Foraminifera taxon details

Triloculina garretti Howe, 1939 †

903998  (urn:lsid:marinespecies.org:taxname:903998)

accepted
Species
marine, brackish, fresh, terrestrial
fossil only
Howe, H. V. (1939). Louisiana Cook Mountain Eocene Foraminifera. <em>Bulletin of the Geological Sur­vey of Louisiana.</em> 14: 1-122. [details]   
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Triloculina garretti Howe, 1939 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=903998 on 2024-03-28
Date
action
by
2016-12-23 07:02:07Z
created

original description Howe, H. V. (1939). Louisiana Cook Mountain Eocene Foraminifera. <em>Bulletin of the Geological Sur­vey of Louisiana.</em> 14: 1-122. [details]   

basis of record Ellis, B. F.; Messina, A. (1940-2015). Catalogue of Foraminifera. <em>Micropaleontology Press, American Museum of Natural History, New York.</em>  [details]   

additional source Smith, L. E.; Sen Gupta, B. K. (2021). Henry V. Howe and his collection of Foraminifera at Louisiana State University. <em>Occasional Papers of the LSU Museum of Natural Science.</em> 91: 1-80., available online at https://sites01.lsu.edu/wp/mnspapers/files/2021/04/Occasional-Paper-91.pdf
note: Holotype, paratype or syntype [details]  Available for editors  PDF available [request] 
From editor or global species database
Holotype HVH 18, Eocene, Claiborne, Cook Mountain Fm.; “from Sample No. 1,” (JBG-18): “A bluff on the left bank of Sabine River, at Goodwin’s shoal, behind the house of Mr. S.J. Speight, near the southwest corner of sec. 31, T. 5 N., R. 12 W.,” Sabine Parish, Louisiana. “The locality is near the old site of Columbus and may be reached by taking an old wagon road 100 yards north of Mr. Speight’s house. This road leads in about 300 yards to the river bank. The locality is a low bluff, by the shoals, about 300 yards downstream, and exposes about eight feet of section from water level up. The section exposed is a marl with a one-foot compact lime bed near the middle.” This “sample came from 0–1 foot below the limestone ledge. The shoals are produced by slumping and the stratigraphic relations are greatly confused.” Collected by Julius B. Garrett in summer 1932. Figured: pl. 2, figs. 3–5. [details]