MarBEF Data System



Deep-Sea taxon details

Leptohalysis Loeblich & Tappan, 1984

556143  (urn:lsid:marinespecies.org:taxname:556143)

accepted
Genus

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marine, brackish, fresh, terrestrial
recent only
feminine
Loeblich, A. R.; Tappan, H. (1984). Some new proteinaceous and agglutinated genera of Foraminiferida. <em>Journal of Paleontology.</em> 58: 1158-1163.
page(s): p. 1160; note: Genus is feminine [details]  Available for editors  PDF available 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Leptohalysis Loeblich & Tappan, 1984. Accessed through: Glover, A.G.; Higgs, N.; Horton, T. (2024) World Register of Deep-Sea species (WoRDSS) at: https://www.marinespecies.org/deepsea/aphia.php?p=taxdetails&id=556143 on 2024-05-08
Glover, A.G.; Higgs, N.; Horton, T. (2024). World Register of Deep-Sea species (WoRDSS). Leptohalysis Loeblich & Tappan, 1984. Accessed at: https://marinespecies.org/DeepSea/aphia.php?p=taxdetails&id=556143 on 2024-05-08
Date
action
by
2010-12-20 09:45:26Z
created
2010-12-22 06:22:46Z
changed
2013-08-17 09:28:49Z
changed
2014-02-27 08:48:43Z
changed
2017-09-25 14:20:39Z
changed
2019-06-23 15:32:30Z
changed

original description Loeblich, A. R.; Tappan, H. (1984). Some new proteinaceous and agglutinated genera of Foraminiferida. <em>Journal of Paleontology.</em> 58: 1158-1163.
page(s): p. 1160; note: Genus is feminine [details]  Available for editors  PDF available 

context source (Deepsea) Kitazato H., Uematsui K., Todo Y., Gooday A.J. (2009). New species of Leptohalysis (Rhizaria, Foraminifera) from an extreme hadal site in the Western Pacific Ocean. <em>Zootaxa.</em> 2059: 23-32., available online at http://www.mapress.com/zootaxa/2009/f/z02059p032f.pdf [details]  Available for editors  PDF available 
From editor or global species database
Diagnosis Test uniserial and rectilinear, globular proloculus followed by an elongate series of gradually enlarging and distally tapering flaskshaped chambers with blunt lower margin; wall very thin, delicate, and flexible, consisting of a single layer of minute quartz and mica grains agglutinated on a proteinaceous base, early stage may have foreign particles widely spaced, later with adjacent grains abutting; aperture a simple terminal opening, may be flush with the surface or slightly produced with a phialine neck, and may have more than one layer of grains immediately around the opening. Holocene; N. Atlantic: England at20m to46m; Norway from 150m to200m; Sweden from 20 m to 515 m. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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