Palaeolimnological assessment of trace element inputs to lakes in the Athabasca Oil Sands Region, Alberta, Canada

• Main Authors: Rose, N, Turner, SD, Yang, H
• Format: Report
• Language: English
• Published: UCL Environmental Change Research Centre 2012
• Subjects: Fort McMurray; Canada; The Ramp; Caribou Mountains; Parallel Lake
• Online Access: https://discovery.ucl.ac.uk/id/eprint/10113840/1/ecrc_report_149_Rose_2012_Alberta.pdf; https://discovery.ucl.ac.uk/id/eprint/10113840/

Undisturbed lake sediment records provide a robust natural archive of conditions within waterbodies. They have been used successfully over a number of decades to determine temporal trends of surface water acidification and to follow the effects of eutrophication. However, lake sediments also provide an archive of changes occurring within lake catchments and of atmospheric pollutants deposited onto lake and catchment surfaces. In August 2006, parallel lake sediment cores were collected from 22 lakes in the Athabasca Oil Sands Region of Alberta by UCL staff as part of the RAMP regional lakes survey. Twelve of these lakes were selected for study covering a range of locations from around the Fort McMurray area to sites in the Caribou Mountains and the Canadian Shield. The main aim of this initial study was to assess the evidence for lake acidification in the region, but analysis also revealed changes in nutrient input and, at one site, mercury (Hg) analysis showed an indication of industrial contamination. This work was reported in Curtis et al. (2010). The analysis undertaken in this initial project was focussed on single radiometrically dated sediment cores (hereafter the ‘A’ cores) from each of the 12 selected lakes. The parallel cores from each lake (the ‘B’ cores) were stored dark, at 4ºC, following their transfer to UCL and hence were available for further analysis. Both sediment cores (A and B) from the remaining 10 lakes remain unstudied. The aim of this current project was to use the stored ‘B’ sediment cores to assess temporal trends and rates of change in trace element input to a subset of the lakes cored in the Athabasca Oil Sands Region of Alberta and compare these with the sediment records of two reference lakes in the Caribou Mountains. This interim report contains details of progress on this work up to end March 2012 and a summary of remaining work under this contract. As a consequence this report focusses on data collected so far. Only limited interpretation is provided and will be undertaken fully ...