Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Journal topic
Volume 9, issue 4
Biogeosciences, 9, 1405–1421, 2012
https://doi.org/10.5194/bg-9-1405-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 9, 1405–1421, 2012
https://doi.org/10.5194/bg-9-1405-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 16 Apr 2012

Research article | 16 Apr 2012

Factors promoting larch dominance in central Siberia: fire versus growth performance and implications for carbon dynamics at the boundary of evergreen and deciduous conifers

E.-D. Schulze1, C. Wirth2, D. Mollicone1,3, N. von Lüpke4, W. Ziegler1, F. Achard3, M. Mund4, A. Prokushkin5, and S. Scherbina6 E.-D. Schulze et al.
  • 1Max-Planck Institute for Biogeochemistry, P.O. Box 100164, 07701 Jena, Germany
  • 2Institute of Biology, University of Leipzig, Johannisalle 21–23, 04103 Leipzig, Germany
  • 3Institute of Environment and Sustainability, Joint Research Centre – TP440, 21027 Ispra, Italy
  • 4Dept. of Ecoinformatics,Bioemetrics and Forest Growth, University of Göttingen, Büsgenweg 4, 37077 Göttingen, Germany
  • 5V. N. Sukachev Institute of Forest, SB-RAS, Krasnoyarsk, Russia
  • 6Centralno-Sibirsky Natural Reserve, Bor, Russia

Abstract. The relative role of fire and of climate in determining canopy species composition and aboveground carbon stocks were investigated. Measurements were made along a transect extending from the dark taiga zone of central Siberia, where Picea and Abies dominate the canopy, into the Larix zone of eastern Siberia. We test the hypotheses that the change in canopy species composition is based (1) on climate-driven performance only, (2) on fire only, or (3) on fire-performance interactions. We show that the evergreen conifers Picea obovata and Abies sibirica are the natural late-successional species both in central and eastern Siberia, provided there has been no fire for an extended period of time. There are no changes in performance of the observed species along the transect. Fire appears to be the main factor explaining the dominance of Larix and of soil carbon. Of lesser influence were longitude as a proxy for climate, local hydrology and active-layer thickness. We can only partially explain fire return frequency, which is not only related to climate and land cover, but also to human behavior.

Stand-replacing fires decreased from 300 to 50 yrs between the Yenisei Ridge and the upper Tunguska. Repeated non-stand-replacing surface fires eliminated the regeneration of Abies and Picea. With every 100 yrs since the last fire, the percentage of Larix decreased by 20%.

Biomass of stems of single trees did not show signs of age-related decline. Relative diameter increment was 0.41 ± 0.20% at breast height and stem volume increased linearly over time with a rate of about 0.36 t C ha−1 yr−1 independent of age class and species. Stand biomass reached about 130 t C ha−1(equivalent to about 520 m3 ha−1). Individual trees of Larix were older than 600 yrs. The maximum age and biomass seemed to be limited by fungal rot of heart wood. 60% of old Larix and Picea and 30% of Pinus sibirica trees were affected by stem rot. Implications for the future role of fire and of plant diseases are discussed.

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