ORIGINAL RESEARCH article
Sec. Microbiological Chemistry and Geomicrobiology
Volume 3 - 2012 | https://doi.org/10.3389/fmicb.2012.00041
Characterization of lead–phytochelatin complexes by nano-electrospray ionization mass spectrometry
- 1 Department of Environmental Toxicology, Eawag, Swiss Federal Institute of Aquatic Science and Technology, Dübendorf, Switzerland
- 2 Department of Environmental Systems Science, ETH Zürich, Institute of Biogeochemistry and Pollutant Dynamics, Zürich, Switzerland
The role of phytochelatins (PCn, metal-binding oligopeptides with the general structure (γGlu-Cys)n-Gly (n = 2–11) in metal detoxification is assumed to be based on immobilization of metals, which prevents binding of metals to important biomolecules. Although induction of phytochelatin synthesis has often been observed in algae upon exposure to metals, direct evidence for binding of the inducing metal to phytochelatins is scarce. In this study, a nano-electrospray ionization mass spectrometry (nano-ESI-MS) method is developed for identification and characterization of Pb(II)–PCn and Zn(II)–PCn complexes. Complexes of Pb(II) with standard PCn (n = 2–4; 0.25 mM Pb(II) and 0.5 mM PCn) were examined by nano-ESI-MS with respect to their stoichiometry. Pb–PCn mass spectra indicated the presence of the [M + H]+ peak of PCn and complexes with various stoichiometries. Analysis of Pb–PC2 allowed the identification of four different complexes observed at m/z 746.10, 952.06, 1285.24, and 1491.20, corresponding to [Pb–PC2]+, [Pb2–PC2]+, [Pb–(PC2)2]+, and [Pb2–(PC2)2]+. Their m/z indicated coordination of Pb(II) by PC2 through the thiol groups of PC cysteine and possibly carboxylic groups. For each of the standard PC3 and PC4, two different complexes were observed, corresponding to Pb–PC3, Pb2–PC3, Pb–PC4, and Pb2–PC4. The measured isotopic patterns were for all complexes identical to the theoretical isotopic patterns. Addition of Zn(II) (0.125–5 mM) to previously formed Pb–PC2 complexes showed the appearance of the [Zn–PC2]+ complexes at m/z 602.05 and the decrease of the [Pb–PC2]+ peak. These findings corroborate the postulated Pb–PC complexes from a previous study using size exclusion chromatography of PC extracted from algae, as well as the concurrent formation of Pb–, Zn–, and Cu–PC complexes in algae.
Phytochelatins (PCs) are known to be induced in response to exposure to various metals in plants (Rauser, 1995; Zenk, 1996) and algae (Gekeler et al., 1988; Ahner et al., 1995; Le Faucheur et al., 2005; Scheidegger et al., 2011a). These metal-binding oligopeptides with the general structure (γ-Glu-Cys)n-Gly (n = 2–11) are assumed to bind metals through thiolate coordination and are involved in metal homeostasis and detoxification. The role of PCs in metal detoxification likely results from immobilization of metals, preventing non-specific binding to important biomolecules, followed by the transport of the Me–PC complexes into the vacuole of the algal cell, or its excretion. In our previous studies, induction of phytochelatins by exposure of Chlamydomonas reinhardtii to Pb(II) has been observed (Scheidegger et al., 2011a). Binding of Pb(II) to phytochelatins has been postulated based on separation of metal complexes from C. reinhardtii by size exclusion chromatography (SEC; Scheidegger et al., 2011b). However, direct evidence for binding of the inducing metal to phytochelatins is scarce. It is therefore of interest to attempt to directly characterize metal–phytochelatin complexes.
Several analytical methods such as chromatographic separation (gel filtration or HPLC) coupled with UV detection, flame atomic absorption spectrometry (AAS), radio-active labeling, differential pulse polarography, and inductively coupled plasma mass spectrometry (ICP-MS) have been used to analyze PCn and metal–phytochelatin complexes (Me–PC; Grill et al., 1985; Maitani et al., 1996; Leopold and Günther, 1997; Leopold et al., 1999; Vacchina et al., 1999, 2000; Schmoger et al., 2000; Scarano and Morelli, 2002; Cruz et al., 2005; Kobayashi and Yoshimura, 2006). These methods, however, do not provide exact molecular weight, stoichiometry, or composition of Me–PCn complexes. In most in vivo studies focusing on Me–PC complex characterization, Me–PC complexes were isolated by gel filtration and the resulting eluate fractions were further analyzed for PC and metal content. PC detection often involves acidification and derivatization, which lead to dissociation of the Me–PC complexes, followed by HPLC analysis. Based on the detected molecular weight range obtained from gel filtration and the PC oligomers detected by HPLC, assumptions on stoichiometry and composition of the Me–PC complexes can be made; however, unambiguous characterization of Me–PC complexes regarding stoichiometry and composition is not possible with these methods.
A technique to precisely detect and characterize the Me–PCn complexes is thus required. Several studies reported identification of Cd–PC, Zn–PC, and As(III)–PC complexes using electrospray ionization mass spectrometry (ESI-MS; Yen et al., 1999; Raab et al., 2005; Navaza et al., 2006; Chekmeneva et al., 2007; Chen et al., 2007; Bluemlein et al., 2008, 2009), but analysis of Me–PC complexes formed with lead has not been reported.
In our previous study, induction of PC2–PC4 synthesis by Pb(II) was observed in the green alga C. reinhardtii (Scheidegger et al., 2011a). Furthermore, formation of PCn complexes with Cu, Zn, and Pb, and possible stoichiometric compositions of Pb–PC complexes were postulated based on the molecular weight obtained from SEC (Scheidegger et al., 2011b). Therefore, the aim of the present study is to develop an ESI-MS method to identify and characterize Me–PCn complexes formed with Pb and to examine the competition with Cu and Zn. Sample composition and ESI-MS conditions to analyze Pb complexes with standard phytochelatins (n = 2–4) are optimized. The stoichiometry of the Pb–PC2–4 complexes is derived.
Materials and Methods
Pb(NO3)2, CuSO4, and ZnSO4 salts, ammonium acetate (NH4CH3COO), ammonium carbonate ((NH4)2CO3; pH 7), polylysine, and 3-morpholinopropanesulfonic acid (MOPS) used in this study were analytical grade and obtained from Sigma-Aldrich (St. Louis, MO, USA). Phytochelatin standards (PC2, PC3, and PC4) were obtained from Invitrogen (San Diego, CA, USA). Formic acid was a suprapure chemical obtained from Merck (Darmstadt, Germany). Ultrafree-MC centrifugal filters (0.45 μm cut-off) were ordered from Millipore AG (Zug, Switzerland).
In preliminary experiments the solvent mixture for the analysis of Pb–PC complexes was optimized. The following sample composition resulted in the highest signal intensities in nano-electrospray ionization mass spectrometry (nano-ESI-MS) analysis. The ratio of PCn to Pb was in the range observed in algal cells (Scheidegger et al., 2011a,b). PCn and Pb were mixed, resulting in final concentrations of 0.5 mM PCn and 0.25 mM Pb(NO3)2 in 100 mM NH4CH3COO and 50 mM (NH4)2CO3. Complex formation was allowed for 15 min at room temperature. Prior to sample analysis 0.1% formic acid was added (pH 6), followed by sample filtration using an Ultrafree-MC centrifugal filter device with a 0.45-μm cut-off.
For competition experiments between Cu or Zn and Pb, standard Pb–PC2 complexes were prepared as described and complex formation was allowed, followed by the addition of the Cu or Zn solution. Cu and Zn concentrations added to the Pb–PC2 complexes were 0.125, 0.25, 0.5, and 5 mM. Acidification was done by addition of 0.1% formic acid. The ratios of Cu and Zn to Pb in the competition experiments were in the range Cu (or Zn): Pb = 0.5–20, and would thus simulate a similar or higher concentration of Cu and Zn than Pb, which may be representative for algal cells.
Mass spectra were acquired and analyzed using the software Xcalibur V2.0.7 (Thermo Fisher Scientific, San Jose, CA, USA). The isotopic distributions for the positively charged molecular ions of Me–PC complexes were generated with the spectrum simulation software integrated in Xcalibur.
Nano-Electrospray Ionization Mass Spectrometry Analysis of ME–PC Complexes
Solvent mixture optimization for nano-ESI-MS analysis of Pb–PCn (n = 2–4) were carried out on a API4000 triple quadrupole mass spectrometer (Applied Biosystems, Rotkreuz, Switzerland) with attached nanospray source (Sciex, NanoSpray® III Source, Zug, Switzerland).
Final analysis of Pb–PCn complexes was carried out on a LTQ Orbitrap XL mass spectrometer (Thermo Fisher Scientific, San Jose, CA, USA). Capillaries for nano-ESI were prepared from coated fused silica tubing (TSP-FS; o.d. 375 μm; i.d. 100 μm; BGB, USA) using a needle puller (Model P-2000, Sutter Instruments Co., Novato, CA, USA). The samples were then analyzed by direct infusion. Between each measurement the syringe was cleaned with MeOH and H2O.
Prior to analysis of Pb–PCn complexes, the instrument performance and calibration was checked with polylysine. The flow rate for standard Pb–PCn complex analysis was 1–3 μL/min. The optimal settings of the mass spectrometer operated in positive electrospray ionization mode were: needle voltage, 1.5 kV; capillary temperature, 200°C; capillary voltage, 11 V; tube lens, 130 V; resolution, 30,000; max. injection time, 100,000 ms; automatic gain control FT, 1 × 106. The spectra were acquired from m/z 300 to 1,600 for Pb–PC2 and from m/z 300 to 2,000 for Pb–PC3 and Pb–PC4. Mass accuracy of the measurement was better than 2 ppm for lower mass ions (<1,000 Da) of signal intensities >10%.
Analysis of Standard Pb–PCn Complexes
The full-scan mass spectrum of the Pb–PC2 complexes (Figure 1) was dominated by the singly charged [M + H]+ ion of PC2 at m/z 540.1427, which matches the elemental composition of protonated PC2 (C18H30N5O10S2) of 540.1429 with an error <0.2 ppm and shows the expected isotopic distribution with a mass assignment <0.5 ppm for signals higher than 10% relative abundance (data not shown). In addition to the protonated molecular ion peaks at m/z 536.3 and 538.4 were also present (data not shown), probably corresponding to oxidized PC2. A singly charged PC2 dimer and its oxidation products could be seen at m/z 1079.2783, 1077.2632, and 1075.2474. The four peaks observed at m/z 746.1034, 952.0641, 1285.2379, and 1491.1964 correspond to the molecular weight of singly charged [Pb–PC2]+, [Pb2–PC2]+, [Pb–(PC2)2]+, and [Pb2–(PC2)2]+ complexes (Figure 1). Pb–PC2 and Pb2–PC2 were present in sufficient intensity to detect the Pb-specific isotopic pattern of both complexes. The measured isotopic pattern of [Pb–PC2]+ in the m/z range 740–752 is shown in Figure 2 (front). The relative intensity of the peaks at m/z 742.11, 744.10, 745.10, and 746.10 was observed in a ratio, which reflects the distribution of Pb isotopes (naturally occurring ratio: 204Pb 1.5; 206Pb 23.6; 207Pb 22.6; 208Pb 52.3%). The measured isotopic pattern matched the theoretical pattern (Figure 2, back), with a mass error of 0.7 ppm or better for signals higher than 10%. Similarly, the isotopic pattern observed for [Pb2–PC2]+ at m/z 944–958, including the isotopic pattern of two Pb ions, matched the simulated spectra (Figure 3), with a mass error of 1.1 ppm or less. The signal intensities of the complexes involving one or two Pb ions and two PC2 molecules [Pb1–2–(PC2)2] were too low for isotope pattern detection.
Figure 1. Nano-ESI-MS full-scan spectrum (m/z 300–1,600) of 0.5 mM PC2 (C18H29N5O10S2) and 0.25 mM Pb(NO3)2 in 100 mM NH4CH3COO, 50 mM (NH4)2CO3, and 0.1% HCOOH (pH 6). X = matrix ions.
Figure 2. Measured (front) and simulated spectrum (back) of the isotopic pattern of the [Pb–PC2]+ complex m/z 740–752. Isotopic distribution of Pb is identified in the peak distribution at m/z 742.11 (204Pb, 1.5%), 744.10 (206Pb, 23.6%), 745.10 (207Pb, 22.6%), and 746.10 (208Pb, 52.3%).
Figure 3. Measured (front) and simulated spectrum (back) of the isotopic pattern of the [Pb2–PC2]+ complex m/z 944–958. Isotopic distribution of two Pb (204Pb 1.5; 206Pb 23.6; 207Pb 22.6; 208Pb 52.3%) is identified in the peak distribution of the m/z 948.06–952.06.
Analysis of Pb–PC3 samples showed the [M + H]+ peak for PC3 at m/z 772.1946 matching the corresponding sum formula (C26H43N7O14S3; data not shown). Similar to PC2, a peak at [M + H-2]+ (m/z 770.1790), not present in the theoretical spectra, was present at high signal intensity. Two peaks at m/z 978.1559 and 1184.1151 corresponding to the molecular weight of singly charged [Pb–PC3]+ (mass error 0.3 ppm) and [Pb2–PC3]+ (mass error 1.2 ppm) were detected. The measured isotopic pattern and the theoretical spectra were almost identical for both detected complexes (Figures 4 and 5).
Figure 4. Measured (front) and simulated spectrum (back) of the isotopic pattern of the [Pb–PC3]+ complex m/z 972–984. Isotopic distribution of Pb (204Pb 1.5; 206Pb 23.6; 207Pb 22.6; 208Pb 52.3%) is identified in the peak distribution at m/z 974.15, 976.15, 977.15, and 978.16.
Figure 5. Measured (front) and simulated spectrum (back) of the isotopic pattern of the [Pb2–PC3]+ complex m/z 1,178–1,190. Isotopic distribution of two Pb (204Pb 1.5; 206Pb 23.6; 207Pb 22.6; 208Pb 52.3%) is identified in the peak distribution of the m/z 1180.11–1184.12.
Analysis of the Pb–PC4 spectra showed the [M + H]+ peak for PC4 at m/z 1004.2406, corresponding to C34H55N9O18S4. Comparison of the [M + H]+ peak at 1004.2406 for PC4 to the theoretical spectra shows an excellent match of the isotopic patterns except for the presence of the [M + H-2]+ peak (m/z 1002.2238) as observed for PC2 and PC3 and the [M + H-4]+ peak (m/z 1000.2084). Two peaks corresponding to the molecular weight of the PC4 complexes, [Pb–PC4]+ and [Pb2–PC4]+, were detected at m/z 1210.1986 (mass error 7.3 ppm) and 1416.1556 (mass error 8.8 ppm). The measured and theoretical isotopic patterns are shown in Figures 6 and 7. In addition, a peak at m/z 605.6035 was observed, matching the isotopic pattern of [Pb–PC4]2+ (data not shown).
Figure 6. Measured (front) and simulated spectrum (back) of the isotopic pattern of the [Pb–PC4]+ complex m/z 1,206–1,218. Isotopic distribution of Pb (204Pb 1.5; 206Pb 23.6; 207Pb 22.6; 208Pb 52.3%) is identified in the peak distribution at m/z 1208.20, 1209.20, and 1210.20.
Figure 7. Measured (front) and simulated spectrum (back) of the isotopic pattern of the [Pb2–PC4]+ complex m/z 1,410–1,422. Isotopic distribution of two Pb (204Pb 1.5; 206Pb 23.6; 207Pb 22.6; 208Pb 52.3%) is identified in the peak distribution of the m/z 1412.15–1416.16.
Competition between Cu or Zn and Pb for PC2 Binding
Addition of Zn to Pb–PC2 complexes resulted in the appearance of the [Zn–PC2]+ peak at m/z 602.0544 already at the lowest Zn concentration (Figure 8A). In addition, the Pb–PC2 peak was observed to decrease with increasing Zn concentration (Figure 8). Increasing metal concentration leads to a decrease of all PC signals and to an increase of the ratio between the [M + H]+ peak for PC2 at m/z 540.14 and the [M + H-2]+ peak at m/z 538.14.The isotopic pattern of [Zn–PC2]+ matched with the theoretical distribution of Zn (naturally occurring ratio: 64Zn 48.6; 66Zn 27.9; 67Zn 4.1; 68Zn 18.8; 70Zn 0.6%; Figure 9).
Figure 8. Nano-ESI-MS full-scan spectrum of competition experiments between Pb and Zn with increasing Zn concentrations from (A–C). The concentrations are (A) 0.125 mM Zn, (B) 0.25 mM Zn, and (C) 0.5 mM Zn. X = matrix ions.
Figure 9. Measured (front) and simulated spectrum (back) isotopic pattern at m/z 602–614. Isotopic pattern of Zn (64Zn 48.6; 66Zn 27.9; 67Zn 4.1; 68Zn 18.8; 70Zn 0.6%) and PC2 is shown at m/z 602.05–609.05.
At the highest Zn concentration (5 mM) and at all Cu concentrations no Zn–PC or Cu–PC complexes were detected (data not shown).
To test the applicability of nano-ESI-MS for the analysis of Me–PC complexes, complexes of Pb with standard PCn (n = 2–4) were analyzed. A method for nano-ESI-MS was developed to characterize in vitro formed Me–PC complexes which might also be used for characterization of in vivo Me–PCn complexes.
Considering that the mass spectra of the Pb–PCn complexes were dominated by the [M + H]+ peak of the corresponding PCn indicates that either not all PC was involved in complex formation, dissociation of Pb–PC complexes occurs during sample analysis, or that the complexes formed were neutral and therefore not visible in the nano-ESI-MS spectra. Furthermore, the relatively low pH 6, needed for optimal ionization, may lead to some complex dissociation.
The PCn seem to occur mainly in charge state 1+ with the conditions used, as no signal was detected that corresponds to the doubly charged ion. The isotopic pattern of analyzed PCn was completely resolved. For all PCn the isotopic distribution matched the theoretical spectra of the corresponding elemental composition and mass accuracy was high (<2 ppm for ions <1,000 Da and with relative intensities higher than 10%). The [M + H-2]+ peaks observed for PC2–PC4 as well as the [M + H-4]+ peak observed for PC4, indicate the formation of one or two intramolecular disulfide bonds between cysteine thiol groups within the PC. The formation of a disulfide bond results in a loss of two hydrogens and therefore a shift from [M + H]+ to [M + H-2]+, which was also observed in other studies (Yen et al., 1999; Navaza et al., 2006).
Analysis of Pb–PC complexes revealed the in vitro formation of Pb–PCn complexes with various stoichiometries and compositions. The m/z detected for the [Pb–PC2]+ complex allows two different covalent complexes, assuming Pb coordination through thiol groups of PC cysteine. Either Pb is coordinated by one thiol group whereas the other is present as reduced thiol group, or the Pb ion is coordinated by both thiol groups present in PC2. In the second case, additional protonation of the complex must occur to result in a singly charged complex detectable by nano-ESI-MS. For the [Pb2–PC2]+ complex the detected m/z corresponds to [PC2+ 2Pb-3]+, indicating a loss of three H+. This observation suggests that in addition to the two protons from the SH-groups, one proton is lost from a carboxylic group. Further studies would be required to examine whether the complex formation between one Pb and PC2 involves only thiol groups or Pb is coordinated by one thiol and one carboxylic group. Similarly, another study observed the loss of 2H+ and 4H+ for the binding of two Cd ions to standard PC5. Binding of a third Cd ion to PC5 was not accompanied by the loss of H+. The authors suggested the formation of complexes that involve two thiol coordinated cadmium ions and a Cd ion which is bound electrostatically to the Cd2–PC5 complex (Yen et al., 1999). To investigate whether the coordination of metals by PC is dependent on the metal and/or the chain length of PC needs to be further investigated.
From mass considerations four Pb–PC2, two Pb–PC3, and two Pb–PC4 complexes were identified. To prove that both Pb and PCn are contributing to the detected signals, the measured isotopic pattern was compared to the theoretical isotopic pattern. The isotopic patterns of the Pb–PC complexes are complex owing to the isotopic pattern of one or more Pb ions coupled to the PCs (naturally occurring ratio: 204Pb 1.5; 206Pb 23.6; 207Pb 22.6; 208Pb 52.3%). This very pronounced lead signature is indicative for the presence of Pb in the [Pb–PC2]+ complex at m/z 740–752. The isotopic pattern of [Pb2–PC2]+ is even more complex, since two Pb ions are present in the complex, but comparison of measured and theoretical isotopic pattern proves the presence of the two Pb ions (Figure 3). Formation of [Pb–PC2] and [Pb2–PC2] complexes was also observed using differential pulse polarography (Alberich et al., 2007). Similar observations were made for Pb–PC3 and Pb–PC4 complexes, showing a good match between measured and theoretical patterns and a loss of 2H+ for each additionally bound Pb ion. Surprisingly no complexes including three and four Pb ions were observed for PC3 and PC4. These results are also in agreement with the complexes observed using voltammetric methods (Alberich et al., 2008). In addition, accurate mass measurements confirmed the proposed elemental compositions.
The appearance of the [Zn–PC2]+ peak in the presence of Zn is indicative of complex formation between PC and Zn, which was confirmed by the isotopic pattern for Zn clearly visible in the zoom spectrum (Figure 9). This competition between Pb and Zn may be expected if their complex stability with PC2 is similar to the stability of their complexes with glutathione, for which somewhat higher stability constants for Pb than for Zn are reported (Martell and Smith, 1989). Binding of Zn by PC3 has been shown in a voltammetric study with multivariate curve resolution, and by PC4 using voltammetry and ESI-MS (Cruz et al., 2005; Chekmeneva et al., 2007). The expected increase of the [Zn–PC2]+ peak with increasing Zn concentration was not observed, maybe due to an increase of oxidized PC2, indicated by the increase of the ratio between m/z 538.14 and 540.14, leading to a loss of potential metal-binding sites. This could also explain the signal loss observed with increasing Zn concentration. In presence of Cu(II), phytochelatin oxidation may also explain why no Cu–PC complexes were detected. Similar observations were done in a study with Cd where a signal loss was observed at concentrations higher than 0.3 mM Cd (Yen et al., 1999).
In a previous study using SEC, the presence of PC complexes with Cu, Zn, and Pb was postulated upon analysis of PC from C. reinhardtii exposed to Pb (Scheidegger et al., 2011b). After extraction of the algal cells under native conditions to preserve the metal complexes, PC2 and PC3 complexes were detected in a molecular weight range between 700 and 5,300 Da. PC2 was mainly observed between 1,000 and 1,600 Da and complexes with Me1–2–(PC2)2 were suggested, with [Pb–(PC2)2]+ and [Pb2–(PC2)2]+ as the probable most abundant Pb species. The results obtained here are in qualitative agreement with this study, as the formation of [Pb–PC2]+, [Pb2–PC2]+, [Pb–(PC2)2]+, and [Pb2–(PC2)2]+ is shown. [Pb–PC2]+ and [Pb2–PC2]+ would appear in the SEC fraction 700–1,050 Da, where PC2 and Pb were also detected. The abundance distribution of these complexes obtained by ESI-MS appears to differ somewhat from the SEC results, but it must be taken into account that the ratio of PC-SH to Pb, as well as the pH were different in these two studies. Furthermore, it must be considered that nano-ESI-MS, albeit a soft ionization technique, may result in dissociation of complexes. The formation of the [Zn–PC2]+ complex after Zn addition also corroborates the results from SEC, which showed the presence of Zn and Cu, as well as Pb, in the PC containing fractions. These results also clearly indicate a possible competition of Zn and Pb for binding to phytochelatins. These findings support the hypothesis that upon induction of PCn by Pb in algae, the PCn may also be bound to other metals.
The application of nano-ESI-MS to examine Me–PC complexes in algae is challenged by practical issues related to the low intracellular concentration of the Me–PC complexes. Therefore, further research is needed to improve the sensitivity for Me–PC complexes by nano-ESI-MS, or respectively to improve sample preparation to obtain a sufficient amount of PCn from the algae. For example, considering the measured concentration of 30 attomol/cell PC2 in C. reinhardtii cells (Scheidegger et al., 2011a), about 1 L of algal suspension (with a cell density of 8.4 × 105 cell/mL) should be preconcentrated into a small volume (<1 mL) to obtain a sufficiently high PC2 concentration for ESI-MS measurements. In addition, differences between in vivo and in vitro formed Me–PC complexes should be further examined to investigate which factors are determining the distribution among the various complexes.
Conflict of Interest Statement
The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
We thank René Schönenberger for help in the laboratory work and the Swiss National Science Foundation for funding this project.
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Keywords: phytochelatin, mass spectrometry, nano-ESI-MS, lead, thiol
Citation: Scheidegger C, Suter MJ-F, Behra R and Sigg L (2012) Characterization of lead–phytochelatin complexes by nano-electrospray ionization mass spectrometry. Front. Microbio. 3:41. doi: 10.3389/fmicb.2012.00041
Received: 05 December 2011;
Accepted: 26 January 2012;
Published online: 13 February 2012.
Edited by:Martha Gledhill, University of Southampton, UK
Reviewed by:Jeffrey M. Dick, Curtin University of Technology, Australia
Claude Fortin, Institut National de la Recherche Scientifique, Canada
Copyright: © 2012 Scheidegger, Suter, Behra and Sigg. This is an open-access article distributed under the terms of the Creative Commons Attribution Non Commercial License, which permits non-commercial use, distribution, and reproduction in other forums, provided the original authors and source are credited.
*Correspondence: Marc J.-F. Suter, Department of Environmental Toxicology, Eawag, Swiss Federal Institute of Aquatic Science and Technology, PO Box 611, CH-8600 Dübendorf, Switzerland. e-mail: email@example.com