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Zhizn Zemli [Life of the Earth] 45, no 3
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Zhizn Zemli [Life of the Earth] 45, no 3

Данные статьи

Description

DOI

10.29003/m3551.0514-7468.2023_45_3/355-362

Авторы:

Authors:

Inisheva, L.I.

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Keywords:

biosphere evolution, swamp soil formation, peat soils, Holocene, taiga, Western Siberia, swampy ecosystems.

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Inisheva, L.I., «Biospheric aspects of swampy soil formation», Zhizn Zemli [Life of the Earth] 45, no 3, 355–362 (2023) (in Russ., abstr. in Engl.). DOI: 10.29003/m3551.0514-7468.2023_45_3/355-362.

Biospheric aspects of swampy soil formation

The article shows that each period of the evolutionary process of the biosphere formation on Earth corresponds to one form of soil formation, namely: underwater (“hydrozemic”), swampy (“atmozemic”), and terrestrial (“lithozemic”). The ancient swamp soil formation is considered, in addition to biomass deposition, to take part in the formation of the oxygen-containing composition of the planet’s gaseous envelope and the release of organisms from the aquatic environment to land. It has been determined that the process of paludification and swamp soils in the past and at present did and do perform the same biospheric functions and should include the entire genetic profile up to the basal rock in the concept of “peat soil”. On the example of the central part of Western Siberia, the process of paludification in the Holocene period is considered. This process is defined as a single, irreversible, progressive process of conjugated changes in their biotic and abiotic components. This ensures autonomy in the development and preservation of mires as a special type of the biogeocenotic cover of Earth. It is shown that the differences in the mire complexes of different botanico–geographical zones and subzones reveal the chronological boundaries of the transformation of swamp biogeocenoses of eutrophic types into mesotrophic and oligotrophic ones. It has been determined that the process of paludification in the taiga zone of the West Siberian Plain is of aggressive nature and the expected warming is a temporary warm period in the interval of cyclical climate.

Список литературы

  1. Bakhnov, V.K., Soil formation (a look into the past and the present) (Novosibirsk: Nauka, 2002) (in Russian).
  2. Vernadsky, V.I., Chemical structure of the Earth’s biosphere and its environment (Moscow: Nauka, 1965) (in Russian).
  3. Vompersky, S.E., “Biospheric significance of swamps in the carbon cycle”, Priroda 7, 44–50 (1994) (in Russian).
  4. Zhukov, V.M., “Climate and the process of swamp formation”, Scientific prerequisites for the development of the marshes of Western Siberia (Moscow: Nauka, 1977) (in Russian).
  5. Inisheva, L.I., Special features of mire ecosystems functioning under the influence of natural and anthropogenic factors (Tomsk: Publishing house TGPU, 2020) (in Russian).
  6. Liss, O.L., Abramova, L.I., Avetov, N.A., Berezina, N.V., Inisheva, L.I., Kurnishkova, T.V., Sluka, Z.A., Tolpysheva, T.Yu., and Shvedchiko-va, N.K., Mire systems and their environmental significance (Tula: Grif, 2001) (in Russian).
  7. Lishtvan, I.I., Kurzo, B.V., Gaydukevich, O.M., Navosha, Yu.Yu., “Resources and qualitative composition of peat raw materials in deposits reserved for thermobiochemical processing”, Prirodopol’zovaniye 1, 188–204 (2019) (in Russian).
  8. Naumov, A.V., “Carbon status of Russia and dynamic equilibrium of the biosphere”, Soil and environment 5 (2), (2022). https://doi.org/10.31251/pos.v5i2.166 (in Russian).
  9. Rozanov, A.Yu., Zavarzin, G.A., “Bacterial paleontology”, Vestnik RAN 67 (3), 241–245 (1997) (in Russian).
  10. Snakin, V.V., “Instability of natural processes: global climate”, Use and protection of natural resources in Russia 3, 3–11 (2022) (in Rus-sian).
  11. Strakhov, N.M., Fundamentals of the theory of lithogenesis 2 (Moscow: Publishing house AN SSSR, 1962) (in Russian).
  12. Syso, A.I., Peregon, A.M., “Swamp formation specificity in the southern part of the Great Vasyugan swamp”, Siberian Ecological J. 2, 245–250 (2009) (in Russian).
  13. Uranov, A.A., “Plants and environment”, Zhizn’ rasteniy 1, 58–86 (1974) (in Russian).
  14. Inisheva, L.I., “Proposals for the Classification of Peat Soils”, Eurasian Soil Science 55 (2), 147–153 (2022). DOI: 10.1134/s1064229322020077.

References

  1. Bakhnov, V.K., Soil formation (a look into the past and the present) (Novosibirsk: Nauka, 2002) (in Russian).
  2. Vernadsky, V.I., Chemical structure of the Earth’s biosphere and its environment (Moscow: Nauka, 1965) (in Russian).
  3. Vompersky, S.E., “Biospheric significance of swamps in the carbon cycle”, Priroda 7, 44–50 (1994) (in Russian).
  4. Zhukov, V.M., “Climate and the process of swamp formation”, Scientific prerequisites for the development of the marshes of Western Siberia (Moscow: Nauka, 1977) (in Russian).
  5. Inisheva, L.I., Special features of mire ecosystems functioning under the influence of natural and anthropogenic factors (Tomsk: Publishing house TGPU, 2020) (in Russian).
  6. Liss, O.L., Abramova, L.I., Avetov, N.A., Berezina, N.V., Inisheva, L.I., Kurnishkova, T.V., Sluka, Z.A., Tolpysheva, T.Yu., and Shvedchiko-va, N.K., Mire systems and their environmental significance (Tula: Grif, 2001) (in Russian).
  7. Lishtvan, I.I., Kurzo, B.V., Gaydukevich, O.M., Navosha, Yu.Yu., “Resources and qualitative composition of peat raw materials in deposits reserved for thermobiochemical processing”, Prirodopol’zovaniye 1, 188–204 (2019) (in Russian).
  8. Naumov, A.V., “Carbon status of Russia and dynamic equilibrium of the biosphere”, Soil and environment 5 (2), (2022). https://doi.org/10.31251/pos.v5i2.166 (in Russian).
  9. Rozanov, A.Yu., Zavarzin, G.A., “Bacterial paleontology”, Vestnik RAN 67 (3), 241–245 (1997) (in Russian).
  10. Snakin, V.V., “Instability of natural processes: global climate”, Use and protection of natural resources in Russia 3, 3–11 (2022) (in Rus-sian).
  11. Strakhov, N.M., Fundamentals of the theory of lithogenesis 2 (Moscow: Publishing house AN SSSR, 1962) (in Russian).
  12. Syso, A.I., Peregon, A.M., “Swamp formation specificity in the southern part of the Great Vasyugan swamp”, Siberian Ecological J. 2, 245–250 (2009) (in Russian).
  13. Uranov, A.A., “Plants and environment”, Zhizn’ rasteniy 1, 58–86 (1974) (in Russian).
  14. Inisheva, L.I., “Proposals for the Classification of Peat Soils”, Eurasian Soil Science 55 (2), 147–153 (2022). DOI: 10.1134/s1064229322020077.