Foraminifera taxon details

Miliammellus Saidova & Burmistrova, 1978

721295  (urn:lsid:marinespecies.org:taxname:721295)

accepted
Genus
Miliammellus legis Saidova & Burmistrova, 1978 (type by original designation)
Silicoloculina Resig, Lowenstam, Echols & Weiner, 1980 · unaccepted (subjective junior synonym in...)  
subjective junior synonym in opinion of Loeblich & Tappan, 1987

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marine, brackish, fresh, terrestrial
recent + fossil
masculine
Burmistrova, I. I. (1978). K stratigrafii glubokovodnykh osadkov vostochnoy chasti Indiyskogo Okeana po bentosnym foraminiferam [On the stratigraphy of deep sea deposits in the eastern part of the Indian Ocean, based on benthic foraminifera], in Morskaya Mikropaleontologiya. <em>Moscow: Akademiya Nauk SSSR, Okeanograficheskaya Komissiya.</em> 163-170.
page(s): p. 169 [details]   
Diagnosis Test small, up to 0.5 mm in length, ovoid, chambers in quinqueloculine arrangement as in the miliolids but slightly more...  
Diagnosis Test small, up to 0.5 mm in length, ovoid, chambers in quinqueloculine arrangement as in the miliolids but slightly more than a half coil in length, so that those of successive whorls are offset, chambers widest at their base and narrowing toward the aperture; wall of imperforate opaline silica, thin, homogeneous, insoluble in hydrochloric acid, ultrastructure of inner and outer organic membranes and a median layer of mineralized tubular rods, the mineralized layer consisting of two sheets of a two-dimensional array of rods aligned parallel to the wall surface, separated by a median layer that has a threedimensional random array of rods in an open mesh, the rods circular to angular in section, test surface smooth; aperture a low arch at the open end of the final chamber, with a broad simple tooth. U. Miocene to Holocene; Bering Sea; Antarctic; N. and central Pacific and Indian Oceans, at abyssal depths below 4,000 m. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Miliammellus Saidova & Burmistrova, 1978. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=721295 on 2024-10-01
Date
action
by
2013-03-08 13:53:47Z
created
2014-04-12 09:19:06Z
changed
2017-12-18 14:39:52Z
changed
2018-09-22 10:23:02Z
changed

original description Burmistrova, I. I. (1978). K stratigrafii glubokovodnykh osadkov vostochnoy chasti Indiyskogo Okeana po bentosnym foraminiferam [On the stratigraphy of deep sea deposits in the eastern part of the Indian Ocean, based on benthic foraminifera], in Morskaya Mikropaleontologiya. <em>Moscow: Akademiya Nauk SSSR, Okeanograficheskaya Komissiya.</em> 163-170.
page(s): p. 169 [details]   

original description  (of Silicoloculina Resig, Lowenstam, Echols & Weiner, 1980) Resig, J. M.; Lowenstam, H. A.; Echols, R. J.; Weiner, S. (1980). An extant opaline foraminifer: test ultrastructure, mineralogy, and taxonomy. <em>Special Publications of the Cushman Foundation for Foraminiferal Research.</em> 19: 205-214.
page(s): p. 211 [details]   

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] 
From editor or global species database
Diagnosis Test small, up to 0.5 mm in length, ovoid, chambers in quinqueloculine arrangement as in the miliolids but slightly more than a half coil in length, so that those of successive whorls are offset, chambers widest at their base and narrowing toward the aperture; wall of imperforate opaline silica, thin, homogeneous, insoluble in hydrochloric acid, ultrastructure of inner and outer organic membranes and a median layer of mineralized tubular rods, the mineralized layer consisting of two sheets of a two-dimensional array of rods aligned parallel to the wall surface, separated by a median layer that has a threedimensional random array of rods in an open mesh, the rods circular to angular in section, test surface smooth; aperture a low arch at the open end of the final chamber, with a broad simple tooth. U. Miocene to Holocene; Bering Sea; Antarctic; N. and central Pacific and Indian Oceans, at abyssal depths below 4,000 m. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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