Foraminifera taxon details
Buccicrenatinae Loeblich & Tappan, 1985 †
721102 (urn:lsid:marinespecies.org:taxname:721102)
accepted
Subfamily
marine, fresh, terrestrial
fossil only
Loeblich, A. R.; Tappan, H. (1985). Some new and redefined genera and families of agglutinated foraminifera; I. <em>The Journal of Foraminiferal Research.</em> 15(2): 91-104., available online at https://doi.org/10.2113/gsjfr.15.2.91
page(s): p. 98 [details] Available for editors
[request]
page(s): p. 98 [details] Available for editors
[request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Buccicrenatinae Loeblich & Tappan, 1985 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721102 on 2024-04-25
Date
action
by
original description
Loeblich, A. R.; Tappan, H. (1985). Some new and redefined genera and families of agglutinated foraminifera; I. <em>The Journal of Foraminiferal Research.</em> 15(2): 91-104., available online at https://doi.org/10.2113/gsjfr.15.2.91
page(s): p. 98 [details] Available for editors [request]
basis of record 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]
page(s): p. 98 [details] Available for editors
[request] basis of record 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] From editor or global species database
Diagnosis Test planispiral with few chambers per whorl, later may uncoil; wall agglutinated, earliest whorls may have solid wall and septa, later with thin but distinctly alveolar wall with coarse alveoles of nearly circular section, chamber cavity open, apertural face solid and nonalveolar below the slitlike opening, base of the septa thickened against the previous whorl and may form a continuous imperforate basal layer, with solid triangular chomatalike mounds against the previous whorl at the position of the septa; aperture areal, ranging from just above the base of the apertural face to terminal, an elongate straight to zig-zag slit in the plane of coiling. U. Jurassic (U. Oxfordian) to U. Cretaceous (Cenomanian). (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]