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Aeolian landscapes of Prebaikalye and Transbaikalye areas

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Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Aeolian landscapes are typical of the area of Prebaikalye and Transbaikalye. They occur both on the shore of Baikal and at various distances from the lake and they are related to areas of boreal forest and steppe. They are characterized by both natural and anthropogenic origin. The former are more typical of Transbaikalye, where they represent old dune forms at different stages of formation, stabilized by pine forest vegetation. These landscapes probably originated at the end of the Pleistocene and the beginning of the Holocene. Anthropogenic aeolian landscapes are more clearly visible and noticeable because of the geomorphologic processes occurring there at present. They occur in both of the regions and they are related to diverse economic activities of man in the past hundred, up to two hundred, years. The dominating type of surface features is that of wind erosion, which is related to old forms being blown away. The accumulative effect of wind is definitely of minor significance there; this can be seen in minor size and diversity of forms. Vegetation, which is clearly psammophylous, adapts itself to these contemporary aeolian processes. This is mostly herbaceous vegetation, or less often shrubs or undershrub. It creates a range of plant communities and associations, frequently of unique nature and with peculiar features of adaptation of plants to life in heavy habitat conditions.
Słowa kluczowe
Rocznik
Tom
Strony
216--230
Opis fizyczny
Bibliogr. 23 poz., rys.
Twórcy
  • Buryat State University, Department of Botany, Ulan-Ude, Russia
autor
  • V. B. Sochava Institute of Geography, Siberian Branch of RAS, Irkutsk, Russia
autor
  • University of Silesia, Faculty of Earth Sciences, Sosnowiec, Poland
autor
  • University of Silesia, Faculty of Biology and Environment Protection, Katowice, Poland
Bibliografia
  • [1] Agafonov B. P., 2002: Vetrovoy litopotok iz ozera Baikal. Doklady Akademii nauk, 382, 5: 688–691.
  • [2] Bazarov D. B., Ivanov A. D., 1957: Sypuchie peski Bryat-Mongolskoy ASSR i mery bor’by s nimi. Buryat-Mongolskoe knizhn. izdat., Ułan-Ude: pp. 85.
  • [3] Bazhenova O. I., Lyubtsova E. M., Ryzhov Yu. V., Makarov S. A., 1997: Prostranstvenno-vremennoy analiz dinamiki erozionnykh processov na yuge Vostochnoy Sibiri. Nauka, Novosibirsk: pp. 208.
  • [4] Chak W. A., 2006: Niektóre cechy rozwoju procesu eolicznego na różnych odcinkach linii brzegowej Zbiornika Brackiego. In: Morfologiczne i sedymentologiczne skutki działalności wiatru. SGP, Poznań: 17–22.
  • [5] Imetkhenov A. B., 1994: Katastroficheskiye yavleniya v beregovoy zone Baikala. Ulan-Ude: pp. 65.
  • [6] Kornutova E. I., Khotina E. B., Zamoruev V. V., 1975: Verkhnepliocenovye i pleistocenovye otlozheniya yuga Zabaikalya. Nedra, Moskva: pp. 136.
  • [7] Obruchev V. A., 1912: Sypuchie peski Selenginskoy Daurii i neobkhodimost’ ikh skoreyshego izuchenia. Trudy Troitskosavsko-Kyakhtinskogo otdela RGO, 15, 3: 53–67.
  • [8] Osadchiy S. S., 1995: Sledy maksimalnoy transgresii Baikala. Geografiya i prirodnye resursy, 4: 179–189.
  • [9] Ovchinnikov G. I., 1998: Nekotorye zakonomernosti raspredeleniya nanosov na osushennykh otmelyakh i beregovykh sklonakh Bratskogo vodokhranilishcha pod vozdeistviem vetrovykh i volnovykh faktorov. In: Współczesne procesy eoliczne. WNoZ UŚ, SGP, Sosnowiec: 61–72.
  • [10] Ovchinnikov G. I., Snytko V. A., Szczypek T., 2002: Barchan on the Argada river (Transbaikalya – Eastern Siberia). Geomorphologia Slovaca, 2, 1. Bratislava: 45-49.
  • [11] Ovchinnikov G. I., Snytko V. A., Szczypek T., Wika S., 2004: The barchan landscape on the Argada river in Barguzin Basin (Transbaikalya). Quaestiones Geographicae, 23. UAM, Poznań: 55-62.
  • [12] Szczypek T., Wika S., Snytko V. A., Buyantuyev A. B., 2000: Facii razvevayemykh peskov Chikoy-Selenginskogo mezhurechya w Zapadnom Zabaikalye. IG SO RAN, Irkutsk: pp. 71.
  • [13] Szczypek T., Wika S., Snytko V. A., Ovchinnikov G. I., Namzalov B.-Ts. B., Dambiev E. Ts., 2005: Eolovoye urochishche Mankhan Elysu v Zabaikalye. IG SO RAN, IZK SO RAN, BGU, Irkutsk-Ulan-Ude: 62 pp.
  • [14] Szczypek T., Wika S., Snytko V. A., Ovchinnikov G. I., Vyrkin V. B., Buyantuev V. A., 2002: Eolovye urochishcha yuzhnoy chasti Barguzinskoy kotloviny (Zabaikalye). IG SO RAN, IZK SO RAN, Irkutsk: pp. 52.
  • [15] Vyrkin V. B., 1986: Sovremennoe eolovoe rel’efoobrazovanie v Barguzinskoy kotlovine. Geografiya i prirodnye resursy, 2: 71–77.
  • [16] Vyrkin V. B., 1998: Sovremennoe ekzogennoe rel’efoobrazovanie kotlovin baikalskogo tipa. IG SO RAN, Irkutsk: pp. 175.
  • [17] Wika S., Imetkhenov A. B., Ovchinnikov G. I., Snytko V. A., Szczypek T., 2006: Eolovye i abrazionnye processy poberezhiy u Zaliva Proval na Baikale. IZK SO RAN, IG SO RAN, BGU, Irkutsk-Ulan-Ude: pp. 56.
  • [18] Wika S., Kozyreva E. A., Trzcinskij Yu. B., Szczypek T., 2006: Ostrova Yarki na Baikale–primer sovremennogo prezobrazovaniya landshaftov. IZK SO RAN, Silezskiy universitet, Irkutsk-Sosnowiec: pp. 69.
  • [19] Wika S., Martyanova G. N., Snytko V. A., Szczypek T., 1999: Bukhta Peschanaya na Baikale (razvevayemye peski i ikh okruzhenie). IG SO RAN, Irkutsk: pp. 60.
  • [20] Wika S., Namzalov B.-C.B., Ovchinnikov G. I., Snytko V. A., Szczypek T., 2003: Prostranstvennaya struktura eolovykh urochishch vostochnogo poberezhya ozera Baikal. IG SO RAN, IZK SO RAN, Irkutsk: pp. 76.
  • [21] Wika S., Ovchinnikov G. I., Snytko V. A., Szczypek T., 2002: Eolovye facii vostochnogo poberezhya Baikala. IG SO RAN, IZK SO RAN, Irkutsk: pp. 56.
  • [22] Wika S., Ovchinnikov G. I., Trzcinskij Yu. B., Tyc A., Szczypek T., 2000: Razvitie prirodnykh processov na beregakh Bratskogo vodokhranilishcha. IZK SO RAN, Irkutsk: pp. 72.
  • [23] Wika S., Snytko V. A., Szczypek T., 1997: Landshafty podvizhnykh peskov ostrova Olkhon na Baikale. IG SO RAN, Irkutks: pp. 63.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-3deefd30-aadc-440f-9b9b-717c16f7e5d2
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