Primary Convener:
Eric Barefoot, University of California Riverside

Convener:
Debsmita Das, University of California Santa Barbara
Marissa Tremblay, Purdue University
Malcolm McMillan, University of Melbourne
Chenliang Wu, Tulane University
Magdalena Curry, North Carolina State University

Early Career Convener:
Luke Gezovich, Colorado School of Mines

Chair:
Chenliang Wu, Rice University
Malcolm McMillan, University of Melbourne

The history of Earth's surface is written by sediment that erodes from hillslopes and deposits in sedimentary basins. Sedimentary landscape dynamics dictate the physical structure of the stratigraphic record, and the radioisotopes preserved in the rocks reflect the transfer of mass across the Earth's surface. Stratigraphic records integrated with geochronometers and thermochronometers reveal the rate, tempo, and timing of events in the geologic past. Contributions to this session will sharpen our understanding of Earth's tectonic, climatic, and biologic history, and the erosional and depositional dynamics that shape its surface.

Index Terms
1130 Geomorphological geochronology
1140 Thermochronology
8169 Sedimentary basin processes
8175 Tectonics and landscape evolution

Cross-Listed:
T - Tectonophysics

Neighborhoods:
3. Earth Covering