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

Seilacherian Ichnofacies have been established, to date, for characterizing relatively stable
depositional settings. Environments characterized by temporally and spatially varying …

The Bohemo‐Iberian regional scale for South Gondwana, involving the 'Mediterranean
Province', comprises five regional stages (Arenigian, Oretanian, Dobrotivian, Berounian and …

Trilobites, key components of early Palaeozoic communities, are considered to have been
invariably fully marine. Through the integration of ichnological, palaeobiological, and …

The Paleozoic tectonic evolution of the northern margin of Gondwana is inferred to comprise
several episodes of continental breakup and ocean opening. However, the timing and …

The distribution of conventional subichnofacies in deep‐water fan systems (ie Ophiomorpha
rudis–Paleodictyon–Nereites‐subichnofacies) depends on the presence of fully turbulent …

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 …

Micro‐organisms producing microbially induced sedimentary structures, particularly
epibenthic cyanobacteria, are not facies‐dependent and could flourish in any environment if …

The stratigraphic architecture, changes of depositional systems in lateral and vertical extent,
and 3D-stacking pattern of second-and third-order sequences of the Cambrian successions …

Abstract Changes in stacking patterns of facies, stratal architecture and shoreline trajectory
along depositional strike are mainly dependent on along-strike differences in factors such as …