Foraminifera taxon details
Quasiendothyroidea Reitlinger, 1961 nom. transl. Hance et al., 2011 †
marine, fresh, terrestrial
fossil only
Hance, L.; Hou, H.; Vachard, D. (2011). Upper Famennian to Visean foraminifers and some carbonate microproblematica from South China – Hunan, Guangxi and Guizhou . <em>Beijing Geological Publishing House: Beijing.</em> 1-359. [details] Available for editors 
[request]
Reitlinger, E. A. (1961). Некоторые вопросы систематики квазиэндотир - Some questions about the systematic of Quasiendothyridae. <em>Академия наук СССР Вопросы микропалеонтологии - Academy of Sciences USSR Questions of Micropaleontology.</em> 5: 31-68., available online at http://www.ginras.ru/library/pdf/05_1961_voprosy_mikropaleontologii.pdf [details] Available for editors [request]
[request] Reitlinger, E. A. (1961). Некоторые вопросы систематики квазиэндотир - Some questions about the systematic of Quasiendothyridae. <em>Академия наук СССР Вопросы микропалеонтологии - Academy of Sciences USSR Questions of Micropaleontology.</em> 5: 31-68., available online at http://www.ginras.ru/library/pdf/05_1961_voprosy_mikropaleontologii.pdf [details] Available for editors
[request]
Description Endothyroid to planispiral coiling, involute to seminvolute. Chambers numerous, quadratic, without sutures. Secondary...
Description Endothyroid to planispiral coiling, involute to seminvolute. Chambers numerous, quadratic, without sutures. Secondary deposits strong: crusts, pseudochomata, chomata. Aperture simple, terminal, basal.
Occurrence. Late early Famennian (DFZ3; uppermost marginifera Zone of conodonts) to latest Famennian (DFZ8; praesulcata Zone). Rarely mentioned in the lowermost sulcata Zone (earliest Tournaisian: Vachard 1988b; Kalvoda, 1990; Kulagina 2013); northern Palaeotethyan (from Belgium to NW Australia) and Uralian (including some terranes of Arctic Alaska, described by Mamet 1997). Two allochthonous localities are mentioned in Corsica (Krylatov & Mamet 1966) and central Iran (Bagheri & Stampfli 2008).
(Vachard and Le Coze (2022)). [details]
Occurrence. Late early Famennian (DFZ3; uppermost marginifera Zone of conodonts) to latest Famennian (DFZ8; praesulcata Zone). Rarely mentioned in the lowermost sulcata Zone (earliest Tournaisian: Vachard 1988b; Kalvoda, 1990; Kulagina 2013); northern Palaeotethyan (from Belgium to NW Australia) and Uralian (including some terranes of Arctic Alaska, described by Mamet 1997). Two allochthonous localities are mentioned in Corsica (Krylatov & Mamet 1966) and central Iran (Bagheri & Stampfli 2008).
(Vachard and Le Coze (2022)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Quasiendothyroidea Reitlinger, 1961 nom. transl. Hance et al., 2011 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1055714 on 2024-04-27
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original description
Hance, L.; Hou, H.; Vachard, D. (2011). Upper Famennian to Visean foraminifers and some carbonate microproblematica from South China – Hunan, Guangxi and Guizhou . <em>Beijing Geological Publishing House: Beijing.</em> 1-359. [details] Available for editors [request]
original description Reitlinger, E. A. (1961). Некоторые вопросы систематики квазиэндотир - Some questions about the systematic of Quasiendothyridae. <em>Академия наук СССР Вопросы микропалеонтологии - Academy of Sciences USSR Questions of Micropaleontology.</em> 5: 31-68., available online at http://www.ginras.ru/library/pdf/05_1961_voprosy_mikropaleontologii.pdf [details] Available for editors [request]
[request] original description Reitlinger, E. A. (1961). Некоторые вопросы систематики квазиэндотир - Some questions about the systematic of Quasiendothyridae. <em>Академия наук СССР Вопросы микропалеонтологии - Academy of Sciences USSR Questions of Micropaleontology.</em> 5: 31-68., available online at http://www.ginras.ru/library/pdf/05_1961_voprosy_mikropaleontologii.pdf [details] Available for editors
[request] From editor or global species database
Description Endothyroid to planispiral coiling, involute to seminvolute. Chambers numerous, quadratic, without sutures. Secondary deposits strong: crusts, pseudochomata, chomata. Aperture simple, terminal, basal.Occurrence. Late early Famennian (DFZ3; uppermost marginifera Zone of conodonts) to latest Famennian (DFZ8; praesulcata Zone). Rarely mentioned in the lowermost sulcata Zone (earliest Tournaisian: Vachard 1988b; Kalvoda, 1990; Kulagina 2013); northern Palaeotethyan (from Belgium to NW Australia) and Uralian (including some terranes of Arctic Alaska, described by Mamet 1997). Two allochthonous localities are mentioned in Corsica (Krylatov & Mamet 1966) and central Iran (Bagheri & Stampfli 2008).
(Vachard and Le Coze (2022)). [details]