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November 2017, № 12 (212), pages 12–15

Nekrasova O.A., Dergacheva M.I., Uchaev A.P. TO RECENT BASE FOR PALEOECOLOGICAL RECONSTRUCTIONS BASED ON HUMUS OF URAL PALEOSOLSWhen carrying out the reconstruction of the natural environment of the past by paleopedology methods the humus composition is used as one of the significant diagnostic features. Interpretation of materials is based on the recent basis — similar characteristics of modern soils of different formation conditions on both the territory of location of the paleosols and adjacent to them. Revealing the Holocene-Pleistocene evolution of the Ural natural environment requires the materials of exploring the specific features of the humus composition of different types of soils in its different regions including the Middle Urals for which data on humus are not generalized. On the basis of the original and literary material data generalisation of the humus composition specific features of the modern Middle Ural types of soils, the closeness of most humus characteristics and the reliable differences of some of them in the most common in this region plain sod-podzolic and brown mountain-forest soils are revealed. It was established that the differences in the content of individual groups of humus substances and the integral index Cha:Cfa are unreliable. Significant differences were revealed only for the following characteristics of humus composition: the content of total organic carbon, as well as FA1a, FA2, and FA3. The parameters of the composition of humus in gray forest soils of the Middle Urals are typical for similar soils of other regions of the Urals and adjacent territories. The obtained limits of variation of the integral indicator of the composition of humus in soddy-podzolic, brown mountain-forest and gray forest soils of the modern Middle Urals, will allow to reconstruct the conditions of humus formation in paleosols in similar bioclimatic conditions. It has been established that the sod-podzolic and brown mountain-forest soils of the Middle Urals, forming within the boundaries of a single bioclimatic zone at different positions in the relief, have close characteristics of the qualitative composition of humus.Key words: soil, humus, paleoecological reconstructions, Ural.


1. Dergacheva, M.I., Zykina, V.S., 1988. Organic Carbon of Paleosols. Novosibirsk: Nauka. 128 pp. (in Russian).

2. Gendler, T.S., Heller, F., Tsatskin, A., Spassov, S., Du Pasquier, J., Faustove, S.S., 2006. Roxolany and Novaya Etuliya-key sections in the western Black Sea loess area: Magnetostratigraphy, rock magnetism, and paleopedology. Quaternary International 152–153, 78–93.

3. Rutter, N.W., Velichko, A.A., Dlussky, K.G., Morozova, T.D., Little, E.C., Nechaev, V.P., Evans, M.E., 2006. New insights on the loess/paleosol Quaternary stratigraphy from key sections in the U.S. Midwest. Catena 67, 15–34.

4. Velichko, A.A., Catto, N.R, Kononov, M.Y., Morozova, T.D., Novenko, E.Yu., Panin, P.G., Ryskov. G.Ya, Semenov, V.V., Timireva, S.N., Titov, V.V., Tesakov A.S., 2009. Progressively cooler, drier interglacials in southern Russia throught the Quaternary: Evidence from the Sea of Azov region. Quaternary International 198, 204–219.

5. Nawrocki, J., Lanczont M., Rosowiecka, O., Bogucki A.B., Magnitostrarigraphy of the loess-paleosol key Palaelolithic section at Korolevo (Transcarpatian, W. Ukraine), Quaternary International (2015), http://dx.

6. Chichagova O.A. On the composition of humus of buried soils of different types of soil formation // Geograf. message. 1961. Vol. 2. P. 74–76.

7. Dergacheva M.I. Archaeological pedology. Novosibirsk: Izdat. SB RAS, 1997. 228 p.

8. Dergacheva, M.I. Pedohumic method in paleoenvironmental reconstructions: an example from Middle Siberia // Quaternary International. 2003. Vol. 106–107. PР. 73–78.

10. Fedeneva I.N., Dergacheva M.I. Soilscape evolution of West Tien Shan during the Late Pleistocene based on humus properties of the Obi-Rakhmat archaeological site. // Quaternary International. 2006. Vol. 156–157. PР. 60–69.

11. Dergacheva M., Nekrasova O., Uchaev A., Bazhina N. Sarykul paleosol in Southern Urals sediments (Russia) // Quaternary International. 2016. Vol. 420. PP. 90–100.

12. Dergacheva M, Fedeneva I, Bazhina N, Zenin V, Nekrasova O. Shestakovo site of Western Siberia (Russia): pedogenic features, humic substances and paleoenvironment reconstructions for last 20–25 ka. Quaternary International. 2016. Vol. 420. PP. 199–207.

13. Reference book on the climate of the USSR. Issue. 9. Part 2. Air and Soil Temperature, Leningrad: Hydrometeorological Publishing House, 1965. 363 p.

14. Reference book on the climate of the USSR. Issue. 9. Part 4. Air humidity and precipitation, 1968. 372 p.

15. Ponomareva V.V., Plotnikova T.A. A technique and some results of humus of chernozems fractionation // Pochvovedenie. 1968. No. 11. P. 104–117.

16. Orlov D.S., Biryukova O.N., Sukhanova N.I. Organic matter of soils of the Russian Federation. Moscow: Nauka, 1996. 256 p.

About this article

Authors: Nekrasova O.A., Dergacheva M.I., Uchaev A.P.

Year: 2017

doi: 10.25198/1814-6457-212-12

Zhanna Anatolievna

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