WoRMS taxon details

Baculogypsinoides Yabe & Hanzawa, 1930

527114  (urn:lsid:marinespecies.org:taxname:527114)

accepted
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marine, brackish, fresh, terrestrial
masculine
Yabe, H.; Hanzawa, S. (1930). Tertiary foraminiferous rocks of Taiwan (Formosa). <em>Science reports of the Tohoku Imperial University. 2nd series, Geology.</em> 14(1), 1-A32: 1-46., available online at http://hdl.handle.net/10097/30231
page(s): p. 43 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Baculogypsinoides Yabe & Hanzawa, 1930. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=527114 on 2024-04-23
Date
action
by
2010-09-25 05:43:40Z
created
2014-05-19 08:48:59Z
changed
2020-05-23 11:00:21Z
changed

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original description Yabe, H.; Hanzawa, S. (1930). Tertiary foraminiferous rocks of Taiwan (Formosa). <em>Science reports of the Tohoku Imperial University. 2nd series, Geology.</em> 14(1), 1-A32: 1-46., available online at http://hdl.handle.net/10097/30231
page(s): p. 43 [details]  Available for editors  PDF available [request] 

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] 
From editor or global species database
Diagnosis Test globular but the three or four large thick and protruding spines may give a triangular to tetrahedral appearance, early chambers of both generations in a low trochospiral coil, with pores in the spiral side and distinct canals in the umbilical side that connect to the anastomosing radial spine canals, spines arise from the earliest whorl of chambers and enlarge rapidly with test growth, postembryonic stage with numerous small chamberlets added on all sides as in Baculogypsina, the pillars projecting as pustules at the surface, intraseptal canals formed by addition of a septal flap from the new chambers; wall calcareous, compact, coarsely perforate; spiral chambers with single basal to areal aperture, later chambers with row of rounded pores adjacent to the suture and may also have areal openings. Holocene; Philippines; Okinawa. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]