The first sandstone unit of the Esdolomada Member of the Roda Formation (hereafter
referred to as 'Esdolomada 1') was formed by a laterally‐migrating, shelf tidal bar. This …

The Western foreland basin in Taiwan originated through the oblique collision between the
Luzon volcanic arc and the Asian passive margin. Crustal flexure adjacent to the growing …

The trace fossil Macaronichnus segregatis is an intrastratal trail occurring in shallow marine
deposits. Previous studies have shown that this trace fossil can be used as a powerful …

The lower Pliocene deposits, crop** out along the Atlantic coast of Cadiz, in the Conil–
Cabo Roche area, formed on a shelf gently deepening towards the W–NW. Up to five types …

The Arda River marine succession (Italy) is an excellent site to apply an integrated approach
to paleoenvironmental reconstructions, combining the results of sedimentology, body fossil …

The new ichnosubspecies Macaronichnus segregatis digiberti from Miocene deposits of
Cádiz, SW Spain, is described. This ichnotaxa shows the characteristic presence of a …

The distribution of trace-making organisms in coastal settings is largely controlled by
changes in physicochemical parameters, which in turn are a response to different climatic …

Bioturbation is an important factor for reservoir quality due to the modification of host rock
petrophysical properties (ie, porosity, permeability, and connectivity). However, there is no …

The Middle Eocene Man Aike Formation of southern Patagonia, Argentina, offers the
opportunity to study the palaeoecological and palaeoenvironmental significance of …

Mineralogical segregation of sand grains distinguishes the trace fossil Macaronichnus
segregatis, which is composed of a felsic burrow infill with a mafic-and mica-rich burrow …