Foraminifera taxon details
Olgaorlovella dublicata (Lipina, 1949) †
1255363 (urn:lsid:marinespecies.org:taxname:1255363)
accepted
Species
Glomospira dublicata Lipina, 1949 † · unaccepted (Opinion of Vachard, Krainer and...)
Opinion of Vachard, Krainer and Lucas (2015)
Pseudoagathammina dublicata (Lipina, 1949) † · unaccepted > superseded combination
marine, brackish, fresh, terrestrial
fossil only
(of Glomospira dublicata Lipina, 1949 †) Lipina, O. A. (1949). Мелкие фораминиферы погребенных массивов Башкирии (Smaller foraminifers from the buried massifs of Bashkiria). <em>Академия наук СССР Труды ИГН-Akademya Nauk SSSR Trudy Instituta Geologicheskikh Nauk.</em> v. 105, ser. geol. no. 35, p. 198-235 (in Russian; French translation BRGM, no. 791)., available online at http://www.ginras.ru/library/pdf/ign105_1949.pdf
page(s): p. 205, pl. 2, figs. 7, 9 (holotype fig. 7).; note: Specific epithet: probably "duplicata" (doubled) intended ("dublicata" does not exist in Latin). [details] Available for editors
[request]
page(s): p. 205, pl. 2, figs. 7, 9 (holotype fig. 7).; note: Specific epithet: probably "duplicata" (doubled) intended ("dublicata" does not exist in Latin). [details] Available for editors
[request]
Original description The shell is regularly coiled, large. The diameter of the test is 0.46-0.77 mm. The initial and late parts of the test are...
Original description The shell is regularly coiled, large. The diameter of the test is 0.46-0.77 mm. The initial and late parts of the test are constructed somewhat differently: in the first two to four whorls the tube is narrow and thin-walled, then there is a sharp thickening of the wall and an increase in the height of the whorl, and the last two to four whorls have a thick massive wall and higher whorls. The structure of the wall also often changes: from fine-grained in the initial whorls it changes to more coarse-grained in the last whorls. The number of whorls is 4-5, the height of the last whorl is 0.088-0.13 mm. The proloculus is quite large, its diameter is 0.075-0.11 mm. The wall thickness in the last whorl is 35-38 μ.
Comparison . The main characteristic feature of this species, which distinguishes it from those described above or described in the literature, is the sharp transition from the initial part of the shell to the late part and their different structure. This form differs from Glomospira regularis sp. nov. by the presence of the transition just mentioned and a different structure of the late part of the test (thick wall, relatively high, uncompressed whorls).
Locality. Yar-Bishkadak and Kusyapkulovo massifs. The form is common.
Age. Found only in the Schwagerina horizon.
Holotype. Specimen No. 25/3269, stored in the Museum of the IGS of the Academy of Sciences of the USSR.
(Lipina (1949)). [details]
Comparison . The main characteristic feature of this species, which distinguishes it from those described above or described in the literature, is the sharp transition from the initial part of the shell to the late part and their different structure. This form differs from Glomospira regularis sp. nov. by the presence of the transition just mentioned and a different structure of the late part of the test (thick wall, relatively high, uncompressed whorls).
Locality. Yar-Bishkadak and Kusyapkulovo massifs. The form is common.
Age. Found only in the Schwagerina horizon.
Holotype. Specimen No. 25/3269, stored in the Museum of the IGS of the Academy of Sciences of the USSR.
(Lipina (1949)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Olgaorlovella dublicata (Lipina, 1949) †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1255363 on 2026-01-09
Date
action
by
original description
(of Glomospira dublicata Lipina, 1949 †) Lipina, O. A. (1949). Мелкие фораминиферы погребенных массивов Башкирии (Smaller foraminifers from the buried massifs of Bashkiria). <em>Академия наук СССР Труды ИГН-Akademya Nauk SSSR Trudy Instituta Geologicheskikh Nauk.</em> v. 105, ser. geol. no. 35, p. 198-235 (in Russian; French translation BRGM, no. 791)., available online at http://www.ginras.ru/library/pdf/ign105_1949.pdf
page(s): p. 205, pl. 2, figs. 7, 9 (holotype fig. 7).; note: Specific epithet: probably "duplicata" (doubled) intended ("dublicata" does not exist in Latin). [details] Available for editors [request]
new combination reference 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> , available online at https://doi.org/10.26879/433 [details] Available for editors [request]
page(s): p. 205, pl. 2, figs. 7, 9 (holotype fig. 7).; note: Specific epithet: probably "duplicata" (doubled) intended ("dublicata" does not exist in Latin). [details] Available for editors
[request]new combination reference 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> , available online at https://doi.org/10.26879/433 [details] Available for editors
[request]From editor or global species database
Original description The shell is regularly coiled, large. The diameter of the test is 0.46-0.77 mm. The initial and late parts of the test are constructed somewhat differently: in the first two to four whorls the tube is narrow and thin-walled, then there is a sharp thickening of the wall and an increase in the height of the whorl, and the last two to four whorls have a thick massive wall and higher whorls. The structure of the wall also often changes: from fine-grained in the initial whorls it changes to more coarse-grained in the last whorls. The number of whorls is 4-5, the height of the last whorl is 0.088-0.13 mm. The proloculus is quite large, its diameter is 0.075-0.11 mm. The wall thickness in the last whorl is 35-38 μ. Comparison . The main characteristic feature of this species, which distinguishes it from those described above or described in the literature, is the sharp transition from the initial part of the shell to the late part and their different structure. This form differs from Glomospira regularis sp. nov. by the presence of the transition just mentioned and a different structure of the late part of the test (thick wall, relatively high, uncompressed whorls).
Locality. Yar-Bishkadak and Kusyapkulovo massifs. The form is common.
Age. Found only in the Schwagerina horizon.
Holotype. Specimen No. 25/3269, stored in the Museum of the IGS of the Academy of Sciences of the USSR.
(Lipina (1949)). [details]
From editor or global species database
Image from synonym