@article{oai:sucra.repo.nii.ac.jp:00012346,
 author = {松丸, 国照},
 issue = {4},
 journal = {Paleontological research},
 month = {Dec},
 note = {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., 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/, text, application/pdf},
 pages = {259--267},
 title = {A new Foraminifera from the upper Middle Eocene of the Ebro Basin,  Spain},
 volume = {3},
 year = {1999}
}