Foraminifera taxon details

Planolinderina Freudenthal, 1969 †

722275  (urn:lsid:marinespecies.org:taxname:722275)

accepted
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marine, brackish, fresh, terrestrial
fossil only
feminine
Freudenthal, T. (1969). Stratigraphy of Neogene deposits in the Khania province, Crete, with special reference to foraminifera of the family Planorbulinidae and the genus Heterostegina. <em>Utrecht micropaleontological bulletins.</em> 1: 1-208., available online at https://dspace.library.uu.nl/handle/1874/205781
page(s): p. 95 [details]  Available for editors  PDF available [request] 
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Planolinderina Freudenthal, 1969 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=722275 on 2024-04-26
Date
action
by
2013-03-08 13:53:47Z
created
2018-01-02 12:19:20Z
changed
2018-10-07 16:09:07Z
changed

original description Freudenthal, T. (1969). Stratigraphy of Neogene deposits in the Khania province, Crete, with special reference to foraminifera of the family Planorbulinidae and the genus Heterostegina. <em>Utrecht micropaleontological bulletins.</em> 1: 1-208., available online at https://dspace.library.uu.nl/handle/1874/205781
page(s): p. 95 [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] 
From editor or global species database
Diagnosis Test small, up to 1 mm in diameter, discoidal, flat to planoconcave, early chambers in a trochoid spire of up to nine chambers in the microspheric generation, juvenile megalospheric stage of protoconch and deuteroconch, later chambers added in cyclic series, periphery rounded, peripheral outline lobulate; wall calcareous, coarsely perforate, surface of the peripheral wall with fine costae paralleling the flat sides of the test, rows of perforations present between the ribs, the flat side of the test may also have fine irregular imperforate ridges; aperture multiple, with a row of three to six small rounded openings on the periphery at the base of each chamber, each bordered by a small imperforate lip, some openings appearing no larger than the pores on other parts of the chamber, but those at the lateral edges of the peripheral margin may be somewhat larger. U. Oligocene (Chattian) to L. Miocene (Burdigalian); France; Southwest Pacific; Australia; Indonesia; India: Kutch. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]