Foraminifera taxon details

Yaberinella Vaughan, 1928 †

722038  (urn:lsid:marinespecies.org:taxname:722038)

accepted
Genus
Yaberinella jamaicensis Vaughan, 1928 † (type by original designation)

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marine, brackish, fresh, terrestrial
fossil only
feminine
Vaughan, T. W. (1928). Yaberinella jamaicensis, a new genus and species of arenaceous Foraminifera. <em>Journal of Paleontology.</em> 2: 7-12.
page(s): p. 8 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Yaberinella Vaughan, 1928 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=722038 on 2024-04-19
Date
action
by
2013-03-08 13:53:47Z
created
2017-12-18 14:39:52Z
changed
2019-12-03 11:48:34Z
changed

original description Vaughan, T. W. (1928). Yaberinella jamaicensis, a new genus and species of arenaceous Foraminifera. <em>Journal of Paleontology.</em> 2: 7-12.
page(s): p. 8 [details]  Available for editors  PDF available [request] 

basis of record 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] 

additional source Hottinger, L. (1969), The foraminiferal genus Yaberinella Vaughan, 1928, remarks on its species and on its systematic position, Eclogae Geologicae Helvetiae 62:745-749. , available online at https://www.e-periodica.ch/digbib/view?pid=egh-001%3A1969%3A62%3A%3A817 [details]   
From editor or global species database
Diagnosis Test operculine to discoidal, large, up to 50 mm in diameter, early stage of microspheric test peneropline with broad and low chambers that may become cyclical; large, globular megalospheric proloculus followed by rapidly enlarging chambe,rs in flaring peneropline coil, numerous oblique septula subdivide the chambers into small chamberlets that communicate through a system of stolons in three planes, longitudinal subepidermal tubes are oriented in the direction of shell growth or radial in the cyclic chambers, in the median part of the test larger tubes are oriented oblique to the direction of growth, alternating in orientation from layer to layer, and vertical passages connect these large tubes to the subepidermal ones; wall calcareous, porcelaneous, may be recrystallized, resulting in poor preservation. M. to U. Eocene; Jamaica. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]