Diversity of the soil biota in burned areas of southern taiga forests (Tver oblast)
Relations between soil biota diversity and its contribution to the performance of some ecosystem functions were assessed based on the results obtained in undisturbed and burned spruce forests near the Central Forest Nature Biosphere Reserve (Tver oblast). In August 2014, in two 4-year-old burned are...
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Published in: | Eurasian soil science Vol. 49; no. 3; pp. 358 - 366 |
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Abstract | Relations between soil biota diversity and its contribution to the performance of some ecosystem functions were assessed based on the results obtained in undisturbed and burned spruce forests near the Central Forest Nature Biosphere Reserve (Tver oblast). In August 2014, in two 4-year-old burned areas, abiotic parameters of the soils, indicators of the state of the microbial communities, the number, taxonomic diversity, and the abundance of the main groups of soil invertebrates (testate amoebae, nematodes, enchytraeids, mites, collembolans, and the mesofauna as a whole) were determined. In the soils of the burned areas, higher CO
2
, CH
4
, and N
2
O emissions were observed. The number of bacterial cells remained similar, and the total length of active mycelium was not significantly different. All this implies a certain intensification of biogenic processes promoting the mobilization of carbon and nitrogen after fire. The number of most of the groups of soil animals was lower (not always significantly) in the burned area than that in the soils of the undisturbed forests. The changes in the taxonomic diversity were specific for each taxon studied. Overall, the diversity of invertebrates was related to the litter thickness. However, the high taxonomic diversity of soil fauna did not always correspond to the active functioning of the ecosystem. Thus, for some taxa, a quite close correlation was found, for instance, between the total number of species (of testate amoebae in particular) and the berry crop, as well as between the soil mesofauna population and the dead wood stock. The total diversity of the investigated taxa included in the detrital trophic web was the most reliable indicator of the carbon stock in the burned areas. |
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AbstractList | Relations between soil biota diversity and its contribution to the performance of some ecosystem functions were assessed based on the results obtained in undisturbed and burned spruce forests near the Central Forest Nature Biosphere Reserve (Tver oblast). In August 2014, in two 4-year-old burned areas, abiotic parameters of the soils, indicators of the state of the microbial communities, the number, taxonomic diversity, and the abundance of the main groups of soil invertebrates (testate amoebae, nematodes, enchytraeids, mites, collembolans, and the mesofauna as a whole) were determined. In the soils of the burned areas, higher CO
2
, CH
4
, and N
2
O emissions were observed. The number of bacterial cells remained similar, and the total length of active mycelium was not significantly different. All this implies a certain intensification of biogenic processes promoting the mobilization of carbon and nitrogen after fire. The number of most of the groups of soil animals was lower (not always significantly) in the burned area than that in the soils of the undisturbed forests. The changes in the taxonomic diversity were specific for each taxon studied. Overall, the diversity of invertebrates was related to the litter thickness. However, the high taxonomic diversity of soil fauna did not always correspond to the active functioning of the ecosystem. Thus, for some taxa, a quite close correlation was found, for instance, between the total number of species (of testate amoebae in particular) and the berry crop, as well as between the soil mesofauna population and the dead wood stock. The total diversity of the investigated taxa included in the detrital trophic web was the most reliable indicator of the carbon stock in the burned areas. Relations between soil biota diversity and its contribution to the performance of some ecosystem functions were assessed based on the results obtained in undisturbed and burned spruce forests near the Central Forest Nature Biosphere Reserve (Tver oblast). In August 2014, in two 4-year-old burned areas, abiotic parameters of the soils, indicators of the state of the microbial communities, the number, taxonomic diversity, and the abundance of the main groups of soil invertebrates (testate amoebae, nematodes, enchytraeids, mites, collembolans, and the mesofauna as a whole) were determined. In the soils of the burned areas, higher C[O.sub.2], C[H.sub.4], and [N.sub.2]O emissions were observed. The number of bacterial cells remained similar, and the total length of active mycelium was not significantly different. All this implies a certain intensification of biogenic processes promoting the mobilization of carbon and nitrogen after fire. The number of most of the groups of soil animals was lower (not always significantly) in the burned area than that in the soils of the undisturbed forests. The changes in the taxonomic diversity were specific for each taxon studied. Overall, the diversity of invertebrates was related to the litter thickness. However, the high taxonomic diversity of soil fauna did not always correspond to the active functioning of the ecosystem. Thus, for some taxa, a quite close correlation was found, for instance, between the total number of species (of testate amoebae in particular) and the berry crop, as well as between the soil mesofauna population and the dead wood stock. The total diversity of the investigated taxa included in the detrital trophic web was the most reliable indicator of the carbon stock in the burned areas. Keywords: soil fauna, biodiversity, functioning, taiga, boreal ecosystems Relations between soil biota diversity and its contribution to the performance of some ecosystem functions were assessed based on the results obtained in undisturbed and burned spruce forests near the Central Forest Nature Biosphere Reserve (Tver oblast). In August 2014, in two 4-year-old burned areas, abiotic parameters of the soils, indicators of the state of the microbial communities, the number, taxonomic diversity, and the abundance of the main groups of soil invertebrates (testate amoebae, nematodes, enchytraeids, mites, collembolans, and the mesofauna as a whole) were determined. In the soils of the burned areas, higher CO2, CH4, and N2O emissions were observed. The number of bacterial cells remained similar, and the total length of active mycelium was not significantly different. All this implies a certain intensification of biogenic processes promoting the mobilization of carbon and nitrogen after fire. The number of most of the groups of soil animals was lower (not always significantly) in the burned area than that in the soils of the undisturbed forests. The changes in the taxonomic diversity were specific for each taxon studied. Overall, the diversity of invertebrates was related to the litter thickness. However, the high taxonomic diversity of soil fauna did not always correspond to the active functioning of the ecosystem. Thus, for some taxa, a quite close correlation was found, for instance, between the total number of species (of testate amoebae in particular) and the berry crop, as well as between the soil mesofauna population and the dead wood stock. The total diversity of the investigated taxa included in the detrital trophic web was the most reliable indicator of the carbon stock in the burned areas. Relations between soil biota diversity and its contribution to the performance of some ecosystem functions were assessed based on the results obtained in undisturbed and burned spruce forests near the Central Forest Nature Biosphere Reserve (Tver oblast). In August 2014, in two 4-year-old burned areas, abiotic parameters of the soils, indicators of the state of the microbial communities, the number, taxonomic diversity, and the abundance of the main groups of soil invertebrates (testate amoebae, nematodes, enchytraeids, mites, collembolans, and the mesofauna as a whole) were determined. In the soils of the burned areas, higher CO sub(2), CH sub(4), and N sub(2)O emissions were observed. The number of bacterial cells remained similar, and the total length of active mycelium was not significantly different. All this implies a certain intensification of biogenic processes promoting the mobilization of carbon and nitrogen after fire. The number of most of the groups of soil animals was lower (not always significantly) in the burned area than that in the soils of the undisturbed forests. The changes in the taxonomic diversity were specific for each taxon studied. Overall, the diversity of invertebrates was related to the litter thickness. However, the high taxonomic diversity of soil fauna did not always correspond to the active functioning of the ecosystem. Thus, for some taxa, a quite close correlation was found, for instance, between the total number of species (of testate amoebae in particular) and the berry crop, as well as between the soil mesofauna population and the dead wood stock. The total diversity of the investigated taxa included in the detrital trophic web was the most reliable indicator of the carbon stock in the burned areas. |
Audience | Academic |
Author | Korobushkin, D. I. Kuznetsova, D. M. Butenko, K. O. Rakhleeva, A. A. Lapygina, E. V. Shakhab, S. V. Yazrikova, T. E. Gongalsky, K. B. Zaitsev, A. S. Gorshkova, I. A. Saifutdinov, R. A. Gorbunova, A. Yu Kosina, N. V. Benediktova, A. I. |
Author_xml | – sequence: 1 givenname: K. B. surname: Gongalsky fullname: Gongalsky, K. B. email: gongalsky@gmail.com organization: Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences – sequence: 2 givenname: A. S. surname: Zaitsev fullname: Zaitsev, A. S. organization: Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences – sequence: 3 givenname: D. I. surname: Korobushkin fullname: Korobushkin, D. I. organization: Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences – sequence: 4 givenname: R. A. surname: Saifutdinov fullname: Saifutdinov, R. A. organization: Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences, Kazan Federal University – sequence: 5 givenname: T. E. surname: Yazrikova fullname: Yazrikova, T. E. organization: Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences, Faculty of Soil Science, Moscow State University – sequence: 6 givenname: A. I. surname: Benediktova fullname: Benediktova, A. I. organization: Faculty of Soil Science, Moscow State University – sequence: 7 givenname: A. Yu surname: Gorbunova fullname: Gorbunova, A. Yu organization: Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences – sequence: 8 givenname: I. A. surname: Gorshkova fullname: Gorshkova, I. A. organization: Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences – sequence: 9 givenname: K. O. surname: Butenko fullname: Butenko, K. O. organization: Skryabin All-Russian Research Institute of Fundamental and Applied Parasitology of Animals and Plants – sequence: 10 givenname: N. V. surname: Kosina fullname: Kosina, N. V. organization: Faculty of Soil Science, Moscow State University – sequence: 11 givenname: E. V. surname: Lapygina fullname: Lapygina, E. V. organization: Faculty of Soil Science, Moscow State University – sequence: 12 givenname: D. M. surname: Kuznetsova fullname: Kuznetsova, D. M. organization: Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences – sequence: 13 givenname: A. A. surname: Rakhleeva fullname: Rakhleeva, A. A. organization: Faculty of Soil Science, Moscow State University – sequence: 14 givenname: S. V. surname: Shakhab fullname: Shakhab, S. V. organization: Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences |
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CitedBy_id | crossref_primary_10_1016_j_apsoil_2018_12_021 crossref_primary_10_1111_oik_05738 crossref_primary_10_1016_j_soilbio_2017_02_006 crossref_primary_10_3103_S0147687421040062 crossref_primary_10_1134_S1067413619040064 crossref_primary_10_1134_S1064229320110113 crossref_primary_10_1007_s00374_020_01441_4 crossref_primary_10_1134_S199542551703012X crossref_primary_10_1016_j_geoderma_2017_07_021 crossref_primary_10_1134_S1064229323700217 crossref_primary_10_1016_j_soilbio_2021_108281 crossref_primary_10_1016_j_apsoil_2019_103491 crossref_primary_10_1016_j_ejsobi_2017_04_001 |
Cites_doi | 10.1007/s00442-004-1741-x 10.1007/s00248-006-9119-8 10.1007/BF02937536 10.1016/j.foreco.2010.04.001 10.1016/S0929-1393(98)00123-1 10.1111/j.1365-2389.2010.01314.x 10.1134/S1064229307060129 10.1146/annurev.phyto.37.1.127 10.1371/journal.pone.0043292 10.1134/S1064229314020045 10.1016/S0038-0717(01)00180-8 10.1073/pnas.1305198110 10.1111/j.1365-2486.2008.01672.x 10.1038/ncomms2328 10.1016/j.apsoil.2012.03.017 10.1038/nclimate1692 10.1016/j.soilbio.2012.07.005 10.2307/2937206 10.1139/x83-105 10.1111/ele.12034 10.1890/12-1243.1 10.1016/j.soilbio.2011.07.016 |
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SubjectTerms | Biodiversity Biological diversity Biosphere Biota Carbon dioxide Dead wood Earth and Environmental Science Earth Sciences Ecological function Ecosystems Forests Forests and forestry Geotechnical Engineering & Applied Earth Sciences Microbial activity Nematoda Nitrous oxide Soil Biology Soil fauna Soil invertebrates Soil sciences Soils Taiga & tundra Taxa Terrestrial ecosystems |
Title | Diversity of the soil biota in burned areas of southern taiga forests (Tver oblast) |
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