Problems of Estimation of Microbial Biomass in Soddy-Podzolic Soils (Forests of the Protected Areas of Moscow Region)

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Abstract

The carbon content of microbial biomass in the soil serves as one of the indicators of its biological activity and is often used in assessing the anthropogenic impact and natural changes on the soil microbiome. Significant spatial and temporal variation of the indicator at the level of ecosystems, soil typological units, land use types, etc. makes it difficult to interpret the data obtained during mass monitoring. The aim of the study is to determine the background values of microbial biomass content in the surface sub-litter layer of soils of protected forests of the Moscow region. A reconnaissance survey of soils of the podzolic series, which are typical for the region and diverse in genesis and granulometric composition, autonomous or with a little additional moisture, formed under mixed southern taiga forests in four protected natural territories, was carried out. The biological activity of soils was estimated by the amount of microbial biomass determined by two methods: by the content of phospholipids and substrate-induced respiration of microbial communities. Significant spatial variability of microbial biomass content was noted both at the site level and at the ecosystem level, and for similar by classification and granulometric composition autonomous soils, it is comparable with local variability within the experimental sites. It is shown that the value of microbial biomass depends mainly on the type of the humidity regime and the granulometric composition, which largely determines the sorption capacity of the soil, and its provision with biophilic elements, and also correlates with the richness of the ground cover that provides the soil microbiome with nutrients. It is shown that in order to obtain correct results for mass monitoring of soil biological activity, unification of the methodology and depth of sampling in the soils of background and anthropogenic-transformed ecosystems is of great importance.

About the authors

O. V. Chernova

Severtsov Institute of Ecology and Evolution of the Russian Academy of Sciences

Author for correspondence.
Email: ovcher@mail.ru
Russian Federation, Moscow

K. S. Duschanova

Institute of Physicochemical and Biological Problems of Soil Science of the Russian Academy of Sciences

Email: ovcher@mail.ru
Russian Federation, Pushchino

A. A. Petrosyan

Institute of Physicochemical and Biological Problems of Soil Science of the Russian Academy of Sciences

Email: ovcher@mail.ru
Russian Federation, Pushchino

T. E. Khomutova

Institute of Physicochemical and Biological Problems of Soil Science of the Russian Academy of Sciences

Email: ovcher@mail.ru
Russian Federation, Pushchino

References

Supplementary files

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2. Fig. 1. Fragment of the map of Soil-ecological zoning of the Russian Federation at a scale of 1:8,000,000 [15] for the territory of the Moscow region with the location of the surveyed protected areas. Surveyed protected areas (full names in the text). Provinces, districts of soil-ecological zoning: E ​​- zone of sod-podzolic soils of the southern taiga, E3 - Central Russian southern taiga province of sod-fine- and shallow-podzolic soils, VI - Kimry district of sod-fine- and shallow-podzolic, gley podzols and peat(ist)-podzolic-gley sandy and sandy loam soils on fluvioglacial and ancient alluvial deposits underlain by moraine loams, XIV - Smolensk-Moscow district of sod-fine- and shallow-podzolic clayey and loamy soils on cover deposits, XVI - Moskvoretsko-Oksky district of sod-fine- and shallow-podzolic and gray forest clayey and heavy loamy soils on weakly carbonate cover deposits sediments, XVII - Meshchersky district of podzols of gley peat(ist) and sod-podzolic illuvial-ferruginous sandy soils on ancient alluvial and fluvioglacial sediments and peat bog upland and lowland soils. L1 - Central Russian broadleaf-forest province of gray forest soils (zones of gray forest soils of deciduous forests), M1 - Central Russian forest-steppe province of podzolized, leached and typical deep and medium-deep chernozems, low- and medium-humus and gray forest soils (zones of podzolized, leached and typical chernozems and gray forest soils of the forest-steppe).

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3. Fig. 2. The carbon content of microbial biomass in soils of protected areas of the Moscow region (10 × 10 m plots, arithmetic mean). FL method: 1 – 0–15 cm layer, 2 – 0–10 cm, 3 – 10–20 cm; SID method: 4 – 0–15 cm layer, 5 – 0–10 cm, 6 – 10–20 cm. Designations of experimental plots in Table 1.

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4. Fig. 3. The share of microbial carbon Cmic/Corg in soils of protected areas of the Moscow region, %. (plots 10 × 10 m, arithmetic mean). FL method: 1 – layer 0–15 cm, 2 – 0–10 cm, 3 – 10–20 cm; SID method: 4 – layer 0–15 cm, 5 – 0–10 cm, 6 – 10–20 cm.

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5. Fig. 4. Distribution of soils of protected areas in the plane of the principal components depending on the physicochemical and biological properties. FG – content of physical clay (<0.01 mm); PU – signs of moisture in the profile; NVV – presence of moisture-loving species; TP – type of ground cover; Corg and C-FL – content of soil organic carbon and microbial carbon by the content of phospholipids, respectively.

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