Foraminifera taxon details

Eoparafusulina linearis (Dunbar & Skinner, 1937) †

1507722  (urn:lsid:marinespecies.org:taxname:1507722)

accepted
Species
Eoparafusulina bispatulata (Williams, 1963) † · unaccepted > junior subjective synonym (Subjective junior synonym Opinion...)  
Subjective junior synonym Opinion of Read and Nestell (2019)
Monodiexodina bispatulata Williams, 1963 † · unaccepted > superseded combination (Opinion of Ueno (2006))
Monodiexodina linearis (Dunbar & Skinner, 1937) † · unaccepted (Opinion of Ueno (2006))
Parafusulina linearis (Dunbar & Skinner, 1937) † · unaccepted > superseded combination
Schwagerina linearis Dunbar & Skinner, 1937 † · unaccepted (Opinion of Ross (1962))
marine, brackish, fresh, terrestrial
fossil only
(of Schwagerina linearis Dunbar & Skinner, 1937 †) Dunbar, C. O.; Skinner, J. W. (1937). Permian Fusulinidae of Texas; in The geology of Texas. <em>Texas University Bulletin.</em> 3701 v.3(2): 517-825., available online at http://hdl.handle.net/2152/24042
page(s): p. 637, pl. 62, 12-15, pl. 63, figs. 1-7.; note: 12. Two immature cotypes, natural size. V.P.M. 14959. 13,14. Same enlarged (X 5). Hueco limestone in the south wall of Victorio Canyon, Sierra Diablo (Loc. 101). 15. Axial section of adult cotype, ...    
12. Two immature cotypes, natural size. V.P.M. 14959. 13,14. Same enlarged (X 5). Hueco limestone in the south wall of Victorio Canyon, Sierra Diablo (Loc. 101). 15. Axial section of adult cotype, showing the typical axial filling (X 10). V.P.M. 14967. Upper part of Wolfcamp formation, westernmost outcrop on Leonard Mountain, Glass Mountains, Texas (Loc. 18). 1,4,5. Axial sections of cotypes (X 10). V.P.M. 14960, 14965, and 14965. 2, 3. Sagittal sections (X 10). The outer whorls appear opaque because filled withmuddy matrix. V.P.M. 14966. 6. Juvenile, axial section, showing the beginning of axial depo- sition at an early stage. 7. A tangential slice, showing the septal fluting in plan. Near the middle, the slice cuts close to the base of the whorl where the tips of opposed septal folds meet to form rounded chamberlets; farther to the right and left the sec- tion rises toward the roof of the whorl, and here the septa appear widely spaced and nearly straight. V.P.M. 14964. Specimens 1 and 4 from the Hueco limestone in the south wall of Victorio Canyon, Sierra Diablo (Loc. 101) ;2, 3, and 8 are from the upper Wolfcamp 2,5 miles N. 35° E. of Hess ranch (Loc. 16) ;and 5, 6, and 7 are from the upper Wolfcamp in the westernmost outcrop on Leonard Moun- tain, Glass Mountains, Texas (Loc. 18).
[details] Available for editors  PDF available [request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Eoparafusulina linearis (Dunbar & Skinner, 1937) †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1507722 on 2025-05-19
Date
action
by
2021-04-27 15:49:21Z
created

original description (of Monodiexodina bispatulata Williams, 1963 †) Williams, T. E. (1963). Fusulinidae of the Hueco group (Lower Permian) Hueco Mountains, Texas. <em>Bulletin of the Peabody Museum of Natural History.</em> 18: 1-122., available online at http://peabody.yale.edu/sites/default/files/documents/scientific-publications/ypmB18_1963.pdf
page(s): p. 33, pl. 1, figs. 1-5 (holotype fig. 1). [details] Available for editors  PDF available [request]

original description (of Schwagerina linearis Dunbar & Skinner, 1937 †) Dunbar, C. O.; Skinner, J. W. (1937). Permian Fusulinidae of Texas; in The geology of Texas. <em>Texas University Bulletin.</em> 3701 v.3(2): 517-825., available online at http://hdl.handle.net/2152/24042
page(s): p. 637, pl. 62, 12-15, pl. 63, figs. 1-7.; note: 12. Two immature cotypes, natural size. V.P.M. 14959. 13,14. Same enlarged (X 5). Hueco limestone in the south wall of Victorio Canyon, Sierra Diablo (Loc. 101). 15. Axial section of adult cotype, ...    
12. Two immature cotypes, natural size. V.P.M. 14959. 13,14. Same enlarged (X 5). Hueco limestone in the south wall of Victorio Canyon, Sierra Diablo (Loc. 101). 15. Axial section of adult cotype, showing the typical axial filling (X 10). V.P.M. 14967. Upper part of Wolfcamp formation, westernmost outcrop on Leonard Mountain, Glass Mountains, Texas (Loc. 18). 1,4,5. Axial sections of cotypes (X 10). V.P.M. 14960, 14965, and 14965. 2, 3. Sagittal sections (X 10). The outer whorls appear opaque because filled withmuddy matrix. V.P.M. 14966. 6. Juvenile, axial section, showing the beginning of axial depo- sition at an early stage. 7. A tangential slice, showing the septal fluting in plan. Near the middle, the slice cuts close to the base of the whorl where the tips of opposed septal folds meet to form rounded chamberlets; farther to the right and left the sec- tion rises toward the roof of the whorl, and here the septa appear widely spaced and nearly straight. V.P.M. 14964. Specimens 1 and 4 from the Hueco limestone in the south wall of Victorio Canyon, Sierra Diablo (Loc. 101) ;2, 3, and 8 are from the upper Wolfcamp 2,5 miles N. 35° E. of Hess ranch (Loc. 16) ;and 5, 6, and 7 are from the upper Wolfcamp in the westernmost outcrop on Leonard Moun- tain, Glass Mountains, Texas (Loc. 18).
[details] Available for editors  PDF available [request]

new combination reference Ueno, K. (2006). The Permian antitropical fusulinoidean genus Monodiexodina: Distribution, taxonomy, paleobiogeography and paleoecology. <em>Journal of Asian Earth Sciences.</em> 26(3-4): 380-404., available online at https://doi.org/10.1016/j.jseaes.2005.07.003 [details] Available for editors  PDF available [request]
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