The Coastal Range in the Mediterranean segment of the Chilean active
margin is a soil mantled landscape able to store fresh water and
potentially support a biodiverse native forest. In this landscape, human
intervention has been increasing soil erosion for ~200
yr, with the last ~45 yr experiencing intensive
management of exotic tree plantations. At the same time, this landscape
has been affected by a prolonged megadrought, and how the anthropogenic
disturbances and hydrometeorologic trends affect sediment transport is
not yet well understood.
In this study we calculate a decadal-scale catchment erosion rate from
suspended sediment loads and compare it with a
10-year-scale catchment denudation rate estimated
from detritic 10Be. We then contrast these rates against the effects of
discrete disturbances and hydroclimatic trends. Erosion/denudation rates
are similar on both time scales, i.e. 0.018 ± 0.005 mm/yr and 0.024 ±
0.004 mm/yr, respectively. Recent human-made disturbances include
logging operations during each season and a dense network of forestry
roads, which increase structural sediment connectivity. Other
disturbances include the 2010 M 8.8 Maule
earthquake, and two widespread wildfires in 2015 and 2017.
A decrease in suspended sediment load is observed during the wet seasons
for the period 1986-2018 coinciding with a decline in several
hydroclimatic parameters. The low 10-year denudation
rate agrees with a landscape dominated by slow soil creep. The low
10-year-scale erosion rate and the decrease in suspended sediments,
however, conflicts with both the observed disturbances and increased
structural (sediment) connectivity. These observations suggest that,
either suspended sediment loads and, thus, catchment erosion, are
underestimated, and/or that decennial sediment detachment and transport
were smeared by decreasing rainfall and streamflow. Our findings
indicate that human-made disturbances and hydrometeorologic trends may
result in opposite, partially offsetting effects on recent sediment
transport, but both contribute to the degradation of the landscape.