The mixed siliciclastic–carbonate Teniet El Klakh Formation (Middle Jurassic, Bajocian)
mainly consists of a monotonous, clay and fine-grained sandstone alternation with some …

The classic trace fossil Ophiomorpha ranks among the most common biogenic sedimentary
structures on earth and has been widely reported from Mesozoic and Cenozoic strata …

Abstract The Kachchh Rift Basin of western India is known for several geological findings
and revelations for more than a century. Earth scientists from India and the globe have …

This study integrates ichnological and sedimentological data to interpret depositional
environments of the carbonate sediments of the Tirgan Formation (Lower Cretaceous) in the …

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 …

The Zoophycos ichnofacies and its main components, Zoophycos isp., Phycosiphon
incertum and Chondrites isp. have been related to marine environments of low energy and …

Abstract The Furada Formation of Asturias, Spain, represents a clastic shallow-marine unit
deposited during the middle Silurian to the Early Devonian. This formation contains …

Early Cretaceous succession of the Oued Fodda Formation in the Ouarsenis Mountains
(northwestern Algeria) is mainly composed of marl–limestone alternations, which are …

The mixed siliciclastic-carbonate Teferguenite Formation (Pragian-Emsian) occurring in the
Ougarta Range (SW Algeria) is subdivided into two members: the Lower Member consists of …

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