Environmental Pollution 112 (2001) 163±169 www.elsevier.com/locate/envpol Relationship between epiphytic lichens, trace elements and gaseous atmospheric pollutants H.F. van Dobben a,*, H.Th. Wolterbeek b, G.W.W. Wamelink a, C.J.F. Ter Braak c a Alterra Green World Research, PO Box 47, 6700 AA Wageningen, The Netherlands Interfaculty Reactor Institute, Delft University of Technology, Mekelweg 15, 2629 JB Delft, The Netherlands c Centre for Biometry Wageningen, CPRO-DLO, PO Box 16, 6700 AA Wageningen, The Netherlands b Received 26 February 1999; accepted 18 March 2000 ``Capsule'': Lichens were shown to be eective accumulator biomonitors for heavy metals in The Netherlands. Abstract A study was conducted to determine the joint eect of gaseous atmospheric pollutants and trace elements on epiphytic lichens. We used our data to test the hypothesis that lichens are generally insensitive to toxic eects of trace elements, and can therefore be used as accumulator organisms to estimate concentrations of these elements in the environment. In a ®eld study in The Netherlands the abundance of epiphytic lichen species was estimated, and their supporting bark was collected. Concentrations of a range of trace elements were determined in the bark, and concentrations of atmospheric trace gases were estimated at the sites of collection. Multivariate statistics were used to determine the relation between the abundance of the species and pollutant concentrations. Atmospheric SO2 and NO2 appeared to be the most important factors determining lichen biodiversity. Nearly all species were sensitive to these compounds. The eect of the other trace elements was very slight; only Sb had a signi®cantly negative eect on the abundance of a few species. It is concluded that lichens can safely be used as accumulator organisms in pollution studies, provided that concentration in lichen thalli re¯ect atmospheric concentrations. # 2001 Elsevier Science Ltd. All rights reserved. Keywords: Lichen; Bark; Trace element; Air pollution; Sensitivity; Multivariate statistics 1. Introduction Lichens are generally considered as useful organisms to monitor air quality. Numerous studies have been undertaken in which lichen biodiversity, or the presence/absence of indicator species, was used as a measure for air quality (Seaward, 1992). Information on the pollutants involved and their working mechanisms is scarce, however. Most authors implicitly (e.g. Barkman, 1958) or explicitly (e.g. De Wit, 1976) state SO2 as the main cause for the decline of lichens in polluted areas, but others claim an additional sensitivity to NO2 (Nash, 1976), O3 (Sigal and Nash, 1983), NH3 (Van Dobben and De Bakker, 1996), ¯uoride (Nash, 1971), heavy metals (Folkesson and Andersson-Bringmark, 1988) or air pollutants in general (Nylander, 1866; Herzig et al., 1989; Garty et al., 1993). * Corresponding author. Tel.: +31-317-477936; fax: +31-317424988. E-mail address: [email protected] (H.F. van Dobben). Besides indicating air quality by their presence or absence, lichens have also been used as accumulator organisms in studies on atmospheric trace element pollution (Lippo et al., 1995; Sloof, 1995; Loppi and Bargagli, 1996). In these studies the elemental concentrations in lichens are considered to re¯ect atmospheric concentration or deposition, irrespective of possible toxic eects. In fact an implicit hypothesis is made in this type of study, namely that trace elements do not have toxic eects on lichens (Purvis, 1996). If the elements under consideration would kill the monitoring organisms they would be absent in the most polluted spots, and estimated concentrations would become biased towards lower values. The aim of our study was to determine the joint eect of gaseous atmospheric pollutants and trace elements on epiphytic lichens. A second aim was to test the implicit hypothesis that trace elements do not have toxic eects on lichens. We recorded epiphytic lichen vegetation, bark chemical composition and atmospheric concentrations of SO2, NO2 and NH3 at 123 sites along a 0269-7491/01/$ - see front matter # 2001 Elsevier Science Ltd. All rights reserved. PII: S0269-7491(00)00121-4 164 H.F. van Dobben et al. / Environmental Pollution 112 (2001) 163±169 number of east±west and north±south transects through The Netherlands. We assumed that atmospheric concentrations of trace elements are re¯ected by their concentrations in bark (cf. Wolterbeek et al., 1996). A multivariate statistical approach was used to determine the joint eect of atmospheric chemistry and bark chemistry on the composition of the lichen vegetation. The analysis focused on determining the eect of trace element in bark after accounting for the eects of gaseous pollutants and a number of ecologically relevant variables (tree species, tree diameter, distance to the coast). 2. Materials and methods 2.1. Sampling Table 1 Minimal, mean and maximal concentrations in bark found in our data, in ppm on a dry weight basisa Element Min. Mean Max. As Br Ca Cd Ce Co Cr Cs Fe Hg K La Na Ni Sb Sc Se Sm Th Zn NH4 NO3 SO4 pH 1.98E-01 6.10E+00 7.94E+03 2.25E-01 1.37E+00 2.35E-02 5.50E+00 6.46E-02 1.40E+01 5.13E-02 2.81E+02 6.62E-01 3.17E+02 2.91E+00 9.00E-01 1.17E-01 2.45E-01 7.43E-02 1.55E-01 5.91E+01 3.77E+00 2.66E-01 6.05E+00 3.85E+00 1.14E+00 1.98E+01 1.62E+04 2.58E+00 4.32E+00 1.34E+00 1.32E+01 2.70E-01 1.88E+03 2.16E-01 1.34E+03 2.05E+00 9.34E+02 1.03E+01 2.15E+00 4.11E-01 6.24E-01 2.77E-01 3.81E-01 1.97E+02 1.64E+01 1.28E+00 2.32E+01 4.66E+00 4.60E+00 6.76E+01 4.67E+04 1.04E+01 1.61E+01 4.28E+00 4.83E+01 1.04E+00 6.94E+03 6.35E+00 3.31E+03 6.99E+00 2.90E+03 3.37E+01 2.69E+01 1.30E+00 1.68E+00 3.65E+00 1.37E+00 7.81E+02 5.43E+01 7.52E+00 9.23E+01 5.40E+00 The sampling stations consisted of rows of 10 trees, distributed along six transects through The Netherlands (see Wolterbeek et al., 1996, for a map). There were 123 sampling stations, on the following tree species: Quercus robur L. (65 stations), Populuscanadensis Moench (43 stations), Salix alba L. (®ve stations) and Ulmushollandica Miller (10 stations). Sampling near farms, villages and industrial sites was avoided. The lichen vegetation of the sampled trees mostly belonged to the alliance Xanthorion parietinae Ochsn. 1928. Sampling was carried out in the period August±October 1990 (for details, see Van Dobben, 1993). The abundance of all lichen species present on the trunks of the trees from the base up to a height of 2 m was estimated and scored on a six-point scale (Van Dobben, 1993). Most species were identi®ed in the ®eld but individuals that were not readily recognisable were sampled for later identi®cation. Nomenclature follows Aptroot et al. (1999). Bark ¯akes of ca. 5 mm thickness were cut from the three middle trees of each station at a height of ca. 1.5 m. These samples were air-dried and ground to a grain size of <1 mm by sieve-milling. Data were obtained from the Dutch Air Quality Monitoring Network (Anonymous, 1990). SO2 and NO2 were estimated as means of hourly measured concentrations (SO2 April±September 1989, NO2 June 1989±May 1990) at monitoring stations, followed by interpolation (Van Egmond et al., 1978) of the concentrations at the sample points. Mean NH3 concentrations were estimated on a 55-km2 grid basis using the 1988 emission data and the atmospheric transport and deposition model TREND (Asman and Van Jaarsveld, 1990). 2.2. Bark analysis 2.4. Statistical analysis Analytical procedures are described in detail by Wolterbeek et al. (1996). Concentrations of NO3, NH4 and SO4 were determined in aqueous extracts using colorimetric methods. pH was measured in the same extract. Lead was determined by graphite-furnace atomic absorption spectrometry (AAS) after digestion in HNO3/HClO4/HF. A large number of other elements (As, Br, Ca, Cd, Ce, Co, Cr, Cs, Fe, Hg, K, La, Na, Ni, Sb, Sc, Se, Sm, Th and Zn) were determined by Instrumental Neutron Activation Analysis (Bode and De Bruin, 1990). All these elements will be further denoted as trace elements. The mean, minimal and maximal contents per element are summarized in Table 1. Redundancy analysis (RDA; Ter Braak, 1994) was used to determine the relation between atmospheric chemistry, bark chemistry and the composition of the lichen vegetation. The analysis was carried out using the program Canoco 4.0 (Ter Braak and Smilauer, 1998). All bark chemical variables except pH were expressed in ppm on a dry weight basis and logarithmized. Air quality variables were expressed in mg mÿ3 and not transformed. The other variables considered were: (1) tree species, determined as the contrast oak versus other tree species (cf. Wolterbeek et al., 1996), and entered as a dummy variable (1=oak, 0=other); (2) tree diameter (DBH in cm, untransformed); and (3) distance to the coast (in km, a Means are geometric means except pH. 2.3. Air pollution H.F. van Dobben et al. / Environmental Pollution 112 (2001) 163±169 untransformed, cf. Van Dobben and De Bakker, 1996). Interaction terms were not considered. The importance of the explanatory variables was determined by stepwise selection. In each step the `extra ®t' was determined for each variable, i.e. the increase in regression sum of squares over all species when adding a variable to the regression model. The variable with the largest extra ®t was then included, and the process was repeated until no variables remained that could signi®cantly improve the ®t. The statistical signi®cance of the eect of including a variable was determined by means of a Monte Carlo permutation test (for details, see Ter Braak and Smilauer, 1998). The results of the multivariate analysis were visualised by means of biplots. A biplot attempts to optimally represent the joint eect of the environmental variables on all species in a single plane (Ter Braak, 1995). In our biplots, species are indicated by their abbreviated names and environmental variables by arrows. Arrows can also be drawn from the origin to each species' point located in the centre of its name (actually these arrows were not drawn to avoid overcrowding of the plot). The cosine of the angle between each pair of arrows (species±species, species±environment, or environment±environment) is a measure for the correlation between that pair of variables (sharp angles indicate positive correlations, obtuse angles indicate negative correlations). In general, species and environmental variables with the longest arrows are best represented in the biplot. Further detail on the interpretation of biplots is given by Ter Braak (1995). In this study the results of a single analysis are presented in two biplots. In a ®rst biplot the eect is shown of all environmental variables that signi®cantly contribute to the ®t of the model. This biplot appeared to be strongly dominated by the eect of a few variables that explain about half of the variance explained by the full model. In this biplot the eect of the less important variables (that still signi®cantly contribute to the ®t of the model) is blurred by these few variables. Therefore, a second biplot was drawn after accounting for the eect of the most dominant variables (technically this was achieved by declaring these variables as covariables in CANOCO). Finally, the eect of the trace elements that most strongly aected the species (as shown by the multivariate analysis) was analysed in detail by (univariate) logistic regression of the presence/absence of the most common species on the trace element concentrations, after accounting for the eect of all other relevant variables. The logistic regression was carried out by the program GENSTAT 5.3 (Payne et al., 1993). 3. Results In total, 72 species were found in the 123 sampling stations. The mean number of species per 165 sampling station was 18. The result of the stepwise selection in RDA is given in Table 2. The full model (i.e. containing all variables that signi®cantly contribute to the ®t) explains ca. 40% variance, about half of which is explained by the air quality variables SO2 and NO2. Tree species and bark pH each explain ca. 4% variance, and small additional percentages variance are explained by tree DBH, atmospheric NH3 and the bark chemical factors Br, Sb, As, Ca, and NH4. Bark concentrations of SO4, NO3 and the remaining trace elements included in the analysis did not have a signi®cant eect on the abundance of the lichen species, and there was no signi®cant eect of distance to the coast. Fig. 1 is the biplot representing the eect of all variables in the model of Table 2. The species shown are those for which this model explained >10% of the variance in their abundance. The biplot clearly shows the dominant eect of SO2 and NO2 (mainly represented along the horizontal axis). All species except Lecanora conizaeoides Nyl. ex Cromb. are negatively correlated with these variables which therefore strongly aect general species richness. A second important source of variation is represented along the vertical axis, which is mainly determined by atmospheric NH3, bark pH and bark Ca on the lower side, and oak which works in the opposite direction. The so-called `nitrophytic' species (e.g. Physcia spp. and Xanthoria spp., cf. Van Dobben and Ter Braak, 1999) have a low position relative to this axis, whereas the `acidophytic' species (e.g. Hypogymnia physodes (L.) Nyl., Evernia prunastri (L.) Ach.) have a high position. Table 2 Result of stepwise selection of variables using redundancy analysis (RDA)a Variable Extra ®t Cumulative ®t Signi®cance Atm. SO2 Atm. NO2 Bark pH Oak Bark Br Bark Sb Bark As Bark Ca Bark NH4 Atm. NH3 Tree DBH 15.7 5.4 4.1 4.5 2.2 1.7 1.7 1.6 1.3 1.0 0.9 15.7 21.1 25.3 29.7 32.0 33.7 35.4 37.0 38.3 39.3 40.2 *** *** *** *** *** *** *** ** ** * * a Variables are given in the order of inclusion. The extra and cumulative ®t are given as percentages relative to the total sum of squares over all species (comparable to the percentage explained variance in univariate regression). Number of observations: 123; total number of species: 72. Signi®cance was determined by Monte Carlo permutation using 999 random permutations. Dierences in the cumulative ®t and the sum of the extra ®t and the cumulative ®t in the preceding row are due to rounding errors. *0.01<P40.05. **0.001<P40.01. ***P40.001 166 H.F. van Dobben et al. / Environmental Pollution 112 (2001) 163±169 Fig. 1. Correlation biplot showing the relations between species (names) and environmental variables (arrows), based on the model in Table 2. See text for further explanation. Eigenvalues: 0.216, 0.093 and 0.029 for the ®rst (horizontal), second (vertical) and third axis (not shown). Only species are shown for which the model explains >10% of its variance. Explanation of species names: Art.rad, Arthonia radiata (Pers.) Ach.; Buel.gris, Buellia griseovirens (Turner & Borrer ex Sm.) Almb.; Cal.lut, Caloplaca luteoalba (Turner) Th. Fr.; Can.aur, Candelariella aurella (Hom.) Zahlbr.; Can.ref, Candelariella re¯exa (Nyl.) Lettau; Can.vit, Candelariella vitellina (Hom.) MuÈll. Arg.; Can.xan, Candelariella xanthostigma (Ach.) Lettau; Cet.chl, Cetraria chlorophylla (Willd.) Vainio; Chaen.f, Chaenotheca ferruginea (Turner & Borrer) Mig.; Clad.sp, Cladonia species; Cli.grif, Cliostomum grithii (Sm.) Coppins; Dim.pin, Dimerella pineti (Ach.) Vezda; Ever.pru, Evernia prunastri (L.) Ach.; Hypoc.sc, Hypocenomyce scalaris (Ach.) M. Choisy; Hyp.phy, Hypogymnia physodes (L.) Nyl.; Hyp.tub, Hypogymnia tubulosa (Schaerer) Havaas; L.carp, Lecanora carpinea (L.) Vainio; L.chlar, Lecanora chlarotera Nyl.; L.coniz, Lecanora conizaeoides Nyl. ex Crombie; L.disp, Lecanora dispersa (Pers.) Sommerf.; L.expal, Lecanora expallens Ach.; L.pulic, Lecanora pulicaris (Pers.) Ach.; L.symm, Lecanora symmicta (Ach.) Ach.; Lec.eleo, Lecidella elaeochroma (Ach.) M. Choisy; Lepr.inc, Lepraria incana (L.) Ach.; Op.niveo, Opegrapha niveoatra (Borrer) J.R. Laundon; P.acet, Parmelia acetabulum (Necker) Duby; P.exasp, Parmelia exasperata De Not.; P.lacin, Parmelia laciniatula (Flagey ex H. Olivier) Zahlbr.; P.revol, Parmelia revoluta FloÈrke; P.saxat, Parmelia saxatilis (L.) Ach.; P.subau, Parmelia subaurifera Nyl.; P.subru, Parmelia subrudecta Nyl.; P.sulc, Parmelia sulcata Taylor; Pert.alb, Pertusaria albescens (Hudson) M. Choisy & Werner; Pert.ama, Pertusaria amara (Ach.) Nyl.; Pert.coc, Pertusaria coccodes (Ach.) Nyl.; Ph.orbic, Phaeophyscia orbicularis (Necker) Moberg; Phl.arg, Phlyctis argena (Sprengel) Flotow; Ph.adsc, Physcia adscendens (Fr.) H. Olivier; Ph.caes, Physcia caesia (Hom.) FuÈrnrohr; Ph.stel, Physcia stellaris (L.) Nyl.; Ph.tene, Physcia tenella (Scop.) DC.; Ph.ente, Physconia enteroxantha (Nyl.) Poelt; Ph.gris, Physconia grisea (Lam.) Poelt; Ps.furf, Pseudevernia furfuracea (L.) Zopf; Pyr.que, Pyrrhospora quernea (Dickson) KoÈrber; R.farin, Ramalina farinacea (L.) Ach.; R.fast, Ramalina fastigiata (Pers.) Ach.; X.cand, Xanthoria candelaria (L.) Th. Fr.; X.par, Xanthoria parietina (L.) Th. Fr.; X.polyc, Xanthoria polycarpa (Hom.) Th. Fr. ex Rieber. The general relation between the occurrence of epiphytic lichens and environmental conditions as shown by this biplot is very similar to the relation reported by Van Dobben and De Bakker (1996) on the basis of an independent dataset. There are two main directions of variation: (1) species poor versus species rich, represented along the horizontal axis and mainly determined by the presence of the atmospheric pollutants SO2 and NO2; and (2) nitrophyte-dominated versus acidophytedominated, represented along the vertical axis and mainly determined by factors related to bark pH. Fig. 1 shows that the abundance of the nitrophytic species is positively correlated with bark pH and Ca concentration, and with atmospheric ammonia (which alkalises bark, cf. Van Dobben and De Bakker, 1996), and negatively correlated with oak (which has a naturally acid bark). For the acidophytes these relations are viceversa. The biplot indicates that Br concentration is positively related to species richness, and that the eect of Ca is similar to the eect of pH. It does not, however, yield clear indications on the eects of the two other trace elements included (As and Sb). The second biplot (Fig. 2) is based on the same model but with the eect of SO2 and NO2 accounted for. In this biplot species are shown for which the model (after adjusting for the eects of SO2 and NO2) explained >3% of their variance. In this plot pH has become the variable with the most important eect (mainly represented along the horizontal axis), together with Ca concentration in bark, and atmospheric NH3. The H.F. van Dobben et al. / Environmental Pollution 112 (2001) 163±169 167 Fig. 2. Correlation biplot showing the relations between species (names) and environmental variables (arrows), based on the model in Table 2 after accounting for the eects of SO2 and NO2. Eigenvalues: 0.100, 0.026 and 0.020 for the ®rst (horizontal), second (vertical) and third axis (not shown). Only species are shown for which the model explains >3% of its variance. See Fig. 1 for an explanation of the species names. horizontal axis now separates the nitrophytic species from the acidophytic ones, like the vertical axis in Fig. 1. The vertical axis is now mainly determined by tree DBH and Br concentration. Species that preferably occur on mature trees tend to have positions at the top of Fig. 2 (e.g. Parmelia acetabulum (Necker) Duby, Ramalina fastigiata (Pers.) Ach.), whereas pioneer species tend to be at the base of the plot (e.g. Xanthoria polycarpa (Hom.) Th. Fr. ex Rieber, Lecanora symmicta (Ach.) Ach.). In this plot the eect of Sb concentration seems to be comparable to the eect of low pH because of its high score on the horizontal axis (i.e. its arrow pointing in a direction opposite to the `pH' arrow). However, As has a very short arrow and its eect is therefore poorly represented in the plot. The results of the univariate logistic regression are shown in Table 3. Out the 35 species with more than 10 occurrences, six are signi®cantly (P40.05) correlated with the Sb concentration (®ve negatively, one positively). None of the species is signi®cantly negatively correlated with the As concentration, and only one is signi®cantly positively correlated with this element. The signi®cantly positive correlations with As and Sb are found for the same species (L. conizaeoides), which is also the only species whose occurrence is positively correlated with the gaseous pollutants SO2 and NO2. This species therefore seems to be truly multi-resistant. In contrast, the species that appear to be most sensitive to Sb (Xanthoria parietina (L.) Th.Fr. and Physconia grisea (Lam.) Poelt) do not have extreme sensitivities to either SO2 or NO2 (cf. Van Dobben and Ter Braak, 1999). 4. Discussion Our results clearly show the order of importance of the factors determining epiphytic vegetation on wayside trees in The Netherlands. Most important are the toxic atmospheric pollutants SO2 and NO2. Nearly all species decrease with increasing concentrations of these compounds, which therefore strongly negatively aect species diversity. This phenomenon is the basis of a large number of bioindicator studies using lichens (e.g. Barkman, 1958; Skye, 1968; LeBlanc and De Sloover, 1970; De Wit, 1976; Anonymous, 1995; Van Dobben and Ter Braak, 1999). Second in the order of importance are the ecological factors that show a natural variation, such as bark pH, tree species and tree DBH. Rather than determining general species diversity, these factors determine the species composition of the vegetation. In the third place are the trace elements. Most of the elements tested in this study did not have a signi®cant eect, with the exception of Br, Ca, Sb and As. Of these four, Ca and Br probably do not have toxic aects, and can be considered as `normal' ecological factors with a natural variation. 168 H.F. van Dobben et al. / Environmental Pollution 112 (2001) 163±169 Table 3 Sign and signi®cance of the regression coecients for the terms As and Sb of the logistic regression equation with modela Species n As Sb Lecanora carpinea (L.) Vainio Lecanora conizaeoides Nyl. ex Cromb. Lecidella elaeochroma (Ach.) Choisy Phaeophyscia orbicularis (Necker) Moberg Physconia grisea (Lam.) Poelt Xanthoria parietina (L.) Th.Fr. 43 63 73 52 14 89 0 +1 0 0 0 0 ÿ1 +1 ÿ1 ÿ2 ÿ1 ÿ2 a SO 2+NO 2+NH 3 +oak+DBH+Ca+Br+NH4 +pH+[As or Sb], with: SO2, NO2, NH3: concentrations of SO2, NO2, NH3 in air, in mg mÿ3; oak; dummy variable; 1=oak, 0=other tree; DBH, tree diameter at 1.50 m above ground level, in cm; As, Sb, Ca, Br, NH4, logarithmised concentrations in bark of As, Sb, Ca, Br, NH4, in ppm; pH, bark pH. The sign of each entry is the sign of the regression coecient and its magnitude denotes signi®cance determined on the basis of t-values: 2=0.001<P40.01; 1=0.01<P40.05; 0=P>0.05. Only species are given with >10 occurences and a signi®cant (P40.05) eect of at least one of the elements As or Sb. Number of observations: 123; total number of species: 72; number of species with >10 occurrences: 35. Ca is positively correlated with bark pH (r=0.34), and both have a very similar eect on the lichen vegetation (Fig. 1). Apparently bark pH is to a certain degree in¯uenced by the presence of Ca-containing buffer substances, which most probably originate from calcareous soil dust. Br is strongly negatively correlated with distance to the coast (r=ÿ0.61). This element is present in seawater in relatively high amounts (Weast et al., 1987), and probably has to be considered as just an indicator for oceanic in¯uence. It is therefore uncertain whether there is a direct in¯uence of Br. Previous studies have shown a general decrease in species diversity at greater distances from the coast (Van Dobben and De Bakker, 1996). In the present study there was no signi®cant in¯uence of distance to the coast, but a positive correlation between the occurrence of most lichen species and Br concentration (Fig. 1). Apparently the joint eect of the intercorrelated variables Br and distance to the coast is best explained by the former one. Their joint eect may be interpreted as either a direct eect of sea-spray ions (i.e. Br or correlated elements), or as the result of a climatic gradient with Br as an indicator for oceanic conditions. A climatic eect with increasing species diversity in more oceanic conditions was hypothesized by Van Dobben and De Bakker (1996). The eects of As and Sb probably come about though direct toxicity, as these elements are known to be toxic to numerous organisms (Gebel, 1997). However, the limited eect of the trace elements considered in this study indicates that there is only a slight risk that lichens are killed by extreme concentrations. Sensitivity could only be shown for a limited number of species, and to a limited number of elements. We therefore conclude that epiphytic lichens can safely be used as accumulator organisms in pollution studies, provided that concentration in lichen thalli do re¯ect atmospheric concentrations. This conclusion is supported by studies in which extreme concentrations (up to several per cents on a dry weight basis) of potentially toxic elements have been recorded in apparently healthy lichen thalli (e.g. Lambinon et al., 1964; Shimwell and Laurie, 1972; Brown and Beckett, 1984; Purvis, 1984), or where lichen communities with a high biodiversity are reported from substrates with high concentrations of potentially toxic metal ions (Purvis and Halls, 1996). Another conclusion is that species sensitive to one element are not automatically sensitive to the others. A comparable conclusion was drawn in an earlier study on the eect of atmospheric trace gases (Van Dobben and Ter Braak, 1999). Although in that study many species were found to signi®cantly respond to any of the gaseous pollutants SO2, NO2 and NH3, only a few signi®cantly responded to all of them, and there were no two species that showed the same type of response (increase or decrease) to all three pollutants. Apparently, lichens in general are not suitable indicators for the general level of pollution as has sometimes been hypothesized (Section 1). Most obvious is their sensitivity to SO2, and in some cases this compound may in itself be indicators for the general level of pollution (Cislaghi and Nimis, 1997). Our conclusions are at variance with those of Herzig et al. (1989), who claim a species-inspeci®c sensitivity of lichens to both trace metals, gaseous pollutants and dust. However, among the trace metals studied by this group (Pb, Cu, Zn, Cd), only Cd substantially contributed to the explained variance in a regression model of lichen species number against pollutant concentrations. Unfortunately, standard deviations of individual regression coecients are not given in this study, and therefore it is not possible to determine whether these correlations represent a real eect or are caused by a correlation with SO2. There seems to be one exception to the general rule of species-speci®c sensitivity, namely L. conizaeoides. This species has apparently adapted itself completely to the industrial environment by developing resistance to both toxic trace gases and trace metals. The resistance of this species to SO2 has also been shown experimentally (Bates et al., 1996). 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