Foraminifera name details

Chernobaculites Conil & Lys, 1977 †

721663  (urn:lsid:marinespecies.org:taxname:721663)

 unaccepted (Subjective junior synonym Opinion of Hance, Hou and Vachard (2011))
Genus

Ordering

  • Alphabetically
  • By status

Children Display

  1. Species Chernobaculites beschevensis (Brazhnikova, 1967) † accepted as Haplophragmina sarbaica subsp. beschevensis (Brazhnikova, 1967) † accepted as Haplophragmina beschevensis (Brazhnikova, 1967) † (unaccepted > superseded combination, Opinion of Hance, Hou and Vachard (2011))
marine, brackish, fresh, terrestrial
fossil only
masculine
Conil, R.; Lys, M. (1977). Les transgressions dinantiennes et leur influence sur la dispersion et l'évolution des foraminifères. <em>Mémoires de l'Institut géologique de l'Université de Louvain.</em> 29: 9-52.
page(s): p. 32 [details]   
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Chernobaculites Conil & Lys, 1977 †. Accessed at: http://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721663 on 2024-04-26
Date
action
by
2013-03-08 13:53:47Z
created
2017-12-07 10:48:17Z
changed
2018-01-25 10:18:05Z
changed
2018-10-19 14:34:15Z
changed

original description Conil, R.; Lys, M. (1977). Les transgressions dinantiennes et leur influence sur la dispersion et l'évolution des foraminifères. <em>Mémoires de l'Institut géologique de l'Université de Louvain.</em> 29: 9-52.
page(s): p. 32 [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 Early stage streptospirally coiled, later planispiral and finally uncoiled and rectilinear, chambers of the enrolled portion chernyshinelline in appearance, rectilinear portion with straight and horizontal septa; wall calcareous, microgranular, with differentiated thick outer agglutinated layer and thin, microgranular inner layer; aperture simple, basal, at the end of the teardrop chambers, becoming terminal in the rectilinear stage. U. Carboniferous (Namurian); USSR; Europe: Pyrenees. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]