Foraminifera taxon details

Multidiscella angulata (Lin, 1984) †

1729406  (urn:lsid:marinespecies.org:taxname:1729406)

  1. Biota
  2. Chromista (Kingdom)
  3. Harosa (Subkingdom)
  4. Rhizaria (Infrakingdom)
  5. Foraminifera (Phylum)
  6. Tubothalamea (Class)
  7. Miliolida (Order)
  8. Miliolina (Suborder)
  9. Cornuspiroidea (Superfamily)
  10. Neodiscidae † (Family)
  11. Multidiscinae † (Subfamily)
  12. Multidiscella † (Genus)
  13. Multidiscella angulata † (Species)
accepted
Species
Arenovidalina angulata (Lin, 1984) † · unaccepted > superseded combination (Opinion of Vachard and Krainer (2022))
Multidiscus angulatus Lin, 1984 † · unaccepted > superseded combination (Opinion of Gaillot and Vachard (2007))
marine
fossil only
(of Multidiscus angulatus Lin, 1984 †) Lin, J. X. (1984). Protozoa. In Yichan Institute of Geology and Mineral Resources (ed.), Biostratigraphy of the Yangtze Gorge area chiefly, (3) Late Paleozoic era. <em>Museum Changzhou, Changzhou City, Jiangsu Province, Geological Publishing House, Beijing.</em> 110–177 (In Chinese), 323–364 (In English).
page(s): p. 140, pl. 6, figs. 25-26. [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Multidiscella angulata (Lin, 1984) †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1729406 on 2024-05-01
Date
action
by
2024-01-15 15:53:47Z
created
Le Coze, François

original description  (of Multidiscus angulatus Lin, 1984 †) Lin, J. X. (1984). Protozoa. In Yichan Institute of Geology and Mineral Resources (ed.), Biostratigraphy of the Yangtze Gorge area chiefly, (3) Late Paleozoic era. <em>Museum Changzhou, Changzhou City, Jiangsu Province, Geological Publishing House, Beijing.</em> 110–177 (In Chinese), 323–364 (In English).
page(s): p. 140, pl. 6, figs. 25-26. [details]  Available for editors  PDF available [request] 

new combination reference Vachard, D.; Krainer, K. (2022). Calcareous algae and foraminifers across the Permian-Triassic boundary interval (uppermost Bellerophon Formation and basal Werfen Formation) in the Dolomites (South Tyrol – Trentino, Italy). <em>Palaeontographica Abteilung A.</em> 324(1-6): 1-173., available online at https://doi.org/10.1127/pala/2022/0128 [details]  Available for editors  PDF available [request] 

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