Abstract Sediment Routing Systems (SRS) and Sediment Generation (SG) are two branches
of sedimentary geology which are complementary, although their full integration remains …

Sediment archives in the terrestrial and marine realm are regularly analyzed to infer
changes in climate, tectonic, or anthropogenic boundary conditions of the past. However …

The Paleocene-Eocene Thermal Maximum (PETM;~ 55.9 Ma) was a geologically rapid
warming period associated with carbon release, which caused a marked increase in the …

Synrift stratigraphy and the distribution of breakup‐related erosional unconformities vary
vastly between passive margins and cannot be explained by classical rifting models. Here …

A hallmark of the rapid and massive release of carbon during the Palaeocene–Eocene
Thermal Maximum is the global negative carbon isotope excursion. The delayed recovery of …

Mineralogical investigations on fluvial sedimentary sequences could provide historical
environmental information on the effects of human activities and natural events. This study …

Landslides are the main source of sediment in most mountain ranges. Rivers then act as
conveyor belts, evacuating landslide-derived sediment. Sediment dynamics are known to …

This paper presents the time and space evolution of crustal deformation and their respective
sedimentary infill of the 600 km wide, asymmetric conjugate rifted margin of the Santos …

Landscape evolution models can be used to assess the impact of rainfall variability on
bedrock river incision over millennial timescales. However, isolating the role of rainfall …

An intensification of the hydrological cycle is an expected consequence of global warming,
and this will likely lead to spatially variable precipitation and drought extremes, and more …