References

geomorf

Геоморфология и палеогеография

Geomorfologiya i Paleogeografiya

2949-17892949-1797

10.31857/S0435428122030178

geomorf-2497

Research Article

Реконструкции на основе палеобиологических методов

Palaeoenvironmental reconstructions based on palaeobiological methods

Изменения окружающей среды Терского берега Белого моря (Кольский полуостров) в голоцене по данным комплексного изучения болота Кузоменский мох

Environmental changes in the Tersky Coast of White Sea (Kola Peninsula) during the Holocene inferred from multy-proxy study of the Kuzomen Moch peatland

Тимирева

С. Н.

Timireva

S. N.

Филимонова

Л. В.

Filimonova

L. V.

Зюганова

И. С.

Zyuganova

I. S.

Кононов

Ю. М.

Kononov

Yu. M.

Романенко

Ф. А.

Romanenko

F. A.

Институт географии РАНРоссияInstitute of Geography RASRussian Federation

Институт биологии Карельского научного центра РАНРоссияInstitute of Biology Karelian Research Centre RASRussian Federation

Московский государственный университет имени М.В. Ломоносова, географический факультетРоссияLomonosov Moscow State University, Faculty of GeographyRussian Federation

2022

04102022

533

Геоморфология

3950

2022

Тимирева С.Н., Филимонова Л.В., Зюганова И.С., Кононов Ю.М., Романенко Ф.А.

Timireva S.N., Filimonova L.V., Zyuganova I.S., Kononov Y.M., Romanenko F.A.

Данная работа распространяется под лицензией Creative Commons Attribution 4.0.

This work is licensed under a Creative Commons Attribution 4.0 License.

https://geomorphology.igras.ru/jour/article/view/2497

Реконструированы процесс заболачивания и история развития растительности за последние 8000 лет в западной части Терского берега (юг Кольского полуострова), в устье реки Варзуга по данным комплексного изучения торфяника Кузоменский Мох. Исследования включали спорово-пыльцевой и ботанический анализы торфа, измерения потерь при прокаливании, AMS радиоуглеродное датирование и морфоскопию песчаных кварцевых зерен. Установлено, что после дегляциации на территории исследований действовали эоловые процессы, позже сменившиеся заболачиванием. Согласно данным анализа морфоскопии песчаных кварцевых зерен, отложения, подстилающие торфяную толщу, имеют ледниковый и водно-ледниковый генезис, но впоследствии песчаные зерна частично были переработаны эоловыми процессами, на что указывают характерные текстуры на их поверхности, связанные с переносом частиц в воздушной среде. Накопление торфяной залежи началось не позднее 7865 ± 45 кал. (календарных) л. н., что может служить признаком затухания эоловых процессов на окружающей территории. На основе ботанического анализа торфа выявлены этапы эволюции болота от эвтрофной до олиготрофной стадии и показано, что развитие локальной растительности болота, очевидно, находилось под влиянием пожаров в период между 7800 и 2700 кал. л. н. Результаты спорово-пыльцевого анализа показали, что история растительности западной части Терского берега Белого моря в течение последних 8000 лет включала серию чередующихся фаз распространения березовых, сосново-березовых и сосновых лесов. Долгопериодная динамика растительности, возможно, была обусловлена изменениями климата и пожарной активности. Ель появилась в лесных сообществах изучаемой территории около 7000 кал. л. н., в течение последних 200 лет ее обилие в древостоях сократилось в результате антропогенного воздействия на растительный покров и пожаров.

This paper presents the first reconstruction of the paludification process and vegetation history during the last 8000 cal years BP in the western part of the Tersky Coast (south Kola Peninsula); in the River Varzuga mouth; based on multi-proxy studies of the Kuzomen Mokh peatland including high resolution pollen and plant macroremains analyses; loss on ignition measurements; AMS radiocarbon dating of the peat; and quartz grain morphoscopy analysis for sandy deposits underlying the peat sequences. The obtained data revealed that the paludification stage was preceded by aeolian processes occurred in the study area during the Late Glacial and Early Holocene. Analysis of quartz sand grain morphoscopy revealed that glacial and fluvioglacial sands underlying peat deposits in Kuzomen Mokh peatland were partly affected by aeolian processes that are indicated by specific textures on the surface of quartz sand grains typical for air transport. Peat accumulation started not later than 7865 ± 45 cal yr. BP assuming a decline of aeolian processes in the study area. Analysis of plant macroremains showed an evolution of mire from the poor fen to ombrotrophic rised bog. Local vegetation successions were obviously influenced by fire in the period between 7800 and 2700 cal yr. BP. According to pollen data vegetation history in the Tersky coast of the White Sea during the last 8000 cal yr. BP included a series of successive phases of birch; birch-pine and pine forests caused probably by climatic changes and fire activity. Picea appeared in the study area around 7000 cal yr. BP and reduced in abundance during the last 200 years due to human impact and fires.

Кольский полуостровзаболачиваниепалеоклиматические реконструкцииспорово-пыльцевой анализботанический состав торфаморфоскопия песчаных кварцевых зерен

Kola Peninsulapaludificationpaleoclimatic reconstructionspollen analysisplant macroremainsquartz grain morphoscopy

Russian Foundation for Basic Research (project No. 20-05-00082), Institute of Geography RAS (No. АААА-А19-119021990091-4 (FMGE-2019-0005)), Institute of Biology of Karelian Research Centre RAS (No. 122031700449-3), Dr. Elena Novenko

References1

Atlas Murmanskoi oblasti (Atlas of the Murmansk region). M.: Kartograficheskaya fabrika (Publ.), 1971. 33 p. (in Russ.)

Belov N.P. and Baranovskaya A.V. Pochvy Murmanskoi oblasti (Soils of the Murmansk Region). Leningrad: Nauka (Publ.), 1969. 148 p. (in Russ.)

Bengtsson L. and Enell M. Chemical analysis / Handbook of Holocene Palaeoecology and Palaeohydrology. 1986. P. 423–451. https://doi.org/10.1002/jqs.3390010111

Blaauw M. Methods and code for 'classical' age-modelling of radiocarbon sequences. Quaternary Geochronology. 2010. Vol. 5. P. 512–518. https://doi.org/10.1016/j.quageo.2010.01.002

Digital Plant Atlas. 2006: https://plantatlas.eu/

Dombrovskaya A.V., Koreneva M.M., and Tyuremnov S.N. Atlas rastitel’nyh ostatkov, vstrechaemyh v torfe (Atlas of plant remains found in peat). Moscow: Gosenergoizdat (Publ.), 1959. 228 p. (in Russ.)

Ekman I. and Iljin V. Deglaciation, the Younger Dryas end moraines and their correlation in the Karelian ASSR and adjacent areas. Eastern Fennoscundian Younger Dryas End Moraines: Excursion Guide. Rainio H. and Saarnisto M. (Eds.). Geological Survey of Finland: Espoo (Publ.), 1991. P. 73–101.

Elina G.A. and Filimonova L.V. Dinamika rastitel’nosti severo-zapada Kol’skogo poluostrova v golotsene (Dynamics of vegetation in north-west of Kola Peninsula in Holocene). Botanicheskiy Zhurnal. 2000. Vol. 85. No. 9. P. 34–55. (in Russ.)

Elina G.A. and Kuznetsov O.L. Paleovegetation and paleogeography of Holocene of Pribelomorskaya lowland in Karelia; prognosis for 1000 years. Aquilo, Series Botanica. 1996. Vol. 36. P. 9–20.

Elina G.A. and Lebedeva R.M. Dinamika rastitel’nosti i paleogeografiya golotsena Karel’skogo berega Pribelomorskoi nizmennosti (Dynamics of vegetation and Holocene palaeogeography of the Karelian coast of the Pribelomorskaya lowland). Botanicheskiy Zhurnal. 1992. Vol. 77. No. 5. P. 17–29. (in Russ.)

Elina G.A. Printsipy i metody rekonstruktsii i kartirovaniya rastitel’nosti golotsena (Principles of and methods for reconstruction and mapping of the Holocene vegetation). Leningrad: Nauka (Publ.), 1981. 159 p. (in Russ.)

Elina G.A., Arslanov H.A., Klimanov V.A., and Usova L.I. Rastitel’nost’ i klimatokhronologiya golotsena Lovozerskoi ravniny Kol’skogo poluostrova (po sporovo-pyl’tsevym diagrammam bugristo-topyanogo bolota) (Vegetation and climate chronology in the holocene of the Lovozerskaya plain in the Kola peninsula (according to sporepollen diagrams of a palsa mire)). Botanicheskii Zhurnal. 1995. Vol. 80. No. 3. P. 1–16. (in Russ.)

Elina G.A., Filimonova L.V., Grabovik S.I., and Kostina V.I. Bolota Kol’skogo poluostrova (Mires of the Kola Peninsula). Trudy KarNC RAN. 2005. Vol. 5. P. 94−110.

Elina G.A., Filimonova L.V., and Lavrova N.B. Palinologicheskie issledovaniya tundrovoi zony Kol’skogo poluostrova: novye metodicheskie podkhody (Palynological investigations of the tundra zone of Kola peninsula: new methodical approaches). Botanicheskii Zhurnal. 2002. Vol. 87. No. 1. P. 3–27. (in Russ.)

Elina G.A., Lukashov A.D., and Yurkovskaya T.K. Pozdnelednikov’e i golotsen vostochnoi Fennoskandii (paleorastitel’nost' i paleografiya). (Late Glacial and Holocene Time in the East Fennoscandia). Petrozavodsk: KarRC RAS Press (Publ.), 2000. 240 p. (in Russ.)

Elina G.A., Lukashov A.D., and Yurkovskaya T.K. Late Glacial and Holocene palaeogeography of Eastern Fennoskandia. The Finnish environment 4. Helsinki: Finnish Environment Institute (Publ.), 2010. 304 p.

Evzerov V.Ya., Elovicheva Ya.K., Lebedeva R.M., and Rayamyae R.A. Stratigrafiya pleistotsenovykh otlozhenii yuzhnoi chasti Kol’skogo poluostrova (Stratigraphy of the Pleistocene deposits of the southern part of the Kola Peninsula). Geologiya pleistotsena Severo-Zapada SSSR. Apatity: Kol’skii filial AN SSSR (Publ.), 1981. P. 97–107. (in Russ.)

Geobotanicheskoe raionirovanie Nechernozem’ya evropeiskoi chasti RSFSR (Geobotanical zoning of the Non-Chernozem region of the European part of the RSFSR). Alexandrova V.D. and Yurkovskaya T.K. (Eds.). Leningrad: Botanic institute (Publ.), 1989. 63 p. (in Russ.)

Giesecke T. and Bennett K.D. The Holocene spread of Picea abies (L.) Karst. in Fennoscandia and adjacent areas. Journal of Biogeography. 2004. Vol. 31. No. 9. P. 1523–1548. https://doi.org/10.1111/j.1365-2699.2004.01095.x

Grichuk V.P. and Zaklinskaya E.D. Analiz iskopaemykh pyl’cy i spor i ego primenenie v paleogeografii (Fossil Pollen and Spores Analysis and its Application in Paleogeography). Moscow: GEOGRAFGIZ (Publ.), 1948. 224 p. (in Russ.)

Grimm E.C. TGView Version 2.0.2. / Springfield: Illinois State Museum, Research and Collections Center. 2004.

Grimm E.C. Tilia 1.7.16. Software / Springfield: Illinois State Museum. Research and Collection Center. 2011.

Heiri O., Lotter A.F., and Lemcke G. Loss on ignition as a method for estimating organic and carbonate content in sediments: reproducibility and comparability of results. Paleolimnology. 2001. Vol. 25. P. 101–110. https://doi.org/10.1023/A:1008119611481

Kalinska-Nartisa E., Lamsters K., Karuss J., Krievans M., Recs A., and Meija R. Quartz grain features in modern glacial and proglacial environments: A microscopic study from the Russell Glacier, southwest Greenland. Polish Polar Research. 2017. Vol. 38. No. 3. P. 265–289. https://doi.org/10.1515/popore-2017-0018

Kats N.Ya., Kats S.V., and Kipiani M.G. Atlas i opredelitel' plodov i semyan, vstrechayushchikhsya v chetvertichnykh otlozheniyakh SSSR (Atlas and a guide to fruits and seeds found in the Quaternary deposits of the USSR). Moscow: Nauka (Publ.), 1965. 366 p. (in Russ.)

Kats N.Ya., Kats S.V., and Skobeeva E.I. Atlas rastitel’nykh ostatkov v torfakh (Atlas of plant residues in peat). Moscow: Nedra (Publ.), 1977. 376 p. (in Russ.)

Kazakov L.A., Pereverzev V.N., and Chamin V.A. Pochvoobrazovanie na estestvennykh i pereveyannykh morskikh peskakh poberezh’ya Belogo morya (Kol’skii poluostrov). (Soil formation on natural and winnowed sea sands of the White Sea coast (Kola Peninsula)). Vestnik MSTU. 2009. Vol.12. No. 4. P. 751–757. (in Russ.)

Khabakov A.V. Ob indeksakh okatannosti galechnikov (On roundness indexes of pebbles). Sovetskaya geologiya. 1946. No. 10. P. 98–99. (in Russ.)

Khotinsky N.A. Golotsen Severnoi Evrazii (The Holocene of Northern Eurasia). Moscow: Nauka (Publ.), 1977. 200 p. (In Russ.)

Khotinsky N.A. Radiouglerodnaya khronologiya i korrelyatsiya prirodnykh i antropogennykh rubezhei golotsena (Radiocarbon chronology and correlation of natural and anthropogenic boundaries of the Holocene). Novye dannye po geokhronologii chetvertichnogo perioda. Moscow: Nauka (Publ.), 1987. P. 39–45. (in Russ.)

Klimanov V.A. and Elina G.A. Climate Change in the North-West of the Russian Plain in the Holocene. Doklady Earth science sections. 1984. Vol. 274. No. 5. P. 1164–1167.

Kolka V.V., Evzerov V.Ya., Moller J.J., and Corner G.D. Peremeshchenie urovnya morei v pozdnem pleistotsene – golocene i stratigrafiya donnykh osadkov izolirovannykh ozer na yuzhnom beregu Kol’skogo poluostrova, v raione poselka Umba (The Late Weichselian and Holocene relative sea-level change and isolation basin stratigraphy at the Umba settlement, southern coast of Kola Peninsula). Izvestiya RAN. Seriya geograficheskaya. 2013. No. 1. P. 73–88 (in Russ.). https://doi.org/10.15356/0373-2444-2013-1-73-88

Korotkina M.Ya. Botanicheskii analiz torfa (Botanical analysis of peat). Metody issledovaniya torfyanykh bolot. Laboratornye i kameral’nye raboty. M.I. Nejshtadt (Ed.). Part 2. Moscow. 1939. P. 5–60. (in Russ.)

Korsakova O.P., Semenova L.R., and Kolka V.V. Otlozheniya srednego i verkhnego neopleistotsena v razreze Varzuga (yuzhnya chast' Kol’skogo poluostrova). (Middle and Upper neopleistocene sediments in the Varzuga section (southern Kola Peninsula)). Regional geology and metallogeny. 2011. Vol. 48. P. 19–24. (in Russ.)

Koshechkin B. I. Golotsenovaya tektonika vostochnoi chaste Baltiiskogo shchita (The Holocene tectonics of the eastern part of the Baltic Shield). Leningrad: Nauka (Publ.), 1979. 158 p. (in Russ.)

Kremenetsky K.V., Patyk-Kara N.G., and Goryachkin S.V. The Holocene Palynostratigraphy and Geochronology of Lacustrine-Palustrine Deposits in the Kola Peninsula. Stratigraphy and Geological Correlation. 1998. Vol. 6. No. 3. P. 87–96.

Kuzmina N.N., Salova T.A., Sudakova N.G., and Feldman T.G. Granulometricheskaya i mineralogicheskaya kharakteristika fatsial’nykh kompleksov noveishikh otlozhenii Priazov’ya (Granulometry and mineralogy of Cenozoic sediments in the Azov region). Noveishaya tektonika, noveishie otlozheniya i chelovek. Moscow: Moscow University Press (Publ.), 1969. P. 119–133 (in Russ.)

Lavrova M.A. Chetvertichnaya geologiya Kolskogo poluostrova (Quaternary Geology of the Kola Peninsula). Moscow–Leningrad: USSR Acad. of Sci. Press (Publ.), 1960. 233 p. (in Russ.)

Lavrova M.A. Osnovnye etapy chetvertichnoi istorii Kolskogo poluostrova (The main stages of the Quaternary history of the Kola Peninsula). Izvestiya Vsesoyuznogo geograficheskogo obschestva. 1947. Vol. 79. No. 1. P. 21–38. (in Russ.)

Lavrova N.B., Kolka V.V., and Korsakova O.P. Nekotorye osobennosti palinospektrov donnykh otlozhenii malykh ozer severnoi chasti Pribelomorskoi nizmennosti (Some features of palynospectra of bottom sediments of small lakes in the northern part of the White Sea Lowland).

Geologiya i poleznye iskopaemye Karelii (Geology and Minerals of Karelia). Petrozavodsk: KarRC RAS (Publ.), 2011. P. 197–202. (in Russ.)

Matishov G.G., Sharapova A.Yu., Tarasov G.A., Snyder J.A., MacDonald G.M., Kremenetski K.V., and Khasankaev V.B. Postglacial Vegetation and Climate in the Central Kola Peninsula. Doklady Earth Sciences. 2005. Vol. 402. No. 4. P. 646–648.

Mazei N.G. and Novenko E.Yu. Primenenie propionovogo angidrida pri podgotovke prob dlya sporovo-pyl’tsevogo analiza (The use of propionic anhydride in the sample preparation for pollen analysis). Nature Conservation Research. Zapovednaya nauka. 2021. Vol. 6. No. 3. P. 110–112. (in Russ.). https://doi.org/10.24189/ncr.2021.036

Minkina C.I. and Varlygin P.D. Opredelenie stepeni razlozheniya torfa (Identification of peat decomposition degree). Polevoe issledovanie. M.I. Nejshtadt (Ed.). Moscow. 1939. P. 115–138. (in Russ.)

Moore P.D., Webb J.A., and Collinson M.E. Pollen analysis. Oxford: Blackwell (Publ.), 1991. 216 p.

Nikitin V.P. Paleocarpological method. Tomsk: Publishing House of Tomsk University, 1969. 89 p. (in Russ.) Nikolaeva S.B., Lavrova N.B., Tolstobrov D.S., and Denisov D.B. Rekonstruktsiya paleogeograficheskikh obstanovok golotsena v raione ozera Imandra (Kol’skii region): rezul’taty paleolimnologicheskikh issledovanii (Reconstructions of Holocene paleogeographic conditions in the lake Imandra area (Kola region): results of paleolimnological studies). Trudy KarNC RAN. 2015. No. 5. P. 34–47. (in Russ.). https://doi.org/10.17076/lim49 80

Novenko E.Yu. Dynamics of landscape and climate in Central and Eastern Europe in the Holocene: paleogeographic aspects for prognosis of possible environmental changes. Ecosystems: Ecology and Dynamics. 2020. Vol. 4. No. 4. P. 81–104.

Panin P.G., Timireva S.N., Konstantinov E.A., Kalinin P.I., Kononov Y.M., Alekseev A.O., and Semenov V.V. Plio-Pleistocene paleosols: Loess-paleosol sequence studied in the Beregovoye section, the Crimean Peninsula. Catena. 2019. Vol. 172. P. 590–618. https://doi.org/10.1016/j.catena.2018.09.020

Payanskaya-Gvozdeva I.I. Struktura rastitel’nogo pokrova severnoi taigi Kol’skogo poluostrova (The structure of vegetation cover of the northern taiga of the Kola peninsula). Leningrad: Botanic institute (Publ.), 1990. 106 p. (in Russ.)

Reimer P.J., Austin W.E.N., Bard E. et al. The IntCal20 Northerthern Hemisphere radiocarbon age calibration curve (0–55 cal kBP). Radiocarbon. 2020. Vol. 62. No. 4. P. 725–757. https://doi.org/10.1017/RDC.2020.41

Repkina T.Yu., Romanenko F.A., Lugovoy N.N., and Gurinov A.L. Antropogennye pustyni poberezh’ya Belogo morya (Man-made deserts of the White Sea coast). Geografiya: razvitie nauki i obrazovaniya. T. 1. SPb.: Asterion, Izd-vo RGPU im. A.I. Gertsena (Publ.), 2020. P. 244–247. (in Russ.)

Repkina T.Yu., Zaretskaya N.E., Lugovoy N.N., Shvarev S.V., Shilova O.S., and Alyautdinov A.R. Istoriya razvitiya ust’evoi oblasti r. Varzugi v golotsene (Terskii bereg Belogo morya) (The Holocene history of the Varzuga river estuary (Tersky coast of the White Sea)). Routs of evolutionary geography – 2021. Issue 2. Materials of the II All-Russian Scientific Conference dedicated to the memory of Professor A.A. Velichko. Moscow: Institute of Geography, RAS (Publ.), 2021. P. 306–310. (in Russ.)

Rukhin L.B. Osnovy litologii. Uchenie ob osadochnykh porodakh (Basics of Lithology). Leningrad: Nedra Publishing House (Publ.), 1969. 704 p. (in Russ.).

The authors declare that there are no conflicts of interest present.