Foraminifera taxon details

Epimonella Vachard in Kolodka et al., 2012 †

1063145  (urn:lsid:marinespecies.org:taxname:1063145)

accepted
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marine, brackish, fresh, terrestrial
fossil only
Kolodka, C.; Vennin, E.; Vachard, D.; Trocme, V.; Goodarzi, M. H. (2012). Timing and progression of the end-Guadalupian crisis in the Fars province (Dalan Formation, Kuh-e Gakhum, Iran) constrained by foraminifers and other carbonate microfossils. <em>Facies.</em> 58(1)[January 2011 online]: 131-153., available online at https://doi.org/10.1007/s10347-011-0265-1
page(s): p. 146 [details] Available for editors  PDF available [request]
Original description Diagnosis: A representative of the Parathuramminida is characterized by elongate chambers and large pseudo- septa. The test...  
Original description Diagnosis: A representative of the Parathuramminida is characterized by elongate chambers and large pseudo- septa. The test is multilocular and uniserial and presents a planispiral to trochospiral coiling. The microgranular wall is dark colored and thin. The last chambers show the development of a proboscis-like terminated by a simple aperture, which is notable at each growth stage. Most of the specimens present spines on their last chamber (between 1 and 3).
Occurrence Epimonella is recorded in Northern England (Anderson 1964). Microproblematica sensu Tien (1979) was described in Late Midian series of Cambodia. Asche- monella sp. sensu Nestell and Nestell (2006) is present in the Capitanian of Texas.
Stratigraphic range: Wordian-Capitanian.
(Vachard in Kolodka et al. (2012)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Epimonella Vachard in Kolodka et al., 2012 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1063145 on 2026-04-16
Date
action
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2018-03-03 20:11:04Z
created
2019-09-15 17:45:45Z
changed

original description Kolodka, C.; Vennin, E.; Vachard, D.; Trocme, V.; Goodarzi, M. H. (2012). Timing and progression of the end-Guadalupian crisis in the Fars province (Dalan Formation, Kuh-e Gakhum, Iran) constrained by foraminifers and other carbonate microfossils. <em>Facies.</em> 58(1)[January 2011 online]: 131-153., available online at https://doi.org/10.1007/s10347-011-0265-1
page(s): p. 146 [details] Available for editors  PDF available [request]
From editor or global species database
Original description Diagnosis: A representative of the Parathuramminida is characterized by elongate chambers and large pseudo- septa. The test is multilocular and uniserial and presents a planispiral to trochospiral coiling. The microgranular wall is dark colored and thin. The last chambers show the development of a proboscis-like terminated by a simple aperture, which is notable at each growth stage. Most of the specimens present spines on their last chamber (between 1 and 3).
Occurrence Epimonella is recorded in Northern England (Anderson 1964). Microproblematica sensu Tien (1979) was described in Late Midian series of Cambodia. Asche- monella sp. sensu Nestell and Nestell (2006) is present in the Capitanian of Texas.
Stratigraphic range: Wordian-Capitanian.
(Vachard in Kolodka et al. (2012)). [details]
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