Quantitative constraints on flood variability in the rock record.

ABSTRACT: Floods determine river behaviour in time and space. Yet quantitative measures of discharge variability from geological stratigraphy are sparse, even though they are critical to understand landscape sensitivity to past and future environmental change. Here we show how storm-driven river floods in the geologic past can be quantified, using Carboniferous stratigraphy as an exemplar. The geometries of dune cross-sets demonstrate that discharge-driven disequilibrium dynamics dominated fluvial deposition in the Pennant Formation of South Wales. Based on bedform preservation theory, we quantify dune turnover timescales and hence the magnitude and duration of flow variability, showing that rivers were perennial but prone to flashy floods lasting 4-16 h. This disequilibrium bedform preservation is

SUBMITTER: McLeod JS 

PROVIDER: S-EPMC10250471 | biostudies-literature | 2023 Jun

REPOSITORIES: biostudies-literature