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Mid- and late-Holocene vegetation history, climate and human impact in the forest-steppe ecotone of European Russia: new data and a regional synthesis

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Abstract

Appropriate management of contemporary environments requires knowledge of their long-term history. We use palaeoecological data to explore how contemporary forest-steppe environments have been shaped by climate change and human impacts through the Holocene using the western Mid-Russian Upland as a case-study. Our paper presents new reconstructions of Mid- and Late Holocene climate, vegetation dynamics and local environmental change based on pollen, plant macrofossil and testate amoeba records from a site at Selikhovo (Mid-Russian Upland, Russia). Eutrophic fen vegetation dominated by Phragmites australis developed around 6800 cal year BP and has been resilient to episodes of local burning and variable input of mineral material through the Holocene. New and previously-published data show that the boundary between broadleaf forest and steppe occupied a similar position to present during the period 7000–4800 cal year BP, despite a warmer and drier climate, but shifted to the south following climate cooling and an increase in precipitation from 4800–2500 cal year BP. A subsequent decline in woodland cover was caused by both climate change and human impacts, with human activity becoming increasingly significant over the last two millennia. Prior to major human disturbance (about 1700 cal year BP) the landscape was dominated by mixed broadleaf-pine forests with some spruce covering about 60 % of the study area. Our results emphasize the variability of steppe-forest habitats over long time periods and the need to consider human impacts and climate change when setting targets for habitat conservation.

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References

  • Aleksandrovskiy AL, Chichagova OA (1998) Radiocarbon age of Holocene paleosols of the East European forest–steppe zone. Catena 34:197–207

    Article  Google Scholar 

  • Bartalev SA, Egorov BA, Ershov DV, Isaev AS, Lupyan EA, Plotnikov DE, Uvarov IA (2011) Satellite mapping of the vegetation cover of Russia by data of the spectroradiometer MODIS. Modern problems of remote sensing of the earth from space 8:285–302 (in Russian)

    Google Scholar 

  • Behre K-E (1988) The role of man in European vegetation history. In: Huntley B, Webb T III (eds) Vegetation history. Kluwer, Dordrecht, pp 633–672

    Chapter  Google Scholar 

  • Bennett KD (1996) Determination of the number of zones in a biostratigraphical sequence. New Phytol 132:155–170

    Article  Google Scholar 

  • Blagoveshenskaya NV (2009) Vegetation history of the central part of the Privolzhskaya Upland in the Holocene. Dissertation, Ul’yanovsk State University (in Russian)

  • 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

    Article  Google Scholar 

  • Bradley RS (2008) Holocene perspectives on future climate change. In: Battarbee RW, Binney HA (eds) Natural climate variability and global warming: a Holocene perspective. Wiley & Sons, Blackwell, pp 254–268

    Chapter  Google Scholar 

  • Core Team R (2012) R: A language and environment for statistical computing. R Foundation for Statistical Computing, Austria

    Google Scholar 

  • Davis BAS, Brewer S, Stevenson ACA, Guiot J, Contributors Data (2003) The temperature of Europe during the Holocene reconstructed from pollen data. Quat Sci Rev 22:1701–1716

    Article  Google Scholar 

  • Dean W Jr (1974) Determination of carbonate and organic matter in calcareous sediments and sedimentary rocks by loss on ignition: comparison with other methods. J Sediment Res 44:242–248

    CAS  Google Scholar 

  • Dombrovskaya AV, Koreneva MM, Turemnov SN (1959) Atlas of plant remains in peat. Nauka, Moscow (in Russian)

    Google Scholar 

  • Ershov DV (2007) Methods of assessment of area covered by forests using satellite imaging MODIS of moderate spatial resolution. Curr Probl Rem Sens Earth Space 2:217–225 (in Russian)

    Google Scholar 

  • Feurdean A, Klotz S, Mosbrugger V, Wohlfarth B (2008) Pollen-based quantitative reconstructions of Holocene climate variability in NW Romania. Palaeogeogr Palaeoclimatol Palaeoecol 260:494–504

    Article  Google Scholar 

  • Feurdean A, Marinova E, Nielsen AB, Liakka J, Veres D, Hutchinson SM, Mihaly Braun M, Timar-Gabor A, Astalos C, Mosburgger V, Hickler T (2015) Origin of the forest steppe and exceptional grassland diversity in Transylvania (central-eastern Europe). J Biogeogr 42:951–963

    Article  Google Scholar 

  • Folomeev BA, Aleksandrovsky AL, Glasko MP, Gonyanyi MI, Guman MA (1990) Ancient settlements and environment in mouth part of Nepryavda river. In: Zaitzev AK (ed) Kulikovo Battle Field: materials of investigation. State Historical Museum-Press, Moscow, pp 10–53

    Google Scholar 

  • Gonianyi MI, Aleksandrovskiy AL, Glasko MP (2007) Northern forest-steppe of the Upper Don River basin at the time of the Kulikovo Battle. State Historical Museum-Press, Moscow (in Russian)

    Google Scholar 

  • Gribova SA, Isachenko TI, Lavrenko EM (1980) Vegetation of the European part of the USSR. Nauka, Leningrad (in Russian)

    Google Scholar 

  • Grichuk VP (1940) Method of treatment of the sediments poor in organic remains for the pollen analysis. Problems Fiz Geogr 8:53–58 (in Russian)

    Google Scholar 

  • Grimm ECA (1987) CONISS: a FORTRAN 77 program for stratigraphically constrained cluster analysis by the method of incremental sum of squares. Comput Geosci 13:13–35

    Article  Google Scholar 

  • Grimm ECA (1990) TILIA and TILIA*GRAPH.PC spreadsheet and graphics software for pollen data. INQUA Working Group Data-Handling Methods Newsl 4:5–7

    Google Scholar 

  • Guiot J (1990) Methodology of the last climatic cycle reconstruction in France from pollen data. Palaeogeogr Palaeoclimatol Palaeoecol 80:49–69

    Article  Google Scholar 

  • Hansen M, DeFries RS, Townshend JRG, Carroll M, Dimiceli C, Sohlberg RA (2003) Global percent tree cover at a spatial resolution of 500 meters: first results of the MODIS vegetation continuous fields algorithm. Earth Interact 7:1–15

    Article  Google Scholar 

  • Kaplan JO, Krumhardt KM, Zimmermann N (2009) The prehistoric and preindustrial deforestation of Europe. Quat Sci Rev 28:3016–3034

    Article  Google Scholar 

  • Katz NY, Katz SV, Skobeva EI (1977) Atlas of plant remains in peat. Nedra-press, Moscow (in Russian)

    Google Scholar 

  • Khotinsky NA (1977) Holocene of Northern Eurasia. Nauka, Moscow (in Russian)

    Google Scholar 

  • Khotinsky NA (1993) Anthropogenic changes in the landscapes of the Russian Plain during the Holocene. Grana 32(Suppl 2):70–74

    Article  Google Scholar 

  • Klimanov VA, Serebryannaya TA (1986) The change of vegetation and climate of the Mid-Russian Upland in the Holocene. USSR Acad Sci Izv Ser Geogr 2:93–101 (in Russian)

    Google Scholar 

  • Klimanov VA, Sirin AA (1997) Dynamics of peat accumulation in beatbogs of the Northern Eurasia during the last 3000 years. Dokl Akad Nauk 354:683–686 (in Russian)

    CAS  Google Scholar 

  • Korhola A, Ruppel M, Seppä H, Väliranta M, Virtanen T, Weckström J (2010) The importance of northern peatland expansion to the late-Holocene rise of atmospheric methane. Quat Sci Rev 29:611–617

    Article  Google Scholar 

  • Krasnoschekova SD, Krasnitskiy LN (2006) Archeology of Orel region. Veshnie vody Press, Orel (in Russian)

    Google Scholar 

  • Krasnov YA (ed) (1999) Archeological map of Russia. Orel region, part 1. Institute of archeology RAS Press, Moscow (in Russian)

  • Krupenina LA (1974) The age and conditions of sedimentation of floodplain deposits of the Rivers Seim and Krom. USSR Acad Sci Izv Ser Geogr 2:82–89 (in Russian)

    Google Scholar 

  • Lamentowicz M, Cedro A, Gałka M, Miotk-Szpiganowicz G, Mitchell EAD, Pawlyta J, Goslar T (2008) Last millennium palaeoenvironmental changes from a Baltic bog (Poland) inferred from stable isotopes, pollen, plant macrofossils and testate amoeba. Palaeogeogr Palaeoclimatol Palaeoecol 265:93–106

    Article  Google Scholar 

  • Lavrushin YA, Spiridonova EA, Bessudnov AN, Smol’yaninov PB (2009) Holocene natural catastrophes in the Upper Don river basin. GEOS, Moscow (in Russian)

    Google Scholar 

  • Lazarova M, Bozilova E (2001) Studies on the holocene history of vegetation in the region of the lake Srebarna (northeast Bulgaria). Veg Hist Archaeobot 10:87–95

    Article  Google Scholar 

  • Leonenko M (1971) Geology of the USSR. The center of the European part of the USSR, vol 5. Nedra-Press, Moscow

    Google Scholar 

  • Lishtvan II, Korol NT (1975) The main properties of peat and methods of its determination. Nauka i Technika, Minsk (in Russian)

    Google Scholar 

  • MacDonald GM, Beilman DW, Kremenetski KV, Sheng Y, Smith LC, Velichko AA (2006) Rapid early development of circumarctic peatlands and atmospheric CH4 and CO2 variations. Science 314:285–288

    Article  CAS  PubMed  Google Scholar 

  • Magyari EK, Chapman JC, Passmore DG, Allen JRM, Huntley JP, Huntley B (2010) Holocene persistence of wooded steppe in the Northern Great Hungarian Plain. J Biogeogr 37:915–935

    Article  Google Scholar 

  • Mann ME, Zhang Z, Rutherford S et al (2009) Global signatures and dynamical origins of the little ice age and medieval climate anomaly. Science 326:1256–1260

    Article  CAS  PubMed  Google Scholar 

  • Mayewski PA, Rohling BE, Stager G (2004) Holocene climate variability. Quat Res 62:243–255

    Article  Google Scholar 

  • Mazei YA, Embulaeva EA (2009) Changes in the communities of soil-dwelling testate amoebae along the forest-steppe gradient in the Middle Volga Region. Arid Ecosyst 37:13–27

    Google Scholar 

  • Moskal-del Hoyo M (2013) Mid-holocene forests from Eastern Hungary: new anthracological data. Rev Palaeobot Palynol 193:70–81

    Article  Google Scholar 

  • Nakagawa T, Tarasov P, Kotoba N, Gotanda K, Yasuda Y (2002) Quantitative pollen-based climate reconstruction in Japan: application to surface and late Quaternary spectra. Quat Sci Rev 21:2099–2113

    Article  Google Scholar 

  • Novenko EY, Glasko MP, Burova OV (2009) Landscape-and-climate dynamics and land use in late holocene forest-steppe ecotone of East European Plain (upper Don River Basin case study). Quat Int 203:113–119

    Article  Google Scholar 

  • Novenko EY, Volkova EM, Glasko MP, Zuganova IS (2012) Palaeoecological evidence for the middle and late Holocene vegetation, climate and land use in the upper Don River basin (Russia). Veget Hist Archaeobot 21:337–352

    Article  Google Scholar 

  • Novenko EYu, Eremeeva AP, Chepurnaya AA (2014a) Reconstruction of Holocene vegetation, tree cover dynamics and human disturbances in central European Russia, using pollen and satellite data sets. Veg Hist Archaeobot 23(Suppl 1):109–119

    Article  Google Scholar 

  • Novenko EY, Rudenko OV, Volkova EM, Zuganova IS (2014b) Vegetation dynamics in the national park “Orlovskoye Polesye” in the late Holocene. Sci Notes Orel State Univ 3:302–310 (in Russian)

    Google Scholar 

  • Novenko EY, Tsyganov AN, Volkova EM, Babeshko KV, Lavrentiev NV, Payne RJ, Mazei YA (2015) The Holocene paleoenvironmental history of central European Russia reconstructed from pollen, plant macrofossil, and testate amoeba analyses of the Klukva peatland, Tula region. Quat Res 83:459–468

    Article  Google Scholar 

  • Olsson F, Gaillard MJ, Lemdahl G, Greisman A, Lanos P, Marguerie D, Marcoux N, Skoglund P, Wäglind J (2010) A continuous record of fire covering the last 10,500 calendar years from southern Sweden—the role of climate and human activities. Palaeogeogr Palaeoclimatol Palaeoecol 291:128–141

    Article  Google Scholar 

  • Overpeck JT, Webb T III, Prentic ICA (1985) Quantitative interpretation of fossil pollen spectra: dissimilarity coefficients and the method of modern analogs. Quat Res 23:87–108

    Article  Google Scholar 

  • Parnell AC, Haslett J, Allen JRM, Buck CE, Huntley B (2008) A flexible approach to assessing synchroneity of past events using Bayesian reconstructions of sedimentation history. Quat Sci Rev 27:1872–1885

    Article  Google Scholar 

  • Payne R (2009) The standard preparation method for testate amoebae leads to selective loss of the smallest shells. Quat Newsl 119:16–20

    Google Scholar 

  • Power MJ, Marlon J, Ortiz N et al (2008) Changes in fire regimes since the last glacial maximum: an assessment based on a global synthesis and analysis of charcoal data. Clim Dyn 30:887–907

    Article  Google Scholar 

  • Reimer PJ, Bard E, Bayliss A, Beck JW, Blackwell PG, Bronk Ramsey C, Buck CE, Cheng H, Edwards RL, Friedrich M, Grootes PM, Guilderson TP, Haflidason H, Hajdas I, Hatté C, Heaton TJ, Hoffmann DL, Hogg AG, Hughen KA, Kaiser KF, Kromer B, Manning SW, Niu M, Reimer RW, Richards DA, Scott EM, Southon JR, Staff RA, Turney CSM, van der Plicht J (2013) IntCal13 and Marine13 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon 55:1869–1887

    Article  CAS  Google Scholar 

  • Serebryannaya TA (1976) Interrelations between forest and steppe on Central Russian Upland in Holocene. In: Dinesman LG (ed) The history of biocenoses of USSR in Holocene. Nauka, Moscow, pp 159–166 (in Russian)

    Google Scholar 

  • Serebryannaya TA (1981) The human impact on vegetation of Central Russian Upland (by palynological data). In: Voropaev GV (ed) Anthropogenic factors in the history of the development of modern ecosystems. Nauka, Moscow, pp 52–60 (in Russian)

    Google Scholar 

  • Sidorchuk A, Panin A, Borisova O (2012) River runoff decrease in North-Eurasian plains during the Holocene optimum. Water Resour 39:69–81

    Article  CAS  Google Scholar 

  • Simpson GL, Oksanen J (2012) Analogue: analogue matching and modern analogue technique transfer function models. (R package version 0.8-2). http://cran.r-project.org/package=analogue

  • Spiridonova EA (1991) Evolution of vegetation cover of Don Basin in upper Pleistocene and Holocene. Nauka, Moscow (in Russian)

    Google Scholar 

  • Sümegi P, Persaits G, Gulyás S (2012) Woodland-grassland ecotonal shifts in environmental mosaics: lessons learnt from the environmental history of the Carpathian Basin (Central Europe) during the holocene and the last ice age based on investigation of paleobotanical and mollusc remains. In: Myster RW (ed) Ecotones between forest and grassland. Springer, New York, pp 17–57

    Chapter  Google Scholar 

  • Sycheva S, Glasko M, Chichagova O (2003) Holocene rhythms of soil formation and sedimentation in the Central Russian Upland. Quat Int 106–107:203–213

    Article  Google Scholar 

  • Ter Braak CA (1995) Ordination. In: Jongman R, ter Braak C, van Tongeren O (eds) Data analysis in community and landscape ecology. Pudoc, Wageningen, pp 91–173

    Chapter  Google Scholar 

  • Troels-Smith J (1955) Karakterisering af lose jordater (characterisation of unconsolidated sediments). Dan Geol Undersogelse 3:39–73 (in Danish)

    Google Scholar 

  • Turner C (1996) The early middle pleistocene in Europe. Balkema, Rotterdam

    Google Scholar 

  • Velichko AA, Faustova MA, Pisareva VV, Gribchenko YN, Sudakova NG, Lavrentiev NV (2011) Glaciations of the East European Plain: distribution and chronology. In: Ehlers J, Gibbard PL, Hughes PD (eds) Quaternary glaciations—extent and chronology. Elsevier, Amsterdam, pp 337–359

    Google Scholar 

  • Volkova EM (2011) Rare mires of the north-western Mid Russia Upland: vegetation and genesis. Bot J 96:55–70 (in Russian)

    Google Scholar 

  • Vomperski SE, Tzyganova OP, Kovalev AG et al (1999) Paludified lands in Russia as a factor of carbon accumulation. In: Zavarzin GA (ed) Global evolution of biosphere. Russian Academy of Science, Moscow, pp 124–145 (in Russian)

    Google Scholar 

  • Wanner H, Beer J, Bütikofer J, Crowley TJ, Cubasch U, Flückiger J, Goosse H, Grosjean M, Joos F, Kaplan JO, Küttel M, Müller SA, Prentice IC, Solomina O, Stocker TF, Tarasov PE, Wagner M, Widmann M (2008) Mid- to late holocene climate change: an overview. Quat Sci Rev 27:1791–1828

    Article  Google Scholar 

  • Williams JW, Shuman B (2008) Obtaining accurate and precise environmental reconstructions from the modern analog technique and North American surface pollen dataset. Quat Sci Rev 27:669–687

    Article  Google Scholar 

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Acknowledgments

This work was supported by the Russian Foundation for Basic Research, Projects 14-05-00550. Microscopic analysis of testate amoeba data was supported by the Grant of the President of Russian Federation (MD-4435.2014.4). The palaecological analysis of testate amoeba data provided by A. Tsyganov and Y. Mazei was supported by Russian Science Foundation (Project 14-14-00891). Analysis of experimental data in respect of project future climate changes was provided by A. Olchev within the framework of the grant of the Russian Science Foundation (14-14-00956).

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Correspondence to Elena Y. Novenko.

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Communicated by Jürgen Dengler.

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Novenko, E.Y., Tsyganov, A.N., Rudenko, O.V. et al. Mid- and late-Holocene vegetation history, climate and human impact in the forest-steppe ecotone of European Russia: new data and a regional synthesis. Biodivers Conserv 25, 2453–2472 (2016). https://doi.org/10.1007/s10531-016-1051-8

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