Introduction

High arctic environments have received increased attention over recent years, as polar regions are considered to be especially sensitive to the effects of global climatic and other environmental changes (Walsh, 1991; Rouse et al., 1997). For example, potential warming from ‘greenhouse gases’ is expected to be accentuated in the High Arctic (Roots, 1989). Other environmental changes, such as increased ultraviolet (UV-B) light penetration and deposition of airborne contaminants, have also been noted recently in high latitude regions (e.g., Landers, 1995).

There is considerable potential for using living and fossil diatom assem blages for tracking environmental trends in high arctic regions (Smol & Douglas, 1996). However, to date, relatively few studies have been completed on the taxonomy, ecology, and paleoecology of high arctic, freshwater diatoms, even though lakes and ponds are dominant features of most arctic landscapes. For example, about 18% (by area) of Canada's surface waters are situated north of 60° N (Statistics Canada, 1987), and Sheath (1986) estimates that tundra ponds cover approximately 2% of the Earth's surface. The heightened interest in high arctic environments, coupled with increased accessibility (e.g., with helicopter support) of these remote regions, has resulted in a recent surge of interest in arctic diatom research. Moreover, proxy techniques such as palynology and dendroecology have some serious limitations in high arctic regions due to the paucity of higher plants (Gajewski et al., 1995). Consequently, paleolimnological approaches using diatoms may become especially important for studies of global environmental change.