Foraminifera taxon details

Sigmoilinitinae Łuczkowska, 1974

721087  (urn:lsid:marinespecies.org:taxname:721087)

accepted
Subfamily

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marine, fresh, terrestrial
recent + fossil
Łuczkowska, E. (1974). Miliolidae (Foraminiferida) from the Miocene of Poland Part II. Biostratigraphy, palaeoecology and systematics. <em>Acta Palaeontologica Polonica.</em> 19 (1): 3-176., available online at https://www.app.pan.pl/archive/published/app19/app19-003.pdf [details] Available for editors  PDF available [request]
Diagnosis Test with two chambers per whorl, early stage with chambers added in planes slightly less than 180¡ apart, the angle...  
Diagnosis Test with two chambers per whorl, early stage with chambers added in planes slightly less than 180¡ apart, the angle gradually increasing until chambers are added in a single plane, later stage may have more than two chambers per whorl. Eocene to Holocene. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Sigmoilinitinae Luczkowska, 1974. Accessed at: http://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721087 on 2025-07-05
Date
action
by
2013-03-07 13:23:50Z
created
2014-04-09 08:47:07Z
changed

original description Łuczkowska, E. (1974). Miliolidae (Foraminiferida) from the Miocene of Poland Part II. Biostratigraphy, palaeoecology and systematics. <em>Acta Palaeontologica Polonica.</em> 19 (1): 3-176., available online at https://www.app.pan.pl/archive/published/app19/app19-003.pdf [details] Available for editors  PDF available [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  PDF available [request]
From editor or global species database
Diagnosis Test with two chambers per whorl, early stage with chambers added in planes slightly less than 180¡ apart, the angle gradually increasing until chambers are added in a single plane, later stage may have more than two chambers per whorl. Eocene to Holocene. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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