Foraminifera taxon details
Pseudohemigordius Nestell & Nestell, 2006 †
1057099 (urn:lsid:marinespecies.org:taxname:1057099)
accepted
Genus
Pseudohemigordius incredibilis Nestell & Nestell, 2006 † (type by original designation)
marine, brackish, fresh, terrestrial
fossil only
masculine
Nestell, G. P.; Nestell, M. K. (2006). Middle Permian (Late Guadalupian) foraminifers from Dark Canyon, Guadalupe Mountains, New Mexico. <em>Micropaleontology.</em> 52(1): 1-50., available online at https://doi.org/10.2113/gsmicropal.52.1.1
page(s): p. 8 [details] Available for editors
[request]
page(s): p. 8 [details] Available for editors
[request]
Original description Description: Test is free, bichambered, with pseudotubular sec- ond chamber, from lens-shaped to low conical, initial part...
Original description Description: Test is free, bichambered, with pseudotubular sec- ond chamber, from lens-shaped to low conical, initial part is pseudoinvolute, one-two last volutions are evolute. Initially the second chamber forms one-two planispiral volutions, with sub- sequent volutions displaced relative to first volutions at small angle, and then the coiling becomes low trochospiral. Wall is calcareous, single layered, microgranular.
Occurrence: USA, New Mexico, Guadalupe Mountains, Dark Canyon, the Amoco #1 core, Tansill Formation, and the Amoco #2 core, upper part of the Yates and lower and middle part of the Tansill formations; Middle Permian (Capitanian); Poland, Galenzice, Core Holes no. 2 and 6; lower Zechstein, the Ammodiscus Zone.
Range: Middle Permian (Capitanian).
(Nestell and Nestell (2006)). [details]
Occurrence: USA, New Mexico, Guadalupe Mountains, Dark Canyon, the Amoco #1 core, Tansill Formation, and the Amoco #2 core, upper part of the Yates and lower and middle part of the Tansill formations; Middle Permian (Capitanian); Poland, Galenzice, Core Holes no. 2 and 6; lower Zechstein, the Ammodiscus Zone.
Range: Middle Permian (Capitanian).
(Nestell and Nestell (2006)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Pseudohemigordius Nestell & Nestell, 2006 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1057099 on 2026-03-06
Date
action
by
original description
Nestell, G. P.; Nestell, M. K. (2006). Middle Permian (Late Guadalupian) foraminifers from Dark Canyon, Guadalupe Mountains, New Mexico. <em>Micropaleontology.</em> 52(1): 1-50., available online at https://doi.org/10.2113/gsmicropal.52.1.1
page(s): p. 8 [details] Available for editors [request]
page(s): p. 8 [details] Available for editors
[request]From editor or global species database
Original description Description: Test is free, bichambered, with pseudotubular sec- ond chamber, from lens-shaped to low conical, initial part is pseudoinvolute, one-two last volutions are evolute. Initially the second chamber forms one-two planispiral volutions, with sub- sequent volutions displaced relative to first volutions at small angle, and then the coiling becomes low trochospiral. Wall is calcareous, single layered, microgranular.Occurrence: USA, New Mexico, Guadalupe Mountains, Dark Canyon, the Amoco #1 core, Tansill Formation, and the Amoco #2 core, upper part of the Yates and lower and middle part of the Tansill formations; Middle Permian (Capitanian); Poland, Galenzice, Core Holes no. 2 and 6; lower Zechstein, the Ammodiscus Zone.
Range: Middle Permian (Capitanian).
(Nestell and Nestell (2006)). [details]
From editor or global species database
Image from typetaxon