Gordon J. Kayahara

Longitudinal patterns of plant diversity in the North American boreal forest

Spatial patterns of plant diversity in the North American boreal forest were examined according to three plant life forms (woody plants, herbaceous plants, and bryophytes) and two taxonomic levels (species and genus), using sixty 9-ha plots sampled in white spruce (Picea glauca (Moench) Voss) and black spruce (Picea mariana (P. Mill.) B.S.P.) ecosystems along a transcontinental transect from the Pacific coast eastwards to the Atlantic coast. The patterns of inventory diversity (represented by alpha diversity), differentiation diversity (represented by the similarity index, habitat-heterogeneity index, similarity decay rate, and length of the first axis in detrended correspondence analysis), and pattern diversity (represented by the mosaic diversity index) were assessed along the transect in both ecosystem types. At the stand level, central North America had the highest alpha diversity in terms of the number of species or genera, and western North America had a higher alpha diversity than eastern North America. At the continental scale, herbaceous plants had the highest beta diversity in terms of floristic change from the eastern to western North America, bryophytes had the lowest beta diversity, and woody plants were in the middle, regardless of ecosystem type and taxonomic level. Central North America had the lowest mosaic diversity across the boreal transect of North America. The white spruce ecosystems had a higher alpha diversity than the black spruce ecosystems regardless of plant life form, taxonomic level and geographic location. The white spruce ecosystems tended to have more bryophytes, less woody plants, and higher species:genus ratio than the black spruce ecosystems. In general, the white spruce and black spruce ecosystems shared the same patterns in diversity changes at different spatial scales, plant life forms, and taxonomic levels across the transect studied. The existing patterns of plant diversity in the North American boreal forest area resulted from a combination of ecological processes and spatial configuration.

Understorey vegetation in boreal Picea mariana and Populus tremuloides stands in British Columbia

Abstract We compared the species composition and species density of vascular plants in the understorey vegetation of boreal forest between Picea mariana (Black spruce) and Populus tremuloides (Trembling aspen) stands in British Columbia, Canada, and related differences in species composition and species density between the two forest types to dominant canopy tree species as well as a wide variety of environmental factors. We analysed 231 stands, distributed in three different climatic regions representing drier, wetter, and milder variations of montane boreal climate. Of these stands 118 were dominated by P. mariana and 113 by P. tremuloides. P. tremuloides stands had higher species density than P. mariana stands in all climatic regions, but species density of each dominance type varied among climatic regions. The floristic composition of the understorey vegetation was markedly different for P. mariana and P. tremuloides dominated stands. A detailed study on the effect of canopy dominance and local environmental factors on the understorey vegetation of the boreal forest was conducted using 88 stands from one of the three climatic regions. Using a combination of ordination and variation partitioning by constrained ordination we demonstrated a small but unique effect of canopy dominance type on the understorey vegetation, while a larger amount of compositional variation was shared with other factors. Our results accord with a scenario in which differences in primary environmental factors and humus form properties, the latter accentuated by the canopy dominants themselves, are the most important causes of higher species density in P. tremuloides stands than in P. mariana stands, as well as differences in species composition among the two canopy dominance types. Processes and time scales involved in the small but significant direct and indirect effects of the canopy dominant on understorey species composition are discussed. Nomenclature: Qian & Klinka (1998). Abbreviations: DMB = Drier montane boreal; MMB = Mild montane boreal; WMB = Wetter montane boreal.

Testing site index-site-factor relationships for predicting Pinus contorta and Picea engelmannii × P. glauca productivity in central British Columbia, Canada

Measures of forest productivity for various site conditions are necessary for forest management planning, where timber production is the objective. This study was undertaken to test whether autecological productivity relationships developed for lodgepole pine (Pinus contorta) and interior spruce (Picea engelmannii×P. glauca) using the biogeoclimatic ecosystem classification system of British Columbia are useful as practical field-based procedures to predict site index. Independent data sets consisting of 111 plots for pine and 114 plots for spruce were collected for use in testing the bias and precision of the models. A regression on residuals (predicted minus test values) indicated that the lodgepole pine model was unbiased in estimating site index (p=0.08). However, there was a lack of precision, with a square root of the mean squared prediction error (root-MSPR) of 2.8 m. Only 56% of the test plots had differences from the predicted values of 2.0 m or less. Residual analysis showed that the interior spruce model was biased in estimating site index (p<0.01), generally predicting greater site index than the test values. The model also lacked precision, with a root-MSPR of 3.2 m. Only 44% of the test plots had differences from the predicted values of 2.0 m or less. Forest managers requiring a site-index prediction tool need to decide whether the degree of accuracy precision provided by these models is acceptable.

Site index of western hemlock (Tsuga heterophylla) in relation to soil nutrient and foliar chemical measures

Abstract To investigate the productivity of western hemlock, relationships between site index and forest floor, mineral soil, and foliar nutrient measures were examined in 101 immature western hemlock stands located in southern coastal British Columbia. Measures of both soil and foliar nitrogen were consistently identified as explanatory variables. In addition, measures of forest-floor-extractable K, mineral soil pH, C:N ratio, extractable K and foliar S, Mg, Cu, Zn, and N:P ratio were found to be important. Except for K, the response of site index to the different variables was consistently one of a rapid initial increase followed by a leveling off, and accompanied by high variation. Western hemlock would not appear to increase in site index with increasing nutrients once past a point of sufficiency associated with sites considered nutrient-poor by conventional forest soil criteria in southern coastal British Columbia. Although the site index of western hemlock in the area studied here was as high as 40 m at 50 years breast height age, and assuming that site index reflects productivity, the highest productivity was not consistently correlated to a site of high nutrient availability as measured by the chemical tests used in this study.

Comparison of soil acidification and intensity of podzolization beneath decaying wood versus non-woody forest floors in coastal BC

Forest managers concerned with maintaining soil productivity must consider the impacts of forestry practices upon the features of a site. One critical feature is the amount and type of organic matter on a site, which may affect soil development. This study addresses the question of whether CWD accumulations increase the intensity of podzolization, thus reducing the long-term productivity of a site.

Vegetation and soil nutrient properties of Black spruce and Trembling aspen ecosystems in the boreal black and white spruce zone

Changes in forest ecosystem vegetation also bring about changes to the associated soil. In order to maintain forest productivity, it is important to know the effects of tree species upon the soil, especially the influence of deciduous versus coniferous tree species. Many deciduous species increase pH, nitrogen, base saturation and/or accumulation of organic matter in the forest floor. The chemical properties of the forest floor may, in turn, influence the chemical properties of the underlying mineral soil. If a tree species significantly alters the soil, then silviculturists may consider crop rotation between deciduous and coniferous trees or growing mixed-species stands to maintain greater nutrient availability and maintain site productivity.

Relationship of site index to estimates of soil moisture and nutrients for western redcedar in south coastal British Columbia

Where timber production is the primary management objective, knowledge of the relationship between the potential productivity of candidate tree species and levels of light, heat, nutrient, moisture and aeration is necessary for speciesand site-specific decision making. For example, foresters need to decide which tree species to regenerate on a particular harvested area to obtain maximum sustainable productivity. Similarily, when considering the application of silvicultural treatments such as spacing or fertilizing, foresters need to determine whether the potential productivity of a particular site warrants the cost of the treatment.