Results 91 to 100 of about 454 (176)
Synapsid tracks with skin impressions illuminate the terrestrial tetrapod diversity in the earliest Permian of equatorial Pangea. [PDF]
Calábková G +3 more
europepmc +1 more source
The early diversification of ray-finned fishes (Actinopterygii): hypotheses, challenges and future prospects. [PDF]
Henderson S +3 more
europepmc +1 more source
© 2020 IOP Publishing Ltd. All rights reserved. Volcanic ash from the Usolka section, which is proposed as an international standard for global correlation of the lower boundaries of the Kasimovian and Gzhelian Stages, is considered.
Sungatullin R.K. +3 more
core
Structural and palaeontological (mainly fusulinids) studies of the area between Gamonedo and Cabrales have shown the existence of more than nine tectonically superposed units showing differences in the uncohformable syn-orogenic successions deposited in ...
Martínez García, E., Villa, E.
core
Late Pennsylvanian carbonate platform facies and coral reef: new insights from southern China (Guizhou Province). [PDF]
Maillet M +8 more
europepmc +1 more source
Conodonts, radiolarians, foraminiferids, and corals provide constraints on the geology and tectonics of the Nechako region. They also support the notion that the Cache Creek Terrane is allochthonous with respect to the North American craton.
H Sano +23 more
core +1 more source
Mechanistic neutral models show that sampling biases drive the apparent explosion of early tetrapod diversity. [PDF]
Dunne EM +4 more
europepmc +1 more source
The systematics and biostratigraphy of the upper Moscovian-upper Gzhelian fusulinid fauna of the Anatolian Platform have been investigated in three stratigraphic sections (Ozbek Tepe, Eskibey and Bademli) from the Eastern and Central Taurides. Forty fusulinid taxa belonging to sixteen genera and three subgenera are identified from the upper Moscovian ...
openaire +1 more source
A new palynozone for the upper Serpukhovian–Bashkirian (uppermost Mississippian–lower Pennsylvanian) strata of the Chacoparaná Basin (Argentina) is formally proposed based on palynological assemblages from the Santiago Temple YCF.CO1, YCF.CO2 and YCF.CO3
Balarino, María Lucía +1 more
core +1 more source

