首页> 外文期刊>Rivista Italiana di Paleontologia e Stratigrafia >CAIROELLA TRICAMERATA N. GEN., N. SP (FORAMINIFERIDA, MILIOLOIDEA) FROM THE LOWER CENOMANIAN OF MONTE CAIRO (SOUTHERN LATIUM, CENTRAL ITALY)
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CAIROELLA TRICAMERATA N. GEN., N. SP (FORAMINIFERIDA, MILIOLOIDEA) FROM THE LOWER CENOMANIAN OF MONTE CAIRO (SOUTHERN LATIUM, CENTRAL ITALY)

机译:CAIROELLA TRICAMERATA N. GEN。,N. SP(FORAMINIFERIDA,MILIOLOIDEA)来自蒙特·开罗(Cateo)较低的切诺曼尼亚人(意大利中南部南部)

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摘要

A new porcelaneous foraminifer, Cairoella tricamerata n. gen., n. sp., is here described from the lower Cenomanian of the Monte Cairo area near Cassino (Southern Latium, Italy). The new taxon is characterized by an early stage with triloculine to quinqueloculine coiling, followed by one or two whorls, each consisting of three or more tubular, curved, flattened and undivided chambers, with depressed sutures; it is ascribed to the superfamily Milioloidea, but the inferred attribution to the family Hauerinidae remains uncertain. In the type-locality its occurrence is restricted to the back-edge facies of the Latium-Abruzzi carbonate platform represented by fossiliferous grain-supported limestone rich in Sellialveolina viallii Colalongo, 1963.
机译:一种新的有孔有孔虫,Cairoella tricamerata n。 gen。,n。在这里,是从Cassino(意大利南部南部)附近的蒙特开罗地区的下西诺曼期描述的。新的分类单元的特征是,早期有三氟喹啉到五氟喹啉的卷曲,随后是一个或两个螺轮,每个螺轮由三个或三个以上管状,弯曲,扁平和不分开的小室组成,缝合线凹陷;它归因于超家族Milioloidea,但尚不确定Hauerinidae家族的归属。在类型区域中,它的发生仅限于以富含Sellialveolina viallii Colalongo的化石颗粒支撑的石灰岩为代表的Latium-Abruzzi碳酸盐平台的后缘相,1963年。

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