Results 211 to 220 of about 46,523 (255)
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Middle Triassic vertebrates of India

Journal of African Earth Sciences, 1999
Abstract Until recently, the Yerrapalli Formation of the Pranhita-Godavari Valley, Deccan, India, was considered as the only Middle Triassic vertebrate-bearing horizon of India. A new faunal assemblage comprising dipnoans, capitosaurids, brachyopids, treamatosaurids, dicynodonts, rhynchosaurs and archosaurs has recently been recovered from the Denwa ...
Saswati Bandyopadhyay   +1 more
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Anisian (Middle Triassic) Conodonts of the Kocaeli Triassic, Western Turkey

Journal of Earth Science, 2021
The present study of Anisian (Middle Triassic) conodonts from the Kocaeli Peninsula (western Turkey) encompasses over 10 species of the families Gondolellidae and Gladigondolellidae, providing Early and Middle Triassic time constraints, Chiosella timorensis (Nogami, 1968); Cornudina oezdemirae Gedik, 1975; Gladigondolella tethydis (Huckriede, 1958 ...
openaire   +2 more sources

Troglomorphism in the middle Triassic crinoids from Poland

The Science of Nature, 2015
In this paper, we document the Middle Triassic marine fauna recovered from the fissure/cave system of Stare Gliny (southern Poland) developed in the Devonian host dolomite. The fossils are mostly represented by in situ preserved and small-sized holdfasts of crinoids (Crinoidea) that are attached to the cave walls.
Krzysztof R, Brom   +2 more
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Permo-Triassic boundary and Lower to Middle Triassic in South Tibet

Journal of Asian Earth Sciences, 1998
Abstract The abundance of conodonts increases sharply across the Permian/Triassic boundary in South Tibet, and as a consequence Griesbachian assemblages are much better defined than Changxingian ones. The “ Otoceras latilobatum bed”, representing the base of the Triassic at Selong, is a condensed biocalcirudite including abundant macrofossils ...
E. Garzanti, A. Nicora, R. Rettori
openaire   +1 more source

Richard owen's giant Triassic frogs: archosaurs from the Middle Triassic of England

Journal of Vertebrate Paleontology, 1997
ABSTRACT The first archosaurs from the Middle Triassic were described unwittingly by Sir Richard Owen in the 1840s. He combined a variety of archosaurian postcranial elements with skull material of temnospondyls, thus producing his image of giant Triassic frogs. Archosaur bones have been collected from Middle Triassic (Anisian) sediments of Warwick and
Michael J. Benton, David J. Gower
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Correlation of Lopingian to Middle Triassic Palynozones

Journal of Earth Science, 2018
Terrestrial floras underwent important changes during the Lopingian (Late Permian), Early Triassic, and Middle Triassic, i.e., before, during, and after the end-Permian mass extinction. An accurate account of these developments requires reliable correlation.
Nowak, Hendrik   +2 more
openaire   +1 more source

Middle Triassic radiolarians from West Timor, Indonesia

Journal of Paleontology, 1999
Moderately well-preserved Middle Triassic radiolarians were recovered from bedded limestone exposed at about 3 km west of Kefamenanu, West Timor, Indonesia. This limestone probably from the Aitutu Formation is considered to be an allochthonous block and is embedded in the Neogene Bobonaro Complex.
K. Sashida   +3 more
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Pistosaurus, a middle Triassic plesiosaur

American Journal of Science, 1948
"Pistosaurus from upper part of middle Triassic in southern Germany is the earliest plesiosaur of which a complete restoration can be given; it still has long legs, not yet ordinary paddles."
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Middle Triassic ostracods from Yunnan, South China

Alcheringa: An Australasian Journal of Palaeontology
The Anisian stage (Middle Triassic) witnessed the explosive diversification of numerous marine taxa following the end-Permian extinction. For marine ostracods, the current knowledge of this event (and its Early Triassic origins) is geographically biased by a severe lack of data from eastern Tethys and eastern Panthalassa.
Forel, Marie-Béatrice   +7 more
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Middle Triassic conodonts from northeastern Spain: biostratigraphic implications

Terra Nova, 2000
The facies development of the Spanish Triassic corresponds to the typical three‐fold subdivision of the Germanic Facies: Buntsandstein, Muschelkalk and Keuper. Two intervals interpreted as epeiric carbonate platforms: lower Muschelkalk (Anisian) and upper Muschelkalk (Ladinian) are recognized during the Middle Triassic of northeastern Spain.
A. Marquez-Aliaga   +3 more
openaire   +1 more source

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