The first occurrence of Crassodontidanidae of Hungary is described. The material consists of a single tooth, currently placed in private collection. Th e specimen was found nearby Magyaregregy, at the so-called Síngödör outcrop, in the Middle Jurassic (Bathonian) Óbánya Limestone Formation. The tooth is characterized by a serrated mesial cutting edge of the main cusp, high root with convex mesial and distal margins. This character combination readily distinguishes the tooth from those of Hexanchidae. Currently, this is the oldest representation of Hexanchiformes in the fossil record of Hungary, which widens our knowledge on the distribution patterns of Crassodontidanidae. Summarized data of the hexanchiform fossil record of Hungary is also ...
Hettangian to Pliensbachian neoselachian tooth assemblages from marine deposits in northwest Europe ...
New placodont remains from the Triassic of Hungary are described here. They come from two different ...
Relatively sparsely found fossil vertebrate remains have been collected with variable intensity from...
Lower Cretaceous (Valanginian-Hauterivian) fish remains, collected in the Közöskút Ravine (nearby Há...
Background. The Cretaceous of southern Europe was characterized by an archipelago setting with fauna...
Abstract Remains of Triassic vertebrates discovered in the Villány Hills (SW Hungary) are describe...
In 2016, two fossil marine reptiles were re-discovered in the collections of the Museo Civico di Sto...
The Nyirád I. outcrop is extremely rich in fossils of marine vertebrates, including chondrichthyans,...
Sampling of a lenticular concentration of vertebrate debris and associated sediments from the lower ...
To actualize the available data regarding Cenozoic fi sh materials housed in the vertebrate fossil c...
© 2017 The Authors. Palaeontology published by John Wiley & Sons Ltd on behalf of The Palaeontolog...
Here, we provide a detailed taxonomic reassessment of a historically collected chondrichthyan dental...
An Early Oligocene (Rupelian, Kiscellian), partially published shark tooth material, une...
Here we describe a new, previously unrecognized elasmobranch microfossil assemblage consisting of is...
Recent collecting of the classic Middle Anisian fossil site of the Akol Hill at Barnag (Nagyvázsony ...
Hettangian to Pliensbachian neoselachian tooth assemblages from marine deposits in northwest Europe ...
New placodont remains from the Triassic of Hungary are described here. They come from two different ...
Relatively sparsely found fossil vertebrate remains have been collected with variable intensity from...
Lower Cretaceous (Valanginian-Hauterivian) fish remains, collected in the Közöskút Ravine (nearby Há...
Background. The Cretaceous of southern Europe was characterized by an archipelago setting with fauna...
Abstract Remains of Triassic vertebrates discovered in the Villány Hills (SW Hungary) are describe...
In 2016, two fossil marine reptiles were re-discovered in the collections of the Museo Civico di Sto...
The Nyirád I. outcrop is extremely rich in fossils of marine vertebrates, including chondrichthyans,...
Sampling of a lenticular concentration of vertebrate debris and associated sediments from the lower ...
To actualize the available data regarding Cenozoic fi sh materials housed in the vertebrate fossil c...
© 2017 The Authors. Palaeontology published by John Wiley & Sons Ltd on behalf of The Palaeontolog...
Here, we provide a detailed taxonomic reassessment of a historically collected chondrichthyan dental...
An Early Oligocene (Rupelian, Kiscellian), partially published shark tooth material, une...
Here we describe a new, previously unrecognized elasmobranch microfossil assemblage consisting of is...
Recent collecting of the classic Middle Anisian fossil site of the Akol Hill at Barnag (Nagyvázsony ...
Hettangian to Pliensbachian neoselachian tooth assemblages from marine deposits in northwest Europe ...
New placodont remains from the Triassic of Hungary are described here. They come from two different ...
Relatively sparsely found fossil vertebrate remains have been collected with variable intensity from...