221 research outputs found

    古生物の進化を見せる博物館建設へ

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    PERMIAN FUSULINACEANS OF THE SURMAQ FORMATION IN THEABADEH REGION, CENTRAL IRAN

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    Fusulinaceans consisting of 56 species belonging to 30 genera are distinguished from the Surmaq Formation distributed in the Abadeh region, central Iran.  Among them, 23 species, including three species newly proposed: Parafusulina tarazi, Skinnerella abadehensis, and Sphaerulina iranensis, are systematically described and discussed.  Many microphotographs of fusulinaceans are illustrated so as to understand their wide intraspecific variation and to compare them with other faunas  from the Tethyan regions.  The Surmaq Formation is biostratigraphically divided into six zones from lower to upper: Darvasites ordinatus, Pseudofusulina quasifusuliniformis, Eopolydiexodina persica, Afghanella schencki, Neoschwagerina occidentalis, and Chusenella abichi. The first zone is probably Yakhtashian, the second is possibly Kubergandian, the third to fifth are Murgabian, and the last is Midian in age, based on the stratigraphic distribution and faunal correlation of neoschwagerinids and schwagerinids in Middle Permian formations of the Tethyan regions.  Schwagerinids are dominant in these six zones, whereas almost all neoschwagerinids and verbeekinids are restricted to the fourth and fifth zones.  Middle Permian fusulinacean faunas in South West Asian and Mediterranean Sea regions are well represented by those of the Surmaq Formation, and paleobiogeographically assignable to Province A (Western Tethyan Province).  Fusulinacean faunas of Province A are largely different from those in Province B (Eastern Tethyan Province) by the very rare occurrence of typical Colania and Lepidolina, and from Province C (Panthalassan Province) by the presence of Afghanella and Sumatrina.&nbsp

    Abodehella, A New Genus of Tetrataxid Foraminifera from the Late Permian

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    A new genus, Abadehella comprising three new species (tarazi, coniformis, and biconvexa) is proposed and described. So far as the morphologic features are concerned, the genus is considered to be a specialized genus in the family Tetrataxidae. This characteristic genus is found from the basal part of the Abadeh Formation in central Iran, the lowest member of the Zewan Formation in Kashmir, the Palaeofusulina limestone in Malaysia, Lepidolina multiseptata limestones in Cambodia and northeast Japan, the Takauchi and Reichelina-Colaniella limestones of the Maizuru belt, and the Lepidolina kumaensis zone of Shikoku in Japan. The stratigraphic occurrence is limited to the Late Permian and the genus is considered to be useful for international correlation
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