Abstract

Bogs are nutrient poor, acidic ecosystems that receive their water and nutrients entirely from precipitation (= ombrogenous) and as a result are sensitive to nutrient loading from atmospheric sources. Bogs occur frequently on the northern Alberta landscape, estimated to cover 6% of the Athabasca Oil Sands Area. As a result of oil sand extraction and processing, emissions of nitrogen (N) and sulfur (S) to the atmosphere have led to increasing N and S deposition that have the potential to alter the structure and function of these traditionally nutrient-poor ecosystems. At present, no detailed protocol is available for monitoring potential change of these sensitive ecosystems. We propose a user-friendly protocol that will monitor potential plant and lichen responses to future environmental inputs of nutrients and provide a structured means for collecting annual data. The protocol centers on measurement of five key plant/lichen attributes, including changes in (1) plant abundances, (2) dominant shrub annual growth and primary production, (3) lichen health estimated through chlorophyll/phaeophytin concentrations, (4) Sphagnum annual growth and production, and (5) annual growth of the dominant tree species (Picea mariana). We placed five permanent plots in each of six bogs located at different distances from the center of oil sand extraction and sampled these for 2 years (2018 and 2019). We compared line intercept with point intercept plant assessments using NMDS ordination, concluding that both methods provide comparable data. These data indicated that each of our six bog sites differ in key species abundances. Structural differences were apparent for the six sites between years. These differences were mostly driven by changes in Vaccinium oxycoccos, not the dominant shrubs. We developed allometric growth equations for the dominant two shrubs (Rhododendron groenlandicum and Chamaedaphne calyculata). Equations developed for each of the six sites produced growth values that were not different from one another nor from one developed using data from all sites. Annual growth of R. groenlandicum differed between sites, but not years, whereas growth of C. calyculata differed between the 2 years with more growth in 2018 compared with 2019. In comparison, Sphagnum plant density and stem bulk density both had strong site differences, with stem mass density higher in 2019. When combined, annual production of S. fuscum was greater in 2019 at three sites and not different at three of the sites. Chlorophyll and phaeophytin concentrations from the epiphytic lichen Evernia mesomorpha also differed between sites and years. This protocol for field assessments of five key plant/lichen response variables indicated that both site and year are factors that must be accounted for in future assessments. A portion of the site variation was related to patterns of N and S deposition.

Highlights

  • Bogs are Sphagnum-dominated, acidic, nutrient poor, peat-accumulating ecosystems found in subarctic, boreal, and cool-temperate regions, mainly in the northern hemisphere (Vitt 2006)

  • Page 3 of 25 743 (Evernia mesomorpha), can we develop a suitable technique for using lichen chlorophyll/phaeophytin ratios as an indicator of lichen health? (5) Using cranked wires how variable is annual growth and net primary production (NPP) of Sphagnum? (6) Can we use leader length of Picea mariana to assess variability in growth of this species? Here we assess the outcomes of these protocols over a 2-year time period for a series of six bog sites in northeastern Alberta, Canada, and provide evidence of whether the variability in responses can be related to growing season N and S deposition from oil sands activities

  • Differences between sites are evident on the nonmetric multidimensional scaling (NMDS) ordination (Fig. 1), with individual sites clustered at different locations on the ordination (Kearl plots are positioned to the upper center, McKay to the upper-right, Anzac to the lower right, McMurray center, Horse Creek to the left center, and JPH4 to the center and lower left)

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Summary

Introduction

Bogs are Sphagnum-dominated, acidic, nutrient poor, peat-accumulating ecosystems found in subarctic, boreal, and cool-temperate regions, mainly in the northern hemisphere (Vitt 2006). All bogs in continental Canada have a canopy dominated by one tree species, Picea mariana, a shrub layer of 5–6 species of Ericaceae and dominated by either Rhododendron (Ledum) groenlandicum or Chamaedaphne calyculata, and a hummocky ground layer mostly dominated by one species of peat moss Sphagnum fuscum (Vitt et al 1995a). Fruticose lichens (especially Evernia mesomorpha and Usnea spp.) are abundant on tree branches (Vitt 2006). These speciespoor plant communities are sensitive to environmental changes and, owing to their ombrogenous water source, are especially sensitive to nutrient loading from atmospheric sources (Wieder et al 2019)

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