Foraminifera taxon details

Neodiscidae Lin, 1984 †

1052862  (urn:lsid:marinespecies.org:taxname:1052862)

accepted
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marine, fresh, terrestrial
fossil only
Gaillot, J.; Vachard, D. (2007). The Khuff Formation (Middle East) and time-equivalents in Turkey and South China: biostratigraphy from Capitanian to Changhsingian times (Permian), new foraminiferal taxa, and palaeogeographical implications. <em>Coloquios de Paleontologia.</em> 57: 37-223., available online at https://hal.archives-ouvertes.fr/hal-00310245
page(s): p. 94; note: Nomen translatum [details]  Available for editors  PDF available [request] 

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. 139; note: As "Neodiscinae". [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Neodiscidae Lin, 1984 †. Accessed at: http://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1052862 on 2024-04-21
Date
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2017-12-29 10:10:26Z
created

original description Gaillot, J.; Vachard, D. (2007). The Khuff Formation (Middle East) and time-equivalents in Turkey and South China: biostratigraphy from Capitanian to Changhsingian times (Permian), new foraminiferal taxa, and palaeogeographical implications. <em>Coloquios de Paleontologia.</em> 57: 37-223., available online at https://hal.archives-ouvertes.fr/hal-00310245
page(s): p. 94; note: Nomen translatum [details]  Available for editors  PDF available [request] 

original description 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. 139; note: As "Neodiscinae". [details]  Available for editors  PDF available [request] 

taxonomy source 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] 
From editor or global species database
Diagnosis Gaillot and Vachard (2007, p. 94): "Large Miliolida test composed of a spherical proloculus followed by an undivided tubular chamber, with a thick wall, diversely coiled but generally composed of an early glomospiroid stage followed by a planispiral stage, evolute or semi-evolute diversely coiled: entirely glomospiral (Crassiglomella gen.nov.), initially glomospiral and then planispiral (or aligned) involute (Neodiscus emend.), glomospiral becoming planispiral evolute or seminvolute (Graecodiscus emend. herein including Hemigordius magnus RAUZER-CHERNOUSOVA in AKOPIAN, 1974 and Neodiscus mirabilis UENO, 1992), planispirally involute compressed (“Arenovidalina” sensu BARYSHNIKOV, ZOLOTOVA & KOSHELEVA, 1982 non HO, 1959) or inflated (Multidiscus s.s., if slightly deviated at the beginning: Neohemigordius WANG & SUN, 1973), agathamminoid, i.e., quinqueloculine (Septagathammina). The chamber is semicircular in section (some flosculinisations are observable in advanced forms of Neodiscopsis gen. nov., see below), the thick wall is reinforced by buttresses at the contact with the preceding whorl. Aperture terminal simple.
?Sakmarian, ?Artinskian-Lopingian with a late Changhsingian acme. Palaeotethys from Greece to southern China; Neotethys: Taurids (Turkey), Zagros (southern Iran), Oman (Batain Plain)." [details]