Fieldwork around the lime-kilns at Zengővárkony (southern Hungary, eastern Mecsek Mts.) has led to the discovery of previously unknown beds of the Hidasivölgy Marl Formation. Based on bio- and lithostratigraphic considerations, here a Valanginian (Hauterivian?) age is assumed. This recently discovered section consists of thin-bedded, greybrownish turbiditic marls and limestones laid down in rhythmic alterations. Excavations of the marl beds have yielded a poorly-preserved, but rich cephalopod fauna. Furthermore, Eutrephoceras ex gr. boissieri has been identified here, and this is the first record of Cretaceous nautiloids from the Mecsek Mountains
A nautilid faunule of seven specimens, comprising Eutrephoceras bouchardianum (d’Orbigny, 1840), Cym...
The Middle Jurassic shelf margin limestones and marly limestones of Western France yield quite numer...
Abstract The Aitamir Formation, situated in the Koppeh Dagh Basin in the northeast of Iran, is known...
This is the first investigation on isolated Early Cretaceous foraminifera fauna from Hungary. The fa...
Recent nautiloid and ammonoid finds from the Middle Triassic Zuhánya Limestone Formation in the Mecs...
Two nautiloid specimens are described from the Transdanubian (West Hungarian) Middle Eocene. The spe...
The post-Triassic Nautiloidea are not as popular theme within fossils cephalopods research as for ex...
The lower part of the Lower Cretaceous Bolos Sandstone Formation as exposed in the Barranco de la Mu...
The brachiopod fauna of the Lower Cretaceous Bersek Marl (Gerecse Mountains, Hungary) is briefly des...
The fossil biota of the upper Valanginian–lower Hauterivian sediment hosted vent (SHV) environment o...
In the Early Cretaceous, the continental rift basin of the Mecsek Mts. (Hungary), was situated on th...
Iharkút is a Late Cretaceous (Santonian) vertebrate-bearing locality in the Bakony Mountains of west...
The majority of originally aragonitic cephalopod shells are typically dissolved and preserved as mou...
Foraminifera studies were carried out on the Štramberk-type limestones which occur as pebbles to sma...
Foraminifera studies were carried out on the Štramberk-type limestones which occur as pebbles to sma...
A nautilid faunule of seven specimens, comprising Eutrephoceras bouchardianum (d’Orbigny, 1840), Cym...
The Middle Jurassic shelf margin limestones and marly limestones of Western France yield quite numer...
Abstract The Aitamir Formation, situated in the Koppeh Dagh Basin in the northeast of Iran, is known...
This is the first investigation on isolated Early Cretaceous foraminifera fauna from Hungary. The fa...
Recent nautiloid and ammonoid finds from the Middle Triassic Zuhánya Limestone Formation in the Mecs...
Two nautiloid specimens are described from the Transdanubian (West Hungarian) Middle Eocene. The spe...
The post-Triassic Nautiloidea are not as popular theme within fossils cephalopods research as for ex...
The lower part of the Lower Cretaceous Bolos Sandstone Formation as exposed in the Barranco de la Mu...
The brachiopod fauna of the Lower Cretaceous Bersek Marl (Gerecse Mountains, Hungary) is briefly des...
The fossil biota of the upper Valanginian–lower Hauterivian sediment hosted vent (SHV) environment o...
In the Early Cretaceous, the continental rift basin of the Mecsek Mts. (Hungary), was situated on th...
Iharkút is a Late Cretaceous (Santonian) vertebrate-bearing locality in the Bakony Mountains of west...
The majority of originally aragonitic cephalopod shells are typically dissolved and preserved as mou...
Foraminifera studies were carried out on the Štramberk-type limestones which occur as pebbles to sma...
Foraminifera studies were carried out on the Štramberk-type limestones which occur as pebbles to sma...
A nautilid faunule of seven specimens, comprising Eutrephoceras bouchardianum (d’Orbigny, 1840), Cym...
The Middle Jurassic shelf margin limestones and marly limestones of Western France yield quite numer...
Abstract The Aitamir Formation, situated in the Koppeh Dagh Basin in the northeast of Iran, is known...