『Abstract
River-borne quartz carries a cosmogenic nuclide memory that is
a function of the catchment-wide erosion rate. This record may
be preserved in fluvial deposits such as river terraces. If the
age of a terrace is independently known and transport time in
the river system is relatively short, then the upstream erosion
rate at the time of terrace deposition can be determined. We have
used cosmogenic nuclides to date river terraces in the lower Meuse
catchment, the Netherlands, and to obtain a 1.3 Ma record of paleoerosion
rates in a 104-km2 drainage basin comprising
the Ardennes Mountains. Paleoerosion rates were uniform within
the range of 25-35 mm/ka from 1.3 to 0.7 Ma. After 0.7 Ma, both
climatic and tectonic boundary conditions changed. The amplitude
and duration of climate cycles increased significantly, resulting
in long periods of sustained low temperatures in the Meuse catchment.
In addition, an episode of magmatic underplating and mafic volcanism
in the nearby Eifel caused up to 250 m of surface uplift in the
Meuse catchment. The main streams in the region have responded
to the perturbation at 0.7 Ma within a few 105 yr.
Our data indicate that the catchment-wide response time is much
longer. Further investigations are required to attribute the observed
increase in paleoerosion rates to one or the other mechanism discussed.』
Introduction
Meuse catchment
Terraces in the West Meuse Valley
Methodology
Terrace dating
Paleoerosion rate determination
Sample processing
Terrace ages
Results
Discussion
Paleoerosion rates
Results
Discussion
Conclusion
Acknowledgments
References cited