Foraminifera taxon details

Pfendericonus Hottinger & Drobne, 1980 †

739483  (urn:lsid:marinespecies.org:taxname:739483)

accepted
Genus
Chrysalidina (Pfendericonus) Hottinger & Drobne, 1980 † · unaccepted (Opinion of Loeblich and Tappan...)  
Opinion of Loeblich and Tappan (1987) nomen translatum

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marine, brackish, fresh, terrestrial
fossil only
masculine
(of Chrysalidina (Pfendericonus) Hottinger & Drobne, 1980 †) Hottinger, L., and K. Drobne, 1980, Early Tertiary conical imperforate foraminifera. Konične imperforatne foraminifere iz starejšega terciarja, Slovenska Akademija Znanosti in Umetnosti, Classis IV Historia Naturalis, Dissertationes 22(3): 187-276.
page(s): p. 216, 222, 224, 257 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Pfendericonus Hottinger & Drobne, 1980 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=739483 on 2024-04-23
Date
action
by
2013-09-05 09:33:42Z
created
2017-11-30 13:17:39Z
changed
2019-10-28 19:23:54Z
changed

original description  (of Chrysalidina (Pfendericonus) Hottinger & Drobne, 1980 †) Hottinger, L., and K. Drobne, 1980, Early Tertiary conical imperforate foraminifera. Konične imperforatne foraminifere iz starejšega terciarja, Slovenska Akademija Znanosti in Umetnosti, Classis IV Historia Naturalis, Dissertationes 22(3): 187-276.
page(s): p. 216, 222, 224, 257 [details]  Available for editors  PDF available [request] 
From editor or global species database
Diagnosis Test with early stage in a high trochospiral coil, up to 3 mm in length, megalospheric test with globular proloculus followed by three to four chambers in the first whorl that has no endoskeletal structures, later with as many as six to ten wedgelike chambers per whorl, and may become uniserial in the final stage, peripheral region of chambers inflated and internally undivided; wall agglutinated, external wall canaliculate; wide umbilicus covered by convex extension of apertural face forming a central shield, successive extensions connected by widely spaced thin vertical endoskeletal pillars arranged in semicircles that alternate in position from chamber to chamber; apertural face strongly inclined to the axis of coiling, at about a 45¡ angle, with apertures in a semicircular row at the edge of the marginal zone, central shield pierced by numerous foramina that are aligned from chamber to chamber, diverging from the apex toward the apertural surface. U. Paleocene (Ilerdian): Pakistan; M. to U. Eocene: Yugoslavia. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]