Foraminifera taxon details

Endotebidae Vachard, Martini, Rettori & Zaninetti, 1994 †

1056297  (urn:lsid:marinespecies.org:taxname:1056297)

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marine, fresh, terrestrial
fossil only
Vachard, D.; Martini, R.; Rettori, R.; Zaninetti, L. (1994). New classification of Triassic Endothyroid Foraminifera. <em>Geobios.</em> 27: 543-557., available online at https://doi.org/10.1016/S0016-6995(94)80249-1 [details]  Available for editors  PDF available [request] 
Description Test free, planispirally coiled with small initial deviations; sometimes lately uncoiled. Profile of coiled part nautiloid...  
Description Test free, planispirally coiled with small initial deviations; sometimes lately uncoiled. Profile of coiled part nautiloid and compressed, with chambers chernyshinellid to endothyroid. Wall granular with carbonate or rarely siliceous agglutinate. Aperture simple basal in the coiled part, to areal to cribrate in the uncoiled part.
Occurrence: Rare in the Artinskian–Kungurian. Present from Middle Permian to Late Triassic, Paleotethyan (rare in Japan and Northern America).
(Vachard in Krainer et al. (2019), p. 54).  [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Endotebidae Vachard, Martini, Rettori & Zaninetti, 1994 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1056297 on 2024-04-20
Date
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2018-01-24 15:10:54Z
created
2018-02-05 15:14:38Z
changed

original description Vachard, D.; Martini, R.; Rettori, R.; Zaninetti, L. (1994). New classification of Triassic Endothyroid Foraminifera. <em>Geobios.</em> 27: 543-557., available online at https://doi.org/10.1016/S0016-6995(94)80249-1 [details]  Available for editors  PDF available [request] 
From editor or global species database
Description Test free, planispirally coiled with small initial deviations; sometimes lately uncoiled. Profile of coiled part nautiloid and compressed, with chambers chernyshinellid to endothyroid. Wall granular with carbonate or rarely siliceous agglutinate. Aperture simple basal in the coiled part, to areal to cribrate in the uncoiled part.
Occurrence: Rare in the Artinskian–Kungurian. Present from Middle Permian to Late Triassic, Paleotethyan (rare in Japan and Northern America).
(Vachard in Krainer et al. (2019), p. 54).  [details]