original description
Cushman, J. A. (1910). A monograph of the Foraminifera of the North Pacific Ocean. Part I. Astrorhizidae and Lituolidae. <em>Bulletin of the United States National Museum.</em> 71(1): 1-134., available online at https://www.biodiversitylibrary.org/page/7878332
page(s): p. 108 [details]
basis of record
Gross, O. (2001). Foraminifera, <B><I>in</I></B>: Costello, M.J. <i>et al.</i> (Ed.) (2001). <i>European register of marine species: a check-list of the marine species in Europe and a bibliography of guides to their identification. Collection Patrimoines Naturels,</i> 50: pp. 60-75 (look up in IMIS) [details]
additional source
Neave, Sheffield Airey. (1939-1996). Nomenclator Zoologicus vol. 1-10 Online. <em>[Online Nomenclator Zoologicus at Checklistbank. Ubio link has gone].</em> , available online at https://www.checklistbank.org/dataset/126539/about [details]
additional source
Loeblich, A. R.; Tappan, H. (1987). Foraminiferal Genera and their Classification. Van Nostrand Reinhold Company, New York. 970pp., available online at https://books.google.pt/books?id=n_BqCQAAQBAJ [details] Available for editors [request]
redescription
Jones, R. W.; Bender, H.; Charnock, M. A.; Kaminski, M. A.; Whittaker, J. E. (1993). Emendation of the foraminiferal genus <i>Cribrostomoides</i> Cushman, 1910, and its taxonomic implications. <em>Journal of Micropalaeontology.</em> 12(2): 181-193., available online at https://doi.org/10.1144/jm.12.2.181 [details]
Present Inaccurate Introduced: alien Containing type locality
From editor or global species database
Diagnosis Test free, enrolled and involute, few chambers per whorl, early stage slightly streptospiral in growth, later becoming planispiral and symmetrical; wall agglutinated, thin, and simple in structure, surface smoothly finished; aperture equatorial, just above the base of the final chamber face, with a narrow lip of finer sand present on both margins, a simple slit in the early chambers, later becoming irregular with fine projections from both margins that may divide the primary aperture into a linear series of irregular to rounded openings near the base of the chamber face. Holocene; Atlantic and Pacific from 186 m to 4,738 m. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]Unreviewed
Habitat Known from seamounts and knolls [details]
From editor or global species database