Hostname: page-component-f554764f5-fr72s Total loading time: 0 Render date: 2025-04-09T08:50:30.704Z Has data issue: false hasContentIssue false
  • English
  • Français

Floodplain Paleosols of Moskva River Basin: Chronology and Paleoenvironment

Published online by Cambridge University Press:  10 September 2018

A Alexandrovskiy ,
E Ershova ,
E Ponomarenko ,
N Krenke  and
V Skripkin
A Alexandrovskiy*
Affiliation:
Institute of Geography, Russian Academy of Sciences, Department of Soil Geography & Evolution, Moscow, Russia
E Ershova
Affiliation:
Moscow State University, Moscow; Institute of Archaeology, Russian Academy of Sciences, Moscow; Kazan Federal University, Kazan, Russia
E Ponomarenko
Affiliation:
Ottawa University, Ottawa, Canada; Kazan Federal University, Kazan, Russia
N Krenke
Affiliation:
Institute of Archaeology, Russian Academy of Sciences, Moscow, Russia
V Skripkin
Affiliation:
Kiev Radiocarbon Laboratory, Institute of Environmental Geochemistry NAS Ukraine, Kiev, Ukraine
*
*Corresponding author. Email: alexradiocarbon@gmail.com.
Get access Rights & Permissions [Opens in a new window]

Abstract

Seven main periods of soil formation can be distinguished in the floodplain of the Moskva (Moscow) River, with the oldest paleosols dated to the Allerød age. We analyzed paleosols buried under alluvial deposits, colluvial sediments, and archaeological deposits within the catchment area of the Moskva River. Paleopedological reconstructions were correlated with the results of the pedoanthracological and palynological analyses. Series of radiocarbon (14C) dates were obtained on humic acids and dispersed macro-charcoal from paleosols and archaeological features. Wide time frames of the floodplain paleosol formation were determined at a 95% probability as 14,600–12,600 cal BP for Soil 7; 9500–7000 cal BP for Soils 6 and 5; 6700–5500 cal BP for Soil 4; 5000–4400 cal BP for Soil 3b; 4100–2700 cal BP for Soil 3a; and 2000–700 cal BP for Soil 2. The dates were compared with the age of archaeological sites from the same areas. The comparison revealed a close correspondence between the ages of the soil charcoal and the timing of archaeological occupations. That allowed us to conclude that the fire occurrence on a regional level was associated mainly with the human occupation. The fire record is especially pronounced in floodplain paleosols, due to both the role of rivers as human migration corridors, and the integral accumulation of combustion products from the entire catchment area in these paleosols.

Keywords

chronologyclimate changefloodplainsgeoarchaeologyHolocenepaleoecologypaleosolspedoanthracology
Type
Soil
Information
Radiocarbon , Volume 60 , Issue 4: 2nd Radiocarbon in the Environment Conference Debrecen, Hungary, July 3–7, 2017 Part 1 of 2 , August 2018 , pp. 1169 - 1184
Copyright
© 2018 by the Arizona Board of Regents on behalf of the University of Arizona 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Article purchase

Temporarily unavailable

References

REFERENCES

Aleksandrovskii, AL. 2004. Phases and rates of soil evolution within river floodplains in the center of the Russian Plain. Eurasian Soil Science 37(11): 1137–1146.Google Scholar
Alexandrovskiy, AL, Chichagova, OA. 1998. The 14C age of humic substances in paleosols. Radiocarbon 40(2):991–997.Google Scholar
Alexandrovskiy, AL, Krenke, NA. 2004. Stages of soil formation on floodplains in the Geoarchaeology of River Valleys. Archaeolingua. Series Minor 18:171–184.Google Scholar
Alexandrovskiy, AL, Glasko, MP. 2014. Stages of the formation of floodplains of plain rivers in the Holocene: concurrent pedogenetic and alluvial processes. Geomorfologiya (3):3–16. In Russian.Google Scholar
Alexandrovskiy, AL, Panin, AV. 2013. Formation of the Moscow River floodplain and its occupation by humans: the valley area at the Zvenigorod biological station case study. The Archaeology of the Moscow Region 9:249–256. In Russian with English abstract.Google Scholar
Alexandrovskiy, AL, Glasko, MP, Folomeev, BA. 1987. Geoarchaeological studies of buried floodplain soils as geochronological levels of the second half of Holocene (Middle Oka River). In: Bulleten Komissii po izucheniyu Chetvertichnogo perioda 56:123–128. In Russian.Google Scholar
Alexandrovskiy, AL, Glasko, MP, Krenke, NA, Chichagova, OA. 2004. Buried soils of floodplains and paleoenvironmental changes in the Holocene. Revista Mexicana de Ciencias Geologicas 21(1): 9–17.Google Scholar
Alexandrovskiy, AL, Ershova, EG, Krenke, NA. 2016. Buried Late-Holocene Luvisols of the Oka and Moskva River floodplains and their anthropogenic evolution according to soil and pollen data. Quaternary International 418:37–48.Google Scholar
Aseev, AA. 1959. Paleogeography of the Middle and Lower Oka Valley in the Quaternary Period. Moscow: Izd. Akad. Nauk SSSR. In Russian.Google Scholar
Barefoot, AC, Hankins, FW. 1982. Identification of Modern and Tertiary Woods. Oxford University Press.Google Scholar
Borisova, O, Sidorchuk, A, Panin, A. 2006. Palaeohydrology of the Seim River basin, Mid-Russian Upland, based on palaeochannel morphology and palynological data. Catena 66:53–73.Google Scholar
Crann, CA, Murseli, S, St-Jean, G, Zhao, X, Clark, ID, Kieser, WE. 2017. First status report on radiocarbon sample preparation at the A.E. Lalonde AMS Laboratory (Ottawa, Canada). Radiocarbon 59(3):695–704.Google Scholar
Efimenko, PP. 1934. Settlements of the Bronze Age discovered in the floodplain of the Don River near the village of Kostyonki. Problems of Precapitalistic Societies 5. In Russian.Google Scholar
Ershova, EG, Krenke, NA. 2014. The study of the natural and cultural landscapes of the Iron Age in the Moskva-River valley using palynological and archaeological methods. Bulletin of Archaeology, Anthropology and Ethnography 26(3):159–172. In Russian with English abstract.Google Scholar
Ershova, EG, Alexandrovskiy, AL, Krenke, NA. 2014. Paleosols, paleovegetation and Neolithic occupation of the Moskva River floodplain, Central Russia. Quaternary International 324:134–145.Google Scholar
Ershova, EG, Alexandrovskiy, AL, Krenke, NA. 2016a. Evolution of landscapes of the Moskva River floodplain in the Atlantic and Subboreal: pedological and palynological records. Catena 137:611–621.Google Scholar
Ershova, EG, Alexandrovskiy, AL, Krenke, NA, Korkishko, DV. 2016b. New pollen data from paleosols in the Moskva River floodplain (Nikolina Gora): Natural and anthropogenic environmental changes during the Holocene. Quaternary International 420:294–305.Google Scholar
Folomeev, BA, Alexandovskiy, AL, Glasko, MP, Guman, MA. 1988. Klimentovskaya stoyanka (k voprosu o khozaisvennoi dejatel’nosti cheloveka I razvitii prirodnoi obstanovki v doline srednei Oki). Proceedings of State Historical Museum 68:168–191. In Russian.Google Scholar
Glasko, MP. 1983. Analysis of the factors determining the intensity of alluviation on the Middle-Oka floodplain in the Middle and Late Holocene. Izvestia Akad. Nauk SSSR Ser. Geogr 5:66–75. In Russian.Google Scholar
Glasko, MP, Folomeev, BA. 1981. Methodology of determination of the rates of accumulation of floodplain alluvium of plain rivers on the basis of archaeological and geomorphological data (by the example of the Middle Oka valleys). Geomorfologiya 3:26–36. In Russian.Google Scholar
Gorodtsov, VA. 1928. On the problem of real chronology of alluvial sedimentation in the rivers of the Oka system. Trudy Sektsii Arkheol. Inst. Arkheolog. i Iskusstvoznaniya (Moscow) 2:12–25. In Russian.Google Scholar
Khotinsky, NA. 1977. The Holocene of Northern Eurasia: The Intercontinental Correlation of Stages of the Vegetation and Climate Dynamics. Мoscow: Nauka. In Russian.Google Scholar
Khotinsky, NA, Folomeev, BA, Guman, MA. 1979. Archaeological and palaeogeographic investigations in the Middle Oka region. Sovetskaya Arkheologia 3:63–81. In Russian with English abstract.Google Scholar
Krenke, N. 2008. Formation of the cultural landscape in the Moscow River Basin from the Bronze Age to medieval times. Anthropology & Archeology of Eurasia 47(1):57–81.Google Scholar
Krenke, NA. 2011. Dyakovo Hillfort: the Culture of the Population of the Moskva Basin in the 1st Millennium BC - 1st Millennium AD. Moscow: IA RAN. In Russian with English abstract.Google Scholar
Krenke, NA. 2012. The Moskva river Basin in the Iron Age – migration period. Archaeologia Baltica 17:91–99.Google Scholar
Krenke, NA, Alexandrovskiy, AL, Ladychenko, AO, Petrov, VV, Yanishevskii, BE. 2001. Reconnaissance studies of the Moskva River floodplain and Moscow forest-parks. In: Archaeological Discoveries of 2000. Moscow: IA RAN:77–80. In Russian.Google Scholar
Krenke, N, Ershov, I, Ershova, E, Lazukin, A. 2013. Corded ware, Fatjanovo and Abashevo culture sites on the flood-plain of the Moskva River. Sprawozdania Archeologiczne 65:413–424.Google Scholar
Milov, L. 2001. The Great Russian Farmer and Specifics of the Russian Historical Process. Moscow: Rossiyskaya Politicheskaya Encyclopediya (ROSSPEN). In Russian.Google Scholar
Panin, AV. 2008. Introductory evidences on the history of forming of the bottom land of the Moscow River in the district Uspenskoe – RANIS. The Archaeology of the Moscow Region 4. Мoscow: AN RAN Press: p 340–343. In Russian with English abstract.Google Scholar
Panin, AV, Matlakhova, E. 2015. Fluvial chronology in the East European Plain over the last 20 ka and its palaeohydrological implications. Catena 130:46–61.Google Scholar
Panin, AV, Sidorchuk, AYu, Baslerov, SB, Borisova, OK, Kovalyukh, NN, Sheremetskaya, ED. 2001. Major stages of the history of river valleys in the center of the Russian Plain in the Late Valdai and Holocene periods: results of the studies in the middle reaches of the Seim River. Geomorfologiya 2:19–34. In Russian.Google Scholar
Plyusnin, II. 1938. Soils of the Volga-Akhtuba Floodplain. Stalingrad: Obl. Knigoizdat. In Russian.Google Scholar
Reimer, PJ, Bard, E, Bayliss, A, Beck, JW, Blackwell, PG, Bronk Ramsey, C, Buck, CE, Edwards, RL, Friedrich, M, Grootes, PM, Guilderson, TP, Hajdas, I, Hatté, C, Heaton, TJ, Haflidason, H, Hogg, AG, Hughen, KA, Kaiser, KF, Kromer, B, Manning, SW, Niu, M, Reimer, RW, Richards, DA, Scott, EM, Southon, JR, Turney, CSM, van der Plicht, J. 2013. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55(3):1869–1887.Google Scholar
Sidorchuk, A, Panin, A, Borisova, O. 2009. Morphology of river channels and surface runoff in the Volga River basin (East European Plain) during the Late Glacial period. Geomorphology 113:137–157. In Russian.Google Scholar
Schweingruber, FH. 1990. Anatomy of European Woods. Stuttgart: Paul Haupt.Google Scholar
Skripkin, VV, Kovalyukh, NN. 1998. Recent developments in the procedures used at the SSCER laboratory for the routine preparation of lithium carbide. Radiocarbon 40:211–214.Google Scholar
Spiridonova, EA, Aljoshinskaya, AS, Kochanova, MD. 2008. The results of palynological investigations in the bottom land of the Moscow River by the village RANIS. The Archaeology of the Moscow Region. Мoscow: AN RAN Press: 347–356. In Russian with English abstract.Google Scholar
Sycheva, SA. 1999. Cycles of soil formation and sediments accumulation in the Holocene (according to 14C data). Eurasian Soil Science 32(6):613–623.Google Scholar
Sycheva, SA. 2006. Long-term pedolithogenic rhythms in the Holocene. Quaternary International 152-153 :192–202.Google Scholar
Sycheva, SA. 2009. Holocene evolution of floodplain soils and landscapes in the Kulikovo field area. Eurasian Soil Science 42(1):13–23.Google Scholar
Sycheva, SA, Usyanov, AA. 1987. Dynamics of water level in the Tuskar River. Soil and archaeological data. Investigation and Optimization of Water Resources in Kursk Region. Kursk: MFGO Press: 75–82. In Russian.Google Scholar
Voropay, LI, Kunitsa, NA. 1970. Fossil soils in the Holocene alluvium of the Dnieper and Dniester rivers. Doklady Akademii nauk SSSR 192(1):147–150. In Russian.Google Scholar
Zaretskaya, NE, Ponomareva, VV, Sulerzhitsky, LD. 2007. Radiocarbon dating of large Holocene volcanic events within South Kamchatka (Russian Far East). Radiocarbon 49(2):1065–1078.Google Scholar
Supplementary material: File

Alexandrovskiy et al. supplementary material

Table S1

Download Alexandrovskiy et al. supplementary material(File)
File 34.9 KB