Lower Liassic involutinids (foraminifera) from the Transdanubian Central Range, Hungary

Blau, Joachim; Haas, Ános

doi:10.1007/bf02985771

Cited by 11 publications

(12 citation statements)

References 4 publications

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“…Remarks: As pointed out by Piller (1978) (kristan, 1957;kuss, 1983;Blau, 1987a, b;eBli, 1993;BöHm et al, 1999); Lower Jurassic of Carpathians (Gaz ª dzicki, 1983); Lower Jurassic of Transdanubian Range, Hungary (Blau & Haas, 1991). Kristan, 1957 Pl 189A, 189B, 191B, 192, 195A, 240, 241, 245A, 276A, 278C, 279, 280, 282, 290A. Description: Specimens are numerous and display various degrees of preservation.…”

Section: Remarksmentioning

confidence: 93%

Rhaetian foraminiferal assemblage from the Dachstein Limestone of Mt. Begunjščica (Košuta Unit, eastern Southern Alps)

Gale¹

2012

Geologija

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Mt. Begunj{~ica (Karavanke Mts., northern Slovenia) structurally belongs to the Ko{uta Unit (eastern Southern Alps). The Dachstein Limestone, building the northern side of the mountain and its main ridge, was deposited on the Julian Carbonate Platform, while grey and red nodular Jurassic limestones of the southern slope represent sedimentation on the Julian High. The massive Dachstein Limestone contains a rich assemblage of benthic foraminifera. Typical representatives of the reef and back-reef area were recognized. The age of the assemblage is dated as Rhaetian, based on the co-presence of species with a Norian and Rhaetian time span, such as Galeanella tollmanni, "Sigmoilina" schaeferae, Alpinophragmium perforatum, Aulotortus tumidus, Variostoma catilliforme, Variostoma cochlea and Variostoma helicta, together with the Rhaetian to Lower Jurassic Involutina turgida. Izvle~ekBegunj{~ica (Karavanke, severna Slovenija) strukturno pripada tektonski enoti Ko{uta (vzhodne Južne Alpe). Dachsteinski apnenec, ki gradi severno stran gore in njen vr{ni greben, se je odlagal na Julijski karbonatni platformi, medtem ko sivi plastnati in rde~i gomoljasti jurski apnenci predstavljajo sedimentacijo na Julijskem platoju. Masivni del dachsteinskega apnenca vsebuje {tevilne bento{ke foraminifere, tipi~ne za grebensko in zagrebensko okolje. Na podlagi prisotnosti vrst z norijsko-retijskim razponom kot so Galeanella tollmanni, "Sigmoilina" schaeferae, Alpinophragmium perforatum, Aulotortus tumidus, Variostoma catilliforme, Variostoma cochlea in Variostoma helicta z retijsko do zgodnjejursko vrsto Involutina turgida je združba retijske starosti.

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Section: Remarksmentioning

confidence: 93%

Rhaetian foraminiferal assemblage from the Dachstein Limestone of Mt. Begunjščica (Košuta Unit, eastern Southern Alps)

Gale¹

2012

Geologija

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“…184/4;Piller 1978;Blau 1987aBlau , 1987bSchröder 1988;Ebli 1993), Carpathians (Gazdzicki 1983), Bakony Mountains (Blau and Haas 1991), Greece (Karakitosis and TsailaMonopolis 1988), and from the Wombat Plateau of north Australia (Röhl et al 1991). Piller (1978) states the stratigraphic range of T. umbo as "Norian-Rhaetian?…”

Section: Descriptionmentioning

confidence: 99%

“…; Liassic", but all described specimens of the world are from Lower Jurassic (Liassic), except those described by Röhl et al (1991). Kristan-Tollmann (1986a described from Upper Triassic (Rhaetian) of central Papua/New Guinea the species Trocholina (Trocholina) granosa Frentzen, which, according to Blau and Haas (1991), should be attributed to T. umbo.…”

Section: Descriptionmentioning

confidence: 99%

“…The species is known also from the Liassic of numerous localities in the Tethyan realm (Alps: Blau 1987aBlau , 1987bCarpathians: Gazdzicki 1983; Bakony Mts. : Blau and Haas 1991;Turkey: Brönni-mann et al 1970). Altiner (2004, 2007) reported this species (without illustrations) from the Norian-Rhaetian of Karakaya complex, northwest Turkey, and Kristan-Tollman (1986a from the Rhaetian of Kuta limestones of Papua/Neu Guinea as well as from Wombat-Plateau (north of Australia).…”

Section: Descriptionmentioning

confidence: 99%

“…Occurrence: Trocholina gracilis was known from the Liassic of the Lienzer Dolomites, Austria (Blau 1987b) and from the Liassic of Sürmeg, Hungary (Blau and Haas 1991). Schröder (1988) illustrated a questionable specimen from the Liassic of the northern Karawanks, Austria.…”

Section: Trocholina Gracilismentioning

confidence: 99%

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Foraminifera and their associations of a possibly Rhaetian section of the Nayband Formation in central Iran, northeast of Esfahan

Senowbari‐Daryan

Rashidi

Torabi

2010

Facies

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The following paper describes the foraminiferal fauna and associated faunal assemblages of the bedded and reef carbonates of the Upper Triassic (most probably Rhaetian) Nayband Formation, which are exposed in a section south of the small town of Bagher-Abad, northeast of Esfahan. Foraminifers are extremely rare in sponge-or coraldominated bioconstructions and in the bedded carbonates of the Nayband Formation in central Iran. Some carbonate beds are composed of bioclastic wackstone/packstone. These are exposed in the solenoporacean horizon at the uppermost part of the section. Here, the aulotortid-and trocholinid-type foraminifers are relatively abundant. The following foraminiferal taxa with diVerent abundances were found within the carbonates of the investigated section:

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The Büdöskút Olistolith, an exotic limestone block from the Bükk mountains (NE-Hungary)

Velledits

Blau

2003

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Lower Liassic involutinids (foraminifera) from the Transdanubian Central Range, Hungary

Cited by 11 publications

References 4 publications

Rhaetian foraminiferal assemblage from the Dachstein Limestone of Mt. Begunjščica (Košuta Unit, eastern Southern Alps)

Rhaetian foraminiferal assemblage from the Dachstein Limestone of Mt. Begunjščica (Košuta Unit, eastern Southern Alps)

Foraminifera and their associations of a possibly Rhaetian section of the Nayband Formation in central Iran, northeast of Esfahan

The Büdöskút Olistolith, an exotic limestone block from the Bükk mountains (NE-Hungary)

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