Plant Ecology

, Volume 213, Issue 6, pp 1027–1035 | Cite as

Compositional vegetation changes and increased red spruce abundance during the Little Ice Age in a sugar maple forest of north-eastern North America

  • Daniel Houle
  • Pierre J. H. Richard
  • Sabary Omer Ndzangou
  • Marc Richer-Laflèche
Article

Abstract

In north-eastern North America, the recent red spruce decline has been linked to atmospheric pollution, notably acid rain, although climate was also advocated as a potential factor. A high resolution lake sediment pollen stratigraphy was obtained to elucidate long-term trends in tree-species abundance in a sugar maple—yellow birch forest. The reconstructed history (~250–1996 A.D.) showed a steady increase of red spruce after 1300 A.D., with a peak between 1600 and 1900 A.D. followed by a strong decline in the last century, while sugar maple and yellow birch experienced an opposite trend. Red spruce abundance reached its apogee during the cool Little Ice Age (LIA) and decreased abruptly when annual temperature in the region increased by 2 °C in the last 125 years. American Beech was much more abundant in the forest before the LIA, typifying a sugar maple—American beech forest as the dominant forest type during the Late Holocene. Our results suggest that climate warming has played an important role in the current red spruce decline, the latter having been initiated well before acidic depositions reached deleterious potential effects on red spruce. Climate warming probably acted as a long-term predisposing factor that was aggravated by atmospheric pollution, in the last decades.

Keywords

Picea rubens Climate warming Paleolimnology Forest dynamics Little Ice Age Acer saccharum 

References

  1. Boucher Y, Arseneault D, Sirois L, Blais L (2009) Logging pattern and landscape changes over the last century at the boreal and deciduous forest transition in Eastern Canada. Landscape Ecol 24:171–184. doi:10.1007/s10980-008-9294-8 CrossRefGoogle Scholar
  2. Boulfroy E, Lessard G, Grenon F, Blanchet P, Alvarez E (2010) Portrait de la forêt préindustrielle de la région de Portneuf. CERFO. Réf. 09-0489-EB-05/02/2010Google Scholar
  3. Bradshaw RHW (1988) Spatially-precise studies of forest dynamics. In: Huntley B, Webb T III (eds) Vegetation History. Kluwer Academic Publishers, Dordrecht, pp 725–751CrossRefGoogle Scholar
  4. Campbell ID, McAndrews JH (1993) Forest disequilibrium caused by rapid Little Ice Age cooling. Nature 366:336–338CrossRefGoogle Scholar
  5. Cleveland WS (1979) Robust locally weighted regression and smoothing scatterplots. J Am Stat Assoc 74(368):829–836Google Scholar
  6. Darcy P, Carignan R (1997) Influence of catchment topography on water chemistry in southeastern Québec Shield lakes. Can J Fish Aquat Sci 54:2215–2227CrossRefGoogle Scholar
  7. Davis MB, Calcote RR, Sugita S, Takahara H (1998) Patchy invasion and the origin of a Hemlock–Hardwoods forest mosaic. Ecology 79:2641–2659Google Scholar
  8. DeHayes DH, Schaberg PG, Hawley GJ, Strimbeck GR (1999) Acid rain impacts on calcium nutrition and forest health. Bioscience 49:789–800CrossRefGoogle Scholar
  9. Delcourt PA, Delcourt HR, Webb Th III (1984) Atlas of mapped distributions of dominance and modern pollen percentages for important tree taxa of eastern North America. American Association of Stratigraphic Palynologists (AASP), Contributions Series 14: 131 ppGoogle Scholar
  10. Duchesne L, Ouimet R, Moore JD, Paquin R (2005) Changes in structure and composition of maple-beech stands following sugar maple decline in Québec, Canada. For Ecol Manag 208:223–236CrossRefGoogle Scholar
  11. Faegri K, Iversen J (1975) Textbook of pollen analysis (3rd edition revised by K. Faegri). Blackwell Scientific Publications, OxfordGoogle Scholar
  12. Gajewski K (1987) Climatic impacts on the vegetation of eastern North America for the past 2000 years. Plant Ecol 68:179–190CrossRefGoogle Scholar
  13. Gajewski K (1988) Late Holocene climate changes in eastern North America estimated from pollen data. Quat Res 29:255–262CrossRefGoogle Scholar
  14. Hamburg SP, Cogbill CV (1988) Historical decline of red spruce population and climatic warming. Nature 331:428–430CrossRefGoogle Scholar
  15. Hawley GJ, Schaberg PG, Eager C, Borer CH (2006) Calcium addition at the Hubbard Brook Experimental Forest reduced winter injury to red spruce in a high-injury year. Can J For Res 36:2544–2549CrossRefGoogle Scholar
  16. Houle D, Paquin R, Ouimet R, Laflamme JG (1999) Atmospheric depositions interactions with a mixed harwood and a coniferous forest canopy at the Lake Clair Watershed. Can J For Res 29:1944–1957CrossRefGoogle Scholar
  17. Houle D, Moore JD, Provencher J (2007) Ice bridges on the St. Lawrence River as an index of winter severity from 1620 to 1910. J Clim 20:757–764CrossRefGoogle Scholar
  18. Johnson AH, Cook ER, Siccama TG (1988) Climate and red spruce growth and decline in the northern Appalachians. Proc Natl Acad Sci 85:5369–5373PubMedCrossRefGoogle Scholar
  19. Jones PD, Briffa KR, Barnett TP, Tett SFB (1998) High-resolution palaeoclimatic records for the last millennium: interpretation, integration and comparison with General Circulation Model control-run temperatures. Holocene 8:455–471CrossRefGoogle Scholar
  20. Landres PB, Morgan P, Swanson FJ (1999) Overview of the use of natural variability concepts in managing ecological systems. Ecol Appl 9(4):1179–1188. doi:10.2307/2641389 Google Scholar
  21. Lazarus BE, Schaberg PG, Dehayes DH, Hawley GJ (2004) Severe red spruce winter injury in 2003 creates unusual ecological event in the northeastern United States. Can J For Res 34:1784–1788CrossRefGoogle Scholar
  22. Leblanc DC, Nicholas NS, Zedaker SM (1992) Prevalence of individual-tree growth decline in red spruce populations of the southern Appalachian Mountains. Can J For Res 22:905–914CrossRefGoogle Scholar
  23. Lindblahd M, Jacobson GL Jr, Schauffler M (2003) The postglacial history of three Picea species in New England, USA. Quat Res 59:61–69CrossRefGoogle Scholar
  24. Long RP, Horsley SB, Hallett RA, Bailey SW (2009) Sugar maple growth in relation to nutrition and stress in the northeastern United States. Ecol App 19:1454–1466CrossRefGoogle Scholar
  25. Lozano-Garcia MDS, Caballero M, Ortega B, Rodriguez A, Sosa S (2007) Tracing the effects of the Little Ice Age in the tropical lowlands of eastern Mesoamerica. Proc Natl Acad Sci 104:16200–16203CrossRefGoogle Scholar
  26. Major JE, Barsi DC, Mosseler A, Campbell M, Rajora OP (2003) Light-energy processing and freezing-tolerance traits in red spruce and black spruce: species and seed-source variation. Tree Physiol 23:685–694PubMedCrossRefGoogle Scholar
  27. Ministère des Ressources naturelles (2002) No publication: DEF-0204 F-09Google Scholar
  28. Oldfield F, Appleby PG (1984) Empirical testing of 210Pb-dating models for lakes sediments. In: Haworth EY, Lund JWG (eds) Lake Sediments and Environmental History. University of Minnesota Press, Minneapolis, pp 93–124Google Scholar
  29. Périé C, Ouimet R, Duchesne L (2006) Évolution contemporaine des principales caractéristiques dendrométriques des stations du RÉSEF. Mémoire de recherche forestière n° 149. ISBN 978-2-550-48118-8Google Scholar
  30. Schaberg PG, DeHayes DH, Hawley GJ, Strimbeck GR, Cumming JR, Murakami PF, Bower CH (2000) Acid mist and soil Ca and Al alter the mineral nutrition and physiology of red spruce. Tree Physiol 20:73–85PubMedCrossRefGoogle Scholar
  31. Shortle WC, Smith KT (1988) Aluminium-induced calcium deficiency syndrome in declining red spruce. Science 240:1017–1018PubMedCrossRefGoogle Scholar
  32. Sugita S (1998) Modelling pollen representation of vegetation. In: Gaillard MJ, Berglund BE, Frenzel B, Huckriede U (eds) Quantification of land surfaces cleared of forests during the Holocene. Palaeokllimaforschung/Palaeoclimate Research 27, Gustav Fischer Verlag, Stuttgart, pp 1–16Google Scholar
  33. Talon B, Payette S, Filion L, Delwaide A (2005) Reconstruction of the long-term fire history of an old-growth deciduous forest in Southern Québec, Canada, from charred wood in mineral soils. Quat Res 64:36–43CrossRefGoogle Scholar
  34. Viau AE, Ladd M, Gajewski K (20110 The climate of North America during the past 2,000 years reconstructed from pollen data, Global and Planetary Change. doi:10.1016/j.gloplacha.2011.09.010

Copyright information

© Springer Science+Business Media B.V. 2012

Authors and Affiliations

  • Daniel Houle
    • 1
    • 2
  • Pierre J. H. Richard
    • 3
  • Sabary Omer Ndzangou
    • 4
  • Marc Richer-Laflèche
    • 4
  1. 1.Forestry DivisionQuebec Department of Natural Resources and WildlifeSainte-FoyCanada
  2. 2.OuranosMontréalCanada
  3. 3.Geography DepartmentUniversity of MontrealOutremontCanada
  4. 4.National Institute of Research, Water, Earth and EnvironmentQuébecCanada

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