Foraminifera taxon details

Sculptobaculites Loeblich & Tappan, 1984 †

737702  (urn:lsid:marinespecies.org:taxname:737702)

accepted
Genus
Evobaculites Korchagin, 1985 † · unaccepted (Subjective junior synonym in...)  
Subjective junior synonym in opinion of Loeblich & Tappan, 1987

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marine, fresh, terrestrial
fossil only
masculine
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. 1161 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Sculptobaculites Loeblich & Tappan, 1984 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=737702 on 2024-04-17
Date
action
by
2013-08-19 08:33:20Z
created
2017-09-25 14:20:39Z
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. 1161 [details]  Available for editors  PDF available [request] 

original description  (of Evobaculites Korchagin, 1985 †) Korchagin, O. A. (1985). K voprosu o sistematike podsemeystva Ammobaculitinae Alekseitchik, 1981 (Foraminifera) [On the question of the systematics of the subfamily Ammobaculitinae Alekseychik, 1981 (Foraminifera)]. <em>Doklady Akademiya Nauk Tadzhikskoi SSR, Dushanbe.</em> 27: 601-604.
page(s): p. 602 [details]   
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
From editor or global species database
Diagnosis Test free, large and robust, planispirally enrolled and slightly evolute early stage may have up to three or more whorls, central area of test depressed to excavated and umbilicate, periphery sharply truncate, chambers inflated to angularly lobulate, five to ten in the prominent coil, may have a much reduced uniserial and rectilinear portion commonly of one or two, rarely three chambers; wall agglutinated, simple in structure, of coarse sand and other mineral grains, but in carbonate facies may agglutinate oolites, calcite prisms from Inoceramus shells, shell fragments, or other foraminifers; aperture a low arch at the base of the apertural face in the enrolled portion, becoming terminal and round in the uncoiled chambers. Jurassic to M. Cretaceous (Albian to Cenomanian); USA: Oklahoma, Texas; USSR: Gissar, Tadzhik. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]