Search

Climate-sensitive height–age models were developed for top height trees of trembling aspen (Populus tremuloides Michx.), jack pine (Pinus banksiana Lamb.), and white spruce (Picea glauca (Moench) Voss) in natural and reclaimed oil sands stands. We used stem analysis data collected from the Athabasca oil sands region in northern Alberta, Canada, and climate data generated by the ClimateWNA model. Height–age trajectories differed between top height trees in natural and reclaimed stands for jack pine and white spruce, but not for trembling aspen. At a given age, white spruce top height trees were taller and jack pine top height trees were shorter in reclaimed stands than those in natural stands, suggesting that it is easier to achieve similar forest productivity for oil sands sites reclaimed with white spruce stands than for sites reclaimed with jack pine stands. The principal climate variables were growing season (May to September) precipitation averaged over the previous 10 years for trembling aspen and jack pine and summer (June to August) precipitation averaged over the previous 10 years for white spruce. These variables had positive effects on the height–age trajectories. [ABSTRACT FROM AUTHOR]

Survival and growth of Siberian larch (SL, Larix sibirica Ledeb.) were compared with those of three conifer species native to Alberta, Canada: lodgepole pine (LP; Pinus contorta var. latifolia Engelm. ex S. Watson), white spruce (WS, Picea glauca (Moench) Voss), and jack pine (JP, Pinus banksiana Lamb.) at 12, 10, and 3 trial locations, respectively. The average data age was 18 years (range: 3 to 27 years). Survival of SL averaged 4.2% and 6.5% worse than LP and WS, respectively, while it was 5% better than JP. SL grew 25%, 94%, and 23% taller than LP, WS, and JP, respectively. Stem forking rates were similar between SL and LP, WS, and JP. The best seed sources for Alberta were mature trees established in Alberta and Saskatchewan of unknown initial provenances. The Russian Altai Mountain source grew well at high elevations, while the Finnish Raivola performed well in the northern, low-elevation area. Open-pollinated progeny tests of 58 families planted in five diverse locations yielded individual-tree narrow-sense heritabilities and family mean heritabilities for height at age 15 of 0.15 and 0.59, respectively. The type B between-site genetic correlation was 0.44, indicating a strong genotype × environment interaction. SL has performed well in Alberta, and its growth can be further improved by selection and breeding from appropriate seed sources. [ABSTRACT FROM AUTHOR]

Ecological processes driving tree success in the early stages of succession are complex and often poorly understood, involving direct and indirect relationships among multiple agents modulated by legacies. Reclamation areas of open-pit mines provide a unique opportunity to study these relationships, as these sites are often homogeneous and have few ecological legacies. Our study evaluated the early performance of three boreal tree species planted at different densities over a large reclaimed landscape (57 ha) in northern Alberta, Canada, that varied in landscape topography, surface soils, and coarse woody material. A range of soil, topographical, and seedling characteristics were measured over five growing seasons. The two surface soils had stark differences in their physical and chemical properties. Overall, seedling survival was high (> 80%) for jack pine (Pinus banksiana) and white spruce (Picea glauca) and somewhat lower (60%) for trembling aspen (Populus tremuloides). All three species grew taller in the fine-textured than in the coarse-textured soils. Linear models identified simple relationships among some of the monitored variables. To further explore more complex relationships, we built a structural equation model for jack pine growth, 2 and 5 years after planting. On coarse-textured soil, the factors controlling pine growth shifted from intrinsic factors of seedling quality in the second growing season to more complex interactions in the fifth growing season, driven by soil nutrients, water availability and colonizing vegetation. We believe these models have the potential to be useful in forest reclamation, by identifying driving factors that could be monitored to indicate reclamation success. [ABSTRACT FROM AUTHOR]

• Tree species determine the soil fungal composition, especially in the root fraction. • Tree effects dominated, even when accounting for chemistry and spatial distribution. • In soil DNA, spruce samples contained more ectomycorrhizal and pine samples more saprotrophic taxa. • Siberian larch soils were associated with a greater abundance of pathogenic taxa. • Sporocarp surveys found more ectomycorrhizal and saprotrophic taxa in pine stands. Gateway Hill is a 104-ha area in the oil sands region of Alberta, which was operationally reclaimed and reforested in the late 1980s and certified as reclaimed in 2007/08. In 2014, ∼30 years after reclamation was completed, we began studies with the main objective to determine the soil fungi present at the site. Sporocarp surveys in 2014 and 2016 were used to supplement metagenomic analyses of soil fungi in jack pine (Pinus banksiana), white spruce (Picea glauca), and Siberian larch (Larix sibirica) stands. Fungal internal transcribed spacer amplicons of DNA extracted from forest floor, root, and fine soil fractions were sequenced using Roche 454 pyrosequencing in 2014. Coarse soil reclamation samples and soil samples from a nearby unmined spruce stand were sequenced with Illumina in 2016. Sequenced community assemblages were first assessed using unconstrained multivariate analyses, and then using (partially) constrained ordination techniques to directly account for the effects of tree species and other confounding factors. Based on soil DNA analyses the relative abundance of ectomycorrhizal taxa was greater in spruce stands, saprotrophs were more abundant in pine stands, and pathogens were more abundant in larch stands. Associations of fungal taxa, mostly saprotrophs and ectomycorrhizae, with tree species were especially prominent in root fractions. The sporocarp survey found sporcarp abundance was greatest in pine stands and they tended to have more ectomycorrhizal taxa and spruce and larch stands more saprotrophic taxa. The effects of tree species on fungal taxa differed between the sporocarp surveys and soil DNA analyses: many of the fungi identified by sporocarp presence were not detected by soil DNA sequencing, whereas the latter method detected many more species in all trophic groups. Both DNA sequencing methods showed that many operational taxonomic units were preferentially associated with either spruce or pine stands. Though not definitive, preliminary examination of soil fungi using the Illumina platform showed that a natural spruce stand at the base of Gateway Hill had greater species richness than did reclaimed spruce stands. The results of this study show that communities of soil fungi have become established since the initiation of reclamation. Further work is underway to compare this reclamation site to other unmined forest sites. [ABSTRACT FROM AUTHOR]