, Volume 81, Issue 1, pp 1–16 | Cite as

Nitrogen dynamics of a boreal black spruce wildfire chronosequence

  • Ben Bond-Lamberty
  • Stith T. Gower
  • Chuankuan Wang
  • Pascal Cyr
  • Hugo Veldhuis
Original paper


This study examined the nitrogen (N) dynamics of a black spruce (Picea mariana (Mill.) BSP)-dominated chronosequence in Manitoba, Canada. The seven sites studied each contained separate well- and poorly drained stands, originated from stand-killing wildfires, and were between 3 and 151 years old. Our goals were to (i) measure total N concentration ([N]) of all biomass components and major soil horizons; (ii) compare N content and select vegetation N cycle processes among the stands; and (iii) examine relationships between ecosystem C and N cycling for these stands. Vegetation [N] varied significantly by tissue type, species, soil drainage, and stand age; woody debris [N] increased with decay state and decreased with debris size. Soil [N] declined with horizon depth but did not vary with stand age. Total (live + dead) biomass N content ranged from 18.4 to 99.7 g N m−2 in the well-drained stands and 37.8–154.6 g N m−2 in the poorly drained stands. Mean soil N content (380.6 g N m−2) was unaffected by stand age. Annual vegetation N requirement (5.9 and 8.4 g N m−2 yr−1 in the middle-aged well- and poorly drained stands, respectively) was dominated by trees and fine roots in the well-drained stands, and bryophytes in the poorly drained stands. Fraction N retranslocated was significantly higher in deciduous than evergreen tree species, and in older than younger stands. Nitrogen use efficiency (NUE) was significantly lower in bryophytes than in trees, and in deciduous than in evergreen trees. Tree NUE increased with stand age, but overall stand NUE was roughly constant (∼ ∼150 g g−1 N) across the entire chronosequence.


Picea mariana Pinus banksiana Populus tremuloides Sphagnum Biogeochemical cycling Boreal forest 


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  1. Amthor JS, Chen JM, Clein JS, Frolking SE, Goulden ML, Grant RF, Kimball JS, King AW, McGuire AD, Nikolov NT, Potter CS, Wang S, ofsy SC (2001) Boreal forest CO2 exchange and evapotranspiration predicted by nine ecosystem process models: intermodal comparisons and relationships to field measurements. J Geophys Res-Atmos 106(D24):33623–33648CrossRefGoogle Scholar
  2. Apps MJ, Kurz WA, Luxmoore RJ, Nilsson LO, Sedjo RA, Schmidt R, Simpson LG,Vinson TS (1993) The changing role of circumpolar boreal forests and tundra in the global carbon cycle. Water Air Soil Poll 70:39–53CrossRefGoogle Scholar
  3. Binkley D (1992) Mixtures of N2-fixing and non-N2-fixing tree species. In: Cannell MGR, Malcolm DC, Robertson P (eds) The ecology of mixed species stands of trees. Blackwell, Oxford, pp 99–123Google Scholar
  4. Bond-Lamberty B, Wang C, Gower ST (2002a) Above- and belowground biomass and sapwood area allometric equations for six boreal tree species of northern Manitoba. Can J For Res 32(8):1441–1450CrossRefGoogle Scholar
  5. Bond-Lamberty B, Wang C, Gower ST (2002b) Annual carbon flux from woody debris for a boreal black spruce fire chronosequence. J Geophys Res-Atmos 108(D3): art. no. 8220 (WFX 1-1 to 1–10)Google Scholar
  6. Bond-Lamberty B, Wang C, Gower ST (2002c) Leaf area dynamics of a boreal black spruce fire chronosequence. Tree Physiol 22(14):993–1001Google Scholar
  7. Bond-Lamberty B, Wang C, Gower ST (2004a) The contribution of root respiration to soil surface CO2 flux in a boreal black spruce fire chronosequence. Tree Physiol 24(12):1387–1395Google Scholar
  8. Bond-Lamberty B, Wang C, Gower ST (2004b) Net primary production and net ecosystem production of a boreal black spruce fire chronosequence. Global Change Biol 10(4):473–487CrossRefGoogle Scholar
  9. Bond-Lamberty B, Wang C, Gower ST (2005) Spatiotemporal measurement and modeling of boreal forest soil temperatures. Agric For Meteorol 131(1–2):27–40CrossRefGoogle Scholar
  10. Bremmer JM (1965) Total nitrogen. Methods of Soil Analysis, Part 2. C. A. Black. Madison, WI. Am Soc Agron 9:1149–1178Google Scholar
  11. Clymo RS (1970) The growth of Sphagnum: methods of measurement. J Ecol 58(1):13–49CrossRefGoogle Scholar
  12. Cole DW, Rapp M (1981) Element cycling in forest ecosystems. In: Reichle DE (ed) Dynamic properties of forest ecosystems. Cambridge University Press, London, pp 341–409Google Scholar
  13. DeLuca TH, Nilsson M-C, Zackrisson O (2002a) Nitrogen mineralization and phenol accumulation along a fire chronosequence in northern Sweden. Oecologia 133:206–214CrossRefGoogle Scholar
  14. DeLuca TH, Zackrisson O, Nilsson M-C, Sellstedt A (2002b) Quantifying nitrogen-fixation in feather moss carpets of boreal forests. Nature 419:917–920CrossRefGoogle Scholar
  15. Dyrness CT, Norum RA (1983) The effects of experimental fires on black spruce forest floors in interior Alaska. Can J For Res 13:879–893Google Scholar
  16. Dyrness CT, Van Cleve K, Levison JD (1989) The effect of wildfire on soil chemistry in four forest types in interior Alaska. Can J For Res 19:1389–1396Google Scholar
  17. Finér L, Mannerkoski H, Piirainen S, Starr M (2003) Carbon and nitrogen pools in an old-growth, Norway spruce mixed forest in eastern Finland and changes associated with clear-cutting. For Ecol Manage 174:51–63CrossRefGoogle Scholar
  18. Flanagan LB, Van Cleve K (1983) Nutrient cycling in relation to decomposition and organic-matter quality in taiga ecosystems. Can J For Res 13:795–817Google Scholar
  19. Flannigan MD, Bergeron Y, Engelmark O (1998) Future wildfire in circumboreal forests in relation to global warming. J Veg Sci 9(4):469–476CrossRefGoogle Scholar
  20. Foster NW, Morrison IK (1976) Distribution and cycling of nutrients in a natural Pinus banksiana ecosystem. Ecology 57:110–120CrossRefGoogle Scholar
  21. Foster NW, Morrison IK, Hazlett PW, Hogan GD, Salerno MI (1995) Changes in nutrient procurement with age and site productivity in jack pine forests. New Zeal J For Ecol 24:169–182Google Scholar
  22. Goldammer JG, Furyaev VV (1996) Fire in ecosystems of boreal Eurasia: ecological impacts and links to the global system. In: Goldammer JG, Furyaev VV (eds) Fire in ecosystems of boreal eurasia, vol 48. Kluwer Academic Publishers, Dordrecht, pp 1–20Google Scholar
  23. Gower ST, Gholz HL, Nakane K, Baldwin VC (1994) Production and carbon allocation patterns of pine forests. Ecol Bull (Copenhagen) 43:115–135Google Scholar
  24. Gower ST, Hunter A, Campbell JS, Vogel JG, Veldhuis H, Harden JW, Trumbore SE, Norman JM, Kucharik CJ (2000) Nutrient dynamics of the southern and northern BOREAS boreal forests. Écoscience 7(4):481–490Google Scholar
  25. Gower ST, Isebrands JG, Sheriff DW (1995) Carbon allocation and accumulation in conifers. In: Smith WK, Hinckley TM(eds) Resource physiology of conifers. Academic Press, San Diego, pp 217–254Google Scholar
  26. Gower ST, Krankina ON, Olson RJ, Apps MJ, Linder S, Wang C (2001) Net primary production and carbon allocation patterns of boreal forest ecosystems. Ecol Appl 11(5):1395–1411Google Scholar
  27. Gower ST, Vogel JG, Norman JM, Kucharik CJ, Steele S, Stow TK (1997) Carbon distribution and aboveground net primary production in aspen, jack pine, and black spruce stands in Saskatchewan and Manitoba, Canada. J Geophys Res 102(D24):29029–29041CrossRefGoogle Scholar
  28. Halliwell DH, Apps MJ (1997) Boreal ecosystem-atmosphere study (BOREAS) biometry and auxiliary sites: soils and detritus data. AB, Forestry Canada, Northern Forestry Centre, EdmontonGoogle Scholar
  29. Harden JW, Mack M, Veldhuis H, Gower ST (2003) Fire dynamics and implications for nitrogen cycling in boreal forests. J Geophys Res-Atmos 108(D3):art. no. 8223Google Scholar
  30. Helmisaari H-S, Makkonen K, Kellomäki S, Valtonen E, Mälkönen E (2002) Below- and above-ground biomass, production and nitrogen use in Scots pine stands of eastern Finland. For Ecol Manage 165:317–326CrossRefGoogle Scholar
  31. Hobbie SE, Nadelhoffer KJ, Högberg P (2002) A synthesis: the role of nutrients as constraints on carbon balances in boreal and arctic regions. Plant Soil 242(1):163–170CrossRefGoogle Scholar
  32. Kasischke ES, Stocks BJ (eds) (2000) Fire, climate change, and carbon cycling in the boreal forest. Springer-Verlag, New YorkGoogle Scholar
  33. Kozlowski TT, Pallardy SG (1997) The physiological ecology of woody plants. Academic Press, San DiegoGoogle Scholar
  34. Laiho R, Prescott CE (2004) Decay and nutrient dynamics of coarse woody debris in northern coniferous forests: a synthesis. Can J For Res 34(4):763–777CrossRefGoogle Scholar
  35. Lambert RL, Lang GE, Reiners WA (1980) Loss of mass and chemical change in decaying boles of a subalpine balsam fir forest. Ecology 61(6):1460–1473CrossRefGoogle Scholar
  36. Landsberg JJ, Gower ST (1997) Applications of physiological ecology to forest management. Academic Press, San DiegoGoogle Scholar
  37. Linder S, Benson ML, Myers BJ, Raison RJ (1987) Canopy dynamics and growth of Pinus radiata. 1 Effects of irrigation and fertilization during a drought. Can J For Res 17(10):1157–1165Google Scholar
  38. Litvak M, Miller S, Wofsy SC, Goulden ML (2002) Effect of stand age on whole ecosystem CO2 exchange in the Canadian boreal forest. J Geophys Res-Atmos 108(D3):art. no. 8225 (WFX 6–1 to 6–11)Google Scholar
  39. Mäkipää R (1995) Effect of nitrogen input on carbon accumulation of boreal forest soils and ground vegetation. For Ecol Manage 79:217–226CrossRefGoogle Scholar
  40. Nadelhoffer KJ (2000) The potential effects of nitrogen deposition on fine-root production in forest ecosystems. New Phytol 147:131–139CrossRefGoogle Scholar
  41. Oȁ9Connell KEB, Gower ST, Norman JM (2003) Net ecosystem production of two contrasting boreal black spruce forest communities. Ecosystems 6(3):248–260CrossRefGoogle Scholar
  42. Reich PB, Grigal DF, Aber JD, Gower ST (1997) Nitrogen mineralization and productivity in 50 hardwood and conifer stands of diverse soils. Ecology 78(2):335–347CrossRefGoogle Scholar
  43. Ruess RW, Hendrick RL, Burton AJ, Pregitzer KS, Sveinbjornssön B, Allen MF, Maurer GE (2003) Coupling fine root dynamics with ecosystem carbon cycling in black spruce forests of interior Alaska. Ecol Monogr 73(4):643–662Google Scholar
  44. Ruess RW, Van Cleve K, Yarie J, Viereck LA (1996) Contributions of fine root production and turnover to the carbon and nitrogen cycling in taiga forests of the Alaskan interior. Can J For Res 26(8):1326–1336Google Scholar
  45. Santantonio D, Hermann RK, Overton WS (1977) Root biomass studies in forest ecosystems. Pedobiologia 17:1–31Google Scholar
  46. SAS Institute Inc (2001) SAS OnlineDoc® Version 8. Cary, NCGoogle Scholar
  47. Schlesinger WH (1997) Biogeochemistry: an analysis of global change. Harcourt Brace & Company, San DiegoGoogle Scholar
  48. Schulze E-D, Schulze W, Kelliher FM, Vygodskaya NN, Ziegler W, Kobak KI, Koch H, Arneth A, Kusnetsova WA, Sogatchev A, Issajev A, Bauer GA, Hollinger DY (1995) Aboveground biomass and nitrogen nutrition in a chronosequence of pristine Dahurian Larix stands in eastern Siberia. Can J For Res 25(6):943–960Google Scholar
  49. Sellers J, Hall FG, Kelly D, Black TA, Baldocchi DD, Berry JA, Ryan MG, Ranson KJ, Crill PM, Lettenmaier DP, Margolis H, Cihlar J, Newcomer J, Fitzjarrald DR, Jarvis PG, Gower ST, Halliwell DH, Williams D, Goodison B, Wickland DE, Guertin FE (1997) BOREAS in 1997: experiment overview, scientific results, and future directions. J Geophys Res 102:28731–28769CrossRefGoogle Scholar
  50. Soil Classification Working Group (1998) The canadian system of soil classification. NRC Research Press, Ottawa, CanadaGoogle Scholar
  51. Steele S, Gower ST, Vogel JG, Norman JM (1997) Root mass, net primary production and turnover in aspen, jack pine and black spruce forests in Saskatchewan and Manitoba, Canada. Tree Physiol 17:577–587Google Scholar
  52. Stocks BJ, Lee BS, Martell DL (1996) Some potential carbon budget implications of fire management in the boreal forest. In: Apps MJ, Price DT (eds) Forest ecosystems, forest management and the global carbon cycle vol 40. Springer, Berlin, p 451Google Scholar
  53. Trumbore SE, Harden JW (1997) Accumulation and turnover of carbon in organic and mineral soils of the BOREAS northern study area. J Geophys Res-Atmos 102(D24):28817–30CrossRefGoogle Scholar
  54. Turetsky MR (2003) The role of bryophytes in carbon and nitrogen cycling. The Bryologist 106(3):395–409CrossRefGoogle Scholar
  55. Turvey ND, Smethurst PJ (1989) Apparent accumulation of nitrogen in soil under radiata pine: misleading results from a chronosequence. Research Strategies for Long-term Site Productivity, Proceedings, IEA/BE A3 Workshop, Seattle, WA, August 1988. IEA/BE Report No. 8, Forest Research Institute, New ZealandGoogle Scholar
  56. Van Cleve K, Oliver L, Schlentner RE, Viereck LA, Dyrness CT (1983) Productivity and nutrient cycling in taiga forest ecosystems. Can J For Res 13:747–767Google Scholar
  57. Van Cleve K, Viereck LA, Schlentner RE (1971) Accumulation of nitrogen in alder (Alnus) ecosystems near Fairbanks, Alaska. Arctic Alpine Res 3:101–1141CrossRefGoogle Scholar
  58. Veldhuis H (1995) Soils of the Tower Sites and Super Site, Northern Study Area (BOREAS), Thompson, Manitoba, Canada. Winnipeg, MB, Agriculture and Agri-Food Canada, Res. Branch, Centre for Land and Biological Resources Research, Manitoba Land Resource Unit, p 61Google Scholar
  59. Viereck LA (1983) The effects of fire in black spruce ecosystems of Alaska and northern Canada. In: Wein RW, MacLean DA (eds) The role of fire in northern circumpolar ecosystems. John Wiley & Sons, New York, pp 201–220Google Scholar
  60. Vitousek PM (1982) Nutrient cycling and nutrient use efficiency. Am Nat 119(4):553–572CrossRefGoogle Scholar
  61. Vitousek PM, Howarth RW (1991) Nitrogen limitation on land and in the sea: how can it occur? Biogeochemistry 13:87–115CrossRefGoogle Scholar
  62. Vitousek PM, Reiners WA (1975) Ecosystem succession and nutrient retention: a hypothesis. BioScience 25(6):376–81CrossRefGoogle Scholar
  63. Vogt KA, Vogt DJ, Bloomfield J (1998) Analysis of some direct and indirect methods for estimating root biomass and production of forests at an ecosystem level. Plant Soil 200:71–89CrossRefGoogle Scholar
  64. Wan S, Hui D, Luo Y (2001) Fire effects on nitrogen pools and dynamics in terrestrial ecosystems: a meta-analysis. Ecol Appl 11(5):1349–1365Google Scholar
  65. Wang C, Bond-Lamberty B, Gower ST (2002) Soil surface CO2 flux in a boreal black spruce fire chronosequence. J Geophys Res 108(D3):art. no. 8224 (WFX 5-1 to 5–8)Google Scholar
  66. Wang C, Bond-Lamberty B, Gower ST (2003) Carbon distribution of a well- and poorly-drained black spruce fire chronosequence. Global Change Biol 9(6):1–14Google Scholar
  67. Wirth C, Schulze E-D, Lühker B, Grigoriev S, Siry M, Hardes G, Ziegler W, Backor M, Bauer GA, Vygodskaya NN (2002) Fire and site type effects on the long-term carbon and nitrogen balance in pristine Siberian Scots pine forests. Plant Soil 242(1):41–63CrossRefGoogle Scholar
  68. Zackrisson O, DeLuca TH, Nilsson M-C, Sellstedt A, Berglund LM (2004) Nitrogen fixation increases with successional age in boreal forests. Ecology 85(12):3327–3334Google Scholar

Copyright information

© Springer Science+Business Media B.V. 2006

Authors and Affiliations

  • Ben Bond-Lamberty
    • 1
  • Stith T. Gower
    • 1
  • Chuankuan Wang
    • 2
  • Pascal Cyr
    • 3
  • Hugo Veldhuis
    • 4
  1. 1.Department of Forest Ecology and ManagementUniversity of WisconsinMadisonUSA
  2. 2.Ecology ProgramNortheast Forestry UniversityHarbinChina
  3. 3.Department of Soil ScienceUniversity of ManitobaWinnipegCanada
  4. 4.Agriculture and Agri-Food CanadaUniversity of ManitobaWinnipegCanada

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