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IRMNG taxon details

Tubiphytidae Vachard, Krainer & Lucas 2012 †

11928479  (urn:lsid:irmng.org:taxname:11928479)

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marine, fresh, terrestrial
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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 [details]   
Taxonomic remark Vachard et al., 2012 referred their new family to Foraminifera, ?Class Miliolata (?= Tubothalamea in IRMNG), however...  
Taxonomic remark Vachard et al., 2012 referred their new family to Foraminifera, ?Class Miliolata (?= Tubothalamea in IRMNG), however Vachard et al., 2015 assign it to Kingdom indeterminate, Phylum indeterminate with the description: Microproblematica probably constituted by the weakly to strongly transformed consortial association of cyanobacterial algae and Miliolata foraminifers. The same authors write: "...concerning the assignment of Tubiphytes [:] The interpretation of Bernier (1984), Vachard et al. (2001), and Vachard and Krainer (2001b) is fundamentally different from that of Maslov (1956) and Senowbari-Daryan and Flügel (1993), because the former authors consider the internal cavity as an important part of the organism; i.e., inherited from an ancestral Miliolata foraminifer." According to Vachard & Le Coze, 2021, "Tubiphytids might be miliolate [foraminifer] and cyanobacterium consortia, derived from the nubeculariin Palaeonubecularia." Earlier, Riding & Guo, 1992 discussed the possible affinity of Tubiphytes as a cyanobacterium, hydrozoan, rhodophyte, poriferan, or foraminiferan and concluded that it is most likely a sponge. [details]
IRMNG (2023). Tubiphytidae Vachard, Krainer & Lucas 2012 †. Accessed at: https://www.irmng.org/aphia.php?p=taxdetails&id=11928479 on 2024-05-03
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2023-07-21 03:42:56Z
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2023-07-21 19:01:24Z
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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 [details]   

basis of record 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 [details]   

additional source 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
note: as ?Class Miliolata (?= Tubothalamea, requires confirmation) [details]   

additional source Vachard, D.; Le Coze, F. (2021). Carboniferous smaller Foraminifera: convergences and divergences. <em>Geological Society, London, Special Publications.</em> 512(1): 247-326., available online at https://doi.org/10.1144/sp512-2020-42 [details]   

taxonomy source Vachard, D.; Krainer, K.; Lucas, S. (2015). Late Early Permian (late Leonardian; Kungurian) algae, microproblematica, and smaller foraminifers from the Yeso Group and San Andres Formation (New Mexico; USA). <em>Palaeontologia Electronica.</em> 18(1): 1-77., available online at https://doi.org/10.26879/433
note: as Kingdom indeterminate, Phylum indeterminate; refer note for additional information [details]   

name verified source 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 [details]   

current name source 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 [details]   

extant flag source 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 [details]   

habitat flag source 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 [details]   
From other sources
Taxonomic remark Vachard et al., 2012 referred their new family to Foraminifera, ?Class Miliolata (?= Tubothalamea in IRMNG), however Vachard et al., 2015 assign it to Kingdom indeterminate, Phylum indeterminate with the description: Microproblematica probably constituted by the weakly to strongly transformed consortial association of cyanobacterial algae and Miliolata foraminifers. The same authors write: "...concerning the assignment of Tubiphytes [:] The interpretation of Bernier (1984), Vachard et al. (2001), and Vachard and Krainer (2001b) is fundamentally different from that of Maslov (1956) and Senowbari-Daryan and Flügel (1993), because the former authors consider the internal cavity as an important part of the organism; i.e., inherited from an ancestral Miliolata foraminifer." According to Vachard & Le Coze, 2021, "Tubiphytids might be miliolate [foraminifer] and cyanobacterium consortia, derived from the nubeculariin Palaeonubecularia." Earlier, Riding & Guo, 1992 discussed the possible affinity of Tubiphytes as a cyanobacterium, hydrozoan, rhodophyte, poriferan, or foraminiferan and concluded that it is most likely a sponge. [details]

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