In the Hunnebergian to Kunda interval (Arenig), the conodont association recorded from Horns Udde (Oelans, Sweden) show a change from cosmopolitan to provincial. After a prominent Precordillera faunal influx in Billingenian, the Vokhov fauna is characterized by taxa typical of the Baltic Province. The change of the conodont fauna is connected with sea level changes and indicates a shallowing of the shelf environment. Sea level fluctuations, within a more general shallowing, are evidenced by changes in the conodont biofacies and supported by Sr and Ca isotope analyses for the interval under consideration
This investigation examines the distribution of conodont elements in the upper Lower Ordovician (Are...
The Katian (Upper Ordovician) facies succession of the Siljan district, central Sweden, records some...
Early Canadian (Lower Ordovician) conodonts have been recorded from loose slabs which were collected...
The Hunnebergian to Kunda conodont succession of the lower Ordovician Orthoceras Limestone on northe...
This paper presents taxonomical description of Early Ordovician conodonts recovered from the limesto...
In the Lower Ordovician platform and slope deposits of western Newfoundland and in platform deposit...
The remotely located Cambro-Ordovician strata in Ny Friesland, NE Spitsbergen, Svalbard, are referre...
The previously established graptolite and chitinozoan Hirnanian-Telychian biostratigraphy in the uni...
One of the few and most complete records of the MDICE (Middle Darriwilian Isotope Carbon Excursion) ...
The Baltoscandia region was a wide platform covered by an epicontinetal sea on the Baltic Craton dur...
The diversity data presented in this paper are based on recently revised collections of conodonts fr...
This update biostratratigraphy of the Scandinavian Oeland Series is the result of sampling on Oeland...
The Ordovician is an important period in the Phanerozoic, with remarkable faunal turnovers, several ...
A diverse conodont collection representing the Oelandodus elongatus-Acodus deltatus deltatus Subzone...
The long time interval after Pander's (1856) original conodont study can in terms of Ordovician cono...
This investigation examines the distribution of conodont elements in the upper Lower Ordovician (Are...
The Katian (Upper Ordovician) facies succession of the Siljan district, central Sweden, records some...
Early Canadian (Lower Ordovician) conodonts have been recorded from loose slabs which were collected...
The Hunnebergian to Kunda conodont succession of the lower Ordovician Orthoceras Limestone on northe...
This paper presents taxonomical description of Early Ordovician conodonts recovered from the limesto...
In the Lower Ordovician platform and slope deposits of western Newfoundland and in platform deposit...
The remotely located Cambro-Ordovician strata in Ny Friesland, NE Spitsbergen, Svalbard, are referre...
The previously established graptolite and chitinozoan Hirnanian-Telychian biostratigraphy in the uni...
One of the few and most complete records of the MDICE (Middle Darriwilian Isotope Carbon Excursion) ...
The Baltoscandia region was a wide platform covered by an epicontinetal sea on the Baltic Craton dur...
The diversity data presented in this paper are based on recently revised collections of conodonts fr...
This update biostratratigraphy of the Scandinavian Oeland Series is the result of sampling on Oeland...
The Ordovician is an important period in the Phanerozoic, with remarkable faunal turnovers, several ...
A diverse conodont collection representing the Oelandodus elongatus-Acodus deltatus deltatus Subzone...
The long time interval after Pander's (1856) original conodont study can in terms of Ordovician cono...
This investigation examines the distribution of conodont elements in the upper Lower Ordovician (Are...
The Katian (Upper Ordovician) facies succession of the Siljan district, central Sweden, records some...
Early Canadian (Lower Ordovician) conodonts have been recorded from loose slabs which were collected...