Foraminifera taxon details

Triasininae Loeblich & Tappan, 1986 †

721150  (urn:lsid:marinespecies.org:taxname:721150)

  1. Biota
  2. Chromista (Kingdom)
  3. Harosa (Subkingdom)
  4. Rhizaria (Infrakingdom)
  5. Foraminifera (Phylum)
  6. Foraminifera incertae sedis (Class)
  7. Involutinida † (Order)
  8. Involutinidae † (Family)
  9. Triasininae † (Subfamily)
accepted
Subfamily

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marine, fresh, terrestrial
fossil only
Loeblich, A. R.; Tappan, H. (1986). Some new and redefined genera and families of Textulariina, Fusulinina, Involutinina and Miliolina (Foraminiferida). <em>The Journal of Foraminiferal Research.</em> 16(4): 334-346., available online at https://doi.org/10.2113/gsjfr.16.4.334
page(s): p. 343 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Triasininae Loeblich & Tappan, 1986 †. Accessed at: https://www.marinespecies.org/Foraminifera/aphia.php?p=taxdetails&id=721150 on 2024-04-23
Date
action
by
2013-03-07 13:23:50Z
created
Hayward, Bruce W.
2017-12-15 15:23:50Z
changed
Le Coze, François

original description Loeblich, A. R.; Tappan, H. (1986). Some new and redefined genera and families of Textulariina, Fusulinina, Involutinina and Miliolina (Foraminiferida). <em>The Journal of Foraminiferal Research.</em> 16(4): 334-346., available online at https://doi.org/10.2113/gsjfr.16.4.334
page(s): p. 343 [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 proloculus and broad and low, undivided, planispirally enrolled and involute second chamber, interior with numerous short cylindrical pillars extending from the chamber floor to the roof; wall calcareous, commonly recrystallized and probably originally aragonitic, secondary thickening may be present in the umbilical region. M. Triassic (Ladinian) to U. Triassic (Rhaetian). (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]

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