,for example, /details.asp?ArticleID=1108. 34.We gratefully acknowledge financial support for this workfrom the Air Force Office of Scientific Research(grantFA9550-06-1-0384).K.G.thanks L.Qu and J.Zhu for helpwith some initial work.Supporting Online Material/cgi/content/full/323/5915/760/DC1Materials and MethodsFigs.S1to S6Table S1References4November2008;accepted16December200810.1126/science.1168049Anomalously Metal-Rich Fluids Form Hydrothermal Ore DepositsJamie J.Wilkinson,1,2*†Barry Stoffell,1‡Clara C.Wilkinson,1,2†Teresa E.Jeffries,2Martin S.Appold3Hydrothermal ore deposits form when metals,often as sulfides,precipitate in abundance from aqueous solutions in Earth’s crust.Much of our knowledge of the fluids involved comes from studies of fluid inclusions trapped in silicates or carbonates that are believed to represent aliquots of the same solutions that precipitated the ores.We used laser ablation inductively coupled plasma mass spectrometry to test this paradigm by analysis of fluid inclusions in sphalerite from two contrasting zinc-lead ore systems.Metal contents in these inclusions are up to two orders of magnitude greater than those in quartz-hosted inclusions and are much higher than previously thought,suggesting that ore formation is linked to influx of anomalously metal-rich fluids into systems dominated by barren fluids for much of their life.H ydrothermal ore deposits,formed fromthe flow of hot solutions through porousor fractured rocks,are the principal source of metals in Earth’s crust(1).Such large accumulations of metal require concentration of elements hundreds or thousands of times above natural abundance,implying high-mass fluxes through small volumes of rock coupled with ef-ficient precipitation.A fundamental control on the formation of hydrothermal deposits is the ability of the fluid to carry metals in solution(2). Yet,paradoxically,for most deposit types formed at low-to-intermediate temperatures,both direct analysis of fluid inclusions and theoretical cal-culation indicate that the concentrations of dis-solved metals are likely to be low,on the order of tens of parts per million(3).Also,samples of modern crustal fluids,such as those from oil fields or mid-ocean ridges,typically contain only a few parts per million of Cu,Zn,and Pb(4,5), although there are exceptions,such as the Salton Sea geothermal brines in California(6)and oil-field waters from central Mississippi(4).A con-sequence is that the other parameters that govern total metal flux in ore formation(average flow velocity and system lifetime)tend toward their likely geological limits in both numerical simu-lations and empirical models based on geologicaland geochronological constraints(7,8).As aresult,it has been suggested that higher-than-normal concentrations of metal in fluids may berequired to form large ore bodies(9).For several decades,a key source of infor-mation on the physical and chemical conditionsof hydrothermal ore formation has been fluidinclusions trapped during mineral growth(10).Inmost deposits,metalliferous ore minerals(com-monly opaque sulfides)occur together with un-economic transparent phases(gangue).Becausefluid inclusions in the opaque phases are noteasily studied by traditional transmitted light mi-croscopy and microanalytical methods,the na-ture of ore-forming fluids and the conditions ofore-mineral precipitation have often been in-ferred from the properties of inclusions trapped inthe associated gangue minerals.However,it isoften difficult to provide unequivocal evidencefor coprecipitation based on textural observationsor isotopic measurements(11);consequently,un-certainty remains concerning the temporal and,therefore,genetic relationship between gangue-hosted inclusions and the ore-forming process.Several studies that used infrared light microsco-py to observe inclusions in opaque minerals suchas wolframite and cassiterite have shown that theproperties of these fluid inclusions may,indeed,be different(12).We analyzed fluid inclusions in sphalerite(ZnS)from two zinc-lead ore systems with theuse of laser ablation inductively coupled plasmamass spectrometry(LA-ICPMS).Primary inclu-sions in sphalerite must represent the ore-formingfluid because they are trapped during growth ofthe ore mineral itself.Unlike bulk analyticalstudies that are limited to a few major elementsand that may sample multiple populations of in-clusions(13),LA-ICPMS allows determinationof trace elements(including ore metals)in single,texturally constrained inclusions.We selected samples from two well-studiedhydrothermal ore systems.The Northern Arkan-sas district of the Ozark Plateau,North America,is an example of low-temperature MississippiV alley–Type(MVT)zinc-lead mineralization,thought to have formed by continent-scale ba-sinal brine migration(14).The Midlands Basinorefield in Ireland contains several large zinc-lead(-barium)ore deposits formed from moderatetemperature fluids generated by deep crustalcirculation of seawater-derived brines duringcontinental rifting(15,16).Both systems areeconomically noteworthy but provide a contrastin terms of sources of metals,sulfur,and hydro-logical regime.Lead is of particular interest be-cause it needs to be concentrated above averagecrustal abundance more than any other commonore-forming element(~4000times)to form apotentially economic accumulation.Samples from Northern Arkansas were col-lected from exposures in the Monte Cristo andPhiladelphia Mines of the Rush subdistrict andfrom the Lucky Dog Mine of the TomahawkCreek subdistrict.They comprise fine-to coarse-grained crystalline quartz and medium-tocoarse-grained pale yellow–to–brown sphalerite.Regionally,precipitation of sphalerite typicallyoverlapped with that of jasperoid and finelycrystalline quartz,and more coarsely crystallinequartz formed later(17).Samples from Irelandwere collected from historic mine exposures anddrill core from the Silvermines deposit,as well asfrom quarry outcrop of quartz-sulfide veins near-by.The deposit samples are composed of mas-sive sulfide dominated by coarse-grained brownsphalerite that replaces early disseminated gran-ular and framboidal pyrite.The vein sample iscomposed of quartz and ankerite,as well asminor sphalerite and galena,and was selected asa representative example of a regionally devel-oped set of feeder veins developed underneaththe ore deposits(18,19).Salinity data derived from freezing experi-ments(20)show that the Northern Arkansasmineralization formed from brines,typical ofMVT deposits(Fig.1).Assuming fluids weretrapped at hydrostatic pressure at depths of<2km,the inferred depth of ore formation(14),wecalculated an isochoric correction of<+10°C torecorded homogenization temperature(T h)val-ues to give true trapping temperatures.Thus,T hcan be regarded as a reasonable approximation offluid temperature during mineral growth.Inclu-sions from the Irish samples display lower salin-1Department of Earth Science and Engineering,Imperial College London,South Kensington Campus,Exhibition Road,London SW72AZ,UK.2Department of Mineralogy, Natural History Museum,Cromwell Road,London SW7 5BD,UK.3Department of Geological Sciences,University of Missouri–Columbia,101Geological Sciences Building, Columbia,MO65211,USA.*To whom correspondence should be addressed.E-mail: j.wilkinson@†Present address:Australian Research Council Centre of Excellence in Ore Deposits(CODES),Private Bag126, University of Tasmania,Hobart,Tasmania7001,Australia.‡Present address:Rio Tinto Mining and Exploration Limited,2Eastbourne Terrace,London W26LG,UK.ity and higher T h values than the MVT fluids (Fig.1),typical for the Irish orefield (11).For the Irish ores,which formed at shallow depth (16,19),any correction to homogenization tem-peratures will again be small so that T h values can be regarded as a good proxy for fluid trapping temperature.Laser ablation analyses were carried out with the use of a New Wave UP213AI,213-nm aperture-imaged laser ablation system (20–22)on primary fluid inclusions interpreted to haveformed during initial mineral growth based on con-ventional petrographic criteria (10).Some second-ary inclusions,formed during later fracturing and annealing,were analyzed for comparison (Fig.2).Lead and other elements of interest in hydrothermal systems such as Ba and Mn are clearly present in the fluid phase,as indicated by their good corre-lation with Cl in inclusion signals (Fig.3).Full data are reported in tables S1and S2(20).Zn concentrations in primary quartz-hosted inclusions from Northern Arkansas are low,rang-ing from 0.12to 12.3parts per million (ppm).In Irish quartz,except for one primary inclusion (14ppm),Zn was below the limitof detection (mean =37.6ppm)because of the small inclu-sion size.Such low Zn concentrations are con-sistent with previously reported bulk analyses of 3.4to 6.0ppm (16).Unfortunately,we were not able to measure the Zn concentration of inclu-sions trapped in sphalerite because of the over-whelming host mineral contribution to the laser ablation signal.A similar problem also occurred for Cu (Fig.3).However,Pb can be used as an indicator of the ore metal content of these inclusions,as it does not substitute appreciably into sphalerite,and its presence there can be cor-rected for (20).In Northern Arkansas,Pb concentrations dis-play a marked bimodal distribution,ranging from 0.2to 3.5ppm in quartz and primarily from 10to 400ppm in sphalerite (Fig.4).This excludes five sphalerite-hosted inclusions that fall in the lower population,interpreted to represent unrecognized secondary inclusions trapping fluid related to the later quartz.The quartz-hosted inclusion data are consistent with a 266-nm LA-ICPMS study that found that fluid inclusions in gangue minerals from the Southeast Missouri MVT district con-tained Pb,Zn,and Cu concentrations below in-strumental detection limits of ~10ppm (23).The Monte Cristo and Philadelphia sphalerites have similar mean Pb concentrations (80ppm)that are lower than the Lucky Dog sphalerites (119ppm).In Ireland,we also observed a distinction between the Pb content of primary inclusions in quartz (3.6to 26ppm)and sphalerite (22to 890ppm)(Fig.4).The quartz-hosted inclusion data are consistent with bulk fluid inclusion analyses for Irish feeder veins that gave Pb concentrations of 11.4to 19.8ppm (16).The more saline pri-mary inclusions in sphalerite 75-85-104have a higher mean Pb concentration (430ppm)than theFig.1.(A )Quartz wafer from Northern Arkansas showing primary growth zones (GZ).(B )Magnification of inset shown in (A)illustrating complex distribution of fluid inclusions,together with some secondary trails (S)and selected primary inclusions (P)within growth clusters.(C )Sphalerite wafer from Ireland showing growth zones defined by fine fluid inclusions and color banding,together with euhedral primary inclusions.(D )Plot of fluid temperature and salinity data derived from microthermometry.Salinity was estimated from the freezing point depression of ice,modeled in the NaCl-H 2O system (20).For Northern Arkansas [data previously shown in (17)],quartz from Monte Cristo and sphalerite (Sp)from Monte Cristo and Philadelphia contain apparently identical primary inclusions.Slightly lower salinity primary inclusions are found in sphalerite from the Lucky Dog mine (20km to the southwest),indicating geographic variability in brine composition.In the Irish Orefield,UG-1sphalerite contains primary and secondary inclusions of a less saline brine [12to 15weight percent (wt %)NaCl equivalent]and a trail of inclusions of more saline fluids (16to 18wt %NaCl equivalent).This cuts a growth zone boundary (Fig.2),indicating that these fluids are younger than this surface and its associated primary inclusions,but the exact timing with respect to other inclusions in the sample is uncertain (U).Fluids in the more saline population are trapped as primary inclusions in sphalerite 75-85-104.The data display a bimodal salinity distribution that mirrors the distribution observed in regional-scale fluid inclusion studies (see histogram at right),suggesting that these modes reflect multiple pulses of districtwide flow affecting a rock volume estimated at >130,000km 3.Analogous brine pulses have been inferred in the recent history of the Salton Trough geothermal field (6).The evidence noted above,together with crosscutting relations observed in other samples,suggests that the higher salinity fluid pulse is later and is associated with the majority of the sphalerite in the district.The inclusions analyzed by LA-ICPMS in sphalerite sample 75-85-104are not plotted because homogenization experiments could not be carried out due to problems with leakage.Fig.2.Transmitted light digital photomontage of double-polished fluid inclusion wafer (~100m m thick)of Irish sphalerite UG-1.Shown are individ-ual fluid inclusions analyzed (numbered)and average determined Pb concentrations for each population of primary,secondary,or uncertain inclusions (same as those referred to in Fig.1).inclusions in sphalerite UG-1(120ppm);sec-ondary inclusions in both samples display similar,lower concentrations.Two secondary inclusions in quartz contained higher metal concentrations (27to 128ppm)(Fig.4)than the primary in-clusions,indicating overprinting by later,more metalliferous fluids such as those trapped in sphalerite.Pb and Zn concentrations are commonly correlated in hydrothermal solutions as a result of their similar geochemical behavior andpotential buffering by their respective sulfides (4,24).This is illustrated by their empirical covariation in modern basin brines (4,6,24–26)and in the quartz-hosted inclusions in this study (above ~1ppm)where both metals were de-termined (Fig.4).This relation allows us to model the likely range of Zn concentrations to be expected in the sphalerite-hosted inclusions at the time of trapping:up to 5000ppm in Irish sphal-erite and 3000ppm in Northern Arkansas.The latter estimate is ~60%of the value predictedtheoretically from thermodynamic data using measured Pb concentrations,assuming galena and sphalerite saturation and making reasonable assumptions about pH and oxygen fugacity (17).Although these are only order-of-magnitude estimates,it is clear that the fluids precipitating sphalerite were markedly enriched in Pb and Zn compared with those precipitating quartz in the two systems.It could be argued that the fluid inclusions in quartz represent spent ore fluids,trapped after sulfide precipitation had already taken place.This is thought to be unlikely in the Irish deposits because the quartz was sampled from largely barren vein systems that formed beneath the ore deposits,in hydrothermal upflow zones (16),and the fluids show no signs of having substantially cooled or mixed (Fig.1),as is known to occur during mineralization (16,19).In the Tri-State MVT district,we found sphalerite-and quartz-hosted brine inclusions to have distinct halogen signatures,indicating that the fluids had separate origins (17).The fertile ore fluids appear to have originated during strong evaporation of seawater at Earth ’s surface,before later burial and expul-sion.This observation contrasts with the barren fluids that evolved from less strongly evaporated seawater (17).The metalliferous fluids are there-fore linked to the paleoclimate and the specific characteristics of the sedimentary aquifer within which they were trapped.The development of low-pH surface brines in the U.S.mid-continent in the Permian via sulfide oxidation (27)is an intriguing possible origin for such metal-prone fluids.Not only will unusually low pH enhance metal solubilization,but the reservoir rocks will be depleted in reduced sulfur that would other-wise limit metal take-up.The nonideal behavior of Cl at high ionic strengths,coupled with low pH and chloride complexing,has been cited as a control of high Zn and Pb concentrations in the most saline modern oil-field waters (6),but this does not account for the low metal concentrations observed in similar salinity brines in some oil fields or those trapped in gangue minerals in this study (Fig.4).Irrespective of the origin,both numerical models (8)and empirical observation(A ).Example of a time-resolved laser spectrum for a fluid inclusion in (primary inclusion 9,Irish sphal-erite 75-85-104).Initially,gas background was acquired and then the laser was turned on at 24s.Signals for 66Zn and 65Cu increase as sphalerite begins to be ablated.The inclusion was breached at ~52s.The signal was integrated offline over an ~16-s interval.The y axis is scaled from maximum to mini-mum recorded counts per second (cps)for each individual isotope.(B )The good corre-lations between the intensity for 35Cl (only present in the fluid inclusion)and all iso-topes measured (except 65Cu)through the integration interval confirms their predomi-nance in the fluid phase.This analysis returned 160ppm Li,530ppm Mg,7740ppm K,17500ppm Ca,530ppm Mn,2750ppm Sr,1770ppm Ba,and 61ppm Pb.Fig.4.Concentrations of Zn versus Pb in quartz-hosted fluid inclusions and histograms showing measured Pb concentrations in quartz-and sphalerite-hosted inclusions,compared with natural brine data from broadly analogous environments.Predicted Pb-Zn covariation for sphalerite-hosted inclusions indicated by fields,based on the extrapolation of empirical Pb-Zn concentrations,including data from modern oil-field waters (24,25)adjusted to mass/mass units and from the Salton Sea geothermal field (6).Both of these data sets have values that fall in our “high-metal ”fluid fields,suggesting that they are anomalously metalliferous and viable ore-forming fluids.Typical Zn:Pb ratios (by mass)for natural fluids are in the range of 1to 10(dashed lines)and tend toward higher values at elevated concentrations.Five data points from the Northern Arkansas data set with low detected Pb are inferred secondary inclusions.Short bars on symbols indicate that the plotted value is a maximum (limit of detection)value for that element.Qz,quartz;Sp,sphalerite;MC,Monte Cristo;PA,Philadelphia;LD,Lucky Dog.Some of the Northern Arkansas data shown are presented in (17),figures 6and 7.of brine heterogeneity in modern sedimentary basins(6)imply inefficiency of mixing and the potential for preservation of individual,metal-charged brine reservoirs that could be tapped at some later time.In the case of Ireland,the origin of metal-enriched fluids is uncertain,although a deepening convective flow system(15)has the capability to extract higher concentrations of metal later in the life of the system due to increasing temperature and possibly also progressive exhaustion of the buffer capacity for pH(by feldspar-mica)or the activity of H2S(by pyrite-Fe silicate)on the convective flow path.The observation that the texturally later brines have higher metal contents is consistent with this model,although their higher salinity is also likely to have contributed to enhanced metal transport.The high Ba content of the metalliferous fluids(up to6000ppm) indicates that the oxidized sulfur content must have been low,limited by barite saturation. Combined with high base metal concentrations that imply low reduced sulfur concentrations,we conclude that a key property of these fluids was low S S(total sulfur concentration).High metal concentrations may pertain in other types of hydrothermal ore systems,such as epithermal or volcanic-hosted massive sulfide deposits.In these environments,periodic injec-tion of metalliferous magmatic fluids may be responsible for the bulk of metal introduction (28–30)into systems otherwise dominated by barren geothermal waters.A number of large, high-temperature,magmatic-hydrothermal de-posits are also known to have formed from magmatic fluids that contained very high con-centrations of ore metals(31–33).Accepting that hydrothermal ores may form specifically from anomalously metal-rich batches of fluid implies geochemically specialized source regions and anepisodicity and potentially short duration of ore-forming events that may be controlled by changesin hydrology.Although the existence of an ef-ficient trap for these metals remains a fundamentalprerequisite for hydrothermal ore formation,ourinterpretation contrasts with the view that manycrustal fluids are viable ore fluids subject to theright perturbations in physicochemical conditionsto cause efficient deposition(24).References and Notes1.H.L.Barnes,A.W.Rose,Science279,2064(1998).2.D.L.Huston,J.Aust.Geol.Geophys17,15(1998).3.T.M.Seward,H.L.Barnes,in Geochemistry ofHydrothermal Ore Deposits,H.L.Barnes,Ed.(Wiley,NewYork,ed.3,1997),pp.435–486.4.J.S.Hanor,in Carbonate-Hosted Lead-Zinc Deposits,Society of Economic Geologists Spec.Publ.4(Society ofEconomic Geologists,Littleton,CO,1996),pp.483–500.5.K.L.Von Damm,Annu.Rev.Earth Planet.Sci.18,173(1990).6.M.A.McKibben,L.A.Hardie,in Geochemistry ofHydrothermal Ore Deposits,H.L.Barnes,Ed.(Wiley,NewYork,ed.3,1997),pp.877–936.7.G.Garven,M.S.Appold,V.I.Toptygina,T.J.Hazlett,Hydrogeol.J.7,108(1999).8.M.S.Appold,G.Garven,Econ.Geol.95,1605(2000).9.C.J.Hodgson,in Giant Ore Deposits,Society of EconomicGeologists Spec.Publ.2(Society of Economic Geologists,Queens Univ.,Golden,CO,1993),pp.1–2.10.E.Roedder,Fluid Inclusions,Reviews in Mineralogy,vol.12(Mineralogical Society of America,Washington,DC,1984).11.J.J.Wilkinson,Lithos55,229(2001).12.A.R.Campbell,K.S.Panter,Geochim.Cosmochim.Acta54,673(1990).13.J.G.Viets,A.H.Hofstra,P.Emsbo,in Carbonate-HostedLead-Zinc Deposits,Society of Economic Geologists Spec.Publ.4(Society of Economic Geologists,Littleton,CO,1996),pp.465–482.14.D.L.Leach,in Sediment-Hosted Zn-Pb Ores(Springer,Berlin,1994),pp.104–138.15.M.J.Russell,in Geology and Genesis of Mineral Depositsin Ireland(Irish Association for Economic Geology,Dublin,1986),pp.545–554.16.J.J.Wilkinson,C.E.Everett,A.J.Boyce,S.A.Gleeson,D.M.Rye,Geology33,805(2005).17.B.Stoffell,M.S.Appold,J.J.Wilkinson,N.A.McClean,T.E.Jeffries,Econ.Geol.103,1411(2008).18.C.E.Everett,J.J.Wilkinson,D.M.Rye,in Fractures,FluidFlow and Mineralization,Geological Society of LondonSpec.Publ.155(Geological Society of London,London,1999),pp.247–276.19.I.M.Samson,M.J.Russell,Econ.Geol.82,371(1987).20.Materials and methods are available as supportingmaterial on Science Online.21.B.Stoffell,J.J.Wilkinson,T.E.Jeffries,Am.J.Sci.304,533(2004).22.T.E.Jeffries,S.E.Jackson,H.P.Longerich,J.Anal.At.Spectrom.13,935(1998).23.M.S.Appold,T.J.Numelin,T.J.Shepherd,S.R.Chenery,Econ.Geol.99,185(2004).24.B.Yardley,Econ.Geol.100,613(2005).25.A.B.Carpenter,M.L.Trout,E.E.Pickett,Econ.Geol.69,1191(1974).26.Y.K.Kharaka et al.,Appl.Geochem.2,543(1987).27.K.C.Benison,R.H.Goldstein,B.Wopenka,R.C.Burruss,J.D.Pasteris,Nature392,911(1998).28.S.F.Simmons,K.L.Brown,Science314,288(2006).29.C.A.Heinrich,Science314,263(2006).30.T.Ulrich,S.D.Golding,B.S.Kamber,K.Zaw,Ore Geol.Rev.22,61(2003).31.T.Ulrich,D.Günther,C.A.Heinrich,Nature399,676(1999).32.A.C.Harris,V.S.Kamenetsky,N.C.White,E.vanAchterbergh,C.G.Ryan,Science302,2109(2003).33.B.Rusk,M.Reed,J.H.Dilles,L.Klemm,C.A.Heinrich,Chem.Geol.210,173(2004).34.This work was supported by an Imperial College AlbertJulius Bursary to B.S.and National Environment ResearchCouncil grant GR9/03047.We thank B.Coles and R.Garcia-Sanchez for laboratory support and the NaturalHistory Museum–Imperial College London Joint AnalyticalFacility for access to instrumentation.The constructivecomments of three anonymous reviewers are appreciated.Supporting Online Material/cgi/content/full/323/5915/764/DC1Materials and MethodsTables S1and S2References8August2008;accepted4November200810.1126/science.1164436Signature of the End-Cretaceous Mass Extinction in the Modern BiotaAndrew Z.Krug,1David Jablonski,1James W.Valentine2The long-term effects of mass extinctions on spatial and evolutionary dynamics have been poorly studied.Here we show that the evolutionary consequences of the end-Cretaceous [Cretaceous/Paleogene(K/Pg)]mass extinction persist in present-day biogeography.The geologic ages of genera of living marine bivalves show a significant break from a smooth exponential distribution,corresponding to the K/Pg boundary.The break reflects a permanent increase in origination rates,intermediate between the Mesozoic rate and the post-extinction recovery pulse. This global rate shift is most clearly seen today in tropical bioprovinces and weakens toward the poles.Coupled with the modern geographic distributions of taxa originating before and after the K/Pg boundary,this spatial pattern indicates that tropical origination rates after the K/Pg event have left a permanent mark on the taxonomic and biogeographic structure of the modern biota, despite the complex Cenozoic history of marine environments.T he major extinctions of the geologic past, each of which removed>50%of well-preserved genera and perhaps>70%of their species(1,2),irreversibly restructured the taxonomic composition of the global biota.Although the broad macroevolutionary conse-quences of mass extinctions are well known(asin the dinosaurs-mammals changeover),theirlong-term effects on the temporal and spatialdynamics of clades and biotas are rarely inves-tigated.For example,the good fit of modern bio-diversity to local temperatures and to refugiafrom recent glaciations(3,4)might imply that therecovery from the most recent major extinction,at the end of the Cretaceous Period65millionyears ago(Ma)[the Cretaceous/Paleogene(K/Pg)extinction],is largely obscured by subsequentevents.Here,we show the lasting influence of theK/Pg mass extinction on the evolutionary andbiogeographic structure of modern biotas,usingbackward survivorship curves(BSCs,also calledprenascence curves),which plot the proportion oftaxa within a cohort that originated before somereference time(5,6).Assuming that rates aretime-specific and taxonomically homogeneous(5),a BSC defines an exponential probabilityfunction governed only by the origination rate(l)of the cohort(7).The slope of a BSC is insen-1Department of Geophysical Sciences,University of Chicago,5734South Ellis Avenue Chicago,IL60637,USA.2Depart-ment of Integrative Biology and Museum of Paleontology,University of California,Berkeley,Berkeley,CA94720,USA.。

巴克敏斯特富勒烯-1989年外文翻译

巴克敏斯特富勒烯-1989年外文翻译

C60:巴克敏斯特富勒烯在以了解星际间和拱星壳中所形成的长链碳的机制为目的的研究中。

石墨被激光器气化,形成了一簇非常稳定的由60个碳原子组成的原子簇。

在什么样的C60结构可以形成十分稳定的原子簇的问题中,我们认为,应该是一种小型化的十二面体,即一个有60个顶点32个面的多边形,其包括12个五边形和20个六边形。

这个东西就像我们常见的如图一所示的足球一样。

构成c60就代表着,每一个被放在顶点的碳原子的化合价由两个单键和一个双键所满足。

它有着许多的共振结构,而且外表很像是芳香族化合物。

制造和发现这种不同寻常的小颗粒与能把碳原子从石墨表面蒸发到高密度氦气流中的蒸馏器有关。

其实这个蒸馏器就是一个强力的脉冲激光器。

这个蒸发激光器是一个由光量开关控制的能够产生出大约30mJ能量的二次简谐波Nd:YAG(钇铝石榴石激光器)。

这些作为气化结果的碳原子簇,就在超声速的C原子流中不断膨胀(生长)。

然后利用准分子激光使其电离,并利用光谱法测量其质量。

气化室如图二所示。

在实验中,先打开脉冲阀,然后再精准的时间控制之后,点火气化激光器,石墨片就被气化在了氦气流中,在其中冷却和进行部分平衡膨胀。

这些膨胀(生长)完成的颗粒然后再被吹到一个电离区内。

然后这些原子簇由一个仔细同步过的脉冲激光器进行单光子激发电离。

碳的气化早先就在一个与之非常相似的仪器内被研究过。

在那项研究中,由190个碳组成的原子簇曾被发现,而且只发现了超过四十个碳原子且原子个数为偶数的原子簇(富勒烯)被发现。

在ref.6的质量波普显示器上,C60是规格超过40的原子团中数量最多的,但他并非完全是主要部分,我们最近重新测试了这个体系,而且发现在这种聚合条件下,C60的峰值可达到与其相邻的的原子团峰值的40倍以上。

图三显示了一系列原子簇的分布,这些分布图线是在气化条件变动的情况下的ref.3中相似的原子簇分布图线进化而来的,在其中C60是主要的。

图三c中,在气化激光器点火被延误直到绝大多数氦电子脉冲停止后,一个巨多量带有38-120个原子的约为高斯分布的原子团产生了。

偏钒酸铵 作为氧化剂

偏钒酸铵 作为氧化剂

偏钒酸铵作为氧化剂英文回答:Ammonium perchlorate (NH4ClO4), commonly known as AP,is a powerful oxidizer used in various applications, suchas rocket propellants, explosives, and fireworks. As an oxidizer, it provides oxygen for the combustion process by releasing oxygen molecules during decomposition.One of the key properties of ammonium perchlorate isits high oxygen content. It contains a large amount of oxygen in its molecular structure, making it an excellent source of oxygen for combustion reactions. When AP decomposes, it releases oxygen gas, which combines with a fuel to sustain and enhance the combustion process.For example, in solid rocket propellants, ammonium perchlorate is mixed with a fuel, such as powdered aluminum. When the propellant is ignited, AP decomposes and releases oxygen gas, which reacts with the aluminum to form aluminumoxide and additional heat. This exothermic reactionsustains the combustion process and provides the thrust required for propulsion.In addition to its high oxygen content, ammonium perchlorate also has other desirable properties for use as an oxidizer. It has a high stability, meaning it can be stored for extended periods without significant degradation. It also has a high solubility in water, which allows it to be easily incorporated into various formulations.However, it is important to handle ammonium perchlorate with care due to its potential for explosive reactions. When mixed with certain organic compounds or fuels, it can become highly sensitive and prone to detonation. Therefore, strict safety measures and proper handling procedures are essential when working with AP.中文回答:偏钒酸铵(NH4ClO4),通常称为AP,是一种强氧化剂,广泛应用于火箭推进剂、炸药和烟花等领域。

Elesstroless Plating 化学镀完整版资料

Elesstroless Plating 化学镀完整版资料

The application of electroless plating
Aerospace Industry
航天工业为化学镀镍的使用大户之一,比较突 出的应用实例是:美国俄克拉荷马航空后勤中 心,自1979年以来,以及西北航空公司自1983 年以来均采用化学镀镍技术修复飞机发动机零 件。普拉特-惠特尼公司的JT8D喷气发动机虽 已经停产,可是迄今仍有上千台这种发动机在 波音727合麦道DC-9飞机上使用。原因是:一 种高磷、压应力的化学镀镍技术用于修复JT8D 六种型号的喷气发动机的叶轮,确保了这种发 动机的重新使用。 为减轻重量,航空工业大量使用铝合金件,经 化学镀镍表面强化后不仅耐蚀、耐磨,而且可 焊,如冲程发动机的活塞头经化学镀镍后提高 了使用寿命。其他还有钛合金件、铍合金件均 采用低应力和压应力的化学镀镍表面保护等措
当与催化 可以控制 这样氧化还 的正常进
表面接触 金属的还 原沉积过程 行,即溶
时,才发 原速率, 才能持续进 液有足够
生金属沉 从而调节 行,镀层连 的使用寿
积过程。 镀覆f Electroless Plating
High corrosion resistance、wear resistance、
The application of electroless plating
Chemical Industry
化学镀广泛地应用于大型反应容器的内壁 保护。当初非常引人注目的应用实例是: 1995年美国通用运输公司(GATX)采用 化学镀保护槽车内壁,防止苛性碱的腐蚀。 应用化学镀镍最为量大面广的是阀门造业。 因为在苛性碱腐蚀条件下,低磷化学镀镍 层的年腐蚀速率约为2.5µm,优于中磷或 高磷化学镀镍层。 化学镀镍层在强氧化性酸,如浓硫酸、浓 硝酸等介质中不耐蚀。对于上述强酸介质, 或者可能水解生成上述强酸的介质中,不 适于使用化学镀镍层。

微波加热条件下氯化锌催化合成乙酸乙酯

微波加热条件下氯化锌催化合成乙酸乙酯

第39卷第2期河南大学学报(自然科学版)Vol.39 No.2 2009年3月Journal of Henan University(Natural Science)Mar.2009微波加热条件下氯化锌催化合成乙酸乙酯陈蔚萍1,陈迎伟2,王慧琴3,乔聪震1(1.河南大学化学化工学院,河南开封475004; 2.塔里木中原钻井液公司,新疆塔里木841000;3.开封东大化工集团,河南开封475003)摘 要:以冰醋酸和无水乙醇为原料,氯化锌为催化剂,采用微波加热法合成乙酸乙酯.探讨了酸醇比、催化剂用量、微波功率和辐射时间对合成乙酸乙酯产率的影响.得出最佳的反应条件为酸醇摩尔比2∶1、催化剂质量百分数1.5%、辐射时间6min和微波功率400W,合成乙酸乙酯的产率为78.36%.关键词:微波;氯化锌;乙酸乙酯;催化中图分类号:O623.611 文献标志码:A文章编号:1003-4978(2009)02-0145-03Synthesis of Ethyl Acetate C atalyzed by Zinc Chlorideunder the Conditions of Microw ave H eatingC H EN Wei2ping1,CH EN Y ing2wei2,WAN G Hui2qin3,Q IAO Cong2zhen1(1.College of Chemist ry and Chemical Engineering,Henan Universit y,Henan Kai f eng475004,China;2.Zhong y uan D rilling Fl ui d Com pany of Talim u,X inj iang Talim u841000,China;3.East bi g Kai f eng Chemical Group,Henan Kai f eng,475003,China)Abstract:By taking the glacial acetic acid and the absolute ethyl alcohol as raw materials,this paper synthesized ethyl acetate by adopting microwane heating method and used zinc chloride as catalyst.The effects of the ratio of acid and alcohol,the comount use of catalyst,the power of microwave and the time radiation on the production of ethyl acetate were discussed in the paper.The optimized reaction conditions were two to1ratio for the mole ratio of acid and alcohol, 1.5mass percent for the catalyst,six minutes for the radiation and four hundred watt for microwave.Under the above conditions,the production of the ethyl acetate was78.36percent.K ey w ords:microwave;zinc chloride;ethyl acetate;catalysis0 引言乙酸乙酯(et hyl acetate,EA)是一种工业用途十分广泛的化合物.它具有优异的溶解性能,是一种快干性的工业溶剂,被广泛用于涂料、醋酸纤维、乙基纤维素、人造革、油毡着色剂、氯化橡胶、乙烯树脂、乙酸纤维树脂、合成橡胶等生产中,也可用于生产复印机用的液体硝基纤维墨水.在纺织工业中用作清洗剂;在食品工业中是最重要的香料添加剂,可作为调香剂的组分;乙酸乙酯也可作为粘合剂用于印刷油墨、人造珍珠的生产;还可用作油漆的稀释剂以及制造药物、染料的原料.因此,乙酸乙酯的合成方法及其催化剂的研究一直被人们所关注.传统的生产工艺是用冰醋酸和无水乙醇为原料,以浓硫酸作催化剂直接合成,但用浓硫酸作催化剂有以下缺点:硫酸是氧化性酸,对反应设备腐蚀严重,生产成本高[1-2].有人用铌酸作催化剂在微波场中合成乙酸乙酯[3],减轻了腐蚀问题,但催化剂成本还比较高.本课题在微波场[4-6]中用氯化锌作催化剂合成乙酸乙酯.该方法可避免传统方法中的腐蚀性强的缺点,并且用微波加热,加热快速、均匀、效率高,操作方便,可大大地缩短反应时间,具有很好的工业应用价值. 收稿日期:2008210212 基金项目:河南省科技攻关项目(0524270049) 作者简介:陈蔚萍,女,河南南阳人,副教授.研究方向:纳米材料,绿色化工.E2mail:chwp@146 河南大学学报(自然科学版),2009年,第39卷第2期1 实验部分1.1 药剂与仪器冰醋酸(分析纯,天津市化学试剂一厂);无水乙醇(分析纯,天津市化学试剂一厂);氯化锌(分析纯,上海新宝精细化工厂);无水碳酸钠(分析纯,河南焦作市化工三厂);氯化钠(分析纯,天津市化学试剂三厂);无水氯化钙(分析纯),4A型分子筛(无锡市荣得利分子筛厂).电热鼓风干燥箱(上海市实验仪器厂);M P25002电子天平(上海恒平科学仪器厂);NJL0722型实验专用微波炉(南京杰全微波设备有限公司);GC217色谱分析仪(日本岛津).1.2 实验方法准确量取一定量的冰醋酸、无水乙醇和并称取适量的氯化锌后加入50mL事先装有几粒沸石的圆底烧瓶中(反应体系为m酸+m醇=30g),稍加振动,放入微波炉中加热(反应体系装有回流装置).在一定的功率下加热一定时间,加热完毕后冷却至室温,过滤取出沸石.烧杯中的滤液加入适量饱和碳酸钠溶液[7],此时有大量气泡产生.直到没有气泡产生用p H试纸检测为中性时,将混合液转入分液漏斗中静止分层除去下层水溶液,上层有机物用适量饱和氯化钠水溶液洗涤.然后分出酯层,再用适量饱和氯化钙水溶液洗涤,最后再用去离子水洗涤后放出废液,用4A型分子筛除去酯中水分,将处理后的溶液倒入250mL圆底烧瓶中进行蒸馏,收集73~78℃的馏分,称重,用乙酸乙酯作为内标,用气相色谱仪测定各样品溶液中乙酸乙酯的含量,计算乙酸乙酯的产率.1.3 实验原理本实验原理是利用无水乙醇和冰醋酸为原料,以氯化锌作催化剂,用微波作为加热源,其基本反应式为C H3C H2O H+CH3COO H ZnCl2 微波CH3COOCH2CH3+H2O 微波是频率在300M Hz~300GHz之间的电磁波,常用于加热的微波频率一般固定在2450M Hz或900M Hz.微波加热是一种内部加热过程,微波可均匀辐射到反应体系的各个部分,使整个物质同时被加热,在极短时间内达到活化状态,出现分子极化﹑摩擦和碰撞而产生热效应.微波辐射不改变化学反应的动力学特征,即微波对化学反应的加速主要归结对极性有机物置于微波电场中,分子的偶极子重新排列,并随着高频交变电场高速振动,需要克服分子原有的热运动和分子相互间作用的干扰和阻碍,发生类似摩擦的作用,产生大量的热.2 结果与讨论2.1 酸醇摩尔比的变化对乙酸乙酯产率的影响在选定的实验条件下,不同酸醇摩尔比对乙酸乙酯产率的影响见表1.表1 醇酸摩尔比对乙酸乙酯产率的影响Tab.1 The effect of the mole ratio of acid and alcohol on the production of ethyl acetaten(H3COO H)∶n(CH3(H2)O H) 2.5∶1 2.0∶1 1.5∶11∶11∶1.51∶2.0乙酸乙酯的产率/%79.0578.3672.2140.8945.2042.43 注:催化剂0.45g,辐射时间6min,辐射功率400W.由表1知,随着酸醇摩尔比的逐渐增大,乙酸乙酯的产率也显著增加,这是因为酯化反应就其动力学而言属于二级反应,与醇和酸浓度的一次方成正比关系,某一组分过量均能提高产率.考虑到原料成本和产率增加的幅度,本实验合适的酸醇摩尔比为2∶1.2.2 催化剂用量的变化对乙酸乙酯产率的影响催化剂用量的变化对乙酸乙酯产率的影响见表2.表2 催化剂用量对乙酸乙酯产率的影响Tab.2 The effect of the amount used of catalyst on the production of ethyl acetate氯化锌用量/g0.300.450.600.750.90乙酸乙酯的产率/%46.6778.3679.7680.9579.30 注:酸醇摩尔比2∶1,辐射时间6min,辐射功率400W.陈蔚萍,等:微波加热条件下氯化锌催化合成乙酸乙酯147由表2知,当催化剂用量较少时,产品产率较低,原因是水解产生的路易斯酸较少.随着催化剂用量的增大产率逐渐增加,考虑到成本,本实验催化剂选用0.45g最佳.2.3 辐射时间的变化对乙酸乙酯产率的影响辐射时间的变化对乙酸乙酯产率的影响见表3.表3 辐射时间对乙酸乙酯产率的影响Tab.3 The effect of radiation time on the preduction of ethyl ecetate时间/min 1.00 3.00 6.009.0012.00乙酸乙酯的产率/%52.8467.8878.3669.8058.95 注:酸醇摩尔比2∶1,催化剂为0.45g,辐射功率400W. 由表3知,乙酸乙酯的产率随辐射时间增长而增大,当达到一个最大值时,随辐射时间增长产率反而下降.这是因为随着反应时间的增长,温度升高,有两方面的因素影响着产率:一是温度高有反应物挥发,造成产率下降;二是热力学方面的因素.合成乙酸乙酯反应的平衡常数与温度的关系为d(ln K)d T=ΔH m,f R T2.式中ΔH m,f为负值,所以温度升高平衡常数减小,当反应时间长时,反应温度升高,反应平衡向乙酸乙酯水解方向移动,从而造成产率下降.在实验条件下,本反应最佳辐射时间为6min左右.2.4 辐射功率的变化对乙酸乙酯产率的影响辐射功率的变化对乙酸乙酯产率的影响见表4.表4 辐射功率对乙酸乙酯产率的影响Tab.4 The effect of radiation power on the production of ethyl acetate功率/W320360400440480乙酸乙酯的产率/%55.8464.9478.3662.4556.69 注:酸醇摩尔比2∶1,催化剂为0.45g,辐射时间6min.由表4知,随着辐射功率的增大,酯化产率也随之增大.在功率为400W时,产率达到最大.随后随着微波功率的增大,酯化产率反而降低,原因是功率越大在达到反应时间6min时的反应温度就越高,温度升高时动力学因素和热力学因素的影响正好相反.即:温度越高反应速度越快,平衡常数越小.在400W以下,6min以内动力学因素占主导地位,所以功率越高,酯的产率越高;在400W以上,6min以内热力学因素占主导地位,所以功率越高酯的产率反而降低.3 结论在微波场中用氯化锌作催化剂催化合成乙酸乙酯,得到了比较满意的结果.反应条件为: n(CH3COO H)∶n(C2H5O H)=2∶1,催化剂质量百分数为1.5%,辐射时间为6min,辐射功率为400W.乙酸乙酯的产率为78.36%.该方法与传统合成方法相比,缩短了实验时间,而且操作简单,反应速度快(用传统加热法反应时间需100min)[8],对设备腐蚀小,体现出省时、节能等优点,具有一定的社会效益和经济效益.参考文献:[1]许波.微波技术应用于酯化反应的研究进展[J].北京石油化工学院学报,2005,13(4):35-36.[2]莫莉萍,周璇,李拥军.微波技术在现代有机合中的应用进展[J].广东化工,2004,1(4):44-45.[3]植中强,李红缨,杨海贵,等.微波催化酯化合成乙酸乙酯[J].化学工程师,2002,89(2):11-12.[4]贾树勇,任玉荣.活性炭负载FeCl3催化合成CH3COOEt的研究[J].宝鸡文理学院学报:自然科学版,2003,23(4):279-280.[5]贾艳宗,马沛生,王彦飞.微波在酯化和水解反应中的应用[J].化工进展,2004,23(6):641-642.[6]李水清,张促宁,谢晖.微波辐射对乙酸乙酯皂化反应的影响[J].化学研究,2005,16(3):47-49.[7]王清廉,沈凤嘉.有机化学实验[M].2版.北京:高等教育出版社,1996:162-163.[8]大连工学院有机化学教研室编.有机化学实验[M].北京:人民教育出版社,1979:137-144.责任编辑:马同森。

含硒光催化剂

含硒光催化剂

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低浓度NaCl_对油葵芽苗菜生长及品质的影响

低浓度NaCl_对油葵芽苗菜生长及品质的影响

第46卷第6期2023年11月河北农业大学学报JOURNAL OF HEBEI AGRICULTURAL UNIVERSITYVol.46 No.6Nov.2023低浓度NaCl对油葵芽苗菜生长及品质的影响尹伟僮,王明姣,范 辉,李青云,薛占军(河北农业大学 园艺学院,河北 保定 071001)摘要:以油葵种子‘S667’为试材,从催芽到芽苗菜收获的整个过程分别连续施用10 d 0(CK)、5、10、15、20和25 mmol/L NaCl溶液,测定油葵芽苗菜的生长、产量和品质指标,探索低浓度NaCl对油葵芽苗菜生长及品质的调控效应。

与对照(CK,0 mmol/L NaCl)相比,15 mmol/L NaCl对油葵芽苗菜的生长和品质的调控效应最明显,其中下胚轴的长度、粗度、可溶性蛋白和Vc含量分别增加41.57%、8.58%、1548.03%和169.57%,子叶的面积、Vc和多酚含量分别增加45.49%、37.10%和81.49%,同时油葵芽苗菜的可食率和经济产量分别提升了13.68%和73.76%,叶绿素总量/类胡萝卜素含量增加了30.77%;但是,低浓度NaCl处理显著降低了油葵芽苗菜下胚轴和子叶的游离氨基酸含量,分别较CK降低了47.00%~77.70%和56.63%~74.96%。

由此可见,施用15 mmol/L NaCl可显著提升油葵芽苗菜的产量和品质。

关 键 词:油葵;芽苗菜;低浓度NaCl;生长;品质中图分类号:S649开放科学(资源服务)标识码(OSID):文献标志码:AEffects of low concentration NaCl on the growth and quality of oilsunflower sproutsYIN Weitong, WANG Mingjiao, FAN Hui, LI Qingyun, XUE Zhanjun(College of Horticulture, Hebei Agricultural University, Baoding 071001, China)Abstract: The oil sunflower ‘S667’ was treated with 0 (CK), 5, 10, 15, 20 and 25 mmol/L NaCl solutions from seedgermination to sprout harvest followed by measurement of the growth, yield and quality indexes of oil sunflower sproutsafter 10 days to explore the effects of low concentration NaCl on the growth and quality of oil sunflower sprouts.Compared with the control (0 mmol/L NaCl), 15 mmol/L NaCl treatment had the most obvious effects on the growth andquality of oil sunflower sprouts, in which the length, thickness, soluble protein and Vc contents of hypocotyl increasedby 41.57%, 8.58%, 1548.03% and 169.57%, respectively, and area, Vc and polyphenol content of cotyledon increasedby 45.49%, 37.10% and 81.49%, respectively. Meanwhile, edible percentage, economic yield and total chlorophyll/carotenoid content of oil sunflower sprouts increased by 13.68%, 73.76% and 30.77%, respectively. However, lowconcentration of NaCl significantly reduced the content of free amino acids in hypocotyl and cotyledon of oil sunflowerseedlings, which decreased by 47.00%-77.70% and 56.63%-74.96% compared with CK, respectively. In conclusion,application of 15 mmol/L NaCl significantly increased the yield and quality of oil sunflower sprouts. Our resultsprovided a simple, safe and effective regulation technology to produce oil sunflower sprouts.Keywords: Oil sunflower; sprouts; low concentration of NaCl; growth; quality收稿日期:2023-06-07基金项目:河北省现代农业产业技术体系设施蔬菜创新团队项目(HBCT2021030213).第一作者:尹伟僮(1997-),女,河北廊坊人,硕士研究生,从事蔬菜栽培生理与品质调控研究.E-mail:**************通信作者:薛占军(1983-),男,内蒙古商都县人,博士,讲师,从事蔬菜栽培生理与品质调控研究.E-mail:****************本刊网址:文章编号:1000-1573(2023)06-0052-06DOI:10.13320/ki.jauh.2023.009253第6期芽苗蔬菜生产因其具有生育周期短、产品质量等级优、生物效率高和对设施及装备要求低等特点,率先实现了工厂化优质高效生产,不同程度地推动了新型芽苗菜产业的快速发展。

大分子有机阴离子盐 锌离子电池

大分子有机阴离子盐 锌离子电池

大分子有机阴离子盐锌离子电池英文回答:Organic ionic salts are a type of large-molecule organic compounds that contain ions. These salts are composed of organic cations and inorganic anions. They can be formed by the reaction between organic bases and inorganic acids. One example of an organic ionic salt is tetraethylammonium chloride (TEACl).Zinc ion batteries, on the other hand, are a type of rechargeable battery that uses zinc ions as the charge carrier. These batteries consist of two electrodes a zinc anode and a cathode made of another material, such as manganese dioxide. When the battery is charged, zinc ions are released from the anode and travel through the electrolyte to the cathode. During discharge, the zinc ions return to the anode, releasing electrons that flow through an external circuit to power a device.The combination of organic ionic salts and zinc ions can be used to create a zinc ion battery. In this type of battery, the organic ionic salt acts as the electrolyte, facilitating the movement of zinc ions between the electrodes. The organic cation in the salt providesstability and helps to prevent the formation of dendrites, which can cause short circuits in the battery.One advantage of using organic ionic salts in zinc ion batteries is their high ionic conductivity. The organic cations can enhance the mobility of zinc ions, allowing for faster charge and discharge rates. Additionally, the organic cations can be tailored to improve the stability and safety of the battery.For example, a zinc ion battery using tetraethylammonium chloride as the electrolyte can have improved performance compared to traditional zinc ion batteries. The TEACl salt provides high ionic conductivity, allowing for faster charging and discharging. The organic cation also helps to stabilize the zinc ions, reducing the risk of dendrite formation.In summary, the combination of organic ionic salts and zinc ions can be used to create high-performance zinc ion batteries. These batteries offer advantages such as high ionic conductivity and improved stability. By harnessing the unique properties of organic ionic salts, we can develop more efficient and reliable energy storage solutions.中文回答:有机阴离子盐是一种含有离子的大分子有机化合物。

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Low Micromolar Zinc Accelerates the Fibrillization of Human Tau via Bridging of Cys-291and Cys-322*Received for publication,August24,2009Published,JBC Papers in Press,October13,2009,DOI10.1074/jbc.M109.058883Zhong-Ying Mo,Ying-Zhu Zhu,Hai-Li Zhu,Jun-Bao Fan,Jie Chen,and Yi Liang1From the State Key Laboratory of Virology,College of Life Sciences,Wuhan University,Wuhan430072,ChinaA hallmark of a group of neurodegenerative diseases such as Alzheimer disease is the formation of neurofibrillary tangles, which are principally composed of bundles of filaments formed by microtubule-associated protein Tau.Clarifying how natively unstructured Tau protein forms abnormal aggregates is of cen-tral importance for elucidating the etiology of these diseases. There is considerable evidence showing that zinc,as an essential element that is highly concentrated in brain,is linked to the development or progression of these diseases.Herein,by using recombinant human Tau fragment Tau244–372and its mutants, we have investigated the effect of zinc on the aggregation of Tau. Low micromolar concentrations of Zn2؉dramatically acceler-ate fibril formation of wild-type Tau244–372under reducing con-ditions,compared with no Zn2؉.Higher concentrations of Zn2؉,however,induce wild-type Tau244–372to form granular aggregates in reducing conditions.Moreover,these non-fibril-lar aggregates assemble into mature Tau filaments when Zn2؉has been chelated by EDTA.Unlike wild-type Tau244–372,low micromolar concentrations of Zn2؉have no obvious effects on fibrillization kinetics of single mutants C291A and C322A and double mutant C291A/C322A under reducing conditions.The results from isothermal titration calorimetry show that one Zn2؉binds to one Tau molecule via tetrahedral coordination to Cys-291and Cys-322as well as two histidines,with moderate, micromolar affinity.Our data demonstrate that low micromolar zinc accelerates the fibrillization of human Tau protein via bridging Cys-291and Cys-322in physiological reducing condi-tions,providing clues to understanding the relationship between zinc dyshomeostasis and the etiology of neurodegen-erative diseases.Tau,a microtubule-associated protein,is the major protein subunit of neurofibrillary tangles(NFTs),2which are found in a group of neurodegenerative diseases such as Alzheimer disease and frontotemporal lobar degeneration(1,2).NFTs are mainly composed of bundles of Tau in the form of paired helical fila-ments(PHFs),straight filaments,or twisted ribbons.It is gen-erally believed that the neuron degeneration in such diseases is very likely to be contributed by the accumulation of these aggregates(3).Thus the characterization of factors involved in abnormal Tau aggregation is of great importance to clarify the etiology of neurodegenerative diseases and assist in the estab-lishment of medical treatment.Tau is one of the largest proteins without recognizable sec-ondary structure and adopts a natively unfolded structure in solution(4).There are two distinct domains of Tau protein,the projection domain and the microtubule binding domain.The microtubule binding domain mainly contains either three or four imperfect repeats(18amino acids in length)separated from one another by inter repeats(13–14amino acids in length) (5).In its normal state,Tau facilitates and stabilizes the assem-bly of microtubules.But under certain pathological conditions, it will detach from microtubules.Some of its small segments adopt a␤-conformation,and further interactions convert them toward formation of aggregates that are rich in␤-sheet struc-tures.These aggregates undergo filament nucleation and elon-gation and form NFTs eventually(1,2,6).The microtubule binding repeat region forms the core of filaments while the rest of the protein retains its largely unfolded structure,which forms the fuzzy coat of the filaments(7–9).Although the mechanism by which Tau protein aggregates is not fully understood,there are increasing evidences showing that a disturbance of brain zinc homeostasis during aging plays a role in the etiology of Alzheimer disease(10–12).Zinc is an integral component of numerous enzymes,transcription fac-tors,and structural proteins.Furthermore,zinc is one of the most abundant transition metals in the brain and is in particu-larly large concentrations in the mammalian brain with an overall concentration ofϳ150␮M(13).The distribution of zinc is not uniform,and up to15%of brain zinc is located inside presynaptic vesicles(13,14).Although the cytosolic free con-centration of Zn2ϩin cultured neurons is generally subnano-molar,in pathological conditions the free concentration of Zn2ϩis altered via several pathways such as presynaptic zinc translocation(15).There is current evidence for a relative increase in intracel-lular zinc in vulnerable regions of the Alzheimer disease brain (16),and abnormally high levels of zinc at millimolar concen-trations have been found in NFTs and senile plaque cores(17, 18).It is estimated that strong activation of Zn2ϩ-containing presynaptic terminals results in transient local synaptic Zn2ϩconcentrations in the100–300␮M range(13,17).Histochem-ically reactive zinc deposits are also found specifically localized to cerebral amyloid angiopathy deposits and NFT-bearing neu-rons(19).It has been reported that there are3-to5-fold increases in zinc in the cortical and accessory basal nuclei of the*This work was supported by National Key Basic Research Foundation of China Grant2006CB910301and by National Natural Science Foundation of China Grants30770421and30970599.1To whom correspondence should be addressed.Tel.:86-27-6875-4902;Fax: 86-27-6875-4902;E-mail:liangyi@.2The abbreviations used are:NFT,neurofibrillary tangles;AFM,atomic forcemicroscopy;DM,double mutant C291A/C322A of Tau244–372;DTT,dithio-threitol;ITC,isothermal titration calorimetry;PHF,paired helical filaments; TEM,transmission electron microscopy;ThT,thioflavin T;WT,wild-typeTau244–372.THE JOURNAL OF BIOLOGICAL CHEMISTRY VOL.284,NO.50,pp.34648–34657,December11,2009©2009by The American Society for Biochemistry and Molecular Biology,Inc.Printed in the U.S.A.by guest on January 13, 2015/Downloaded fromamygdala and in the neuropil of Alzheimer disease patients,as compared with age-matched controls(20).Zinc has been shown to accelerate the aggregation of amyloid ␤peptides(21,22),trigger the fibrillization of methionine oxi-dized␣-synuclein(23),and cause an aggregation of Dcp1a pro-tein in an RNA-dependent manner(24).There are also results indicating that Ca2ϩand Mg2ϩcan selectively induce the for-mation of PHF-Tau aggregation(25),whereas Al3ϩ,Cu2ϩ,and Fe2ϩ/Fe3ϩcan bind to Tau(26–28).However,whether Zn2ϩhas an effect on the aggregation of Tau has not been reported so far,which leaves us to answer the physiological question whether the alteration of zinc can affect Tau aggregation and thus play a role in the pathology of neurodegenerative diseases such as Alzheimer disease.In the present study,by using several biophysical methods, such as thioflavin T binding,atomic force microscopy(AFM), transmission electron microscopy(TEM),and isothermal titra-tion calorimetry(ITC),we investigated the impact of zinc onthe aggregation of human Tau fragment Tau244–372.Ourresults indicated that low micromolar zinc dramatically accel-erated fibril formation of wild-type Tau244–372in the presenceof dithiothreitol(DTT),but had no obvious effects on fibrilli-zation kinetics of single mutants C291A and C322A and double mutant C291A/C322A.Further,we demonstrated that Zn2ϩbound to Tau molecules via tetrahedral coordination to Cys-291,Cys-322,and two histidines with moderate,micromolar affinity,and thus concluded that low micromolar zinc pro-moted the fibrillization of human Tau protein via bridging of Cys-291and Cys-322in physiological reducing conditions. EXPERIMENTAL PROCEDURESMaterials—Heparin(average molecular massϭ6kDa)and thioflavin T(ThT)were purchased from Sigma.DTT was obtained from Ameresco Chemical Co.(Solon,OH).All the metal cations used were chloride forms of analytical grade.All other chemicals used were made in China and were of analytical grade.The buffers used in this study were treated with ion-exchange resins to remove trace amounts of divalent cations present as contaminants in the solutions.Plasmids and Proteins—The cDNA-encoding human Taufragment Tau244–372was amplified using the plasmid forhuman Tau40(kindly provided by Dr.Michel Goedert)as atemplate.The PCR-amplified Tau244–372was subcloned intopRK172vector.Single cysteine mutants C291A and C322A anddouble mutant C291A/C322A of Tau244–372were generatedusing primers GCAACGTCCAGTCCAAGGCTGGCTCAA-AGG/CCTTTGAGCCAGCCTTGGACTGGACGTTGC for C291A and GTGACCTCCAAGGCTGGCTCATTAGGCAA-CATC/GATGTTGCCTAATGAGCCAGCCTTGGAGG-TCAC for C322A.Single histidine mutants H330A and H362A and histidine-less mutant H268A/H299A/H329A/H330A/ H362A were generated in a similar manner.Plasmids contain-ing target sequences were transformed into Escherichia coli BL21(DE3)strain.The expression of recombinant human Taufragment Tau244–372and its mutants was induced with400␮Misopropyl-␤-D-thiogalactopyranoside and cultured for3h.Cell pellets of2-liter culture were collected and re-suspended in80 ml of buffer A(20m M phosphate buffer containing2m M DTT,pH7.0)and then sonicated at250watts for30min.500m MNaCl was added into the mixture,and then the mixture was boiled at100°C for15min.After centrifugation at17,000ϫgfor30min at4°C,supernatant was collected and dialyzed against buffer A extensively.The sample was then loaded to anSP-Sepharose column and washed with400ml of buffer A.The target protein was obtained by washing the column using500ml of20m M phosphate buffer containing2m M DTT and0–400m M NaCl.The Tau fragment was then concentrated and dialyzed against50m M Tris-HCl buffer containing2m M DTT(pH7.5)extensively,and then stored atϪ80°C.Purified Tau protein was analyzed by SDS-PAGE with one band and con-firmed by mass spectrometry.The concentration of human Tau fragment was determined according to its absorbance at214nm with a standard calibration curve drawn by bovine serum albumin as described(29).ThT Binding Assays—A2.5m M ThT stock solution was freshly prepared in50m M Tris-HCl buffer(pH7.5)and passed through a0.22-␮m pore size filter before use to remove insol-uble particles.Under standard conditions,10␮M Tau244–372was incubated without agitation in50m M Tris-HCl buffer(pH7.5)containing1m M DTT and20␮M ThT with or withoutZn2ϩat37°C for up to1h in the presence of fibrillization inducer heparin used in a Tau:heparin molar ratio of4:1.The fluorescence of ThT was excited at440nm with a slit width of7.5nm,and the emission was measured at480nm with a slitwidth of7.5nm on an LS-55luminescence spectrometer (PerkinElmer Life Sciences).The preparation of the samples before the first measurement took1min.The polymerization for Tau244–372and its cysteine mutantsin96-well plates were set up by a mixture of20␮M Tau protein,5␮M heparin,50␮M ThT,and0–80␮M Zn2ϩeither in the presence or in the absence of1m M DTT in50m M Tris-HCl buffer containing100m M NaCl(pH7.5).The reaction compo-nents were mixed quickly and immediately read for8h(with DTT)or3h(without DTT)at37°C in SpectraMax M2 microplate reader(Molecular Devices,Sunnyvale,CA)using excitation at440nm and emission at480nm with a wave-length cut-off at475nm.Each sample was run in triplicate or quadruplicate.Kinetic parameters were determined by fit-ting ThT fluorescence intensity versus time to a sigmoidal equation(30),FϭF0ϩ͑Aϩct͒/͕1ϩexp[k͑t mϪt͔͒}(Eq.1)where F is the fluorescence intensity,k is the rate constant forthe growth of fibrils,and tmis the time to50%of maximal fluorescence.The initial baseline during the lag time isdescribed by F.The final baseline after the growth phase hasended is described by Aϩct.The lag time is calculated as tmϪ2/k.Sarkosyl-insoluble Tau SDS-PAGE—The Sarkosyl-insolubleTau experiments were carried out according to the method described by Aoyagi and co-workers(31)with minor changes.Tau polymerization was set up by incubating a mixture of10␮MTau244–372,2.5␮M heparin,1m M DTT,and0–100␮M Zn2ϩin50m M Tris-HCl buffer(pH7.5)at37°C without agitation.Ali-quots(100␮l)of assembly mixtures were taken out and addedLow Micromolar Zinc Accelerates Tau Fibrillizationby guest on January 13, 2015/Downloaded frominto 500␮l of 50m M Tris-HCl buffer (pH 7.5)containing 1%Sarkosyl.The mixture was left at room temperature for 30min and then centrifuged in an Optima LE-80K ultracentrifuge (Beckman Coulter,Fullerton,CA)at 150,000ϫg for 30min.The supernatant (Sarkosyl-soluble Tau)was removed,and the pellet (Sarkosyl-insoluble Tau)was re-suspended in 50␮l of SDS sample buffer containing 5%2-mercaptoethanol and sub-jected to 15%SDS-PAGE.After the electrophoresis the gels were stained with Coomassie Blue.Transmission Electron Microscopy —The formation of fila-ments by human Tau fragment was confirmed by electron microscopy of negatively stained samples.Sample aliquots of 10␮l were placed on copper grids and left at room temperature for 1–2min,rinsed with H 2O twice,and then stained with 2%(w/v)uranyl acetate for another 1–2min.The stained samples were examined using an H-8100transmission electron microscope (Hitachi,Tokyo,Japan)operating at 100kV.AFM —The formation of filaments by human Tau fragment was further confirmed by AFM.Sample aliquots of 10␮l were deposited onto freshly cleaved mica,left on the surface for 10min,and rinsed with H 2O twice.Then the solution was dried in a desiccator for 12h.AFM images were acquired in tapping mode with an SPM-9500J3scanning probe microscope (Shi-madzu,Kyoto,Japan).Several regions of the mica surface were examined to confirm that similar structures existed through the sample.Isothermal Titration Calorimetry —ITC experiments on the interaction of Zn 2ϩwith Tau 244–372and its mutants were car-ried out at 25.0°C using an iTC 200titration calorimetry (Micro-Cal,Northampton,MA).Freshly purified Tau proteins (wild-type Tau 244–372,single mutants C291A,C322A,H330A,and H362A,double mutant C291A/C322A,and histidine-less mutant H268A/H299A/H329A/H330A/H362A)were dialyzed against 50m M Tris-HCl buffer (pH 7.5)containing 1m M EDTA,overnight at 4°C and then dialyzed against 50m M Tris-HCl buffer (pH 7.5)extensively to remove EDTA.A solution of 100–200␮M Tau proteins was loaded into the sample cell (200␮l),and a solution of 2.8–6.0m M Zn 2ϩwas placed in the injec-tion syringe (40␮l).The first injection (0.3␮l)was followed by 24–27injections of 1␮l.Dilution heats of Zn 2ϩwere measured by injecting Zn 2ϩsolution into buffer alone and were sub-tracted from the experimental curves prior to data analysis.The stirring rate was 600rpm.The resulting data were fitted to a single set of identical sites model using MicroCal ORIGIN soft-ware supplied with the instrument,and the standard molarenthalpy change for the binding,⌬b H m 0,the dissociation con-stant,K d ,and the binding stoichiometry,n ,were thus obtained.The standard molar free energy change,⌬b G m 0,and the stand-ard molar entropy change,⌬b S m 0,for the binding reaction were calculated by the fundamental equations of thermodynamics (32).⌬b G m 0ϭRT ln K d(Eq.2)⌬b S m 0ϭ͑⌬b H m 0Ϫ⌬b G m 0͒/T(Eq.3)RESULTSThe Presence of Zn 2ϩInfluenced Tau Aggregation —The enhanced fluorescence emission of the dye ThT has been fre-quently used for monitoring the kinetics of amyloid fibril for-mation,which is a specific marker for the ␤-sheet conformation of fibril structures (33,34).Because Tau 244–372consists of the four-repeat microtubule binding domain forming the core of PHFs in Alzheimer disease and assembles more readily than full-length Tau protein into filaments in vitro ,we employed such a Tau fragment for studying kinetics of Tau fibril forma-tion.As shown in Fig.1,the kinetic curves of the ThT fluores-cence intensity at 480nm for Tau 244–372fibrillization were con-sistent with a nucleation-dependent elongation model (35),in which the lag phase corresponded to the nucleation phase,and the exponential part to a fibril growth (elongation)phase.Bivalent cations such as Mg 2ϩ,Mn 2ϩ,Ca 2ϩ,Zn 2ϩ,and Cu 2ϩand trivalent cation Fe 3ϩwere incubated separately with phys-iological concentrations of Tau 244–372at 37°C in the presence of DTT.As shown in Fig.1A ,in the absence of cation,the lag phase for wild-type Tau 244–372polymerization was ϳ500s,whereas the addition of Mg 2ϩ,Mn 2ϩ,Ca 2ϩ,Fe 3ϩ,and Cu 2ϩat a low micromolar concentration (10␮M )decreased the lag phase in different ranges.In the presence of 10␮M Zn 2ϩ,how-ever,the lag phase was dramatically diminished,indicating that low micromolar concentrations of Zn 2ϩgreatly accelerated fibril formation of wild-type Tau 244–372,compared with no Zn 2ϩ,and the enhancing effect of Zn 2ϩwas more remarkable than those of other cations such as Mn 2ϩ,Fe 3ϩ,and Cu 2ϩ.Clearly,the nucleation of Tau fragment was much more accel-erated by 10␮M Zn 2ϩthan the following step of elongation (Fig.1A ).Meanwhile,when wild-type Tau 244–372was incubated with 100␮M cations,the kinetic curve of Tau 244–372in the presence of Zn 2ϩwas also quite different from those of other cations except Fe 3ϩ(Fig.1B ).The lag phase was too short to be observed,but the maximum intensity became much lower in the presence of 100␮M Zn 2ϩthan that in the absence of cation,indicating the aggregation of Tau 244–372was significantly altered by higher concentrations of Zn 2ϩ.Both cases indicated that the presence of Zn 2ϩ,compared with other cations,signif-icantly altered the aggregation of Tau in reducing conditions and factors other than electrostatic interactions must play a role in this phenomenon.To get a better understanding about the effect of zinc on Tau aggregation,we performed ThT binding assays at various con-centrations of Zn 2ϩ.As shown in Fig.1C ,the addition of 5–20␮M Zn 2ϩaccelerated fibril formation of wild-type Tau 244–372under reducing conditions,but the enhancing effect of Zn 2ϩwas most significant when the concentration of Zn 2ϩwas 10␮M ,which is equal to that of Tau fragment.When the concen-tration of Zn 2ϩwent higher,the kinetic curves still went up instantly,almost without a lag phase,but the final ThT intensi-ties decreased 65and 76%for 50and 100␮M Zn 2ϩ,respectively (Fig.1C ).The phenomenon that the presence of Zn 2ϩsignifi-cantly reduced the lag phase indicated that Zn 2ϩhad a strong enhancing effect on the nucleation of Tau protein.However,smaller exponential growth at higher molar ratios of Zn 2ϩto Tau suggested fewer filaments but other forms of Tau aggre-gates were formed,compared with no Zn 2ϩ.To semi-quantify the aggregates of Tau protein formed in the presence of Zn 2ϩat different concentrations,we carried out Sarkosyl-insoluble SDS-PAGE experiments and assessedLow Micromolar Zinc Accelerates Tau Fibrillizationby guest on January 13, 2015/Downloaded fromTau 244–372aggregation under reducing conditions by meas-uring the Sarkosyl-insoluble Tau as described (31).As shown in Fig.1D ,a clear band corresponding to Sarkosyl-insoluble Tau filaments was observed when wild-type Tau 244–372was incu-bated in the absence of Zn 2ϩfor 40min,whereas the Sarkosyl-insoluble Tau band was observed when Tau 244–372was incu-bated with Zn 2ϩat low micromolar concentrations (5–10␮M )for a much shorter time (15–10min).Furthermore,when Tau 244–372was incubated for 40min,the intensity of the Sar-kosyl-insoluble Tau band in the presence of 10␮M Zn 2ϩwas remarkably higher than that in the absence of Zn 2ϩ.This find-ing further supports the observation mentioned above that lowmicromolar concentrations of Zn 2ϩdramatically accelerate fibril forma-tion of wild-type Tau 244–372in reducing conditions,compared with no Zn 2ϩ.At higher concentra-tions of Zn 2ϩ(50–100␮M ),how-ever,no Sarkosyl-insoluble Tau band was observed even at 40min (Fig.1D ),indicating that fewer fila-ments but other forms of Tau aggre-gates,Sarkosyl-soluble Tau aggre-gates,were formed at higher molar ratios of Zn 2ϩto Tau under reduc-ing conditions.Morphology of Tau Aggregates Varied with Molar Ratios of Zn 2ϩto Tau —TEM and AFM were employed to study the morphology of wide-type Tau 244–372incubated with Zn 2ϩat different concentra-tions for 60min (Fig.2).The addi-tion of low micromolar concentra-tions of Zn 2ϩ(5or 10␮M )had no significant effect on the morphology of Tau samples monitored by TEMand AFM,and long and branched fibrils as well as a few short fila-ments (Fig.2,A–C )and some fila-ments with a length of 200–500nm (Fig.2,G–I )were observed in these three samples.When the concen-tration of Zn 2ϩincreased (50or 100␮M )until the molar ratio of Zn 2ϩto Tau exceeded equality,however,FIGURE 1.The presence of Zn 2؉altered Tau 244–372fibrillization kinetics.A ,10␮M Tau 244–372was incubated with 10␮M cation (open circle ,Mg 2ϩ;filled triangle ,Mn 2ϩ;filled inverted triangle ,Ca 2ϩ;filled circle ,Zn 2ϩ;filled square ,Fe 3ϩ;and open triangle ,Cu 2ϩ)or without cation (open square );B ,10␮M Tau 244–372was incubated with 100␮M cation (open circle ,Mg 2ϩ;filled triangle ,Mn 2ϩ;filled inverted triangle ,Ca 2ϩ;filled circle ,Zn 2ϩ;filled square ,Fe 3ϩ;and open triangle ,Cu 2ϩ)or without cation (open square );C ,10␮M Tau 244–372was incubated with 0–100␮M Zn 2ϩ(open square ,0␮M ;filled triangle ,5␮M ;filled circle ,10␮M ;filled inverted triangle ,20␮M ;filled rhombus ,50␮M ;and filled square ,100␮M ).The buffer used was 50m M Tris-HCl buffer (pH 7.5)containing 1m M DTT,2.5␮M heparin,and 20␮M ThT,and ThT binding assays were carried out at 37°C.D ,10␮M Tau 244–372was incubated with 0–100␮M Zn 2ϩcontaining 2.5␮M heparin and 1m M DTT in 50m M Tris-HCl buffer (pH 7.5)at 37°C.Aliquots were taken at 0,5,10,15,30,and 40min,respectively,and then incubated with Tris-HCl buffer containing 1%Sarkosyl followed by centrifuging at 150,000ϫg for 30min.Pellets were re-suspended with sample buffercontaining 5%2-mercaptoethanol and subjected to 15%SDS-PAGE.Gels were stained with CoomassieBlue.FIGURE 2.Transmission electron micrographs (A–F )and AFM images (G–L )of Tau 244–372aggregates formed with Zn 2؉.10␮M Tau 244–372was incubatedwith 0–100␮M Zn 2ϩ(A and G ,0␮M ;B and H ,5␮M ;C and I ,10␮M ;D and J ,20␮M ;E and K ,50␮M ;and F and L ,100␮M )containing 2.5␮M heparin and 1m M DTT in 50m M Tris-HCl buffer (pH 7.5)at 37°C for 60min.A 2%(w/v)uranyl acetate solution was used to negatively stain the fibrils (A–F ).The scale bars represent 200nm.Low Micromolar Zinc Accelerates Tau Fibrillizationby guest on January 13, 2015/Downloaded fromTau 244–372filaments became much fewer and shorter,and abundant granular aggregates (ϳ30nm in diameter)were observed (Fig.2,E ,F ,K ,and L ).Maeda and co-workers (36)have observed similar aggregates and have suggested that such granular Tau aggregates may be an intermediate form of Tau bining the results from TEM and AFM,we concluded that the morphology of wild-type Tau 244–372aggregates varied with molar ratios of Zn 2ϩto Tau in reducing conditions.At lower molar ratios,Tau aggregates were mainly composed of filaments,which was similar to those in the absence of Zn 2ϩ.But at higher molar ratios,filaments became much fewer and shorter,and granular aggregates became prevalent.In other words,higher concentrations of Zn 2ϩinduced wild-type Tau 244–372to form granular aggregates under reducing conditions.Characterization of the Effect of Zinc on Tau Aggregation at Differ-ent Stages —We then checked whether the enhancing effect of Zn 2ϩon the aggregation of Tau was dependent on the incubation time or different compositions of Tau protein.We added 10or 100␮M Zn 2ϩafter incubation for 5,15,and 30min,when Tau 244–372was no longer pure monomers.As shown in Fig.3(A–D ),Zn 2ϩadded at 15min in the growth phase or at 30min in the final equilibrium phase did not facilitate fibril formation of Tau 244–372under reducing condi-tions;on the contrary,it slowed down or even blocked the growth phase.Furthermore,10␮M Zn 2ϩadded at 5min in the lag phase had no obvious effect on fibril formation of Tau 244–372,and 100␮M Zn 2ϩadded at 5min slowed down the growth phase in reducing condi-tions (data not shown).The above results suggested that the enhancing effect on fibrillization kinetics of Tau by low micromolar concentra-tions of Zn 2ϩwas mainly due to its direct interaction with Tau mono-mers,but not protofibrils or fibrils.It is this interaction that accelerated the nucleation of Tau protein.To verify whether the effect of Zn 2ϩwas chelator-reversible,we added 1m M EDTA into systems containing Tau 244–372incubated with 10or 100␮M Zn 2ϩseparately.As shown in Fig.3(E and F ),the addition of EDTA at 15min in thegrowth phase did not change fibrillization kinetics of Tau in the presence of 10␮M Zn 2ϩ,suggesting that,once the nucle-ation of Tau had been finished,the binding of Zn 2ϩto Tau was no longer necessary for the filament elongation and matura-tion.But in the presence of 100␮M Zn 2ϩ,the addition of EDTA at 15min did alter the fibrillization kinetics by accelerating the elongation of Tau protein remarkably and reaching a final ThT intensity ϳ17%larger than that in the absence of Zn 2ϩ.Higher concentrations of Zn 2ϩinduced Tau to form granular aggre-gates under reducing conditions (Fig.2).Moreover,such non-fibrillar aggregates assembled into mature Tau filaments when Zn 2ϩhad been chelated by EDTA (Fig.3F).FIGURE 3.Effect of Zn 2؉on Tau 244–372fibrillization at various time points.10␮M Tau 244–372was incubatedwithout Zn 2ϩ(black curves )and then titrated with 10␮M Zn 2ϩor 100␮M Zn 2ϩat 15min (A and C )or 30min (Band D )respectively (red curves ).E ,10␮M Tau 244–372was incubated with 10␮M Zn 2ϩ(black curves )and then titrated with aliquots of 1m M EDTA at 15min (red curves ).F ,10␮M Tau 244–372was incubated with 100␮M Zn 2ϩ(black curves )and then titrated with 1m M EDTA at 15min (red curves ).The beginning of titrations is indicated by black arrows ,and the curves are compared with 10␮M Tau 244–372incubated without Zn 2ϩ(green curves ).The buffer used was 50m M Tris-HCl buffer (pH 7.5)containing 1m M DTT,2.5␮M heparin,and 20␮M ThT,and ThT binding assays were carried out at 37°C.Low Micromolar Zinc Accelerates Tau Fibrillizationby guest on January 13, 2015/Downloaded fromEffect of Zn 2ϩon Tau Aggregation under Reducing or Oxida-tive Conditions —Neuronal cells normally have a reducing envi-ronment maintained by an excess of glutathione (1,5,37).To mimic the reducing environment present in normal neuronal cells and block the formation of an intramolecular disulfide bond,DTT,a strong reducing agent,was used in this study.We carried out ThT binding assays in the presence and absence of DTT to compare the effect of Zn 2ϩon Tau aggregation under reducing conditions with that in oxidizing conditions.Addi-tionally,100m M NaCl was added into the polymerization mix-ture to mimic the physiological salinity.It has been reported that Tau aggregation is highly sensitive to elevated ionic strength (38).As shown in Fig.4A ,in the presence of DTT and 100m M NaCl,the results were quite similar to those obtained in the presence of DTT but without salt (Fig.1),except that the lag time of Tau fibrillization was much longer than that in the absence of salt as expected.When wild-type Tau 244–372was incubated with low micromolar concentrations of Zn 2ϩ,the kinetic curves of Tau fibrillization grew much faster and reached a plateau around 3h,compared with Ͼ8h in the absence of Zn 2ϩ,once again indicating that low micromolar concentrations of Zn 2ϩdramatically accelerated fibril forma-tion of wild-type Tau 244–372under physiological reducing conditions.While in the absence of DTT (Fig.4E ),the kinetic curve of Tau fibrillization showed no detectable increase within 3h in the absence of Zn 2ϩ.But when Tau 244–372was incubated with different concentrations of Zn 2ϩ,the kinetic curves showed instant increases in oxidizing conditions even at higher molar ratios of Zn 2ϩto Tau.It is quite different from those obtained inreducing conditions,which showed smaller exponential growth and much lower final ThT intensities at higher molar ratios of Zn 2ϩto Tau (Fig.4A ).This comparison suggests that higher concentrations of Zn 2ϩinduced Tau to form granular aggregates only under reducing conditions.Cys-291and Cys-322Are Key Residues in the Interaction of Zn 2ϩwith Tau —There are two cysteine residues,Cys-291and Cys-322,in full-length human Tau protein (441amino acids).They are located in repeats 2and 3of the four-repeat microtu-bule binding domain (37,39).Little is known about the role of such cysteine residues in Tau assembly,because their substitu-tion with other amino acids has no effect on Tau filament mor-phology (40).In this study,Tau 244–372mutants containing sin-gle and double cysteine mutations were designed,and ThT binding assays using such mutants were performed to provide information about the binding sites of zinc in Tau protein and the role of Cys-291and Cys-322in Tau assembly.Table 1sum-marizes the kinetic parameters obtained for fibril formation of wild-type Tau 244–372and its cysteine mutants in the presence of low micromolar concentrations of Zn 2ϩunder reducing con-ditions.Unlike wild-type Tau 244–372,4–10␮M Zn 2ϩhad no obvious effects on fibrillization kinetics of single mutants C291A and C322A and double mutant C291A/C322A in reduc-ing conditions (Fig.4,B –D ,and Table 1),indicating that low micromolar zinc accelerated the fibrillization of human Tau protein via bridging Cys-291and Cys-322.But higher concen-trations of Zn 2ϩdid not have uniform effects on fibrillization kinetics of Tau 244–372mutants under reducing conditions:an inhibitory effect on C291A (Fig.4B ),an enhancing effect on C322A (Fig.4C ),and no obvious enhancing effect onC291A/FIGURE 4.Cys-291and Cys-322are key residues in the interaction of Zn 2؉with Tau 244–372.The top panels show the ThT binding assays of 20␮M wild-type (WT )Tau 244–372(A ),20␮M single mutants C291A (B ),and C322A (C )or double mutant C291A/C322A (D )incubated with 0–80␮M Zn 2ϩ(black ,0␮M ;red ,4␮M ;green ,10␮M ;blue ,20␮M ;cyan ,40␮M ;and magenta ,80␮M )in the presence of 1m M DTT.The bottom panels show the ThT binding assays of 20␮M WT Tau 244–372(E ),20␮M single mutants C291A (F ),and C322A (G )or double mutant C291A/C322A (H )incubated with 0–80␮M Zn 2ϩ(black ,0␮M ;red ,4␮M ;green ,10␮M ;blue ,20␮M ;cyan ,40␮M ;and magenta ,80␮M )in the absence of DTT.The assays were carried out at 37°C,and the samples were incubated in 50m M Tris-HCl buffer (pH 7.5)containing 100m M NaCl,5␮M heparin and 50␮M ThT.Low Micromolar Zinc Accelerates Tau Fibrillizationby guest on January 13, 2015/Downloaded from。

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