WoRMS taxon details
Globorotalioidea Cushman, 1927
- Family Candeinidae Cushman, 1927
- Family Globorotaliidae Cushman, 1927
- Family Pulleniatinidae Cushman, 1927
marine, fresh, terrestrial
Cushman, J. A. (1927). An outline of a re-classification of the Foraminifera. <em>Contributions from the Cushman Laboratory for Foraminiferal Research.</em> 3(1): 1-105., available online at https://cushmanfoundation.allenpress.com/Portals/_default/files/pubarchive/cclfr/3cclfr1.pdf
page(s): p. 91; note: Introduced as family Globorotaliidae Cushman, 1927 [details] Available for editors
[request]
page(s): p. 91; note: Introduced as family Globorotaliidae Cushman, 1927 [details] Available for editors
[request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Globorotalioidea Cushman, 1927. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=465814 on 2025-04-05
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Nomenclature
original description
Cushman, J. A. (1927). An outline of a re-classification of the Foraminifera. <em>Contributions from the Cushman Laboratory for Foraminiferal Research.</em> 3(1): 1-105., available online at https://cushmanfoundation.allenpress.com/Portals/_default/files/pubarchive/cclfr/3cclfr1.pdf
page(s): p. 91; note: Introduced as family Globorotaliidae Cushman, 1927 [details] Available for editors [request]
page(s): p. 91; note: Introduced as family Globorotaliidae Cushman, 1927 [details] Available for editors
[request]Other
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]
[request]From editor or global species database
Diagnosis Test trochospiral, periphery rounded to carinate; wall finely lamellar, perforate, of optically radial calcite, with inner organic lining and a primary organic membrane calcified on both sides to produce a primary bilamellar structure, but with thicker outer calcite layers; surface smooth, nonspinose, but may be pustulose or pitted, inflational pustules most prominent in the apertural region, pits when present are bordered by ridges and have one or more large pores at the center; primary aperture interiomarginal and extraumbilical-umbilical, may be bordered by an imperforate lip; supplementary sutural apertures and bullae may occur, accompanied by infralaminal accessory apertures. L. Paleocene (L. Danian) to Holocene. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
