Neue Pseudosuchier Und Coelurosaurier Aus Dem Württembergischen Keuper

Huene, Friedrich von

doi:10.1111/j.1463-6395.1921.tb00489.x

Cited by 34 publications

(18 citation statements)

References 4 publications

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“…We know of no such disagreement in the primary literature on Aetosaurus (e.g., O. Fraas, 1877;Huene, 1921;Walker, 1961;Wild, 1989;Heckert and Lucas, 1998;Small, 1998;Lucas et al, 1998b or on aetosaurs in general (Walker, 1961;Parrish, 1994;Heckert et al, 1996;Heckert and Lucas, 2000;Parker, 2007). We conclude that there is no valid reason to question the use of Aetosaurus as a Revueltian index taxon.…”

Section: Revueltianmentioning

confidence: 89%

Global Triassic tetrapod biostratigraphy and biochronology

Lucas

1998

Palaeogeography, Palaeoclimatology, Palaeoecology

329

276

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Section: Revueltianmentioning

confidence: 89%

Global Triassic tetrapod biostratigraphy and biochronology

Lucas

1998

Palaeogeography, Palaeoclimatology, Palaeoecology

329

276

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“…Elsewhere in the northern half of Pangaea, crocodylomorphs have been found in the Triassic of both the Germanic Basin and the United Kingdom (Huene 1921;Crush 1984). Abundant skeletal material of a single species of crocodylomorph, Terrestrisuchus gracilis, was found in least five different latest Triassic fissure fills in Carboniferous limestones from southwestern England and Wales (Crush 1984;Whiteside & Marshall 2008).…”

Section: Distribution and Biogeographymentioning

confidence: 98%

Early Crocodylomorpha

Irmis

Nesbitt

Sues

2013

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Non-crocodyliform crocodylomorphs, often called ‘sphenosuchians’, were the earliest-diverging lineages of Crocodylomorpha, and document the stepwise acquisition of many of the features that characterize extant crocodylians. The first crocodylomorph fossils are approximately 230 million years old (upper Carnian, Late Triassic), and at least one of these early lineages persisted until at least 150 million years ago (Late Jurassic). These taxa occupied a wide variety of terrestrial environments from equatorial regions to high-paleolatitudes during the early Mesozoic. Despite a quarter-century of quantitative phylogenetic work, the interrelationships of early crocodylomorphs remain in a state of flux, though recent studies suggest that these lineages are paraphyletic with respect to Crocodyliformes, rather than forming a monophyletic early offshoot of Crocodylomorpha as some previously hypothesized. Nearly all early crocodylomorphs were upright quadrupedal small-bodied taxa, but lumping them all together as small cursorial faunivores masks ecological and morphological disparity in diet and limb functional morphology. With the accelerated pace of recent discovery of new specimens and taxa, future consensus on early crocodylomorph phylogeny will provide a solid framework for understanding their change in diversity and disparity through time, potential biogeographic patterns, and the morphological transformation leading to Crocodyliformes.

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“…Eine schwache Panzemng, bestehend aus einzelnen knfchernen, fiber den Dornforts~itzen der Wirbe] liegenden Osteodermen trat in der Evolution der Beptilien erstmals bei einigen Eosuchiern der Permotrias auf (Gow, 1975;CAm~OLL, 1976 (HuENE, 1986(HuENE, , 1988RE~FF, 1942).…”

Section: Entwicklung Eines Panzersunclassified

“…Im Ubergang vonder ,halbaufgerichteten" zur ,,voll-erhobenen" Stellung der Gliedmal3en konnten sich dann bipede, also auf den Hintergliedmal3en zweibeinig laufende Reptilien entwickeln. Als Beispiel sei der etwa 1 m lange Thecodontier Saltoposuchus ans der Obertrias Wiirttembergs angefiihrt (HuENE, 1921), der sich rennend und wahrscheinlich auch springend nur anf den Hintergliedmal3en fortbewegte.…”

Section: Verbesserung Der Gliedmaflenstelhmgunclassified

“…Dennoch ist es fiitselhaft, warum nach der explosionshaften Entfaltung und Blfitezeit der Reptilien in der Trias sehon mit dem Ende der Trias verschiedene ttepfilgruppen pl6tzlieh und weltweit verschwinden (CoLBEaT, 1958 b (COLBERT, 1971(COLBERT, --1974COLBERT • KITCHING, 1981;BARTHOLOMAI, 1979). Ein Vergleich dieser Faunen mit Untertrias-Faunen in Lauasia scheint bislang nur in NordruI31and mSglich (HUENE, 1940). Erst in der Mittelund Obertrias gelingt die Korrelation terrestriseher Gondwana-und LaurasiaFaunen, was auf eine enge Naehbarsehaft beider Superkontinente in jener Zeit hindeutet.…”

Section: Aussterbenunclassified

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Die Evolution der Reptilien in der Triaszeil

Wild

1982

Geol Rundsch

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AbstraetThe Triassic is the period of the main radiation of the reptiles. Numerous new orders are developing such as the thecodonts, saurisehians and ornithisehians [dinosaurs], the erocodilians, pterosaurs, sauropterygians, lizards, the sphenodonts and rhynehosaurs, generally classified as rhynchocephalians, the ehelonians, iehthyosaurs, placodonts and therapsids. Their phylogenetic relations are still partly unknown. The step towards conquering new habitats on land, in the sea and in the air, the trend towards gigantic size, the development of armour, the improvement of gait and the aehievment of endothenny enabled the reptiles to dominate the earth absolutely during the Mesozoic. Moreover the obviously explosive evolution of the reptiles in the Triassie led to the development of two new classes of vertebrates, the birds and the mammals. Some Triassic reptiles can be used for paleogeographie reconstruction and stratigraphic correlation based on their wide distribution, great independence from the environment and rapid evolution.

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Neue Pseudosuchier Und Coelurosaurier Aus Dem Württembergischen Keuper

Cited by 34 publications

References 4 publications

Global Triassic tetrapod biostratigraphy and biochronology

Global Triassic tetrapod biostratigraphy and biochronology

Early Crocodylomorpha

Die Evolution der Reptilien in der Triaszeil

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