1996
DOI: 10.2307/3236386
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Dynamics of understory vegetation in an old‐growth boreal coniferous forest, 1988–1993

Abstract: Abstract. Understorey vegetation changes in a South Norwegian old‐growth coniferous forest were studied between 1988 and 1993 in 200 1‐m2 vegetation plots. Our aims were to quantify the amount of between‐year compositional change, and to elaborate the environmental basis for long‐term vegetation change, including the previously identified gradient structure with a major gradient related to topography (and soil nutrient status and soil depth) and a minor gradient reflecting paludification and canopy coverage. … Show more

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Cited by 89 publications
(74 citation statements)
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References 65 publications
(59 reference statements)
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“…The strongest descriptors of the ordination patterns were catchment and diversity variables, closely followed by the Ellenberg indices, while the forest stand variables showed weak correlations with the floristic patterns for the field layer. In a more extensive study of forest understorey vegetation in Norway, Økland and Eilertsen (1996) concluded that the plant communities were affected by both catchment location and soil acidification, but not by N deposition, and the present study supports this conclusion.…”
Section: Discussionsupporting
confidence: 85%
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“…The strongest descriptors of the ordination patterns were catchment and diversity variables, closely followed by the Ellenberg indices, while the forest stand variables showed weak correlations with the floristic patterns for the field layer. In a more extensive study of forest understorey vegetation in Norway, Økland and Eilertsen (1996) concluded that the plant communities were affected by both catchment location and soil acidification, but not by N deposition, and the present study supports this conclusion.…”
Section: Discussionsupporting
confidence: 85%
“…Furthermore, an ordination made using all species resulted in a significant (p \ 0.05) effect of time, although it only explained 7% of the variation in the species data. Weak temporal changes over 5 years in boreal understorey were also found by Økland and Eilertsen (1996). The weak temporal effect is not surprising as the catchments span a broad biogeographical gradient, from boreo-nemoral to true northern boreal, and factors other than within-catchment temporal variation are expected to be important over such a gradient (Salemaa et al 2008).…”
Section: Discussionmentioning
confidence: 88%
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“…Some small changes can be explained by short-term variability (cf. Økland, 1995;Økland and Eilertsen, 1996). Changes is bryophytes and lichens can be partly attributed to wrong determination by some authors (especially Sphagnum or Calypogeia species), overlooking (Pohlia and Cephalozia species), and/or local disturbances (e.g.…”
Section: Vegetation Changesmentioning
confidence: 99%
“…E-mail address: neuhauslova@ibot.cas.cz (Z. Neuhäuslová). Økland, 1994, 1995Økland and Eilertsen, 1996). Most studies have followed the impact of air pollution on changes in the occurrence and abundance of plants.…”
Section: Introductionmentioning
confidence: 99%