Scientific contribution of G.I. Rychagov to the study of the Caspian Sea and its' basin

Cover Page

Cite item

Full Text

Open Access Open Access
Restricted Access Access granted
Restricted Access Subscription Access

Abstract

Based on many years of geomorphological studies over the coast of the largest lake in the world, the outstanding Russian geomorphologist G.I. Rychagov formulated the idea of the Caspian Sea as a complex self-regulating system in which the altitude position of the basin level is determined not only by the values of the components of the water balance, but also by the topography of the bottom and the land adjacent to its' water area. Regarding the modern (Holocene) stage of its' development, the author determined the amplitude of level fluctuations in the range of absolute values from –25 to –30 m. The long-term forecast for the development of the Caspian Sea level was justified twice during the author’s lifetime. The experience of paleogeographical studies of the Caspian coast allowed G.I. Rychagov to formulate and solve a number of scientific and methodological issues. First of all, it showed the high information content of geomorphological data and geomorphological analysis in paleogeographical and forecasting work. Thus, data on the depths of incision of the mouth areas of the valleys of small rivers flowing into the Caspian Sea, in addition to the heights of the surfaces of the Neo-Caspian marine terraces, turned out to be excellent indicators of the magnitude of sea level fluctuations. The close connection between the development of the Caspian Sea and the processes in its' basin required a detailed study of its' largest part – the Volga River basin. The key site here was the Satinsky educational and scientific polygon in the basin of the middle reaches of the Protva River. Many years of comprehensive work under the leadership of G.I. Rychagov made the Satinsky polygon one of the most studied geologically and geomorphologically in the central region of the East European Plain. The geomorphological and complex paleogeographical method of studying the relief of the territory and the Middle-Upper Neopleistocene strata composing it allow us to consider the test site as a stratotypic area for the Middle Neopleistocene of the region. The independence of two glaciations of the Middle Neopleistocene – Moscow and Dnieper – was shown.

Full Text

Restricted Access

About the authors

A. V. Bredikhin

Lomonosov Moscow State University

Email: KuzMiArGeo@yandex.ru
Russian Federation, Moscow

S. I. Bolysov

Lomonosov Moscow State University

Email: KuzMiArGeo@yandex.ru
Russian Federation, Moscow

S. I. Antonov

Lomonosov Moscow State University

Email: KuzMiArGeo@yandex.ru
Russian Federation, Moscow

M. A. Kuznetsov

Lomonosov Moscow State University

Author for correspondence.
Email: KuzMiArGeo@yandex.ru
Russian Federation, Moscow

References

  1. Afanasyev A.N. (1967). Kolebaniya gidrometeorologicheskogo rezhima na territorii SSSR (Fluctuations in the hydrometeorological regime on the territory of the USSR). M.: Nauka (Publ.). 232 p. (in Russ.)
  2. Antonov S.I., Rychagov G.I., Malaeva E.M. et al. (2000). Climatostratigraphic units of the Moscow horizon of the southwestern Moscow region. Stratigrafija. Geologicheskaya korrelyatsiya. Iss. 8. № 3. P. 100–112. (in Russ.)
  3. Antonov S.I., Rychagov G.I., Sudakova N.G. (2004). Middle Pleistocene glaciations of the Center of the Russian Plain. Byulleten’ komissii po izucheniyu chetvertichnogo perioda. № 65. P. 5–16. (in Russ.)
  4. Antonov S.I., Rychagov G.I. (1993). Fluvial lithomorphogenesis in the Protva river basin. Vestnik Moskovskogo Universiteta. Seriya. 5. Geografiya. № 6. P. 68–76. (in Russ.)
  5. Antonov S.I., Rychagov G.I., Sudakova N.G. (1991). On the question of Middle Pleistocene stratigraphy of the Moscow region. Vestnik Moskovskogo Universiteta. Seriya. 5. Geografiya. № 6. P. 24–31. (in Russ.)
  6. Bezrodnykh Y., Yanina T., Sorokin V. et al. (2020). The Northern Caspian Sea: Consequences of climate change for level fluctuations during the Holocene. Quat. Int. № 540. P. 68–77. https://doi.org/10.1016/j.quaint.2019.01.041
  7. Birjukov I.P., Faustova M.A., Shik S.M. (2001). Central sector of the ice sheet. In: Oledeneniya srednego pleistotsena Vostochnoi Evropy. M.: GEOS (Publ.). P. 31–36. (in Russ.)
  8. Elektronnyi atlas Kaspiiskogo morya (Electronic atlas of the Caspian Sea) [Electronic data]. Access way: http://de.geogr.msu.ru/casp/ (access date: 23.02.2024).
  9. Gelfan A., Panin A., Kalugin A. et al. (2024). Hydroclimatic processes as the primary drivers of the Early Khvalynian transgression of the Caspian Sea: new developments. Hydrol. Earth Syst. Sci. V. 28. P. 241–259. https://doi.org/10.5194/hess-28-241-2024
  10. Gvozdeckiy N.A., Zhuchkova V.K. (Eds.). (1963). Fiziko-geograficheskoe raionirovanie nechernozemnogo tsentra (Physico-geographical zoning of the non-chernozem center). Moscow: MGU (Publ.). 451 p. (in Russ.)
  11. Hoogendoorn R.M., Boels J.F., Kroonenberg S.B. et al. (2005). Development of the Kura Delta, Azerbaijan; a record of Holocene Caspian sea-level changes. Mar. Geol. V. 222–223. P. 359–380. https://doi.org/10.1016/j.margeo.2005.06.007
  12. Ignatov E.I., Kaplin P.A., Lukyanova S.A., Solovyova G.D. (1992). Recent Caspian transgression: impact on the coastal dynamics. Geomorphologiya. No. 1. P. 12–21.
  13. Kakroodi A.A., Leroy S.A.G., Kroonenberg S.B. et al. (2015). Late Pleistocene and Holocene sea-level change and coastal paleoenvironment evolution along the Iranian Caspian shore. Mar. Geol. V. 361. № 1. P. 111–125. https://doi.org/10.1016/j.margeo.2014.12.007
  14. Koordinatsionnyi komitet po gidrometeorologii Kaspiiskogo morya (KASPKOM) (Coordination Committee for Hydrometeorology of the Caspian Sea (CASPCOM)). [Electronic data]. Access way: https://www.caspcom.com/files/CASPCOM%20Bulletin%20No.%2026_1.pdf (access date 22.03.2024).
  15. Koriche S.A., Singarayer J.C., Valdes P.J. et al. (2022). What are the drivers of Caspian Sea level variation during the late Quaternary? Quat. Sci. Rev. № 283. P. 1–19. https://doi.org/10.1016/j.quascirev.2022.107457
  16. Kosarev A.N., Kuraev A.V., Nikonova R.E. (1996). Features of modern hydrological conditions of the Northern Caspian Sea. Vestnik Moskovskogo Universiteta. Seriya. 5. Geografiya. № 5. P. 47–53. (in Russ.)
  17. Kroonenberg S.B., Abdurakhmanov G.M., Badyukova E.N. et al. (2007). Solar-forced 2600 BP and Little Ice Age highstands of the Caspian Sea. Quat. Int. V. 173. P. 137–143. https://doi.org/10.1016/j.quaint.2007.03.010
  18. Lahijani H., Leroy S.A.G., Arpe K. et al. (2023). Caspian Sea level changes during instrumental period, its impact and forecast: A review. Earth-Sci. Rev. V. 241. Article 104428. https://doi.org/10.1016/j.earscirev.2023.104428
  19. Lilienberg D.A. (1988). Geomorphological-geodynamic direction in assessing the mobility of morphostructures and variability of the earth’s surface. Izvestiya AN SSSR. Seriya geograficheskaya. № 6. P. 110–120. (in Russ.)
  20. Maev E.G. (1993). Fluctuations in the level of the Caspian Sea: the role of geological factors. Vestnik Moskovskogo Universiteta. Seriya. 5. Geografiya. № 4. P. 49–56. (in Russ.)
  21. Mamedov A.M. (1976). Types of manifestation of mud volcanoes in the South Caspian depression. Doklady AN AzSSR. Iss. 32. № 5. P. 25–29. (in Russ.)
  22. Mihailov V.N., Korotaev V.N., Rychagov G.I. et al. (Eds.). (2013). Ust’ya rek Kaspiiskogo regiona: istoriya formirovaniya, sovremennye gidrologo-morfologicheskie protsessy i opasnye gidrologicheskie yavleniya (River mouths of the Caspian region: history of formation, modern hydrological and morphological processes and dangerous hydrological phenomena). M.: GEOS (Publ.). 703 p. (in Russ.)
  23. Mihajlov V.N., Povalishnikova E.S. (1998). Once again about the reasons for changes in the level of the Caspian Sea in the twentieth century. Vestnik Moskovskogo Universiteta. Seriya. 5. Geografiya. № 3. P. 35–38. (in Russ.)
  24. Naderi Beni A., Lahijani H., Mousavi Harami R. et al. (2013). Caspian Sea level changes during the last millennium: historical and geological evidences from the south Caspian Sea. Climate of the Past. V. 52. № 1. P. 1645–1665. https://doi.org/10.5194/cp-9-1645-2013
  25. Overeem I., Kroonenberg S.B., Veldkamp A. et al. (2003). Small-scale stratigraphy in a large ramp delta: Recent and Holocene sedimentation in the Volga delta, Caspian Sea. Sediment. Geol. V. 159. № 3–4. P. 133–157. https://doi.org/10.1016/S0037-0738(02)00256-7
  26. Panin A.V., Sidorchuk A.Yu., Ukraintsev V.Yu. (2021). The contribution of glacial melt water to annual runoff of Volga River in the Last Glacial Epoch. Water resources. V. 48. P. 877–885. https://doi.org/10.31857/s0321059621060146
  27. Rodkin M.V., Kostjejn Dzh. K. (1995). On the relationship between the Caspian water balance and groundwater regime and seismicity. In: Sbornik referatov Mezhdunarodnoi konferentsii “Kaspiiskii region: ekonomika, ekologiya, mineral’nye resursy. Moskva, iyun’ 20-23, 1995. Moscow: P. 42. (in Russ.)
  28. Rozanov L.L. (1982). On the capacity of the Caspian Sea basin in the Holocene. Izvestiya AN SSSR. Seriya geograficheskaya. № 2. P. 114–122. (in Russ.)
  29. Rychagov G.I., Antonov S.I., Gunova V.S. et al. (2019). Development of the Protva River valley in the Late Neopleistocene. Vestnik Moskovskogo Universiteta. Seriya. 5. Geografiya. № 4. P. 88–99. (in Russ.)
  30. Rychagov G. I., Antonov S.I., Sudakova N.G. (2007). Glacial rhythms of the Middle Pleistocene of the Center of the Russian Plain (based on materials from the Satin stratoregion). Vestnik Moskovskogo Universiteta. Seriya. 5. Geografiya. № 4. P. 15–22. (in Russ.)
  31. Rychagov G.I, Antonov S.I. (Eds.). (1992). Kompleksnyi analiz srednechetvertichnykh otlozhenii Satinskogo uchebnogo poligona: Uchebnoye posobie (Complex analysis of mid-Quaternary deposits of the Satinskii training site: Textbook). Moscow: MGU (Publ.). 128 p. (in Russ.)
  32. Rychagov G.I, Antonov S.I. (Eds.). (1996). Stroenie i istoriya razvitiya doliny r. Protvy (The structure and history of the development of the Protva River Valley). Moscow: MGU (Publ.). 129 p. (in Russ)
  33. Rychagov G.I, Antonov S.I. (Eds.). (2001). Uchebno-nauchnye geograficheskie stantsii vuzov Rossii (Educational and scientific geographical stations of Russian universities). Moscow: Geograficheskii facultet (Publ.). 589 p. (in Russ.)
  34. Rychagov G.I. (1993). Level regime of the Caspian Sea over the last 10,000 years. Vestnik Moskovskogo Universiteta. Seriya. 5. Geografiya. № 2. P. 38–49. (in Russ.)
  35. Rychagov G.I. (1997). Pleistotsenovaya istoriya Kaspiiskogo morya (Pleistocene history of the Caspian Sea). Moscow: MGU (Publ.). 268 p. (in Russ.)
  36. Rychagov G.I. (2011). Fluctuations in the level of the Caspian Sea: causes, consequences, forecast. Vestnik Moskovskogo Universiteta. Seriya. 5. Geografiya. № 2. P. 4–12. (in Russ.)
  37. Rychagov G.I. (2016). The Hyrcanian stage in the history of the Caspian Sea. Geomorfologiya. № 1. P. 3–17. (in Russ). https://doi.org/10.15356/0435-4281-2016-1-3-17
  38. Rychagov G.I. (2017). A geographical approach to the reconstruction of paleogeographic events. Byulleten’ komissii po izucheniyu chetvertichnogo perioda. № 75. P. 112–134. (in Russ.)
  39. Rychagov G.I. (2019). To the methods of geomorphological research (geomorphological lessons of the Caspian). Geomorfologiya. № 4. P. 27–39. (in Russ.). https://doi.org/10.31857/S0435-42812019427-39
  40. Rychagov G.I., Aleshinskaja Z.V., Antonov S.I. et al. (1989). New sections of Mikulin deposits in the center of the Russian Plain. In: Chetvertichnyi period. Stratigrafiya. XXVIII sessiya Mezhdunaradnogo Geologicheskogo Kongressa. M.: Nauka (Publ.). P. 35–42. (in Russ.)
  41. Rychagov G.I., Antonov S.I., Sudakova N.G. (2012). On glacial stratigraphy and paleogeography of the center of the East European Plain. Vestnik Moskovskogo Universiteta. Seriya 5. Geografiya. № 1. P. 36–44. (in Russ.)
  42. Rychagov G.I., Mihajlov V.N., Povalishnikova E.S. (1999). Is environmental and economic damage inevitable in conditions of instability of the Caspian Sea level? Vestnik Moskovskogo Universiteta. Seriya 5. Geografiya. № 5. P. 47–55. (in Russ.)
  43. Shik S.M. (1985). Problems of correlation of lower Quaternary sediments of the Don glacial tongue region and the Moscow region. In: Kraevye obrazovaniya materikovykh oledenenii. Materialy VII Vsesoyuznogo soveshchaniya. Moscow: Nauka (Publ.). P. 183–185. (in Russ.)
  44. Shik S.M., Birjukov I.P. (1989). Lower and Middle Pleistocene stratigraphy of the central regions of the European territory of the USSR. In: Chetvertichnyi period. Stratigrafiya. XXVIII sessiya Mezhdunarodnogo Geologicheskogo Kongressa. Moscow: Nauka (Publ.). P. 27–35. (in Russ.)
  45. Shilo N.A. (1989). The nature of Caspian level fluctuations. Doklady AN SSSR. Iss. 305. № 2. P. 412–416. (in Russ.)
  46. Shtejenberg V.V. (1981). Ground motion near the source of an earthquake. Izvestiya AN AzSSR. Seriya: Fizika Zemli. № 6. P. 18–31. (in Russ.)
  47. Sidorchuk A.Yu., Panin A.V., Borisova O.K. (2008). Climate-induced changes in surface runoff on the North-Eurasian plains during the late glacial and Holocene. Water Resources. V. 35. P. 386-396. https://doi.org/10.1134/S0097807808040027
  48. Sidorchuk A.Yu., Ukraintsev V.Yu., Panin A.V. (2021). Estimating annual Volga runoff in the Late Glacial Epoch from the size of river paleochannels. Water resources. V. 48. P. 864–876. https://doi.org/10.31857/S0321059621060171
  49. Sudakova N.G., Antonov S.I., Vvedenskaya A.I. et al. (2013). Paleogeographical patterns of development of morpholithosystems of the Russian Plain. Raionirovanie. Stratigrafiya. Geoekologiya. Moscow: Geograficheskii facul’tet MGU (Publ.). 96 p. (in Russ.)
  50. Sudakova N.G., Rychagov G.I., Antonov S.I. et al. (2008). Rekonstruktsiya paleogeograficheskikh sobytii srednego neopleistotsena Tsentra Russkoi ravniny (Reconstruction of paleogeographic events of the Middle Neopleistocene of the Center of the Russian Plain). Moscow: Geograficheskii facul’tet MGU (Publ.). 167 p. (in Russ.)
  51. Svitoch A.A. (2015). Paleogeography of the Greater Caspian Sea. Vestnik Moskovskogo Universiteta. Seria 5. Geografia. № 4. P. 69–80. (in Russ.)
  52. Tekhniko-ekonomicheskii doklad po zashchite narodno-khozyaistvennykh ob”ektov i naselennykh punktov pribrezhnoi polosy v predelakh Dagestanskoi ASSR, Kalmytskoi ASSR i Astrakhanskoi oblasti ot navodnenii v svyazi s povysheniem urovnya Kaspiiskogo morya. Osnovnye polozheniya (Technical and economic report on the protection of national economic facilities and settlements of the coastal strip within the Dagestan Autonomous Soviet Socialist Republic, the Kalmyk Autonomous Soviet Socialist Republic and the Astrakhan Region from floods due to rising levels of the Caspian Sea. Basic provisions). (1992). Moscow: Jekopros (Publ.). 48 p. (in Russ.)
  53. Velichko A.A. (1980). On the age of moraines of the Dnieper and Don glacial tongues. In: Vozrast i rasprostranenie maksimal’nogo oledeneniya Vostochnoi Evropy. Moscow: Nauka (Publ.). P. 7–19. (in Russ.)
  54. Velichko A.A., Udarcev V.P., Morozova T.D. et al. (1977). On the different ages of moraines of the Dnieper and Don blades of the cover glaciation of the East European Plain. Doklady AN SSSR. Iss. 232. № 5. P. 1142–1145. (in Russ.)
  55. Yanina T.A., Sorokin I.M., Bezrodnykh Yu.P., et al. (2014). The Hyrcanian stage in the Pleistocene history of the Caspian Sea. Vestnik Moskovskogo Universiteta. Seriya 5. Geografiya. № 3. P. 3–9. (in Russ),
  56. Yanina T.A., Sorokin I.M., Bezrodnykh Yu.P., Romanyuk B. (2018). Late Pleistocene climatic events reflected in the Caspian Sea geological history (based on drilling data). Quat. Int. V. 465. Part A. P. 130–141.

Supplementary files

Supplementary Files
Action
1. JATS XML
Download
2. Fig. 1. Georgy Ivanovich Rychagov (1924–2020)

Download (95KB)
Indexing metadata
3. Fig. 2. The Caspian Sea level oscillations: (а) – during the Neopleistocene (Rychagov, 1997). The main stages of the history of the Caspian Sea: 1 – baku, 2 – khazar, 3 – early khvalynian, 4 – late khvalynian, 5 – neo-caspian (horizontal scale is arbitrary); (б) – in the Holocene (Rychagov, 1993). Stages of the neo-caspian transgression: 1 – initial (the longest one), 2 – maximal (turalinskaya), 3 – ulluchaiskaya, 4 – modern one. The letters indicate: M – mangyshlakskaya regression; D – derbentskaya regression; H – zone of the natural sea-level oscillations during Sub-atlantic stage of the Holocene (“zone of risk”); (в) – during the 20th century (Makhachkala); (г) – during the year

Download (178KB)
Indexing metadata
4. Fig. 3. Perennial oscillations (1900–1997): 1 – of the average annual Volga water discharge at the delta apex near Upper Lebiajiy village; 2 – of Volga water discharge under sliding 6-year average; 3 – average annual water levels (in absolute heights) in the Caspian Sea (Makhachkala); 4 – difference integral curve of Volga runoff (Mikhailov, Povalishnikova, 1998)

Download (204KB)
Indexing metadata
5. Fig. 4. Change in the direction of the prevailing winds (arrows above) at different stages of the Neo-Caspian transgression. 1 – initial (longest); 2 – maximal (turalinskaya); 3 – ulluchayskaya; 4 – modern. The letters indicate: M – mangyshlak regression; D – derbent regression, H – “risk zone” (zone of natural sea level fluctuations in the sub-atlantic stage of the Holocene) (Rychagov, 1997, with additions)

Download (68KB)
Indexing metadata
6. Fig. 5. Geology-geomorphologic structure and hypsometric position of basal horizons of the Neo-Caspian terraces in the near-mouth sites of river valleys: (a) – Rubaschay (Daghestan), (б) – Ulluchay (Daghestan), (в) – Atachay (Azerbaijan) under sea-level –28.6 m (Rychagov, 1997)

Download (145KB)
Indexing metadata
7. Fig. 6. “Risk zone” of modern Caspian Sea level fluctuations (50–100 years) (http://de.geogr.msu.ru/casp/)

Download (870KB)
Indexing metadata
8. Fig. 7. Scheme of transgressive development of the coastal zone of the Caspian Sea (Ignatov et al., 1992, with additions by G.I. Rychagov (2019)): (a) – with slopes of the underwater coastal slope <0.0001; (б) – from ~0.0005 to 0.001; (в) – from ~0.005 to 0.01; (г) – >0.01. Legend: 1 – initial position of the sea level; 2 – transgressive sea level; 3 – erosion lenses; 4 – sediment accumulation; 5 – previous shore profile; 6 – modern shore profile

Download (135KB)
Indexing metadata
9. Fig. 8. Overview map of the Satino stratigraphical area. 1 – forests; 2 – meadows; 3 – swamps; 4 – populated areas; 5 – geodetic signs; 6 – main support geological cuts; 7 – boreholes (a – geological, б – hydrogeological); 8 – position of the Satino educational and scientific station; 9 – line of the profile shown in fig. 9 (Sudakova et al., 2008)

Download (975KB)
Indexing metadata
10. Fig. 9. Geological-geomorphological profile II–II (village Benitsy – village Butovka): 1 – boulders; 2 – gravel and pebbles; 3 – sand; 4 – silt; 5 – clay; 6 – loam; 7 – cover loam; 8 – foliated marl; 9 – limestone; boulder loams (moraine): 10 – late (Kaluga) stage of the Middle Pleistocene Moscow glaciation, 11 – early (Borovskaya) stage of the Moscow glaciation, 12 – Middle Pleistocene Dnieper glaciation, 13 – Lower Pleistocene Oka glaciation; 14 – ground wedges and cryoturbation; 15 – buried soils; 16 – lower boundary of the Moscow horizon; 17 – stratigraphic boundaries (a – reliable, б – estimated); 18 – geological workings (a – boreholes, б – clearing); 19 – absolute TL and RTL dating, ka (Sudakova et al., 2008)

Download (460KB)
Indexing metadata
11. Fig. 10. Correlation table of the Chekalinsky and Satinsky summary sections. For symbols, see fig. 9 (Rychagov et al., 2007)

Download (986KB)
Indexing metadata
12. Fig. 11. Proposed scheme of stratigraphic units of the Middle Neopleistocene of the Center of the Russian Plain (Sudakova et al., 2008)

Download (81KB)
Indexing metadata
13. Fig. 12. Location of objects for studying recent deposits in the central region of the Russian Plain. 1 – strator districts (I – Chekalinsky, II – Satinsky, III – Moscow, IV – Klinsko-Dmitrovsky, V – Verkhnevolzhsky, VI – Rostovsky); 2 – Satinsky training ground; boundaries of glaciations: 3 – Moscow, 4 – Kalinin, 5 – Ostashkov. (Sudakova et al., 2013)

Download (222KB)
Indexing metadata

Copyright (c) 2024 Russian Academy of Sciences

Согласие на обработку персональных данных с помощью сервиса «Яндекс.Метрика»

1. Я (далее – «Пользователь» или «Субъект персональных данных»), осуществляя использование сайта https://journals.rcsi.science/ (далее – «Сайт»), подтверждая свою полную дееспособность даю согласие на обработку персональных данных с использованием средств автоматизации Оператору - федеральному государственному бюджетному учреждению «Российский центр научной информации» (РЦНИ), далее – «Оператор», расположенному по адресу: 119991, г. Москва, Ленинский просп., д.32А, со следующими условиями.

2. Категории обрабатываемых данных: файлы «cookies» (куки-файлы). Файлы «cookie» – это небольшой текстовый файл, который веб-сервер может хранить в браузере Пользователя. Данные файлы веб-сервер загружает на устройство Пользователя при посещении им Сайта. При каждом следующем посещении Пользователем Сайта «cookie» файлы отправляются на Сайт Оператора. Данные файлы позволяют Сайту распознавать устройство Пользователя. Содержимое такого файла может как относиться, так и не относиться к персональным данным, в зависимости от того, содержит ли такой файл персональные данные или содержит обезличенные технические данные.

3. Цель обработки персональных данных: анализ пользовательской активности с помощью сервиса «Яндекс.Метрика».

4. Категории субъектов персональных данных: все Пользователи Сайта, которые дали согласие на обработку файлов «cookie».

5. Способы обработки: сбор, запись, систематизация, накопление, хранение, уточнение (обновление, изменение), извлечение, использование, передача (доступ, предоставление), блокирование, удаление, уничтожение персональных данных.

6. Срок обработки и хранения: до получения от Субъекта персональных данных требования о прекращении обработки/отзыва согласия.

7. Способ отзыва: заявление об отзыве в письменном виде путём его направления на адрес электронной почты Оператора: info@rcsi.science или путем письменного обращения по юридическому адресу: 119991, г. Москва, Ленинский просп., д.32А

8. Субъект персональных данных вправе запретить своему оборудованию прием этих данных или ограничить прием этих данных. При отказе от получения таких данных или при ограничении приема данных некоторые функции Сайта могут работать некорректно. Субъект персональных данных обязуется сам настроить свое оборудование таким способом, чтобы оно обеспечивало адекватный его желаниям режим работы и уровень защиты данных файлов «cookie», Оператор не предоставляет технологических и правовых консультаций на темы подобного характера.

9. Порядок уничтожения персональных данных при достижении цели их обработки или при наступлении иных законных оснований определяется Оператором в соответствии с законодательством Российской Федерации.

10. Я согласен/согласна квалифицировать в качестве своей простой электронной подписи под настоящим Согласием и под Политикой обработки персональных данных выполнение мною следующего действия на сайте: https://journals.rcsi.science/ нажатие мною на интерфейсе с текстом: «Сайт использует сервис «Яндекс.Метрика» (который использует файлы «cookie») на элемент с текстом «Принять и продолжить».