Abstract

Habitat degradation associated with resource development is a major ecological concern, particularly in Canada’s boreal zone where limited information on biodiversity is available. Habitat degradation can lead to reductions in biodiversity and ecosystem function, especially when drivers of variability and diversity patterns have not been identified for a region of interest. In this study, the distribution of diatom genera in the Peace–Athabasca Delta in northeastern Alberta was examined in relation to seasonal, geographic, and alkalinity gradients. Grab samples of six abiotic variables (total dissolved nitrogen, total dissolved phosphorus, dissolved iron, turbidity, pH, and specific conductance (SPC)) were taken from 12 remote wetlands over three sampling periods, and regressed against an ordination of diatom community composition to identify key environmental drivers of diatom community variation. Indirect gradient analysis identified two major gradients among sites. First, separation of sites among sampling periods showed successional seasonal changes in diatom community composition. Second, separation of sites from the Peace sub-delta and Birch sub-delta showed a gradient of geographic separation. Direct gradient analysis failed to explain the underlying drivers of these two gradients, but did show that alkalinity is a key driver of diatom community composition in the Embarras sub-delta, and that these sites could be particularly vulnerable to community changes associated with acidification.

Highlights

  • Resource development can have a significant impact on the surrounding landscape

  • Dry hydrological conditions could be associated with shifts in water quality and corresponding changes in the diatom community composition

  • Habitats in the Peace–Athabasca Delta (PAD) are sensitive to water level fluctuations in the lower Athabasca River (Wolfe et al, 2008; Timoney, 2009; Monk, Peters & Baird, 2012) and flooding is important in a wetland complex like the PAD as this generally contributes to the replenishment of nutrients and sediments from the river channel to the associated perched basin wetlands

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Summary

Introduction

In Canada’s oil sands region, emissions of oxidized sulfur and nitrogen associated with mining activity have the potential to acidify surrounding boreal lake ecosystems (Hazewinkel et al, 2008) when these compounds are returned to the landscape in the form of acid precipitation (Beamish, 1976; Galloway et al, 1978; Cowling & Linthurst, 1981). Higher run-off increases the sediment and nutrient load of receiving waters leading to an increased potential for high turbidity associated with high levels of total suspended solids and eutrophication. Along with impacts from resource development, changes in receiving waters are intensified by warmer and drier conditions associated with climate change in Canada’s north that reduce water levels through higher rates of evaporation (Rouse et al, 1997)

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