The Turkey Lakes Watershed Study (TLWS) was initiated in 1980 to assess the effects of anthropogenic perturbation on Shield ecosystems. The goal of the study was to obtain a whole-ecosystem analysis of the biogeochemical processes that control pollutant–ecosystem interactions and thence to promote the development and validation of system models. It is a cooperative effort that includes investigators from Environment Canada (National Water Research Institute, Meteorological Service of Canada, and Canadian Wildlife Service), Natural Resources Canada (Great Lakes Forestry Centre), and Fisheries and Oceans Canada (Great Lakes Laboratory for Fisheries and Aquatic Science), as well as several universities. The initial impetus for research in the TLW arose from the desire to assess and understand the aquatic and terrestrial effects of acidic deposition. The TLW (Figure 1) is located 50 km north of Sault Ste. Marie, Ontario, on the Canadian Shield near the northern margin of the Great Lakes–St. Lawrence forest region. The basin, which is 10.5 km in area, is situated predominantly on metamorphic silicate bedrock (greenstone) overlain by thin to absent glacial tills. These geological conditions make the basin moderately sensitive to acidic deposition. The terrestrial and aquatic resources within the basin are representative of the surrounding Algoma district, although for an Ontario site, the TLW has relatively high relief (290 m) and precipitation (mean, more than 1200 mm y ). The forest is an uneven-aged, mature-toovermature, old-growth hardwood system dominated by sugar maple (Acer saccharum Marsh.) and yellow birch (Betula alleghaniensis Britton). The drainage system is composed of many intermittent and perennial first-order streams draining into and through a chain of four dimictic lakes that range in size from 5.8 to 52.0 ha and in mean depth from 2.2 to 12.2 m. There is a chemical gradient in the aquatic system such that higherelevation waters are more dilute (that is, they have lower Ca and alkalinity concentrations) than lower-elevation waters. The TLW ultimately drains into the Batchawana River and thence to Lake Superior. For greater detail on basin characteristics, see Jeffries and others (1988). From time to time, study participants have conducted workshops to present, discuss, and integrate the findings from the scientific investigation now being done in the TLW (for example, see the Canadian Journal of Fisheries and Aquatic Sciences, 1988, vol. 45, Suppl. 1, pages 1–178,). This issue of Ecosystems presents six papers from a 1999 workshop that summarize the results from either long-term monitoring of conditions in the TLW or specific research projects. According to Sirois and others (2001), mean annual wet SO4 2 deposition declined from 31 mmol m 2 during 1981–1984 to 18 mmol m 2 during 1994–97. Two of the following papers address trends or responses in precipitation or surface-water chemistry that were contemporaneous with this change in acid input. Three other papers consider some of the physical and chemical processes that regulate watershed biogeochemistry, and another describes the development and application of a predictive soil acidification model that was designed to assess whether the reduced acid Received 19 September 2000; accepted 19 September 2000. *Corresponding author; e-mail: dean.jeffries@cciw.ca Ecosystems (2001) 4: 501–502 DOI: 10.1007/s10021-001-0023-2 ECOSYSTEMS
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