Foraminifera taxon details

Pseudoendothyridae Mamet in Mamet et al., 1970 †

1059508  (urn:lsid:marinespecies.org:taxname:1059508)

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  1. Genus Pseudoendothyra Mikhailov, 1939 †
  2. Genus Kangvarella Saurin, 1962 † (uncertain > nomen dubium, Probably a Reitlingerina = Pseudoendothyra auct.)
marine, fresh, terrestrial
fossil only
Mamet, B., Mikhailoff, N., and Mortelmans G. (1970). La stratigraphie du Tournaisien et du Viséen inférieur de Landelies. Comparaison avec les coupes du Tournaisis et du bord nord du synclinal de Namur. <em>Mémoires de la Société belge de Géologie, de Paléontologie et d'Hydrologie.</em> série 8, 9: 1–81. [details]   
Description Tests lenticular or nautiloid, planispirally coiled with deviations in the primitive genera. Chomata weak to moderate,...  
Description Tests lenticular or nautiloid, planispirally coiled with deviations in the primitive genera. Chomata weak to moderate, generally in monticules. Wall differentiated with calcitic grains (luminotheca), false diaphanotheca or transformed in neosparite. Aperture terminal simple.
Occurrence: Late Visean-Early Permian; Paleotethyan and Uralian carbonate platforms.
(Kobayashi and Vachard (2022)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Pseudoendothyridae Mamet in Mamet et al., 1970 †. Accessed at: http://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1059508 on 2024-04-24
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2018-02-10 22:48:58Z
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original description Mamet, B., Mikhailoff, N., and Mortelmans G. (1970). La stratigraphie du Tournaisien et du Viséen inférieur de Landelies. Comparaison avec les coupes du Tournaisis et du bord nord du synclinal de Namur. <em>Mémoires de la Société belge de Géologie, de Paléontologie et d'Hydrologie.</em> série 8, 9: 1–81. [details]   
From editor or global species database
Description Tests lenticular or nautiloid, planispirally coiled with deviations in the primitive genera. Chomata weak to moderate, generally in monticules. Wall differentiated with calcitic grains (luminotheca), false diaphanotheca or transformed in neosparite. Aperture terminal simple.
Occurrence: Late Visean-Early Permian; Paleotethyan and Uralian carbonate platforms.
(Kobayashi and Vachard (2022)). [details]