, 2005). The distribution of study catchments transects the Canadian cordillera between about 53 and 56° N latitude (Fig. 1). Study catchments on Vancouver Island represent the Insular Mountains, but at a more southerly latitude of about 49° N. The distribution of catchments is heterogeneous between physiographic RO4929097 molecular weight regions, a consequence of accessibility limitations, geographic focuses of the individual studies, and, to a lesser extent, the geographic occurrences of lakes. The interior Skeena Mountains and the northwest portion of the Interior Plateau are overrepresented. The Coast Mountains are sparsely represented and the Insular Mountain lakes

are highly concentrated in a small coastal region of Vancouver Island. The Rocky Mountains are not represented in the dataset beyond a few study

catchments in the foothills region. Study catchments on Vancouver Island and in the central to eastern Interior Plateau are from the Spicer (1999) dataset. The Vancouver Island is the most seismically active region of this study, although no major earthquakes have occurred during the latter half of 20th century, which GSI-IX ic50 is our primary period of interest for assessing controls of sedimentation. The northwestern study catchments, representing the Coast Mountains, Skeena Mountains, and the northwest interior are from the Schiefer et al. (2001a) dataset. The Coast Mountain catchments have the steepest and most thinly mantled slopes. The eastern most study catchments, representing the Foothills-Alberta Plateau are from the Schiefer and Immell (2012) dataset. These eastern lake catchments have experienced considerable land use disturbance associated with oil and filipin gas exploration and extraction, in addition to forestry activities, whereas all other catchment regions have primarily experienced only forestry-related

land use impacts. Many of the study catchments outside Vancouver Island and the Coast Mountains have probably experienced fires during the last half century, but we do not assess fire-related impacts in this study. More detailed background information on the individual catchments and various study regions is provided by Spicer (1999), Schiefer et al. (2001a), and Schiefer and Immell (2012). Study lakes ranged in size from 0.06 to 13.5 km2 (mean = 1.51 km2) and contributing catchment areas ranged in size from 0.50 to 273 km2 (mean = 28.5 km2). Methods used for lake selection, sediment sampling and dating, and GIS processing of catchment topography and land use history, were highly consistent between the Spicer (1999), Schiefer et al. (2001a), and Schiefer and Immell (2012) studies.