Vegetation History and Archaeobotany

, Volume 24, Issue 2, pp 319–330 | Cite as

Representation of Picea pollen in modern and surface samples from Central European Russia

  • Maria B. Nosova
  • Elena E. Severova
  • Olga A. Volkova
  • Jana V. Kosenko
Original Article

Abstract

Picea pollen abundance (percentage and PAR) was investigated in 23 Tauber pollen traps located in the mixed coniferous-broadleaved forest zone, broadleaved forest zone and forest-steppe zone in the European part of Russia. Modern data were compared with fossil pollen diagrams. In the modern spectra of non-forest zones average Picea pollen percentage is about 1 %, the highest values (up to 3 %) are usually connected with open locations and reflect the regional component of pollen rain. Within the coniferous forest belt average pollen abundance is about 10 %, but this value varies considerably from 1 to 40 % depending on local characteristics of sampling points. The lowest Picea pollen percentages (1 % and less) are observed in the pollen spectra of oligo- and mesotrophic mires, thus the level of 1 % can be significant for Picea and can indicate the continuous range of Picea. For an appropriate interpretation of low Picea pollen abundance in fossil samples the abundance should be analyzed together with other components of the pollen spectra. Large areas of Picea forests are not always reflected in pollen spectra as a high Picea percentage/PAR, as in unfavorable climatic or hydrological conditions the pollen production of Picea forests can be very low. Comparison of fossil and modern pollen spectra shows that a modern analogue of Holocene Picea forests in Central European Russia has not yet been discovered.

Keywords

Picea Holocene Modern pollen Surface samples Tauber trap Russia 

References

  1. Birks JJB, Gordon AD (1985) Numerical methods in Quaternary pollen analysis. Academic Press, LondonGoogle Scholar
  2. Blagoveschenskaya NV (1995) Subrecent pollen spectra and their comparison with modern vegetation of central part of Privolgskaya Upland. Russ Bot J 80:1,778–1,788 (in Russian)Google Scholar
  3. Bobrov EG (1970) History and systematic of genus Picea A Dietr. News High Plants Syst 7:5–40 (in Russian)Google Scholar
  4. Davydova NN, Subetto DA, Khomutova VI, Sapelko TV (2001) Late Pleistocene–Holocene paleolimnology of three northwestern Russian lakes. J Paleolimnol 26:37–51CrossRefGoogle Scholar
  5. Eisenhut G (1961) Untersuchungen über die Morphologie und Ökologie der Pollenkörner heimischer und fremdländischer Waldbäume. Parey, HamburgGoogle Scholar
  6. Fedorova RV (1952a) The distribution of pollen and spores by flowing water. Proc Geogr Inst Acad Sci USSR 52:46–72 (in Russian)Google Scholar
  7. Fedorova RV (1952b) Quantitative patterns of pollen distribution by air. Proc Geogr Inst Acad Sci USSR 52:91–103 (in Russian)Google Scholar
  8. Feurdean A, Tantau I, Farcas S (2011) Holocene variability in the range distribution and abundance of Pinus, Picea abies and Quercus in Romania; implications for their current status. Quat Sci Rev 30:3,060–3,075CrossRefGoogle Scholar
  9. Filimonova LV (2005) Late Galcial and Holocene Vegetation dynamics in the middle taiga subzone of Karelia. Palaeoecological aspects. Dissertation, Petrozavodsk (in Russian)Google Scholar
  10. Giesecke T (2005) Moving front or population expansion: How did Picea abies (L.) Karst. become frequent in central Sweden? Quat Sci Rev 24:2,495–2,509CrossRefGoogle Scholar
  11. Giesecke T, Bennett KD (2004) The Holocene spread of Picea abies (L.) Karst. in Fennoscandia and adjacent areas. J Biogeogr 31:1,523–1,548CrossRefGoogle Scholar
  12. Goncharenko GG, Potenko VV (1991) Genetic variability and differentiation in Picea abies (L.) Karst. and P. obovata Ledeb. populations. Genetics 27:1,759–1,772 (in Russian)Google Scholar
  13. Gribova SA, Isachenko TI, Lavrenko EM (eds) (1980) Vegetation of the European part of the USSR. Nauka, LeningradGoogle Scholar
  14. Grichuk VP, Zaklinskaya ED (1948) Fossil pollen and spores analysis and its using in palaeogeography. Moscow (in Russian)Google Scholar
  15. Grimm EC (1991) TILIA and TILIA graph. Illinois State Museum, Springfield, USAGoogle Scholar
  16. Hafsten U (1986) The establishment of spruce forest in Norway, traced by pollen analysis and radiocarbon datings. Striae 24:101–105Google Scholar
  17. Hättestrand M, Jensen C, Hallsdottir M, Vorren KD (2008) Modern pollen accumulation rates at the north-western fringe of the European boreal forest. Rev Palaeobot Palynol 151:90–109CrossRefGoogle Scholar
  18. Hicks S (1999) The relationship between climate and annual pollen deposition at northern tree-lines. Chemosphere 1:403–416Google Scholar
  19. Hicks S (2001) The use of annual arboreal pollen deposition values for delimiting tree-lines in the landscape and exploring. Rev Palaeobot Palynol 117:1–29CrossRefGoogle Scholar
  20. Hicks S, Sunnari A (2005) Adding precision to the spatial factor of vegetation reconstructed from pollen assemblages. Plant Biosyst 139:127–134CrossRefGoogle Scholar
  21. Hicks S, Latałowa M, Ammann B, Pardoe H, Tinsley H (eds) (1996) European Pollen Monitoring Programme—project description and guidelines. University of OuluGoogle Scholar
  22. Huntley B, Birks HJB (1983) An atlas of past and present pollen maps for Europe, 0–13,000 years ago. Cambridge University Press, New YorkGoogle Scholar
  23. Ilves EO, Sarv AA (1975) Spruce moving dynamics in Estonia in postglacial time. Status of methodological researches in the absolute geochronology. 192–197 (in Russian)Google Scholar
  24. Jazvenko SB (1992) Modern pollen production and Holocene history of mountain forests of Transcaucasia. Dissertation, Moscow State University (in Russian)Google Scholar
  25. Jenssen C, Vorren K-D, Morkved B (2007) Annual pollen accumulation rate (PAR) at the boreal and alpine forest-line of northwestern Norway, with special emphasis on Pinus sylvestris and Betula pubescens. Rev Palaeobot Palynol 144:337–361CrossRefGoogle Scholar
  26. Kiseleva KV (1976) Spruce. Biological flora of Moscow. Region 3:2–26 (in Russian)Google Scholar
  27. Kozharinov AV, Borisov PV, Gorshakova II (2010) Paleohabitats of Norway spruce (Picea abies (L.) Karst.) in the territory of Eastern Europe within the latest 13,500 years. Reg Res Russ 1:71–82Google Scholar
  28. Krutovskii KV, Bergmann F (1995) Introgressive hybridization and phylogenetic relationships between Norway, Picea abies (L.) Karst., and Siberian, P. obovata Ledeb., spruce species studied by isozyme loci. Heredity 74:464–480CrossRefGoogle Scholar
  29. Kuoppamaa M, Huusko A, Hicks S (2009) Pinus and Betula pollen accumulation rates from the northern boreal forest as a record of interannual variation in July temperature. J Quat Sci 24:513–521CrossRefGoogle Scholar
  30. Kupriyanova LA (1951) Investigations of pollen and spores from the soil surface of High Arctic. Russ Bot J 36:258–269 (in Russian)Google Scholar
  31. Latałowa M, Van der Knaap WO (2006) Late quaternary expansion of Norway spruce Picea abies (L.) Karst. in Europe according to pollen data. Quat Sci Rev 25:2,780–2,805Google Scholar
  32. Lisitsyna OV, Giesecke T, Hicks S (2011) Exploring pollen percentage threshold values as an indication for the regional presence of major European trees. Rev Palaeobot Palynol 166:311–324CrossRefGoogle Scholar
  33. Mal’gina EA (1950) The experience of comparison of pollen dispersion of some trees with their ranges within European part of USSR. Proc Geogr Inst Acad Sci USSR 46:256–270 (in Russian)Google Scholar
  34. Moe D (1970) The post-glacial immigration of Picea abies into Fennoscandia. Bot Notiser 123:61–66Google Scholar
  35. Nosova MB (2008) Holocene forest vegetation dynamics in the Central Forest Natural Reserve (on the basis of palynological analysis). Dissertation, Main Botanical Garden RAS, Moscow (in Russian)Google Scholar
  36. Nosova MB (2009) Holocene pollen diagrams as a source of the information about antropogenic impact on vegetation in prehistoric period (on an example of Central Forest Natural Reserve, Russia). Bulletin Moscovskogo Obshestva Isrytateley Prirody 114:30–36 (in Russian)Google Scholar
  37. Novenko EYu, Volkova EM, Nosova NB, Zuganova IS (2009) Late Glacial and Holocene landscape dynamics in the southern taiga zone of East European Plain according to pollen and macrofossil records from the Central Forest State Reserve (Valdai Hills, Russia). Quat Int 207:93–103CrossRefGoogle Scholar
  38. Novenko EY, Nosova MB, Krasnorutskaya KV (2011) Features of surface pollen spectra of south taiga of East-European Plain. News of Tula State Univ. Nat Sci 2:345–354 (in Russian)Google Scholar
  39. Overpeck JT, Webb T III, Prentice IC (1985) Quantitative interpretation of fossil pollen spectra: dissimilarity coefficients and the method of modern analogue. Quat Res 23:87–108CrossRefGoogle Scholar
  40. Poska A, Pidek IA (2010) Pollen dispersal and deposition characteristics of Abies alba, Fagus sylvatica and Pinus sylvestris, Rostocze region (SE Poland). Veget Hist Archaeobot 19:91–101CrossRefGoogle Scholar
  41. Pravdin LF (1975) European spruce and Siberian spruce. Nauka, Moscow (in Russian)Google Scholar
  42. Prentice IC (1978) Modern pollen spectra from lake sediments in Finland and Finnmark, north Norway. Boreas 7:131–153CrossRefGoogle Scholar
  43. Saarse L, Niinemets E, Poska A, Veski S (2009) Is there a relationship between crop farming and the Alnus decline in the eastern Baltic region. Veget Hist Archaeobot 19:17–28CrossRefGoogle Scholar
  44. Savelieva LA (2007) Features of the spruce and alder migration in the Holocene in North-West European part of Russia (on the basis of palynological analysis of swamp and lake sediments). Dissertation, St. Petersburg State University (in Russian)Google Scholar
  45. Schmidt-Vogt H (1977) Die Fichte—Ein Handbuch in zwei Bänden. Band I: Taxonomie–Verbreitung–Morphologie–Waldgesellschaften. Parey, HamburgGoogle Scholar
  46. Seppä H, Hicks S (2006) Integration of modern and past pollen accumulation rate (PAR) records across the arctic tree-line: a method for more precise vegetation reconstructions. Quat Sci Rev 25:1,501–1,516CrossRefGoogle Scholar
  47. Serebrianiy LR (1974) Migration of spruce on the east and north of Eurasia in Late- and Postglacial times. Bull Quatern Comm 41:13–23 (in Russian)Google Scholar
  48. Stockmarr J (1971) Tablets with spores used in absolute pollen analysis. Pollen Spores 13:615–621Google Scholar
  49. Sugita S, Gaillard M-J, Broström A (1999) Landscape openness and pollen records: a simulation approach. Holocene 9:409–421CrossRefGoogle Scholar
  50. Sugita S, Hicks S, Sormunen H (2010) Absolute pollen productivity and pollen–vegetation relationships in northern Finland. J Quat Sci 25:724–736CrossRefGoogle Scholar
  51. Tanţău I, Reille M, De Beaulieu J-L, Fărcaş S (2006) Late Glacial and Holocene vegetation history in the southern part of Transylvania (Romania): pollen analysis of two sequences from Avrig. J Quat Sci 21:49–61CrossRefGoogle Scholar
  52. Van der Knaap WO, Van Leeuwen JFN, Finsinger W, Gobet E, Pini R, Schweizer A, Valsecchi V, Ammann B (2005) Migration and population expansion of Abies, Fagus, Picea and Quercus since 15000 years in and across the Alps, based on pollen-percentage threshold values. Quat Sci Rev 24:631–644Google Scholar
  53. Zernitskaya V, Mikhailov N (2009) Evidence of early farming in the Holocene pollen spectra of Belarus. Quat Int 203:91–104CrossRefGoogle Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2014

Authors and Affiliations

  • Maria B. Nosova
    • 1
  • Elena E. Severova
    • 2
  • Olga A. Volkova
    • 2
  • Jana V. Kosenko
    • 2
  1. 1.Main Botanical Garden RASMoscowRussia
  2. 2.Higher Plants DepartmentMoscow State UniversityMoscowRussia

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