Abstract Eight stratigraphic transects, 40–140 km long reveal, for the first time on a regional
scale, a comprehensive picture of facies architecture of the highly preserved Late …

The Upper Maastrichtian fluvial Hell Creek Formation of the Fort Peck Lake area, Montana
(and regional equivalents) is notable for its vertebrate fossils and for the K-Pg mass …

Integrated sedimentological and micropaleontological data were used for the construction of
a 93 km-long stratigraphic cross-section parallel to the modern Adriatic shoreline (northern …

The complex and non‐linear fluvial river dynamics are characterized by repeated periods of
fluvial erosion and re‐deposition in different parts of the floodplain. Understanding the fluvial …

The principles of stratigraphic paleobiology can be readily applied to the nonmarine fossil
record. Consistent spatial and temporal patterns of accommodation and sedimentation in …

Epicontinental basins are extremely prone to major paleogeographic changes, and this will
directly affect any organic matter (OM) preserved in the depositional record. In this study the …

Abstract The Danube Basin, located in the junction of the Eastern Alps and Western
Carpathians, comprises up to 600 m thick alluvial succession, which was previously …

The relationship between fluvial systems and base-level changes, controlled mainly by sea-
level fluctuations and tectonic activity, on time scales of 103–104 years, is important for …

Paleosols are recurrent features in alluvial successions and provide information about past
sedimentary dynamics and climate change. Through sedimentological analysis on six …

Integrated stratigraphic‐compositional studies on alluvial successions provide a valuable
tool to investigate the provenance of detritus in multi‐source systems. The Po Plain is an …