Several specimens of trace fossil Bichordites monastiriensis were discovered in two shallow water Oligocene sandstone beds from Valsugana (Trentino, NE Italy) representing the oldest documented occurrence for this ichnospecies. They are grazing−crawling (pascichnion−repichnion) structures and are occasionally associated with enlarged structures that can be interpreted as resting traces (cubichnia) and assigned to the ichnogenus Cardioichnus. The resulting Bichordites–Cardio− ichnus compound trace fossil is here described for the first time. In the basal part of some specimens, skeletal remains of Eupatagus ornatus were found in life position. This founding enables to widen the spectrum of known Bichordites trace− makers. Exceptional conditi...
The poorly known, helical spiral trace fossil Avetoichnus luisae Uchman & Rattazzi, 2011 has been in...
Invertebrate trace fossil assemblages from the Hettangian (Early Jurassic) alluvial plain deposits o...
SUMMARY- Stratinomic indications by trace fossils in Eocene to Miocene turbidites and hemipelagites ...
Several specimens of trace fossil Bichordites monastiriensis were discovered in two shallow water Ol...
The pascichnial trace fossil Bichordites kuzunensis isp. nov. occurs as an epichnial complex structu...
The analysis of Bichordites ichnofabric has been performed in laminated calcarenites of Upper Pleist...
Echinoid grazing traces present on ostreid valves constituting a shell-ground were studied. The shel...
A spatangoid-produced ichnofabric is described from the Miocene Bateig Limestone, SE Spain. This ich...
The ichnology of the Pleistocene sand sequence of Gravina is described. The trace fossils provide ev...
The Saignon ichnosite, located in the Apt syncline, yielded a high density of footprints with hundre...
The Sácaras Formation (Albian, Lower Cretaceous) of the Serra Gelada succession (Prebetic of Alican...
A new study of the ichnotaxonomy and palaeoecology of the Late Pennsylvanian San Giorgio Basin’s tra...
The trace fossil assemblages exposed at the Armorano road section in the Monte Sporno unit, Northern...
The ichnospecies Paradictyodora flabelliformis is reported for the first time from the Pliocene "Arg...
Five, 3-8 cm-thick calcarenitic turbiditic beds belonging to overbank deposits in the marginal secto...
The poorly known, helical spiral trace fossil Avetoichnus luisae Uchman & Rattazzi, 2011 has been in...
Invertebrate trace fossil assemblages from the Hettangian (Early Jurassic) alluvial plain deposits o...
SUMMARY- Stratinomic indications by trace fossils in Eocene to Miocene turbidites and hemipelagites ...
Several specimens of trace fossil Bichordites monastiriensis were discovered in two shallow water Ol...
The pascichnial trace fossil Bichordites kuzunensis isp. nov. occurs as an epichnial complex structu...
The analysis of Bichordites ichnofabric has been performed in laminated calcarenites of Upper Pleist...
Echinoid grazing traces present on ostreid valves constituting a shell-ground were studied. The shel...
A spatangoid-produced ichnofabric is described from the Miocene Bateig Limestone, SE Spain. This ich...
The ichnology of the Pleistocene sand sequence of Gravina is described. The trace fossils provide ev...
The Saignon ichnosite, located in the Apt syncline, yielded a high density of footprints with hundre...
The Sácaras Formation (Albian, Lower Cretaceous) of the Serra Gelada succession (Prebetic of Alican...
A new study of the ichnotaxonomy and palaeoecology of the Late Pennsylvanian San Giorgio Basin’s tra...
The trace fossil assemblages exposed at the Armorano road section in the Monte Sporno unit, Northern...
The ichnospecies Paradictyodora flabelliformis is reported for the first time from the Pliocene "Arg...
Five, 3-8 cm-thick calcarenitic turbiditic beds belonging to overbank deposits in the marginal secto...
The poorly known, helical spiral trace fossil Avetoichnus luisae Uchman & Rattazzi, 2011 has been in...
Invertebrate trace fossil assemblages from the Hettangian (Early Jurassic) alluvial plain deposits o...
SUMMARY- Stratinomic indications by trace fossils in Eocene to Miocene turbidites and hemipelagites ...