WoRMS taxon details

Hoeglundina Brotzen, 1948

112169  (urn:lsid:marinespecies.org:taxname:112169)

accepted
Genus

Ordering

  • Alphabetically
  • By status

Children Display

marine, brackish, fresh, terrestrial
recent + fossil
feminine
Brotzen, F. (1948). The Swedish Paleocene and its Foraminiferal Fauna. <em>Årsbok Sveriges Geologiska Undersökning.</em> n° 493 t. 42(2): 1-140.
page(s): p. 92 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Hoeglundina Brotzen, 1948. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=112169 on 2024-04-25
Date
action
by
2004-12-21 15:54:05Z
created
2012-03-26 03:49:26Z
changed
2014-04-25 09:52:37Z
changed
2014-08-17 10:21:35Z
changed
2016-12-05 14:56:55Z
changed
2017-09-30 10:42:54Z
changed

Creative Commons License The webpage text is licensed under a Creative Commons Attribution 4.0 License


original description Brotzen, F. (1948). The Swedish Paleocene and its Foraminiferal Fauna. <em>Årsbok Sveriges Geologiska Undersökning.</em> n° 493 t. 42(2): 1-140.
page(s): p. 92 [details]  Available for editors  PDF available [request] 

basis of record Gross, O. (2001). Foraminifera, <B><I>in</I></B>: Costello, M.J. <i>et al.</i> (Ed.) (2001). <i>European register of marine species: a check-list of the marine species in Europe and a bibliography of guides to their identification. Collection Patrimoines Naturels,</i> 50: pp. 60-75 (look up in IMIS[details]   

additional source Loeblich, A. R.; Tappan, H. (1987). Foraminiferal Genera and their Classification. Van Nostrand Reinhold Company, New York. 970pp., available online at https://books.google.pt/books?id=n_BqCQAAQBAJ [details]  Available for editors  PDF available [request] 
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
From editor or global species database
Diagnosis Test trochospiral, close coiled, biconvex, chambers enlarging gradually, eight or nine in the final whorl, internal partition flat, earlier ones resorbed as new chambers are added so that only the final chamber contains an intact partition, sutures curved backward at the periphery on the spiral side, straight and oblique on the umbilical side, periphery subacute, carinate; wall calcareous, aragonitic, radial, lamellar, finely perforate, surface smooth; aperture lateromarginal and slitlike, parallel to the peripheral keel and opening on the umbilical side, those of earlier chambers commonly closed by shell material, may have a secondary interiomarginal aperture, intercameral foramen interiomarginal. Paleocene to Holocene; cosmopolitan. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]