Foraminifera name details

Rugososchwagerina kansasensis (Beede & Kniker, 1924) †

1514212  (urn:lsid:marinespecies.org:taxname:1514212)

 unaccepted
Species
marine, brackish, fresh, terrestrial
fossil only
(of Schwagerina kansasensis Beede & Kniker, 1924 †) Beede, J. W.; Kniker, H. T. (1924). Species of the genus Schwagerina and their stratigraphic significance. <em>Austin: Texas University Bulletin.</em> 2433: 1-100., available online at http://hdl.handle.net/2152/54040
page(s): p. 30 pl. 5 : 7 : 8 fig. 1-5 : 6 : 4 (holotype pl. 5 fig. 1).; note: 1. Axial section, type of species. Shows evenly and deeply- folded septa, minute initial chamber, and broad axial zone. X15. 2. Slightly excentric section. X 12.15. (The initial chamber . of this ...    
1. Axial section, type of species. Shows evenly and deeply- folded septa, minute initial chamber, and broad axial zone. X15. 2. Slightly excentric section. X 12.15. (The initial chamber . of this species· is so minute and the first volutions so closely wound that it is very difficult to get a true axial section.) 3. Slightly excentric section of specimen from the W olfcamp formation, Brewster County, Texas. X 12.5. (These specimens are heavily impregnated with iron.) 4. Axial section of specimen from same locality. X 11. 5. Part of axial section showing exceptionally well the very thin folded septa of the axial region. The septa of this species are nearly devoid of pores. One or two are shown in this figure. Neva limestone.
[details] Available for editors  PDF available [request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2021). World Foraminifera Database. Rugososchwagerina kansasensis (Beede & Kniker, 1924) †. Accessed at: https://www.marinespecies.org/foraminifera.../aphia.php?p=taxdetails&id=1514212 on 2025-05-22
Date
action
by
2021-06-07 16:37:18Z
created

original description (of Schwagerina kansasensis Beede & Kniker, 1924 †) Beede, J. W.; Kniker, H. T. (1924). Species of the genus Schwagerina and their stratigraphic significance. <em>Austin: Texas University Bulletin.</em> 2433: 1-100., available online at http://hdl.handle.net/2152/54040
page(s): p. 30 pl. 5 : 7 : 8 fig. 1-5 : 6 : 4 (holotype pl. 5 fig. 1).; note: 1. Axial section, type of species. Shows evenly and deeply- folded septa, minute initial chamber, and broad axial zone. X15. 2. Slightly excentric section. X 12.15. (The initial chamber . of this ...    
1. Axial section, type of species. Shows evenly and deeply- folded septa, minute initial chamber, and broad axial zone. X15. 2. Slightly excentric section. X 12.15. (The initial chamber . of this species· is so minute and the first volutions so closely wound that it is very difficult to get a true axial section.) 3. Slightly excentric section of specimen from the W olfcamp formation, Brewster County, Texas. X 12.5. (These specimens are heavily impregnated with iron.) 4. Axial section of specimen from same locality. X 11. 5. Part of axial section showing exceptionally well the very thin folded septa of the axial region. The septa of this species are nearly devoid of pores. One or two are shown in this figure. Neva limestone.
[details] Available for editors  PDF available [request]

new combination reference Kahler, F.; Kahler, G. (1966). Fusulinida (Foraminiferida): Teil 3. <em>Fossilium Catalogus: I: Animalia.</em> 113: 539-870. [details] Available for editors  PDF available [request]