Foraminifera taxon details

Silicosigmoilina akkeshiensis Yoshida, 1963 †

1394359  (urn:lsid:marinespecies.org:taxname:1394359)

  1. Biota
  2. Chromista (Kingdom)
  3. Harosa (Subkingdom)
  4. Rhizaria (Infrakingdom)
  5. Foraminifera (Phylum)
  6. Tubothalamea (Class)
  7. Miliolida (Order)
  8. Miliamminidae (Family)
  9. Silicosigmoilina † (Genus)
  10. Silicosigmoilina akkeshiensis † (Species)
accepted
Species
Silicosigmoilina (Bramletteia) akkeshiensis Yoshida, 1963 † · unaccepted (Opinion of Beckmann in Bolli et...)  
Opinion of Beckmann in Bolli et al. (1994)
marine, fresh, terrestrial
fossil only
(of Silicosigmoilina (Bramletteia) akkeshiensis Yoshida, 1963 †) Yoshida, S. (1963). Upper Cretaceous Foraminifera from the Nemuro Group Eastern Hokkaido, Japan. <em>Journal of Hokkaido Gakugei University.</em> 13(2): 211-258., available online at http://s-ir.sap.hokkyodai.ac.jp/dspace/handle/123456789/5763
page(s): p. 223(64) pl. 5 fig. 1-2 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Silicosigmoilina akkeshiensis Yoshida, 1963 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1394359 on 2024-04-19
Date
action
by
2019-12-25 18:21:46Z
created
Le Coze, François

original description  (of Silicosigmoilina (Bramletteia) akkeshiensis Yoshida, 1963 †) Yoshida, S. (1963). Upper Cretaceous Foraminifera from the Nemuro Group Eastern Hokkaido, Japan. <em>Journal of Hokkaido Gakugei University.</em> 13(2): 211-258., available online at http://s-ir.sap.hokkyodai.ac.jp/dspace/handle/123456789/5763
page(s): p. 223(64) pl. 5 fig. 1-2 [details]  Available for editors  PDF available [request] 

new combination reference Beckmann, J. P. 1994. Late Albian to Early Eocene. In: Bolli, H.M.; Beckmann, J.P.; Saunders, J.B. (Editors), Benthic foraminiferal biostratigraphy of the south Caribbean Region, pp 47-228. Cambridge University Press.  [details]  Available for editors  PDF available [request] 

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