Foraminifera taxon details

Latitubiphytes Vachard, Krainer & S.G.Lucas, 2012 †

1719570  (urn:lsid:marinespecies.org:taxname:1719570)

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marine, fresh, terrestrial
fossil only
feminine
Vachard, D.; Krainer, K.; Lucas, S. G. (2012). Pennsylvanian (Late Carboniferous) calcareous microfossils from Cedro Peak (New Mexico, USA). Part 1: Algae and Microproblematica. <em>Annales de Paléontologie.</em> 98(4): 225-252., available online at https://doi.org/10.1016/j.annpal.2012.06.003
page(s): p. 246 [details] Available for editors  PDF available [request]
Description Description: Tubiphytid thick-walled and with a large, undivided chamber Wall dark, microgranular or porcelaneous. Aperture...  
Description Description: Tubiphytid thick-walled and with a large, undivided chamber Wall dark, microgranular or porcelaneous. Aperture inconspicuous.
Occurrence: Late Pennsylvanian–early Permian of Turkey, Urals (Russia), Spain and Carnic Alps (Vachard et al , 2012) Missourian–Wolfcampian of New Mexico (Krainer et al , 2017a) Sakmarian of Greece (Vachard et al ,1993b).
(Krainer et al. (2019)). [details]

Original description Diagnosis. Groups of tubular chambers thick-walled. Proloculus and/or juvenaria not known. Wall difficult to define, black,...  
Original description Diagnosis. Groups of tubular chambers thick-walled. Proloculus and/or juvenaria not known. Wall difficult to define, black, not porcelaneous, not microgranular. Aperture probably simple at the end of tube or absent because already resorbed.
Occurrence. Earliest Kasimovian (or latest Moscovian) to Early Permian in Russia. In New Mexico, Latitubiphytes n. gen. appears at the base of the Missourian dated by Eowaeringella in the Big Hatchet Mountains (Vachard et al., unpublished data, pl. 15, figs. 3–6, 8), and remains present up to the Early Permian of the Hueco Group (Krainer et al., 2005). True Tubiphytes are numerous since the earliest Wolfcampian (Krainer et al., 2009, Plate 3, fig. 3).
(Vachard et al. (2012)). [details]
Foraminifera (2025). Latitubiphytes Vachard, Krainer & S.G.Lucas, 2012 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1719570 on 2026-04-19
Date
action
by
2023-11-22 10:16:45Z
created
2023-11-22 13:51:44Z
changed
2024-02-19 07:00:29Z
changed
2024-04-02 11:25:51Z
changed
2024-04-02 14:30:53Z
changed

original description Vachard, D.; Krainer, K.; Lucas, S. G. (2012). Pennsylvanian (Late Carboniferous) calcareous microfossils from Cedro Peak (New Mexico, USA). Part 1: Algae and Microproblematica. <em>Annales de Paléontologie.</em> 98(4): 225-252., available online at https://doi.org/10.1016/j.annpal.2012.06.003
page(s): p. 246 [details] Available for editors  PDF available [request]
From editor or global species database
Description Description: Tubiphytid thick-walled and with a large, undivided chamber Wall dark, microgranular or porcelaneous. Aperture inconspicuous.
Occurrence: Late Pennsylvanian–early Permian of Turkey, Urals (Russia), Spain and Carnic Alps (Vachard et al , 2012) Missourian–Wolfcampian of New Mexico (Krainer et al , 2017a) Sakmarian of Greece (Vachard et al ,1993b).
(Krainer et al. (2019)). [details]

Original description Diagnosis. Groups of tubular chambers thick-walled. Proloculus and/or juvenaria not known. Wall difficult to define, black, not porcelaneous, not microgranular. Aperture probably simple at the end of tube or absent because already resorbed.
Occurrence. Earliest Kasimovian (or latest Moscovian) to Early Permian in Russia. In New Mexico, Latitubiphytes n. gen. appears at the base of the Missourian dated by Eowaeringella in the Big Hatchet Mountains (Vachard et al., unpublished data, pl. 15, figs. 3–6, 8), and remains present up to the Early Permian of the Hueco Group (Krainer et al., 2005). True Tubiphytes are numerous since the earliest Wolfcampian (Krainer et al., 2009, Plate 3, fig. 3).
(Vachard et al. (2012)). [details]
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