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Volume 2012 (2012), Article ID 521582, 7 pages
Selected Metals in Various Fractions of Soil and Fungi in a Swedish Forest
1Department of Soil and Environment, Swedish University of Agricultural Sciences, P.O. Box 7014, 750 07 Uppsala, Sweden
2Department of Ecology, Zhytomyr State Technological University, 103 Cherniakhovsky Street, 10005 Zhytomyr, Ukraine
Received 14 April 2012; Accepted 11 May 2012
Academic Editors: S. Loppi and P. Rautio
Copyright © 2012 Mykhailo Vinichuk.
The patterns of uptake and distribution of Co, Ni, Cu, Zn, Cd, and Pb in the soil-mycelium-sporocarps compartments in various transfer steps are presented. I attempted to find out whether there is a difference between the uptake of metals from soil to fungi (mycelium/soil ratio) and transport within fungal thalli (sporocarps/mycelium ratio). The concentration of Cu, Zn, and Cd increased in the order bulk soil < soil-root interface (or rhizosphere) < fungal mycelium < fungal sporocarps. The concentration of Co, Ni, and Pb decreased in the order bulk soil (or rhizosphere) < fungal mycelium < soil-root interface < fungal sporocarps. The uptake of Cu, Zn, and Cd during the entire transfer process in natural conditions between soil and sporocarps occurred against a concentration gradient. Mycorrhizal fungi (mycelium and sporocarps) only absorbed Co, Ni, and Pb but did not accumulate these elements in their thalli. Metal accumulation within fungal mycelium biomass in the top forest soil layer (0–5 cm) may account for about 5% of the total amount of Co, 4% Ni, 7% Cu, 8% Zn, 24% Cd, and 3% Pb.
Ectomycorrhizal fungi are major components of fungal community in the soils of most boreal and temperate forests. The mycelium of soil fungi plays a crucial role in nutrient cycling and nutrient uptake into plants from soil via the formation of symbiotic mycorrhizal associations . Mycorrhizal fungi increase the surface absorbing area of roots and enhance nutrient uptake into the host plant: this is due to the physical geometry of the mycelium and its ability to mobilise nutrients from organic substrates through the action of extracellular catabolic enzymes .
Mycorrhizal mycelia have the ability to take up mineral nutrients  and mycorrhizal fungi acquire both essential macronutrients, such as phosphorus , and are efficient at taking up and accumulating microelements . This includes the accumulation of both nonessential elements and trace metals [5, 6], such as the heavy metal cadmium (Cd), an element of concern for food quality as its behaviour is analogous to essential metals, and essential nutrient elements such as zinc (Zn) and the trace element copper (Cu). Cd, Zn, and Cu accumulate in mushroom thalli [7, 8]. Sporocarps of many macrofungi might contain extremely high levels of heavy metals, with Cd being among the most intensively accumulated metal [9–13]. Relatively high Cu and Zn concentrations (bioaccumulation values higher than 1) in certain species of wild growing fungi are also reported [8, 11, 12, 14].
Thus, soil fungi, especially fungal sporocarps, are involved in the recycling heavy metals in forest ecosystems through bioaccumulation . In addition, the mycelium of ectomycorrhizal fungi has the potential for taking up metallic elements from the soil and transporting them within the fruiting body , which can have important consequences for the retention, mobility, and availability of these elements in forest ecosystems.
However, the capacity for retaining metal among species of fungi is wide  and the capability of fungi to accumulate elements differs . Essential nutrients, such as cobalt (Co) and nickel (Ni), and nonessential lead (Pb) appear to be excluded from fungi, as they do not accumulate [18, 19].
Fungal sporocarps comprise only a few percentage of the total mycelia biomass in a forest ecosystem . This means that a majority of fungal biomass in soil is located within the upper soil horizons below the soil surface . However, the ability of fungal mycelium to accumulate metal contents in mycelia is unclear and few studies are available [18, 22].
Although ectomycorrhizal fungi profoundly affect forest ecosystems through mediating nutrient uptake and maintaining forest food webs, the accumulation of metals at each transfer step from bulk soil to fungal sporocarps is unclear. The rhizosphere appears important for understanding the transfer of metals from soil to fungi. However, the fungi/soil concentration ratio for metals is not well studied under field conditions nor is much known about whether there is a difference between the uptake of metals from soil to fungi (mycelium/soil ratio) and transport within fungal thalli (sporocarps/mycelium ratio).
We attempted to quantify the uptake and distribution of Co, Ni, Cu, Zn, Cd, and Pb in the soil-mycelium-sporocarps compartments in various transfer steps: bulk soil, rhizosphere, soil-root interface, fungal mycelium, and sporocarps.
2. Materials and Methods
2.1. Sampling Area
The study area was located near Forsmark, in a forest ecosystem on the east coast of central Sweden (60°22′N, 18°13′E). The soil at the site is sandy or clay till. The field layer consists of bilberry (Vaccinium myrtillus L.), bracken (Pteridium aquilinum (L.) Kuhn.), coltsfoot (Tussilago farfara L.), horsetail (Equisetum silvaticum L.), and stone bramble (Rubus saxatilis L.). The tree layer comprises pure Norway spruce (Picea abies (L.) H. Karst.) or spruce mixed with Scots Pine (Pinus sylvestris L.), both about 100 years old. Further details about the site are presented by Lundin et al. . Ten sampling plots (approx. 10 m2 each) were established 20–50 m apart within the ecosystem, in an area of approximately 2.0 ha. The dominant trees were spruce on plots 1–7 and Scots Pine on plots 8–10.
2.2. Sampling of Soil and Fungi
Samples of soil and fungal sporocarps were collected from 10 sampling plots during September to November 2003. Four replicate soil samples were collected around and directly underneath fungal sporocarps (from an area of about 0.5 m−2) within each 10-m2 plot. After the removal of fresh leaves and litter, soil cores were taken to a depth of 10 cm with a cylindrical steel tube 5.7 cm in diameter. These soil cores were divided horizontally in situ into two 5 cm thick layers and stored in plastic bags at 4°C until analysis.
The sporocarps of 12 different fungal species were collected and cleaned of extraneous material: the species level was identified in the laboratory. The sporocarps were dried at 35°C to constant weight for determination of Co, Ni, Cu, Zn, Cd, and Pb concentration. Portions of soil samples taken from 0–5 and 5–10 cm depth were also used for chemical analyses. The majority of the prepared mycelia were assumed to belong to the same species, with some inclusion of other species, as whether mycelia extracted from the soil samples and sporocarps belonged to the same species was not determined.
2.3. Preparation of Fungal Mycelium and Fractionation of Soil
Soil portions (30–50 g) were used for extracting fungal mycelium. The fungal structures were isolated from the soil samples (0–5 cm layer) with forceps and under a dissection microscope (magnification 64x), small amounts of distilled water were added to the sample to disperse the soil. The prepared fraction of mycelium contained aseptate and septate hyphae, strands and rhizomorphs, sclerotia, and a small number of mycorrhizal root tips. The method for mycelium preparation is described by . Mycelium samples were dried at 35°C to constant weight for determination of Co, Ni, Cu, Zn, Cd, and Pb. The amount of mycelium obtained from each soil sample varied between 30 and 60 mg dry weight (DW) per gram of soil.
The soil samples (0–5 cm layer) were partitioned according to the method described by . Large roots, stones, and pieces of wood were removed, and the remaining soil was gently sieved through a 2 mm mesh. This sieved material was termed the bulk soil fraction. The soil aggregates containing roots that remained on the sieve were crumbled and gently squeezed between the fingers, resulting in the separation of more soil from the roots; this was termed the rhizosphere fraction. The residue, which was called the soil-root interface fraction, consisted of the finest roots with adhering soil particles. In the total, nine samples of bulk soil fraction and mycelium, 12 samples of fungal sporocarps (each sample represents one species), and 6 samples of rhizosphere and soil-root interface fraction were analysed for Co, Ni, Cu, Zn, Cd, and Pb concentration.
2.4. Chemical Analyses and Radiometry
Soil organic matter content (OMC) was determined by heating a known mass of soil to 550°C. Soil pH was determined in a 1 : 5 soil : water suspension (5 g of soil).
For element analyses, a 2.5 g portion of each sample was mixed with 5 mL mL 30% hydrogen peroxide. The mixture was then digested in a microwave oven, diluted with MQ water (water that has been purified using an ion exchange cartridge), and analysed with an inductively coupled plasma technique. Alkali metals were analysed at the laboratories of ALS Scandinavia AB, Luleå, a company within the ALS Laboratory Group, and all analyses were accompanied by rigorous quality control measures. Accuracy was assessed with peach leaves NIST 1547 (NIST, Gaithenburg, Nebraska, USA), a plant certified reference material with a matrix sufficiently close to fine roots and fungal material. The recoveries were 102.4% for Co, 101.4% for Ni, 103.5% for Cu, 99.4% for Zn, 104.6% for Cd, and 101.9% for Pb. For soil, CRM SO−2 (heavy metals in soil) has been used, but has no certified values for Co, Ni, Cu, Zn, Cd, or Pb: a detailed procedure of measurements is available in . Bioconcentration ratios (BCR) were defined as the concentration of the element (mg kg−1 DW) in a specific fraction divided by the concentration of the element (mg kg−1 DW) in bulk soil for the 0–10 cm soil layer.
2.5. Statistical Analyses
Data were analysed by one-way analysis of variance. Relationships between Co, Ni, Cu, Zn, Cd, and Pb concentrations in different soil fractions and fungi were determined with Pearson correlation coefficients and 2-sample t-test. All statistical analyses were run with Minitab (2010 Minitab Inc.) software.
3.1. Soil Characteristics
At the site, soil pH was high: in the 0–5 cm layer, the mean pH was 5.2 (range 3.8–6.9), and in the 5–10 cm layer, mean pH was 5.1 (range 3.6–7.1). For the entire 0–10 cm layer, the highest soil pH values (6.5–6.9) were in plots 1, 2, and 5: the pH values in the other plots were ranged from 3.7 to 5.1.
Soil organic matter content (OMC) at the study site was also high. The mean OMC in the 0–5 cm layer was 66.2% (range 36.4–97.7), and in the 5–10 cm layer, the mean OMC was 52.9% (range 21.2–96.6). For the 0–10 cm soil layer, the OMC values were high in plots 5 (84.0%), 8 (85.9%), and 9 (97.7%). The pH and OMC values did not correlate to the uptake of the metals in either fungal sporocarps or mycelia, except for a moderate correlation between pH and Cu content in mycelium (, ) and sporocarps (0.56 ns), and a moderate correlation (0.641 ns) between OMC and Pb content in mycelium.
3.2. Metal Concentrations in Soil and Fungal Compartments
The concentration of Co, Ni, Cu, and Cd in bulk soil was not significantly different from the concentration in the rhizosphere, although values for all metals were slightly higher in the rhizosphere fraction (Table 1).
Zinc and Pb concentrations were lower in the rhizosphere fraction than in bulk soil. The Cd concentration was higher and Pb concentration was lower in the soil-root interface fraction than in bulk soil: the concentration of Co, Ni, Cu, and Zn was similar to in the bulk soil and rhizosphere fractions. In the fungal mycelium fractions, Zn and Cd concentrations were significantly () higher than in the bulk soil and rhizosphere fractions. Fungal mycelium fraction was noticeably, although not statistically significant, concentrated with Cu: the concentration of lead in mycelium was lower than in the bulk soil and rhizosphere fractions.
The Cd concentration in the soil-root interface fraction was 4.0-fold higher than in bulk soil and 5.7-fold higher in mycelium than in bulk soil (Table 2). Zinc concentration was 2.2-fold higher in the soil-root interface fraction and 2.4-fold higher in the mycelium than in bulk soil. Copper concentrations varied considerably among the samples but there were no significant differences among the different soil fractions analysed (Table 2). The bioconcentration ratio in sporocarps generally followed a similar pattern, but the enrichment of Cd, Zn, and Cu in the sporocarps was more obvious (Table 2).
Based on the bioconcentration ratios, fungal sporocarps accumulated larger amounts of Cu, Zn, and Cd than mycelium. For example, Cu concentrations in fungal sporocarps collected from the same plots, where soil samples and mycelium were extracted, were about 1.8-fold higher than Cu concentrations found in mycelium. The concentrations of Zn in fungal sporocarps were about 1.4-fold higher than in the corresponding fungal mycelium and Cd was about 1.5-fold higher (Tables 2 and 3).
The bioconcentration ratios for each element varied among the species of fungal sporocarps sampled (Table 3). In general, most analysed species, except Lactarius deterrimus and Cortinarius odorifer tended to accumulate Cu. Most fungal species, except saprotrophic fungi Hypholoma capnoides and Collybia peronata, accumulated Zn. All fungal sporocarps, except Suillus granulatus, accumulated Cd. The bioconcentration ratio values for Cd were high: the BCR for Cortinarius armeniacus was above 30. The concentration of Co, Ni, and Pb in sporocarps was lower than the concentration in bulk soil and mycelium. Among other species, Cortinarius armeniacus and Cortinarius sp. had the highest content of all metals studied (Table 3).
3.3. Relationships between Copper, Zinc, and Cadmium in Soil and Fungi
Although not significant, there was an obvious relationship between the concentration of Co and Ni in mycelium and concentration in soil from which mycelium was extracted (Figures 1(a) and 1(b)). Sporocarps and mycelium Cu concentrations did not depend on soil concentrations, but Zn concentrations correlated to soil concentrations in both sporocarps and mycelium (Figures 1(c) and 1(d)). There were no significant correlations between Cd in soil and Cd in mycelium or sporocarps (Figure 1(e)). Sporocarps concentration of Co and Ni and its soil concentration did not depend. There was a weak correlation in Pb concentration in both sporocarps and mycelium only (Figure 1(f)).
There were no significant correlations between the concentrations of the metals studied in fungi and soil pH or soil organic matter content (data not shown), except for Pb in sporocarps and soil OMC (, ). Ni concentration in sporocarps negatively correlated with soil pH (, ns).
There were considerable amounts of the metals studied in all analyzed species of fungi and significant differences in the capability of accumulating these elements. Mycorrhizal fungi accumulate copper extensively [8, 27], and in this study, copper concentration increased in the following order: bulk soil < soil-root interface < rhizosphere < fungal mycelium < fungal sporocarps. However, statistically higher concentrations of copper were only found in fungal sporocarps, compared to bulk soil. Copper accumulation (BCR > 1) was found in a majority of the sporocarps species analysed. Although mycelium had about 2-fold higher copper concentration, this was not significantly different from the concentration in bulk soil. Despite uncertainty in the calculated values of the metal content in mycelium and sporocarps, these findings were in an agreement with previous studies [12, 14], where concentration of Cu in fungal sporocarps is higher than in topsoil. Thus, the ability to accumulate copper is greater in mycorrhizal fungi sporocarps than in mycelium. The values for the mean Cu concentration in mycelium were lower than the values reported for ectomycorrhiza ( μg g−1 mycorrhiza) from the top organic layer of coniferous forest soils in Norway : a plausible explanation might be that soils in Norway were contaminated with Cu.
Zinc also concentrated in mushroom thalli. Zinc concentrations increased in the following order: bulk soil < soil-root interface < fungal mycelium < fungal sporocarps. However, there was a 2-fold (fungal mycelium) and 3-fold (sporocarps) higher concentration of Zn than in bulk soil. The data agreed with results from other studies [14, 27], although there is only limited data available for zinc concentration in mycelium extracted from the soil where sporocarps grow. According to Berthelsen et al. , the mean Zn concentration is μg g−1 of mycorrhiza, which is much higher than values obtained in this study. One difference may be due to the study area, the study area of Berthelsen et al.  is located in a part of Norway exposed to considerable amounts of airborne deposition of heavy metals such as Cd and Zn.
Cadmium concentrations increased in the following order: bulk soil < rhizosphere < soil-root interface < fungal mycelium < fungal sporocarps. Fungi appeared to have a high preference for Cd, as the accumulation of Cd by fungi, both mycelium and especially fungal sporocarps, was pronounced, with a mean BCR of about 6 : 1 for mycelium and 9 : 1 for sporocarps. The accumulation of Cd by fungal sporocarps is apparently species dependent . Extremely high levels of Cd are reported from fruiting bodies of some of fungi, especially the toxic Amanita sp. [13, 28]. This could explain the species variation for both mycelium and sporocarps: the standard deviation values for Cd were as high as the mean values. However, both fungi and other fractions, for example, the rhizosphere and soil-root interface fractions, were noticeably enriched with Cd, although this was only significant for the soil-root interface fraction.
The capability of fungal species for accumulating essential (Co, Ni) and nonessential (Pb) metals differs [16, 17]. The Co, Ni, and Pb concentrations were generally evenly distributed between soil fractions and mycelium, whereas the concentration of these metals in sporocarps was lower. Lead elimination from the sporocarps was more pronounced: the concentration in sporocarps was about 70 times lower than in bulk soil and about 50 times lower than in mycelium. Similarly, Campos et al.  observe only absorption of Pb, but not accumulation, in the ectomycorrhizal fungus Cantharellus cibarius. The differences in metal concentrations between the mycelium and the sporocarps (assuming they belonged to the same species) indicate that there is no further transport of Co, Ni, and Pb within sporocarps after being taken up by mycelium from soil, that is, active transport from mycelium to sporocarps for those metals is absent. Apart of this, Cd, Cu, and Zn are soluble elements, while Co, Ni, and Pb are much less soluble. Pb in organic soils is more strongly bound to soil, whereas, for example, Cd is only weakly bound . These findings indicated that fungi (both mycelium and sporocarps) accumulate Cd to Zn and Cu, and Co, Ni, and Pb were excluded from the sporocarps and not accumulated. Based on the BCR values for fungal sporocarps and mycelium (Table 2), the accumulation of the metals could be ranked in the following order: Cd2+ > Zn2+ > Cu2+, with a relative ratio of 100 : 41 : 38. In terms of the amount of metals accumulated per mass unit by both mycelium and sporocarps, the metals could be ranked in decreasing order: Zn2+ > Cu2+ > Pb2+ > Cd2+ > Ni2+ > Co2+, with a relative ratio of 180 : 45 : 13 : 5 : 4 : 1.
The analyse of relationships between the concentrations of the metals in soil, mycelia, and fungal sporocarps indicated only essential Zn concentration in soil correlated with the concentration in sporocarps, and to certain degree in mycelium. The concentrations of Cu and Cd in fungi did not correlate with the concentrations in soil, whereas mycelium concentration of Co, Ni, and Pb was only weakly or moderately (not significantly) related to soil concentration. The extent of metal transfer from soil to fungi is apparently species-specific and influenced by both the bioavailability of the metals and the age of the mushroom . The variation in metal contents between edible mushrooms species also depends on the ability of the species to extract elements from the substrate  and competitive interaction between metals affects nutrient uptake capacities of the fungi .
The estimated values for soil mycelium biomass ranged from 30 to 60 mg DW of mycelium per one gram DW of soil (0–5 cm layer). Assuming a dry bulk density with 0.4 g cm−3 in the upper layers of soil in the Forsmark area , fungal mycelium was an important constituent of the organic surface soil and comprised between 3 and 6% by volume in the upper 5 cm of the forest soil. Based on the metal concentration in the bulk soil fraction and mycelium extracted from the same soil, fungal mycelium might accumulate appreciable amounts of the soil metals. The amount of Cd accumulated in fungal structures accounted for 15.5–31.7% of the total amount of Cd in soil. The fungal content of Zn in the top soil layer accounted for 5.4 and 10.9% of the total and fungal mycelium comprised between 4.6 and 9.1% of the total Cu content in soil. In fungal mycelium, the accumulation of Co was 3.5–6.9%, Ni was 2.6–5.2%, and Pb was 2.0–3.9%. The estimation of fungal biomass in soil may be relevant, as Berthelsen et al.  report similar data for fungal biomass in a Norwegian forest soil. Although the fungal contents of Cu, Zn, and Cd presented here were lower than reported by Berthelsen et al. , the discrepancy may be due to the difference in concentration level of metals in soil. The area in Norway has been exposed to airborne deposition of heavy metals, which can explain the higher accumulation by mycelium of fungi. Another source of discrepancy is the difference in methods used for mycelium estimation. Here a direct method was used, which meant mycelium biomass might have been underestimated rather than overestimated, whereas the ergosterol method used in Norway  may lead to overestimated mycorrhizal fungal biomass values. The fungal content of Pb (2–4%) supported previous reports of <3% of the soil Pb content .
The concentration of Cu, Zn, and Cd in mycelium was about 2–5 times higher than in bulk soil and the concentrations in sporocarps were about 1.5–2 times higher than in mycelium. The concentration of Co and Ni in mycelium was similar to the concentrations in other soil fractions (bulk soil, rhizosphere, soil-root interface); whereas, the concentrations in sporocarps were about 5–9 times lower than in mycelium. The concentration of Pb in mycelium was about 1.5 times lower than in other soil fractions (bulk soil, rhizosphere, soil-root interface) and about 50 times lower than in mycelium. The uptake of Cu, Zn, and Cd during the entire transfer process between soil and sporocarps occurs against a concentration gradient. The mycorrhizal fungi (mycelium and sporocarps) only absorbed cobalt, nickel, and lead but did not accumulate these metals in thalli.
The author would like to thank Professor K. Johanson, Drs. I. Nikolova and A. Taylor for their assistance with experiments and to the staff of the Analytica Laboratory, Luleå, for ICP-AES and ICP-SFMS analyses. The project was financially supported by SKB (Swedish Nuclear Fuel) and Waste Management Co.
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