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- W2188293314 abstract "The Torinosu and Torinosu-type limestones in Japan are originated from the reefal facies of the ancient continental margin, transported to continental slopes, and emplaced as allochthonous blocks within siliciclastic rocks. Foraminifers are controlled by limestone facies, and common in fine-grained, muddy, bioclastic limestones and rare or absent in limestones (boundstones) with many reef building metazoans. Twenty-eight species assignable to 20 genera are identified in the type locality of the Torinosu limestone in the Sakawa area. Dominant and characteristic species are Pseudocyclammina lituus (Yokoyama), Broeckinella magna Septfontaine, Freixialina planispiralis Ramalho, Rectocyclammina sp. A, Charentia cuvillieri Neumann, and Everticyclammina kelleri (Henson). Based on the comparison of biostratigraphic distribution of these species in the western Tethyan regions, the Sakawa foraminiferal fauna is assigned to Berriasian to Valanginian age, probably Late Berriasian to Early Valanginian age." @default.
- W2188293314 created "2016-06-24" @default.
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- W2188293314 date "2014-01-01" @default.
- W2188293314 modified "2023-09-27" @default.
- W2188293314 title "Early Cretaceous (Berriasian to Valanginian) foraminifers from the Torinosu limestone at the type locality of Sakawa, Shikoku, Japan" @default.
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