2007
DOI: 10.3759/tropics.16.151
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Spatial and topographic patterns of canopy gap formation in a mixed dipterocarp forest in Sarawak, Malaysia

Abstract: A B S T R A C T W e o b s e r v e d s p a t i a l a n d topographic patterns of canopy gap formation in

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Cited by 8 publications
(16 citation statements)
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“…We expected filtering due to moisture limitation at higher elevations; however, trait means shifted toward species and individuals with higher SLA, contrary to expectations that dry conditions favor low SLA (Wright et al 2004, ). Instead, the increase in SLA may be related to greater disturbance from tree fall and landslides at higher elevations that create light gaps and favor younger successional strategies (Ohkubo et al 2007).…”
Section: Discussionmentioning
confidence: 99%
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“…We expected filtering due to moisture limitation at higher elevations; however, trait means shifted toward species and individuals with higher SLA, contrary to expectations that dry conditions favor low SLA (Wright et al 2004, ). Instead, the increase in SLA may be related to greater disturbance from tree fall and landslides at higher elevations that create light gaps and favor younger successional strategies (Ohkubo et al 2007).…”
Section: Discussionmentioning
confidence: 99%
“…Thus marginal sites with low resource (e.g., light) availability should filter out fast‐growing, poorly defended species, causing low latex diversity within sites but high diversity across sites (Janzen 1974, Fine et al 2004, ). At our study site, light availability may be greater at higher elevations on steep ridges where disturbance from tree fall and landslides is likely highest (Ohkubo et al 2007), although soil nutrients are more abundant at lower elevations in valleys ().…”
Section: Introductionmentioning
confidence: 99%
“…Third, the four forest types vary not only in belowground resources, but also in slope. The loam soil and parts of the fine loam soil comprise steep slopes with greater occurrence and larger sizes of landslips than do the clay, low-lying parts of fine loam, and sandy loam soils (Ohkubo 2007a(Ohkubo , 2007bYamakura et al 1996). Steep slopes would result in larger, more frequent canopy openings and could explain why the decline in understorey irradiance was not monotonic with increases in soil resource availability.…”
Section: Causes and Consequences Of Soil-related Variation In Light Rmentioning
confidence: 99%
“…Furthermore, elevation and slope vary significantly among soil types: the sandy loam and clay soils occur at the highest and lowest elevations, respectively, and the loam and fine loam soils occur at intermediate elevations in Lambir (Baillie et al 2006). The loam and fine loam soils are located on steep slopes, where there are more frequent landslips (Ohkubo 2007a(Ohkubo , 2007b.…”
Section: Study Sitementioning
confidence: 99%
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