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Foraminifera taxon details

Nonionoidea Schultze, 1854

465849  (urn:lsid:marinespecies.org:taxname:465849)

accepted
Superfamily

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marine, brackish, fresh
Schultze, M. J. S. (1854). Über den Organismus der Polythalamien (Foraminiferen), nebst Bemerkungen über die Rhizopoden im allgemeinen. <em>Ingelmann, Leipzig.</em> 1-68., available online at https://books.google.pt/books?id=o7rk00_xueQC [details] 
Diagnosis Test enrolled and planispiral to slightly asymmetrical; wall perforate, commonly of hyaline oblique calcite and appearing...  
Diagnosis Test enrolled and planispiral to slightly asymmetrical; wall perforate, commonly of hyaline oblique calcite and appearing optically granular but rarely may be optically radial; aperture equatorial and interiomarginal, less commonly areal, a group of pores, a series of sutural openings, or a peripheral slitlike opening in each chamber that lies slightly to one side of the periphery. U. Cretaceous (Coniacian) to Holocene. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Nonionoidea Schultze, 1854. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=465849 on 2024-11-01
Date
action
by
2010-03-25 10:31:03Z
created
2013-03-08 14:25:27Z
changed

original description Schultze, M. J. S. (1854). Über den Organismus der Polythalamien (Foraminiferen), nebst Bemerkungen über die Rhizopoden im allgemeinen. <em>Ingelmann, Leipzig.</em> 1-68., available online at https://books.google.pt/books?id=o7rk00_xueQC [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  PDF available [request]
From editor or global species database
Diagnosis Test enrolled and planispiral to slightly asymmetrical; wall perforate, commonly of hyaline oblique calcite and appearing optically granular but rarely may be optically radial; aperture equatorial and interiomarginal, less commonly areal, a group of pores, a series of sutural openings, or a peripheral slitlike opening in each chamber that lies slightly to one side of the periphery. U. Cretaceous (Coniacian) to Holocene. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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