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Post-pirogenic Transformation of Soils and Soil Carbon Stocks in Sub-Tundra Woodlands of Kolyma Lowland: a Cascading Effect and Feedbacks

https://doi.org/10.15356/0373-2444-2015-3-129-140

Abstract

It is found that the high diversity of the upland ecosystems in sub-tundra woodlands of the Lower Kolyma River is caused by frequent fi res. The type of successions, the power of the active layer, the degree of gleization of the soil profi le, the intensity of cryogenic processes of mass transfer, the size of carbon stocks, the classificatory status of soils depends on the strength and duration of the fi re. Post-pirogenic transformation of vegetation, soils and tree species evolve according to the cascade principle, when every previous change generates and enhances subsequent change, i.e. feedback mechanisms are working actively. In the first years after the fire the expected reduction in carbon stocks of organic horizons (–3.4 kilogram of carbon per square meter) is observed, however, in the later stages the post-pirogenic effect of surplus (relative to initial) accumulation of organic matter at mineral surfaces (+1.7 kilogram of carbon per square meter) occurs. Such consequences of fi res as the lowering-lifting of roof permafrost and the intensification of cryogenic mass transfer in conditions of active organic matter accumulation of upper horizons can lead to post-pirogenic increase of the carbon pool of mineral depth (+2.5 kilogram of carbon per square meter). The time required to recover after a severe fire the initial stocks of soil carbon is 60–200 years.

About the Author

N. S. Mergelov
Institute of Geography, Russian Academy of Sciences
Russian Federation
Moscow


References

1. Bogdanov V.V. Infl uence of surface wild fi res on soil organic substance in cryolite zone of Central Evenkia, Extended Abstract of Cand. Sci. (Biol.) Dissertation, Krasnoyarsk, 2010. 20 p.

2. Vedrova E.F., Mukhortova L.V., Bezkorovainaya I.N., et al. Organic matter of soils under larch forests of the northern taiga in the Niznyaya Tunguska River basin. Eurasian Soil Sci., 2002, vol. 35, no. 8, pp. 857–864.

3. Gabysheva L.P. The effect of wild fi res on structure and phytomass of forest communities of Central Yakutia. Sovr. Probl. Nauki Obraz., 2012, no. 6, p. 569. (In Russ.).

4. Gubin S.V. Dynamics of formation of structure of tundra permafrost nongleyic soils (tundra cryozems). Pochvovedenie, 1993, no. 10, pp. 62–70. (In Russ.).

5. Gubin S.V. Paleogeografi cheskie aspekty pochvoobrazovaniya na Primorkikh nizmennostyakh Yakutii (Paleogeographic Aspects of Soil-Formation on Marine Lowlands of Yakutia). Pushchino: Otd. Nauchno-Tekh. Inform., Nauchn. Tsentra Biol. Issled., 1987. 27 p.

6. Gubin S.V. Late Pleistocene soil-formation on loessglacial deposits of Northeastern Eurasia, Extended Abstract of Doctoral (Biol.) Dissertation, Pushchino, 1999. 36 p.

7. Gubin S.V. and Lupachev A.V. Approaches to selection and analysis of buried soils in permafrost massifs of sediments of glacial complex. Kriosfera Zemli, 2012, vol. 14, no. 2, pp. 79–84. (In Russ.).

8. Isaev A.P. Resistance of permafrost forests to anthropogenic factors. Usp. Sovrem. Estestvozn., 2012, no. 11, pp. 41–43. (In Russ.).

9. Klassifi katsiya pochv Rossii (Classifi cation of Soils of Russia), Shishov L.L., et al. Eds. Moscow: Pochv. Inst. im. V.V. Dokuchaeva, Ross. Akad. Nauk, 1997. 235 p.

10. Kobak K.I. Bioticheskie komponenty uglerodnogo tsikla (Biotic Components of Carbon Cycle). Leningrad: Gidrometeoizdat Publ., 1988. 246 p.

11. Mazhitova G.G. About peculiarities of soil-formation on yedomas of Kolyma lowland. Pochvovedenie, 1989, no. 9, pp. 15–25. (In Russ.).

12. Mergelov N.S. and Targulian V.O. Accumulation of organic matter in the mineral layers of permafrostaffected soils of coastal lowlands in East Siberia, Eurasian Soil Sci., 2011, vol. 44, no. 3, pp. 249–260.

13. Prokushin A.S. Vodorastvorimoe organicheskoe veshchestvo v kriogennykh pochvakh pirogennykh suktsessii. Annotatsiya k otchetu po rezul’tatam realizatsii proekta Rossiiskogo Fonda Fundamental’nykh Issledovanii no. 05-05-64208 (Water-Soluble Organic Substances in Cryogenic Soils of Pyrogenic Successions: Annotation to the Report on the Results of the Russian Foundation for Basic Research Project no. 05-05-64208), 2005.

14. Tarabukina V.G. and Shumilov Yu.V. Pyrogenic transformation of forest soil in cryolitozone, in Mater. III mezhd. konf. “Produktivnost’ i ustoichivost’ lesnykh pochv,” Petrozavodsk, 7–11 sentyabrya 2009 g. (Proc. III Int. Conf. “Productivity and Resistance of Forest Soils,” Petrozavodsk, September 7–11, 2009). Petrozavodsk: Karel. Nauch. Tsentr, Ross. Akad. Nauk, 2009, pp. 112–116. (In Russ.).

15. Tarabukina V.G. and Savvinov D.D. Vliyanie pozharov na merzlotnye pochvy (Influence of Wild Fires on Permafrost Soils). Novosibirsk, 1990. 120 p.

16. Timofeev P.A., Isaev A.P., Shcherbakov I.P., et al. Lesa srednetaezhnoi podzony Yakutii (Forests of Mid-Taiga Subzone of Yakutia). Yakutsk: Yakut. Nauch. Tsentr, Sib. Otd., Ross. Akad. Nauk, 1994. 140 p.

17. Tishkov A.A. Biogeographical consequences of natural and anthropogenic climate changes. Biol. Bull. Rev., 2012, vol. 2, no. 2, pp. 132–140.

18. Tishkov A.A. Fires in steppes and savannah, Vopr. Stepevedeniya, 2003, no. 4, pp. 9–15. (In Russ.).

19. Tyrtikov A.P. Les na severnom predele v Azii (Forest on Northern Edge of Asia). Moscow: KMK Publ., 1995. 144 p.

20. Fominykh L.A. The peculiarities of soil formation in the Kolyma tundra. Eurasian Soil Sci., 1997, vol. 30, no. 8, pp. 811–819.

21. Chestnykh O.V., Zamolodchikov D.G., and Karelin D.V. Resources of organic carbon in the soils of tundra and forest-tundra ecosystems in Russia. Russ. J. Ecol., 1999, vol. 30, no. 6, pp. 392–398.

22. Balshi M.S., et al. The role of historical fire disturbance in the carbon dynamics of the pan-boreal region: a process-based analysis. J. Geophys. Res.: Biogeosci., 2007, vol. 112, no. 2, p. 29.

23. Beer C., Lucht W., Gerten D., et al. Effects of soil freezing and thawing on vegetation carbon density in Siberia: a modeling analysis with the Lund-PotsdamJena Dynamic Global Vegetation Model (LPJ-DGVM). Global Biogeochem. Cycles, 2007, vol. 21, GB1012.

24. Chapin F.S. III, et al. Role of land-surface changes in arctic summer warming. Science, 2005, vol. 310(5748), pp. 657–660.

25. Euskirchen E.S., McGuire A.D., Chapin F.S., et al. Changes in vegetation in northern Alaska under scenarios of climate change, 2003–2100: implications for climate feedbacks. Ecol. Appl., 2009, vol. 19(4), pp. 1022–1043.

26. Fontaine S., et al. Stability of organic carbon in deep soil layers controlled by fresh carbon supply. Nature, 2007, vol. 450, pp. 277–280.

27. Fontaine S., Bardoux G., Abbadie L., and Mariotti A. Carbon input to soil may decrease soil carbon content. Ecol. Lett., 2004, vol. 7, pp. 314–320.

28. Grosse G., et al. Vulnerability of high-latitude soil organic carbon in North America to disturbance. J. Geophys. Res., 2011, vol. 116, pp. 1–23.

29. Heimann M. and Reichstein M. Terrestrial ecosystem carbon dynamics and climate feedbacks. Nature, 2008, vol. 451, pp. 289–292.

30. Koven C., Friedlingstein P., Ciais P., et al. The effects of cryoturbation and insulation by organic matter on the formation of high-latitude soil carbon stocks in a land surface model. Geophys. Res. Lett., 2009, vol. 36, pp. 1–5.

31. MacDonald G.M., Kremenetski K.V., and Beilman D.W. Climate change and the northern Russian treeline zone. Philos. Trans. R. Soc. Lond., B, 2008, vol. 363(1501), pp. 2285–2299.

32. Parisien M.A., et al. Contributions of ignitions, fuels, and weather to the spatial patterns of burn probability of a boreal landscape. Ecosystems, 2011, vol. 14(7), pp. 1141–1155.

33. Scheffer M., Hirotaa M., Holmgren M., et al. Thresholds for boreal biome transitions. Proc. Natl. Acad. Sci. U.S.A., 2012, vol. 109(52), pp. 21384–21389.

34. Wirth C. Fire regime and tree diversity in boreal forests: implications for the carbon cycle, in Forest Diversity and Function: Temperate and Boreal Systems. New York: Springer-Verlag, 2005, pp. 309–344.


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For citations:


Mergelov N.S. Post-pirogenic Transformation of Soils and Soil Carbon Stocks in Sub-Tundra Woodlands of Kolyma Lowland: a Cascading Effect and Feedbacks. Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya. 2015;(3):129-140. (In Russ.) https://doi.org/10.15356/0373-2444-2015-3-129-140

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