Trace fossils in storm-generated beds of shelf siliciclastic settings have been investigated
mostly to understand the effect of waves in the infauna distribution. It is possible to identify a …

Coastal mud belts, which lie parallel to the coast just seaward of the shoreface, are one of
the most important settings where shallow‐marine muddy deposits accumulate. However …

Skolithos piperock is prevalent in Cambrian shallow marine deposits but diminishes
throughout the Paleozoic. This study reports an interval with Skolithos piperock from the …

Fine-grained rocks have historically been interpreted as a product of the settling of fine
fractions in low-energy environments. However, recent studies have suggested that in these …

The study of sedimentary organic matter (SOM) is essential for understanding
paleoenvironmental conditions and depositional settings of geological formations. This …

Omission surfaces represent a gap in the sedimentary record on a particular environment,
constituting an important tool for basin analyses. Nevertheless, not always these surfaces …

Recent work has focused on erecting new Seilacherian ichnofacies for depositional
environments subject to recurring temporal and spatial variations in physico-chemical stress …

Trace fossils are not generally utilized as biostratigraphic indicators due to their long
stratigraphic ranges. Despite the use of intricate behavioral traces in the absence of other …

Lingulids are significant infaunal elements of Lower to Middle Devonian in the Paraná
Basin, Brazil, with Lingulichnus traces sometimes found in association with in situ lingulids …

The ichnology between marine and non-marine environments is a key field of work
concerning the understanding of the variation of environmental parameters in inland-to …