, Volume 15, Issue 7, pp 1065–1082 | Cite as

Carbon Accumulation Patterns During Post-Fire Succession in Cajander Larch (Larix cajanderi) Forests of Siberia

  • Heather D. AlexanderEmail author
  • Michelle C. Mack
  • Scott Goetz
  • Michael M. Loranty
  • Pieter S. A. Beck
  • Kamala Earl
  • Sergey Zimov
  • Sergey Davydov
  • Catharine C. Thompson


Increased fire activity within boreal forests could affect global terrestrial carbon (C) stocks by decreasing stand age or altering tree recruitment, leading to patterns of forest regrowth that differ from those of pre-fire stands. To improve our understanding of post-fire C accumulation patterns within boreal forests, we evaluated above- and belowground C pools within 17 Cajander larch (Larix cajanderi) stands of northeastern Siberia that varied in both years since fire and stand density. Early-successional stands (<20-year old) exhibited low larch recruitment, and consequently, low density, aboveground larch biomass, and aboveground net primary productivity (ANPPtree). Mid-successional stands (21- to 70-year old) were even-aged with considerable variability in stand density. High-density mid-successional stands had 21 times faster rates of ANPPtree than low-density stands (252 vs. 12 g C m−2 y−1) and 26 times more C in aboveground larch biomass (2,186 vs. 85 g C m−2). Density had little effect on total soil C pools. During late-succession (>70-year old), aboveground larch biomass, ANPPtree, and soil organic layer C pools increased with stand age. These stands were low density and multi-aged, containing both mature trees and new recruits. The rapid accumulation of aboveground larch biomass in high-density, mid-successional stands allowed them to obtain C stocks similar to those in much older low-density stands (~8,000 g C m−2). If fire frequency increases without altering stand density, landscape-level C storage could decline, but if larch density also increases, large aboveground C pools within high-density stands could compensate for a shorter successional cycle.


larch Siberia carbon fire succession stand age density climate warming 



We would like to thank our collaborators at the Northeast Science Station and members of the Polaris Project for their assistance with travel and research logistics. Special thanks to T. Kajimoto and colleagues for providing raw biomass data for larch trees sampled near Cherskii, which we used to develop our allometric equations. Funding for this research was provided by NASA Ecosystems and Carbon Cycle Grant NNX08AG13G, NOAA Global Carbon Cycle Grant NA080AR4310526, and an international supplement to NSF OPP Grant 0806271.

Supplementary material

10021_2012_9567_MOESM1_ESM.doc (169 kb)
Supplementary material 1 (DOC 169 kb)


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Copyright information

© Springer Science+Business Media, LLC 2012

Authors and Affiliations

  • Heather D. Alexander
    • 1
    Email author
  • Michelle C. Mack
    • 1
  • Scott Goetz
    • 2
  • Michael M. Loranty
    • 2
  • Pieter S. A. Beck
    • 2
  • Kamala Earl
    • 1
  • Sergey Zimov
    • 3
  • Sergey Davydov
    • 3
  • Catharine C. Thompson
    • 4
  1. 1.Department of BiologyUniversity of FloridaGainesvilleUSA
  2. 2.Woods Hole Research CenterFalmouthUSA
  3. 3.Northeast Science StationPacific Institute of Geography, Far East Branch of the Russian Academy of SciencesCherskiiRepublic of Sakha (Yakutia), Russian Federation
  4. 4.National Park ServicePort AngelesUSA

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