A new Foraminifera from the upper Middle Eocene of the Ebro Basin, Spain

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概要

• 論文の詳細を見る

• rights: 日本古生物学会rights: 本文データは学協会の許諾に基づきCiNiiから複製したものであるrelation: IsVersionOf: http://ci.nii.ac.jp/naid/110002695217/Serraia cataloniensis gen. et sp. nov. is differentiated from other pellatispiracean Foraminifera by the presence of one or more intercalary whorls of median chambers winding in the same direction as the primary whorl, and by frequent protoconchal and deureroconchal diverticula and a short spire of chambers around the deuteroconch. S. cataloniensis is described from the La Tossa Formation of the Bartonian regressive cycle of sedimentation in the Ebro Basin, Barcelona region, Spain.

• 日本古生物学会の論文
• 1999-12-30

著者

• Matsumaru K

  Saitama Univ. Urawa Jpn

• MATSUMARU KUNITERU

  Department of Geology, Faculty of Education, Saitama University Urawa

• Matsumaru Kuniteru

  Department Of Geology Faculty Of Education Saitama University

関連論文

• Late Oligocene larger foraminifera from the Komahashi-Daini Seamount, Kyushu-Palau Ridge and their tectonic significance
• 高知県足摺岬の清水累層から産する初期中新世(アキタニアン期)大型有孔虫〔英文〕
• Element profiles and Ir concentration of Cretaceous-Tertiary (K-T) boundary layers at Medetli, Golpazari, northwestern Turkey
• A new Foraminifera from the upper Middle Eocene of the Ebro Basin, Spain

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