Eighteen ichnospecies (trvo new) referred to 17 ichnogenera (one new) as well as formally unclassified equilibńchnia, fugichnia and faecal pellets constifute a diverse and well-preserved invertebrate trace fossil suite present in storm deposits within the Fran-ciszka X marine horizon of the lŁuśov Beds (Late Carboniferous Namurian A, Pen-dleian) as exposed in the Kozłowa Góra quarry, Upper Silesia, Poland. The new forms are Fimbrirubichnus biseriąlis igen. et isp. n., which is interpreted as the work of a deposirfeeding bellerophont gastropod, and Cylindńchnus candel,abrus isp. n. An emended diagnosis of the ichnospecies Parahaentzschelinia ardelia is given. Presence of the trace fossils marks a marine influence, so that they can be utilize...
The study and application of ichnology, or trace fossils, have evolved substantially since trace fos...
Upper Cretaceous fine-grained rocks (the “Plänermergel”) from the Stołowe Mountains are in general s...
Quartz arenites and wackes with intercalations of silty shales of the Ociesęki Formation were analys...
Eighteen ichnospecies (two new) referred to 17 ichnogenera (one new) as well as formally unclassifie...
Abundant and moderately diverse trace fossil assemblage have been discovered for the first time in m...
In the sandstones and conglomerates of the Idzików Conglomerate Member (Coniacian), exposed in the I...
The following trace fossils have been recognised in the Lower Muschelkalk of Raciborowice Gorne (Nor...
The discovery of a Zoophycos-group trace fossil questionably attributed to Echinospira is reported f...
Invertebrate trace fossil assemblages from the Hettangian (Early Jurassic) alluvial plain deposits o...
The late Carboniferous–early Permian was a period of major environmental change, with the rainforest...
The ichnogenus Paleodictyon is documented from the Carboniferous (Mississippian - late Toumaisean) n...
The Coniacian quartz sandstones (Żerkowice Member, Rakowice Wielkie Formation) that crop out at quar...
The discovery of a Zoophycos-group trace fossil questionably attributed to Echinospira is reported f...
The Middle Turonian sediments of the Nysa Kłodzka Graben (Bystrzyca Sandstone in the Stara Bystrzyca...
Warstwy lgockie i godulskie są głównymi jednostkami litostratygraficznymi jednostki śląskiej na półn...
The study and application of ichnology, or trace fossils, have evolved substantially since trace fos...
Upper Cretaceous fine-grained rocks (the “Plänermergel”) from the Stołowe Mountains are in general s...
Quartz arenites and wackes with intercalations of silty shales of the Ociesęki Formation were analys...
Eighteen ichnospecies (two new) referred to 17 ichnogenera (one new) as well as formally unclassifie...
Abundant and moderately diverse trace fossil assemblage have been discovered for the first time in m...
In the sandstones and conglomerates of the Idzików Conglomerate Member (Coniacian), exposed in the I...
The following trace fossils have been recognised in the Lower Muschelkalk of Raciborowice Gorne (Nor...
The discovery of a Zoophycos-group trace fossil questionably attributed to Echinospira is reported f...
Invertebrate trace fossil assemblages from the Hettangian (Early Jurassic) alluvial plain deposits o...
The late Carboniferous–early Permian was a period of major environmental change, with the rainforest...
The ichnogenus Paleodictyon is documented from the Carboniferous (Mississippian - late Toumaisean) n...
The Coniacian quartz sandstones (Żerkowice Member, Rakowice Wielkie Formation) that crop out at quar...
The discovery of a Zoophycos-group trace fossil questionably attributed to Echinospira is reported f...
The Middle Turonian sediments of the Nysa Kłodzka Graben (Bystrzyca Sandstone in the Stara Bystrzyca...
Warstwy lgockie i godulskie są głównymi jednostkami litostratygraficznymi jednostki śląskiej na półn...
The study and application of ichnology, or trace fossils, have evolved substantially since trace fos...
Upper Cretaceous fine-grained rocks (the “Plänermergel”) from the Stołowe Mountains are in general s...
Quartz arenites and wackes with intercalations of silty shales of the Ociesęki Formation were analys...