Foraminifera taxon details

Eulepidina H. Douvillé, 1911 †

722308  (urn:lsid:marinespecies.org:taxname:722308)

accepted
Genus
Lepidocyclina (Eulepidina) H. Douvillé, 1911 † · unaccepted (Opinion of Douvillé (1917) Nomen...)  
Opinion of Douvillé (1917) Nomen translatum
Lepidocyclina (Trybliolepidina) Yabe & Hanzawa, 1929 † · unaccepted (Subjective junior synonym in...)  
Subjective junior synonym in opinion of Loeblich & Tappan, 1987 nom. transl.
Trybliolepidina van der Vlerk, 1928 † · unaccepted (Subjective junior synonym Opinion...)  
Subjective junior synonym Opinion of Loeblich & Tappan, 1987

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marine, brackish, fresh, terrestrial
fossil only
feminine
Douvillé, H. (1917). Sur l'âge des couches à Lépidocyclines de l'Aquitaine. <em>Compte Rendu des Séances de Ia Société Géologique de France.</em> 1917: 144-146.
page(s): p. 145; note: Nomen translatum. [details] 

(of Lepidocyclina (Eulepidina) H. Douvillé, 1911 †) Douvillé, H. (1911). Les foraminifères dans le Tertiaire des Philippines. <em>The Philippine Journal of Science, D.</em> 6(2): 53-80., available online at https://www.biodiversitylibrary.org/page/34354759
page(s): p. 59 [details] OpenAccess publication
Diagnosis Test discoidal, large bilocular megalospheric nucleoconch from 1 mm to 3 mm in diameter, small spherical to cuboidal...  
Diagnosis Test discoidal, large bilocular megalospheric nucleoconch from 1 mm to 3 mm in diameter, small spherical to cuboidal protoconch nearly or completely surrounded by larger deuteroconch, the two touching tangentially at the latter's roof and floor, both surrounded by a thick wall pierced by numerous stolons that lead to the equatorial auxiliary chambers and originate new spirals of equatorial chambers, stolons from the protoconch also connect with early lateral auxiliary chambers; microspheric test with very tiny protoconch and deuteroconch followed by four to six chambers with proximal stolons only, then by chambers with two stolons, each giving rise to two spirals, large spatulate equatorial chambers may appear hexagonal, lateral chambers low and irregular, rounded to polygonal, those of successive layers alternating and may occur in groups around imperforate pillars; wall calcareous, that of the median layer with multiple grooves and ridges associated with the stolons; cyclic stolons connect equatorial chambers of the same annulae, and two sets of stolons that cross connect to adjacent chambers of adjacent cycles, perforations in the floor and roof of equatorial chambers connect with adjoining lateral chambers that also have perforate roofs and floors and side walls with stolons. M. Oligocene (Rupelian) to L. Miocene (Aquitanian); North America; South America; Europe; Africa; Asia; Australia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Eulepidina H. Douvillé, 1911 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=722308 on 2025-05-28
Date
action
by
2013-03-08 13:53:47Z
created
2018-01-04 09:46:50Z
changed
2018-09-30 13:26:56Z
changed

original description Douvillé, H. (1917). Sur l'âge des couches à Lépidocyclines de l'Aquitaine. <em>Compte Rendu des Séances de Ia Société Géologique de France.</em> 1917: 144-146.
page(s): p. 145; note: Nomen translatum. [details] 

original description (of Lepidocyclina (Eulepidina) H. Douvillé, 1911 †) Douvillé, H. (1911). Les foraminifères dans le Tertiaire des Philippines. <em>The Philippine Journal of Science, D.</em> 6(2): 53-80., available online at https://www.biodiversitylibrary.org/page/34354759
page(s): p. 59 [details] OpenAccess publication

original description (of Trybliolepidina van der Vlerk, 1928 †) Vlerk, I. M. van der. (1928). Het genus Lepidocyclina in het Indo-Pacifische gebied. <em>Wetenschappelijke mededeelingen van de Dienst van den mijnbouw in Nederlandsch- Oost-Indië.</em> 8: 7-88.
page(s): p. 10, 13 [details] 

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 discoidal, large bilocular megalospheric nucleoconch from 1 mm to 3 mm in diameter, small spherical to cuboidal protoconch nearly or completely surrounded by larger deuteroconch, the two touching tangentially at the latter's roof and floor, both surrounded by a thick wall pierced by numerous stolons that lead to the equatorial auxiliary chambers and originate new spirals of equatorial chambers, stolons from the protoconch also connect with early lateral auxiliary chambers; microspheric test with very tiny protoconch and deuteroconch followed by four to six chambers with proximal stolons only, then by chambers with two stolons, each giving rise to two spirals, large spatulate equatorial chambers may appear hexagonal, lateral chambers low and irregular, rounded to polygonal, those of successive layers alternating and may occur in groups around imperforate pillars; wall calcareous, that of the median layer with multiple grooves and ridges associated with the stolons; cyclic stolons connect equatorial chambers of the same annulae, and two sets of stolons that cross connect to adjacent chambers of adjacent cycles, perforations in the floor and roof of equatorial chambers connect with adjoining lateral chambers that also have perforate roofs and floors and side walls with stolons. M. Oligocene (Rupelian) to L. Miocene (Aquitanian); North America; South America; Europe; Africa; Asia; Australia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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