Fazies und Ablagerungsbedingungen eines karbonatischen Mounds (Tithon-Berrias, SW-Japan)

Kano, Akihiro

doi:10.1007/bf02536794

Cited by 20 publications

(29 citation statements)

References 19 publications

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“…Kano et al, 2006 e.g. Kano, 1988;Kano andJiju, 1995 Shiraishi andKano, 2004;Ohga et al, 2013Kano, 1988Kano and Jiju, 1995 Figs. 6A, 7 50-100 m e.g.…”

Section: Aplosmilia Acanthogyra Enallheria Isastrea Latomeandra Stylimentioning

confidence: 99%

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大分県東部・四浦半島に分布する後期ジュラ紀の礁性石灰岩の堆積環境と厚歯二枚貝の産状

Kakizaki

Furuyama

Kano

2015

Jour. Geol. Soc. Japan

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“…Kano et al, 2006 e.g. Kano, 1988;Kano andJiju, 1995 Shiraishi andKano, 2004;Ohga et al, 2013Kano, 1988Kano and Jiju, 1995 Figs. 6A, 7 50-100 m e.g.…”

Section: Aplosmilia Acanthogyra Enallheria Isastrea Latomeandra Stylimentioning

confidence: 99%

“…6A, 7 50-100 m e.g. Kano, 1988;Kano and Jiju, 1995 35 m Stylina Isastrea Bacinella-Lithocodium e.g. Leinfelder et al, 1993;Dupraz and Strasser, 1999Dupraz and Strasser, 2002 22 m Kauffman and Sohl, 1979;Ross andSkelton, 1993 Starobogatov, 1992 e.g.…”

Section: Aplosmilia Acanthogyra Enallheria Isastrea Latomeandra Stylimentioning

confidence: 99%

大分県東部・四浦半島に分布する後期ジュラ紀の礁性石灰岩の堆積環境と厚歯二枚貝の産状

Kakizaki

Furuyama

Kano

2015

Jour. Geol. Soc. Japan

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“…Previous sedimentological studies (e.g. Kano 1988;Kano and Jiju 1995) showed that the Torinosu Limestone includes a reefal facies mainly composed of reef-builders such as corals and stromatoporoids. Unfortunately, these studies paid little attention to microencrusters and microbialites, although two genera had been observed in paleontological studies of the Torinosu Limestone (Girvanella; Yabe and Toyama 1928 and Lithocodium;Endo 1961).…”

Section: Introductionmentioning

confidence: 99%

Composition and spatial distribution of microencrusters and microbial crusts in upper Jurassic?lowermost Cretaceous reef limestone (Torinosu Limestone, southwest Japan)

Shiraishi

Kano

2004

Facies

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Tethyan microencrusters and microbial crusts, most of them previously unknown in Japanese Mesozoic biotas, are present in the uppermost Jurassic-lowermost Cretaceous Torinosu Limestone distributed in southwestern Japan. They construct reefal facies together with reefforming metazoans. Bacinella irregularis and Lithocodium aggregatum are quantitatively most important, while subordinate constituents include Thaumatoporella parvovesiculifera, Koskinobullina socialis, Iberopora bodeuri, Girvanella sp. and "Tubiphytes" morronensis. They are especially common in the shallow-water reefal facies, but appear micritic in outcrops. Microencrusters and microbial crusts can only be recognized in thin sections, and they grow around the reef building metazoans and form bindstone. Each microencruster exhibits some specific spatial distribution associated with its paleoecology. Similarities with the taxonomic composition of the upper Jurassic Tethyan microencruster association imply that the community extended geographically at least to the Tethyan gateway where the Japanese Island Arc was located.

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“…In regions representing the Tethys and the western Panthalassa, stromatoporoids were important reef-building organisms (Fagerstrom 1987;Copper 1988;Leinfelder et al 2005) and formed a wide range of organic constructions from huge reef complexes to small carbonate mounds (e.g. Turnsek et al 1981;Kano 1988). Stromatoporoids have previously been described from the Jurassic-Cretaceous succession of the Middle East (Hudson 1954(Hudson , 1955Okla 1986;Toland 1994;Schumann 1995), which represents one of the largest hydrocarbon reservoirs in the world.…”

Section: Introductionmentioning

confidence: 99%

Facies and depositional environment of the uppermost Jurassic stromatoporoid biostromes in the Zagros Mountains of Iran

Kano

Kakizaki²,

Takashima³

et al. 2007

GFF

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Abstract:The uppermost Jurassic (Tithonian) stromatoporoid biostromes occur as horizontally extended, up to 2.5 m thick lenses in a shallow marine carbonate sequence in the northwestern part of the Zagros Mountains, Iran. Stromatoporoids, accompanied by corals and calcareous algae, form floatstone and rudstone textures. The initial establishment of these potential reef-building organisms may have been related to substrate stabilization, likely due to exposure events. The stromatoporoids show two types of growth forms. Columnar forms, including the new species Cladocoropsis lindstroemi, are enclosed in a micritic matrix in low-energy environments. Laminar-domical forms piled up their skeletons on other species, or formed bulbous structures by encrusting other organisms. This study is the first description of Mesozoic stromatoporoids from Iran.

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Fazies und Ablagerungsbedingungen eines karbonatischen Mounds (Tithon-Berrias, SW-Japan)

Cited by 20 publications

References 19 publications

大分県東部・四浦半島に分布する後期ジュラ紀の礁性石灰岩の堆積環境と厚歯二枚貝の産状

大分県東部・四浦半島に分布する後期ジュラ紀の礁性石灰岩の堆積環境と厚歯二枚貝の産状

Composition and spatial distribution of microencrusters and microbial crusts in upper Jurassic?lowermost Cretaceous reef limestone (Torinosu Limestone, southwest Japan)

Facies and depositional environment of the uppermost Jurassic stromatoporoid biostromes in the Zagros Mountains of Iran

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