Gastropod response to a marked carbon isotopic geochemical anomaly across the Early–Middle Frasnian transition (Palmatolepis transitans–Palmatolepis punctata conodont zones) has been analysed along the southern Laurussian shelf, mainly within the Dyminy Reef in the Holy Cross Mountains. Gastropods are represented by three reefal associations (Kowalatrochus sanctacrucensis, Euryzone kielcensis, and Grabinopsis guerichi associations), and an impoverished open−shelf Straparollus laevis assemblage. The most severe diversity crisis is connected to the disappearance of local low−energy muddy habitats, as a result of a transgressive pulse (Middlesex Event) and benthic habitat changes tied to strongly fluctuating carbon cycling; this has been obser...
Early to Middle Frasnian (E–MF) epicontinental sequences are investigated in five representative loc...
Late Frasnian Atrypida (Brachiopoda) from the Holy Cross Mountains, Poland, include 15 taxa and were...
The Late Devonian mass extinction event near the Frasnian/Famennian (F/F) boundary has been analysed...
Gastropod response to a marked carbon isotopic geochemical anomaly across the Early–Middle Frasnian ...
Frasnian gastropods from the Kowala Formation (north-western part of the Holy Cross Mountains, Polan...
The lower Frasnian (transitans Zone with Ancyrodella priamosica = MN 4 Zone) rhythmic basin successi...
The unique goniatite−rich pyritic level, 1.6 m thick, exposed at Kostomłoty (Holy Cross Mountains, c...
The lower Frasnian (transitans Zone with Ancyrodella priamosica = MN 4 Zone) rhythmic basin successi...
inaudita, and H. rhinophyuosa are common in late Frasnian to early Famennian rhythmic, calcareous−ma...
The unique goniatite−rich pyritic level, 1.6 m thick, exposed at Kostomłoty (Holy Cross Mountains, c...
The new trench Z−17 situated in the Dębnik anticline (Cracow Region, southern Poland) exposed strata...
The brachiopod faunas from deposits recording the Early–Middle Frasnian transition of Poland are poo...
Late Frasnian Atrypida (Brachiopoda) from the Holy Cross Mountains, Poland, include 15 taxa and were...
Amongst several known Paleozoic gastropod species having transverse septa in the apical parts of she...
Well exposed Early–Middle Frasnian (E–MF, Palmatolepis transitans to Palmatolepis punctata zonal int...
Early to Middle Frasnian (E–MF) epicontinental sequences are investigated in five representative loc...
Late Frasnian Atrypida (Brachiopoda) from the Holy Cross Mountains, Poland, include 15 taxa and were...
The Late Devonian mass extinction event near the Frasnian/Famennian (F/F) boundary has been analysed...
Gastropod response to a marked carbon isotopic geochemical anomaly across the Early–Middle Frasnian ...
Frasnian gastropods from the Kowala Formation (north-western part of the Holy Cross Mountains, Polan...
The lower Frasnian (transitans Zone with Ancyrodella priamosica = MN 4 Zone) rhythmic basin successi...
The unique goniatite−rich pyritic level, 1.6 m thick, exposed at Kostomłoty (Holy Cross Mountains, c...
The lower Frasnian (transitans Zone with Ancyrodella priamosica = MN 4 Zone) rhythmic basin successi...
inaudita, and H. rhinophyuosa are common in late Frasnian to early Famennian rhythmic, calcareous−ma...
The unique goniatite−rich pyritic level, 1.6 m thick, exposed at Kostomłoty (Holy Cross Mountains, c...
The new trench Z−17 situated in the Dębnik anticline (Cracow Region, southern Poland) exposed strata...
The brachiopod faunas from deposits recording the Early–Middle Frasnian transition of Poland are poo...
Late Frasnian Atrypida (Brachiopoda) from the Holy Cross Mountains, Poland, include 15 taxa and were...
Amongst several known Paleozoic gastropod species having transverse septa in the apical parts of she...
Well exposed Early–Middle Frasnian (E–MF, Palmatolepis transitans to Palmatolepis punctata zonal int...
Early to Middle Frasnian (E–MF) epicontinental sequences are investigated in five representative loc...
Late Frasnian Atrypida (Brachiopoda) from the Holy Cross Mountains, Poland, include 15 taxa and were...
The Late Devonian mass extinction event near the Frasnian/Famennian (F/F) boundary has been analysed...