Foraminifera name details

Parafusulina cuniculata (Igo, 1967) †

734842  (urn:lsid:marinespecies.org:taxname:734842)

 unaccepted (Opinion of Vachard et al. (2000))
Species
marine, brackish, fresh, terrestrial
fossil only
(of Pseudofusulina cuniculata Igo, 1967 †) Igo, H. (1967). Permian fusulinids of Nyukawa, Central Japan. Part 3 Some fusulinids from the Upper Sote Formation and the Ozu Formation. <em>目白学園女子短期大学研究紀要 Mejiro Gakuen Women's Junior College memoir.</em> 4: 1-19.
page(s): pp. 8-9 pl. 6 fig. 1-6; note: Fide Leven and Campbell (1998), p. 153 [details] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Parafusulina cuniculata (Igo, 1967) †. Accessed at: http://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=734842 on 2025-05-16
Date
action
by
2013-07-15 12:47:30Z
created
2017-04-17 10:28:11Z
changed
2021-12-17 10:38:26Z
changed

original description (of Pseudofusulina cuniculata Igo, 1967 †) Igo, H. (1967). Permian fusulinids of Nyukawa, Central Japan. Part 3 Some fusulinids from the Upper Sote Formation and the Ozu Formation. <em>目白学園女子短期大学研究紀要 Mejiro Gakuen Women's Junior College memoir.</em> 4: 1-19.
page(s): pp. 8-9 pl. 6 fig. 1-6; note: Fide Leven and Campbell (1998), p. 153 [details] 

basis of record Hayward, B.W.; Tendal, O.S.; Carter, R.; Grenfell, H.R.; Morgans, H.E.G.; Scott, G.H.; Strong, C.P.; Hayward, J.J. (2012). Phylum Foraminifera: foraminifera, xenophyophores, in: Gordon, D.P. (Ed.) (2012). New Zealand inventory of biodiversity: 3. Kingdoms Bacteria, Protozoa, Chromista, Plantae, Fungi. pp. 242-287. [details] Available for editors  PDF available [request]

new combination reference Leven, E. J.; Campbell, H. J. (1998). Middle Permian (Murgabian) fusuline faunas, Torlesse Terrane, New Zealand. <em>New Zealand Journal of Geology and Geophysics.</em> 41(2): 149-156., available online at https://doi.org/10.1080/00288306.1998.9514799
page(s): p. 153 fig. 4E,F [details] 
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
   

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