The trace fossil Yakutatia emersoni is recorded and described from the Late Ordovician-Early Silurian Matapedia and Grog Brook groups of northwest New Brunswick and southwest Casp6. The recording has three important consequences. First, it represents the first report of the trace fossil outside its type locality on Kodiak Island, Alaska. Second, it extends the stratigraphic range of the ichnospecies, previously known only from the Cretaceous, back to the Late Ordovician, probably Gamachian. Third, it confirms the preferred environment in which the producing organism inhabited as deep water marine. RÉSUMÉ On rapporte et décrit la trace fossile Yakutatia emersoni dans les groupes de Matapedia et de Grog de l’Ordovicien t...
Offshore marine deposits of hemipelagic dark-gray shales comprising the Middle Devonian Mahantango F...
Several new localities of the trace fossil, Diplichitos, have been found in the Permo-Carboniferous ...
ABSTRACT. The Eureka Sound FormatioG a thick sedimentary unit in the Cana-dian Arctic having a late ...
Late Ordovlcian-Early Silurian flysch slope deposits of the Matapedia Group of the Matapedia Basin o...
The trace fossil Neonereites multiserialis Pickerill and Harland is recorded and described from the ...
The ichnogenus Paleodictyon is documented from the Carboniferous (Mississippian - late Toumaisean) n...
The Siegas Formation (Silurian - early Liandovery) of northwestern New Brunswick represents. In part...
The ichnogenus Oikobesalon is here described from the Ordovician of Baltica for the first time. All ...
The first indication of organic activity in Lower Paleozoic siliciclastic turbidites of the Miramich...
none4siPaleontological survey in the remote Yukon-Charley Rivers National Preserve in Alaska led to ...
The discovery of a Zoophycos-group trace fossil questionably attributed to Echinospira is reported f...
none4siA paleontological reconnaissance survey on Cretaceous and Tertiary terrestrial units along th...
The Tonganoxie Sandstone Member (Stranger Formation) records part of the infill of an estuarine vall...
During the growth of the Rocky Mountains in the Cretaceous, there was a major sea level rise event t...
The Saint-Nicolas Formation (Sillery Group) of the Chaudière nappe in southern Québec is a...
Offshore marine deposits of hemipelagic dark-gray shales comprising the Middle Devonian Mahantango F...
Several new localities of the trace fossil, Diplichitos, have been found in the Permo-Carboniferous ...
ABSTRACT. The Eureka Sound FormatioG a thick sedimentary unit in the Cana-dian Arctic having a late ...
Late Ordovlcian-Early Silurian flysch slope deposits of the Matapedia Group of the Matapedia Basin o...
The trace fossil Neonereites multiserialis Pickerill and Harland is recorded and described from the ...
The ichnogenus Paleodictyon is documented from the Carboniferous (Mississippian - late Toumaisean) n...
The Siegas Formation (Silurian - early Liandovery) of northwestern New Brunswick represents. In part...
The ichnogenus Oikobesalon is here described from the Ordovician of Baltica for the first time. All ...
The first indication of organic activity in Lower Paleozoic siliciclastic turbidites of the Miramich...
none4siPaleontological survey in the remote Yukon-Charley Rivers National Preserve in Alaska led to ...
The discovery of a Zoophycos-group trace fossil questionably attributed to Echinospira is reported f...
none4siA paleontological reconnaissance survey on Cretaceous and Tertiary terrestrial units along th...
The Tonganoxie Sandstone Member (Stranger Formation) records part of the infill of an estuarine vall...
During the growth of the Rocky Mountains in the Cretaceous, there was a major sea level rise event t...
The Saint-Nicolas Formation (Sillery Group) of the Chaudière nappe in southern Québec is a...
Offshore marine deposits of hemipelagic dark-gray shales comprising the Middle Devonian Mahantango F...
Several new localities of the trace fossil, Diplichitos, have been found in the Permo-Carboniferous ...
ABSTRACT. The Eureka Sound FormatioG a thick sedimentary unit in the Cana-dian Arctic having a late ...