Bioaccumulation of Selected Metals and Non-Metals in Mycelium and Fruit Bodies of Ectomycorrhizal Fungi
IF 0.3
Q4 GEOLOGY
Т. О. Єльнікова, Ю. Н. Мандро
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引用次数: 1
Abstract
Purpose. We attempted to quantify the contribution of wild-growing mycelium of ectomycorrhizal fungi to the soil level of selected metals and non-metals in upper (0−10 cm) layer of forest soil of boreal forest ecosystems. The content of selected elements were also analyzed and compared in such fractions of soil as bulk soil, rhizosphere and soil-root interface. Specifically we analyzed the content of phosphorus (P), manganese (Mn), iodine (I), chromium (Cr), nickel (Ni), copper (Cu), zinc (Zn), cadmium (Cd), cobalt (Co), mercury (Hg) lead (Pb) and arsenic (As). Methods. The concentration of the elements in the samples (dry weight, d.w.) was determined by the mass spectrometric method (ICP-MS) in the laboratory ALS Scandinavia AB, Luleå according to the method given in Rodushkin et al. [13]. Statistical data processing was performed using dispersion analysis (ANOVA) and Pearson correlation coefficients. Software Minitab (© 2010 Minitab Inc.). Results. It has been shown that concentration of phosphorus in the mycelium of fungi is about 1.5 times, and in the fruit bodies is about 7 times higher of that the plant plant tissue (soil+root interface). The concentration of manganese in the mycelium is about the same as in the bulk soil and much lower in the fraction of rhizosphere. Iodine, chromium and nickel are not accumulated, neither the mycelium of fungi nor in their fruitful bodies. Copper, zinc and cadmium are accumulated in both fruit bodies and mycelium of the studied species intensively. The concentration of cadmium in the mycelium is found to be about three times higher than in the bulk soil fraction, and about twice as high as in the fraction of rhizosphere. At such concentrations of cadmium in mycelium, the later may account from 16.2 to 32.3% of the total amount of cadmium in the upper, 0-10 cm layer of forest soils. The content of cobalt and mercury in the mycelium appeared to be somewhat higher in the bulk soil, about the same as in the rhizosphere fraction, and significantly higher than in the soil-root interface fraction. Fungi did not accumulate lead neither in the mycelium nor in their fruit bodies, whereas arsenic does not accumulated in soil-root interface and only weakly accumulated by fungal fruit bodies. Conclusions As a result of the study, it was found that the content of most of the analyzed metals and non-metals in the mycelium of ectomycorrhizal fungi of the upper (0-10 cm) soil enriched with organic matter in the forest ecosystem, except for cadmium and phosphorus, does not exceed 10% of their total amount. At the same time, the content of cadmium in the mycelium of fungi was the highest − 16.2 to 32.3%, which indicates the ability of fungi to accumulate this metal. It is suggested that the percentages of the content of the elements studied in the mycelium of upper layers of forest soil is rather underestimated than overestimated.
外生菌根真菌菌丝和子实体中选定金属和非金属的生物积累
目的。我们试图定量分析野生外生菌根真菌菌丝体对北方森林生态系统森林土壤上层(0 ~ 10 cm)土壤中选定金属和非金属含量的贡献。并对土壤体土、根际土、根际土等土壤组分中选定元素的含量进行了分析比较。具体来说,我们分析了磷(P)、锰(Mn)、碘(I)、铬(Cr)、镍(Ni)、铜(Cu)、锌(Zn)、镉(Cd)、钴(Co)、汞(Hg)、铅(Pb)和砷(As)的含量。方法。样品中元素的浓度(干重,d.w)采用质谱法(ICP-MS)测定,方法参照Rodushkin et al.[13]。统计数据处理采用离散分析(ANOVA)和Pearson相关系数。软件Minitab(©2010 Minitab Inc.)。结果。研究表明,真菌菌丝体中磷浓度约为植物组织(土壤+根界面)的1.5倍,果实体中磷浓度约为植物组织(土壤+根界面)的7倍。菌丝体中锰的浓度与散装土壤中锰的浓度大致相同,而根际部分锰的浓度要低得多。碘、铬和镍既不会在真菌的菌丝体中积累,也不会在它们的果实体中积累。铜、锌、镉在本研究种的子实体和菌丝体中富集。发现菌丝体中的镉浓度约为散装土壤部分的三倍,约为根际部分的两倍。在菌丝体中镉的这种浓度下,后者可能占森林土壤上层0-10 cm层镉总量的16.2%至32.3%。菌丝中钴和汞的含量在块状土壤中略高,与根际部分大致相同,显著高于土壤-根界面部分。真菌在菌丝体和子实体中均不积累铅,而砷在土壤-根界面中不积累,仅在真菌子实体中积累较弱。结论研究发现,在森林生态系统有机质富集的上层(0 ~ 10 cm)土壤中,除镉和磷外,所分析的外生菌根真菌菌丝中大部分金属和非金属的含量均不超过其总量的10%。同时,真菌菌丝体中镉的含量最高,为16.2% ~ 32.3%,说明真菌具有富集镉的能力。结果表明,森林土壤上层菌丝体中所研究的元素含量百分比被低估了,而不是高估了。
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