The Neogene VP Sites of Czechoslovakia: A Contribution to the Neogene Terrestric Biostratigraphy of Europe Based on Rodents

Fejfar, Oldřich

doi:10.1007/978-1-4899-2513-8_15

Cited by 27 publications

(37 citation statements)

References 7 publications

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“…The mammal fauna of Lišov (MN 7-8) from the Domanín Fm. supports the dating into the late Middle Miocene (Fejfar 1989(Fejfar , personal communication 2007 , which is probably comparable with the flora of Gozdnica in Poland (Gozdnica Series, Pannonian), contains a few rare mastixioids and is characterised by prevailing deciduous "Arctotertiary" elements. Thus the new palaeobotanical data from South Bohemia make possible the Middle Badenian age for the oldest tektite-bearing unit, the Vrábče Member, considered putatively as the basal part of the Domanín Formation, and prove only a short time gap between the rain of tektites and their first re-deposition.…”

Section: Conclusion To Biostratigraphy and Correlationsupporting

confidence: 69%

“…The Mydlovary Formation dated to the KarpatianLower Badenian by fauna (Čtyroký & Fejfar 1962;Fejfar 1974Fejfar , 1989Bůžek et al 1988) and flora (Řeháková in Vrána et al 1980, Knobloch & Kvaček 1996 does not contain tektites. The Domanín Formation was established on the basis of the diatomology (Řeháková 1969a, b) and dated into the Middle Miocene (Upper Badenian to Sarmatian) on account of the correlation with similar diatom assemblages in the Handlová Basin in the Central Paratethys (Řeháková 1980).…”

Section: Geological Setting Of Tektite-bearing Sediments In South Bohmentioning

confidence: 99%

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A new mastixioid florula from tektite-bearing deposits in South Bohemia, Czech Republic (Middle Miocene, Vrábče Member)

Ševčı́k¹,

Kvaček²,

Mai³

2007

Bull. Geosci.

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A mastixioid assemblage consisting of seed cones of Pinus hampeana and fruits of Carya globosa, Diplopanax limnophilus and Eomastixia saxonica has been recovered in tektite-bearing deposits at Dobrkovská Lhotka near Trhové Sviny on the southern periphery of the České Budějovice Basin, South Bohemia. Although its diversity is low, the assemblage is characteristic enough to be correlated with the Middle Miocene floras of the Central Paratethys area (Wieliczka at Kraków - Middle Badenian) and with comparable floras in the Boreal Province (Kleinleipisch and Klettwitz Floral Assemblages in Germany - Middle Miocene). The obtained data corroborate the Badenian age for the Vrábče Member, the oldest tektite-bearing unit from where the fossils were collected (?the basal part of the Domanín Formation) and prove a short time span between the rain of tektites (Ries event, 15-14.5 Ma) and the deposition of this unit

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Section: Conclusion To Biostratigraphy and Correlationsupporting

confidence: 69%

Section: Geological Setting Of Tektite-bearing Sediments In South Bohmentioning

confidence: 99%

A new mastixioid florula from tektite-bearing deposits in South Bohemia, Czech Republic (Middle Miocene, Vrábče Member)

Ševčı́k¹,

Kvaček²,

Mai³

2007

Bull. Geosci.

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“…Die Tuffe wurden in den 70-er Jahren durch Beseitigung des Abraums in Dětaň aufgeschlossen. Die Säugetierarten (Fejfar 1974, 1990, Fejfar und Storch 1994, Fejfar et al 2003, enthalten für das Unteroligozän repräsentative Indexformen (Abb. 4) Schlämmen von Feinsanden (1961-1967 wurde eine Fauna von Kleinsäugern mit einer Anzahl von Indexarten gewonnen.…”

Section: Grundlagen Der Korrelationenunclassified

“…4). Die Fauna von Ořechov war die erste Säugetierfauna in Europa, die direkt mit der marinen Abfolge der Paratethys korreliert wurde -d.h. mit dem oberen Teil der Ottnang-Stufe der Paratethys (Cicha et al 1972, Fejfar und Roček 1986, Fejfar 1990 (Mein 1989, Daxner-Höck 1998. Alter: Untermiozän, UnterburdigalOberaquitan; Paratethys: Eggenburg, Säugetierstufe unteres Orleanium, Biozone MN 3a.…”

Section: Grundlagen Der Korrelationenunclassified

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A revision of Trichopeziza lizonii, T. sulphurea and T. violascens (Ascomycota, Helotiales) from the herbarium PRM with notes on type material of Peziza sulphurea

Chilebicka¹,

Komari²

2013

Acta Mus. Nat. Pragae ser.B, hist.nat.

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MAMMALS FROM THE EARLY MIOCENE OF THE CHOMUTOV BASIN -I. CHALICOTHERIIDAE (MAMMALIA, PERISSODACTYLA).Abstract. The site described is the brown coal open pit mine Tušimice, part Merkur-North, Chomutov Basin in northwestern Bohemia. Its fauna is defined as a distinct level of the mammalian faunas of the Tertiary of the Czech Republic. From this quarry, the most complete and numerous material of Chalicotheriidae from the Early Miocene of Eurasia is described in detail as Phyllotillon schlosseri sp. nov. The species is characterized as a member of the subfamily Schizotheriinae by the sharp cusps of its narrow upper molars, and a clear separation of metaconid and metastylid of the lower molars. The nearly equal strength of protoloph and metaloph in the upper premolars is also markedly different from Chalicotheriinae. Within Miocene Schizotheriinae, the species represents a basal stage of evolution, distinguishable from the Oligocene genera by loss of the hypoconulid of its last lower molars, and the fusion of the first and second phalanges of the second digit to a duplex bone. Eurasian Early Miocene samples of this stage are almost exclusively dental remains. From the North American genera Moropus and Tylocephalonyx, the material under consideration is distinguished by the lingual lengthening, which means progressive molarisation of the upper premolars. In contrast to Moropus, the metacarpals are considerably shorter, combined with several other autopodial characters. The only Eurasian named genus of this stage is Phyllotillon, from the Lower Miocene of Baluchistan. The Bohemian species is distinguished from the type species P. naricus (PILGRIM, 1908) by the more distally projecting mesostyle of the more shortened M3, and the weaker metacone rib of the upper molars. It has not been possible to determine whether differences of proportions in both species are caused by individual variability. The peculiar, somewhat smaller species "Chalicotherium" wetzleri KOWALEVSKY, 1874 is ranged into the genus Moropus because of its evolutionary level. It is clearly different from Phyllotillon schlosseri sp. nov. The differences from the earliest representative of the more modern stage of evolution, Metaschizotherium bavaricum KOENIGSWALD, 1932 are also observed in detail. The high percentage of chalicotheres is a special trait of the fauna, probably caused by ecological conditions. Analysis of the flora may give new insights into the mode of life and nourishment of this mammalian family.n Mammalia, Chalicotheriidae, Early Miocene, Chomutov basin, North-Western Bohemia, Czech Republic.

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Myoglis meini (de Bruijn, 1965 [1966]) (Mammalia: Gliridae) aus dem Miozän von Hambach 6C (NW-Deutschland)

Nemetschek

Mörs

2003

Paläontol. Z.

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The Neogene VP Sites of Czechoslovakia: A Contribution to the Neogene Terrestric Biostratigraphy of Europe Based on Rodents

Cited by 27 publications

References 7 publications

A new mastixioid florula from tektite-bearing deposits in South Bohemia, Czech Republic (Middle Miocene, Vrábče Member)

A new mastixioid florula from tektite-bearing deposits in South Bohemia, Czech Republic (Middle Miocene, Vrábče Member)

A revision of Trichopeziza lizonii, T. sulphurea and T. violascens (Ascomycota, Helotiales) from the herbarium PRM with notes on type material of Peziza sulphurea

Myoglis meini (de Bruijn, 1965 [1966]) (Mammalia: Gliridae) aus dem Miozän von Hambach 6C (NW-Deutschland)

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