Vestnik On-line
Orenburg State University april 26, 2024   RU/EN
Headings of Vestnik
Pedagogics
Psychology
Other

Search
Vak
Антиплагиат
Orcid
Viniti
ЭБС Лань
Rsl
Лицензия Creative Commons

July 2017, № 8 (208), pages 95-98

doi: 10.25198/1814-6457-208-95

Fedeneva I.N., Dergacheva M.I. HUMUS OF POSTLITHOGENOUS AND SYNLITHOGENOUS PALEOSOLS AND ITS USE AT PALEOECOLOGICAL RECONSTRUCTIONSWhen paleosols’ studying and their using at paleoecological reconstruction there is a problem of detection such signs of an ancient pedogenesis which would allow to compare and generalize the data characterizing the paleosols, created according to different models — as a result of synlithogenous and postlithogenous soil formation. Such signs are humus parameters, which reflect elementary processes of humus formation, depend on climatic conditions and remain during geological time. Late Pleistocene paleosols of different regions of Altai Mountains studying has shown that using of humus characteristics at paleosols diagnostics and reconstructions of paleoecological conditions can be carried out, irrespective of soil formation model. Paleosols of mountain regions can have a safe soil profile only in case of a postlithogenous pedogenesis which is characteristic of long warm stages of paleogeographic history whereas in a cold climate the pedogenesis is accompanied by active processes of sedimentation, and it is possible to speak about synlithogenous soil formation. In this case reliable reconstruction of paleoecological conditions can be carried out with using of a complex of characteristics of the humic substances remaining in deposits. For comparison of the paleosols created according to various models of a pedogenesis in the territory of Altai Mountains the indicators that are most often used at paleosols diagnostics — the characteristics of humus substances groups were used. Humus characteristics of the paleosols most widespread in a Late Pleistocene in the territory of Altai have been considered. It has allowed revealing that average humus parameters of various types and subtypes of paleosols, concerned to synlithogenous and postlithogenous models of soil formation, are similar.Key words: paleoecological reconstruction, synlithogenous and postlithogenous soil formation, humic substances of paleosols.

Download
References:

1. Targulian V.O. Soil memory: formation, carriers, and existential diversity // Soil in Memory: Soil as a Memory of Biosphere-Geosphere-Anthroposphere Interactions. — Moscow, LKI Publishers, 2008. — P. 24–57 (in Russian).

2. Birkeland P.W. Soils and Geomorphology. — New York: Oxford University Press, 1999. — 430 pp.

3. Kraus M.J. Paleosols in clastic sedimentary rocks: their geologic applications // Earth-Science Reviews. — 1999. — V. 47. — P. 41–70.

4. Retallack G.J. Soils of the Past. An Introduction to Paleopedology. — Oxford: Blackwell Science, 2001. — 404 pp.

5. Yaalon D.H. Soil Forming processes in time and space // Paleopedology. — Jerusalem, Israel University Press, 1971. — P. 29–39.

6. Dergacheva M.I. Archaeological Pedology. — Novosibirsk: Siberian Branch, Russian Academy of Sciences, 1997. — 231 p. (in Russian).

7. Dergacheva M.I. Humus as a Carrier of Soil Memory // Soil in Memory: Soil as a Memory of Biosphere-Geosphere-Anthroposphere Interactions. — Moscow, LKI Publishers, 2008. — P. 530–560 (in Russian).

8. Volkov I.A., Zykina V.S. The southern part of the West Siberian Plain (an environment according to studying of subaeral thickness) / /Development of landscapes and climate of Northern Eurasia: Late Pleistocene –Holocene; elements of forecast. — Moskow: Nauka, 1993. — v. 1. — P.32–36 (in Russian).

9. Morozova T.D. Development of a soil cover of Europe in Late Pleistocene. — Moskow: Nauka, 1981. — 281 pp. (in Russian).

10. Sirenko N.A., Turlo S.I. Development of soils and vegetation of Ukraine in Pliocene and a Pleistocene. — Kiev: Naukova dumka, 1986. — 186 pp. (in Russian).

11. Chlachula J., Rutter N.W., Evans M.E. A late Quaternary loess-paleosol record at Kurtak, southern Siberia // Canad. J. Earth Sci. — 1997. — v.34. — P.679–686.

12. Derbyshire E., Keen D., Kemp R.A. et al. Loess–palaeosol sequences as recorders of palaeoclimatic variations during the last glacial–interglacial cycle: some problems of correlation in North-Central China // Quaternary Proceedings. — 1995. — v. 4. — P. 7–18.

13. Velichko A.A., Morozova T.D., Nechaev V.P. et al. Loess-paleosol-cryogenic formation and structure near the northern limit of loess deposition, East European Plain, Russia // Quaternary International. — 2006. — v. 152-153. — P. 25–41.

14. Dergacheva M.I. Diagnostics and reconstruction of paleoecological conditions by a pedohumic method // Methodical approaches to use of biological indicators in a palaeoecology. — Kazan: Kazan University, 2011. — P. 193–239 (in Russian).

15. Dergacheva M.I. Pedohumic method in paleoenvironmental reconstructions: an example from Middle Siberia // Quaternary International. — 2003. — v. 106-107. — P. 73-78.

16. Dergacheva M., Fedeneva I., Bazhina N., Nekrasova O., Zenin V. Shestakovo site of Western Siberia (Russia): pedogenic features, humic substances and paleoenvironment reconstructions for last 20–25 ka // Quaternary International. 2016. Vol. 420. P. 199–207. DOI 10.1016/j.quaint.2015.10.087.

17. Archaeology, geology and Paleogeography of Pleistocene and Holocene of Gorny Altai / Derevyanko A.P., Agadjanian A.K., Baryshnikov G.F., Dergacheva M.I. et al. — Novosibirsk: Institute of Archaeology and Ethnography Siberian Branch, Russian Academy of Sciences, 1998. — 176 pp. (in Russian).

18. Dergacheva M.I., Derevyanko A.P., Fedeneva I.N. Evolution of the environment of Altai Mountains in Late Pleistocene and Holocene (reconstruction on signs of a pedogenesis). — Novosibirsk: Institute of Archaeology and Ethnography Siberian Branch, Russian Academy of Sciences, 2006. — 144 pp. (in Russian).

19. The Problems of paleoecology, geology and archaeology of the Paleolithic of Altai Mountains / Derevyanko A.P., Glinskiy S.V., Dergacheva, M.I. et al. — Novosibirsk: Institute of Archaeology and Ethnography Siberian Branch, Russian Academy of Sciences, 1998. — 312pp (in Russian, resume of each chapter in English).


About this article

Authors: Fedeneva I.N., Dergacheva M.I.

Year: 2017

doi: 10.25198/1814-6457-208-95

Editor-in-chief
Sergey Aleksandrovich
MIROSHNIKOV

Crossref
Cyberleninka
Doi
Europeanlibrary
Googleacademy
scienceindex
worldcat
© Электронное периодическое издание: ВЕСТНИК ОГУ on-line (VESTNIK OSU on-line), ISSN on-line 1814-6465
Зарегистрировано в Федеральной службе по надзору в сфере связи, информационных технологий и массовых коммуникаций
Свидетельство о регистрации СМИ: Эл № ФС77-37678 от 29 сентября 2009 г.
Учредитель: Оренбургский государственный университет (ОГУ)
Главный редактор: С.А. Мирошников
Адрес редакции: 460018, г. Оренбург, проспект Победы, д. 13, к. 2335
Тел./факс: (3532)37-27-78 E-mail: vestnik@mail.osu.ru
1999–2024 © CIT OSU