1995
DOI: 10.5558/tfc71219-2
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Direct seeding of black spruce in northwestern Ontario: Temporal changes in seedbed coverage and receptivity

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Cited by 15 publications
(19 citation statements)
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“…The coefficient of variation (CV = the standard deviation divided by the mean) across years ranges between 0.30 to 0.60 for mineral soil, 0.08 to 0.29 for humus, and 0.34 to 0.53 for burnt O f . While this is based on only 3 years, these CV values are similar to those obtained on mineral soil with repeated (3 years) sowing by Walker et al (1986; white spruce) and Fleming and Mossa (1995;black spruce). (Note that two of our species have aerial seed banks, but we can nonetheless use those data to make statements about the relative temporal variation in S g .)…”
Section: Possible Causes Of Early Mortalitymentioning
confidence: 69%
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“…The coefficient of variation (CV = the standard deviation divided by the mean) across years ranges between 0.30 to 0.60 for mineral soil, 0.08 to 0.29 for humus, and 0.34 to 0.53 for burnt O f . While this is based on only 3 years, these CV values are similar to those obtained on mineral soil with repeated (3 years) sowing by Walker et al (1986; white spruce) and Fleming and Mossa (1995;black spruce). (Note that two of our species have aerial seed banks, but we can nonetheless use those data to make statements about the relative temporal variation in S g .)…”
Section: Possible Causes Of Early Mortalitymentioning
confidence: 69%
“…Recall that the burnt O f seedbeds were not manipulated in any way. Unlike the 3-year sowing experiments of Walker et al (1986) and Fleming and Mossa (1995) on mineral soil, there was no clear tendency for the age-specific survivorship to worsen with time-sincedisturbance (scarification in their studies) as we tested for a trend in the survivorship values using a modification of the χ 2 test (Zar 1999, p. 565). Of the nine triplets in Table 5, only three showed a significant decline in S g with timesince-fire (pine on mineral soil, and white spruce on mineral soil and humus).…”
Section: Age-specific Survivorship and Time-since-firementioning
confidence: 91%
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“…8). On this soil type, slash reduction (FT, 5750 stems·ha −1 ) and exposure of mineral soil (FTB, 7980 stems·ha −1 ) resulted in these high recruitment numbers, presumably due to improved seedbed receptivity (Fleming and Mossa 1995;Prévost 1997). Interestingly enough, even with blading off the logging debris and O horizon, the species composition on the FTB treatment plots was dominated by jack pine (Pj 80 Sb 10 Bw 10 ).…”
Section: Stand-level Productivity Responsementioning
confidence: 94%
“…Furthermore, substantial nutrient reserves in the forest floor of mature fire-origin boreal stands (Foster et al 1995) may reduce the overall impact of nutrient removals by whole-tree harvesting. Compaction -disc trenching effects Similar planted-tree growth responses in the WT and WT T after the initial establishment phase suggest that the beneficial effects of disc trenching are relatively short-lived, with seedbeds being covered by litter (Fleming and Mossa 1995) and roots extending beyond the area of treatment influence within a few years. However, on some sites (e.g., Mattsson and Bergsten 2003), including those with highly competitive ericaceous shrubs (e.g., Kalmia angustifolia L.) (Thiffault et al 2004), there may be continued growth benefits from scarification.…”
Section: Fifteen-year Biomass-removal Effectsmentioning
confidence: 95%