By exploring the complexities of different combinations of anthropogenic and natural land use/covers, streams could be restored and managed to provide the greatest ecosystem benefit as the natural world gives way to the Anthropocene. We thank Andrew Bradley Scott and Robert Buchkowski for field and laboratory assistance. We thank the anonymous reviewers for their comments and suggestions, which have helped improve this manuscript. Funding for this study was provided by Canada’s Natural Protein Tyrosine Kinase inhibitor Sciences and Engineering Research Council (NSERC) Discovery Grant to M.A.X. and an NSERC Undergraduate Student Research Award to E.T. In addition, C.J.W.

acknowledges support from a postdoctoral fellowship from the Ontario Ministry of Research and Innovation. “
“Elevated transfer of fine-grained sediment (silt and clay) in drainage systems can adversely impact aquatic ecosystems in downstream channels and water bodies. Effects of fine sediment include direct and indirect harm to fish, invertebrates, and aquatic plants, as well as E7080 diminished water quality for human use (Kerr, 1995 and Miller et al., 1997). Contemporary land use can elevate sediment delivery from forested catchments by increasing erosion rates on cleared slopes, initiating erosion on road surfaces, and increasing sediment transfer to watercourses by induced mass wasting (Church, 2010). The combined effect (i.e. cumulative effect; Reid (1993))

of land use activities

on watershed sediment transfer to downstream water bodies is difficult to assess because of the lack of adequate sediment gauge records, especially in remote and mountainous regions where sediment transfer is highly episodic and long-term catchment monitoring is rare. The sampling and analysis of lacustrine (lake) sediment deposits can be effective for determining anthropogenic impacts on past sediment delivery from the contributing catchment (Foster, 2010). Lakes act as a primary sink in the sediment cascade, and rates MG-132 mw of lake sediment accumulation reflect integrated upstream and upslope processes of sediment transfer, as well as internal lake processes. The lake sediment approach can avert some of the typical limitations of drainage basin studies of land use impacts on sediment transfer. Lake deposits represent a continuous record of historical sediment transfer, enabling the selection of appropriate time scales of analysis and the determination of background conditions and long-term trends. Chronological control is needed for such reconstructions, and 210Pb radiometric dating has been commonly applied for the purpose of studying sediment transfer associated with contemporary (20th century to current) land use activities, including urbanization (e.g. Ruiz-Fernández et al., 2005), agriculture (e.g. McCarty et al., 2009), grazing (e.g. Garcia-Rodriguez et al., 2002), mining (e.g.