WoRMS taxon details

Heterostegina d'Orbigny, 1826

112238  (urn:lsid:marinespecies.org:taxname:112238)

accepted
Genus
Heterostegina depressa d'Orbigny, 1826 (type by subsequent designation)
Grzybowskia Bieda, 1950 · unaccepted (Subjective junior synonym in...)  
Subjective junior synonym in opinion of Loeblich & Tappan, 1987
Heterostegina (Vlerkinella) Eames, Clarke, Banner, Smout & Blow, 1968 · unaccepted (Subjective junior synonym in...)  
Subjective junior synonym in opinion of Loeblich & Tappan, 1987

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marine, brackish, fresh, terrestrial
recent + fossil
Orbigny, A. D. d'. (1826). Tableau méthodique de la classe des Céphalopodes. <em>Annales des Sciences Naturelles.</em> vol. 7: 96-169, 245-314., available online at http://biodiversitylibrary.org/page/5753959
page(s): p. 305 [details]   
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Heterostegina d'Orbigny, 1826. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=112238 on 2024-04-23
Date
action
by
2004-12-21 15:54:05Z
created
2006-09-13 06:47:38Z
changed
Martinez, Olga
2010-09-20 10:05:34Z
changed
2014-05-19 08:48:59Z
changed
2017-01-08 12:24:29Z
changed

Creative Commons License The webpage text is licensed under a Creative Commons Attribution 4.0 License


original description Orbigny, A. D. d'. (1826). Tableau méthodique de la classe des Céphalopodes. <em>Annales des Sciences Naturelles.</em> vol. 7: 96-169, 245-314., available online at http://biodiversitylibrary.org/page/5753959
page(s): p. 305 [details]   

original description  (of Heterostegina (Vlerkinella) Eames, Clarke, Banner, Smout & Blow, 1968) Eames, F. E.; Clarke, W. J.; Banner, F. T.; Smout, A. H.; Blow, W. H. (1968). Some larger foraminifera from the Tertiary of Central America. <em>Palaeontology.</em> 11: 283-305., available online at https://www.palass.org/sites/default/files/media/publications/palaeontology/volume_11/vol11_part2_pp283-305.pdf
page(s): p. 291 [details]  Available for editors  PDF available [request] 

original description  (of Grzybowskia Bieda, 1950) Bieda, E. (1950). O nowych i mało znanych otwornicach z fliszu Karpat Polskich - Sur quelques foraminifères nouveaux ou peu connus du flysch des Karpates Polonaises. <em>Rocznik Polskiego Towarzystwa Geologicznego.</em> 18: 151-179., available online at https://geojournals.pgi.gov.pl/asgp/article/view/10982/9473
page(s): p. 151 (Polish), 167 (French) [details]  Available for editors  PDF available [request] 

basis of record Gross, O. (2001). Foraminifera, <B><I>in</I></B>: Costello, M.J. <i>et al.</i> (Ed.) (2001). <i>European register of marine species: a check-list of the marine species in Europe and a bibliography of guides to their identification. Collection Patrimoines Naturels,</i> 50: pp. 60-75 (look up in IMIS[details]   

additional source Neave, Sheffield Airey. (1939-1996). Nomenclator Zoologicus vol. 1-10 Online. <em>[Online Nomenclator Zoologicus at Checklistbank. Ubio link has gone].</em> , available online at https://www.checklistbank.org/dataset/126539/about [details]   

additional source 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] 
 
 Present  Inaccurate  Introduced: alien  Containing type locality 
From editor or global species database
Diagnosis Test involute to evolute, centrally thickened, megalospheric proloculus followed by up to sixteen operculinoid and unfolded septa, larger and relatively rare microspheric test with about thirty unfolded septa, then with chamberlets formed by complete secondary septa produced by folds of the septal flap, no communication between adjacent chamberlets of the same chamber, marginal cord consists of an anastomosing bundle of canals in the peripheral band that are continuous with those in the spiral septum of earlier whorls, intraseptal canals formed from part of former marginal canals as new chamber is added, and connect the marginal canals of successive whorls, secondary sutural canals in the septula forming the chamberlets connect successive sutural canals, and those in peripheral position may lead into the marginal canals, apertures of proloculus and early undivided chambers form the primary stolons or apertural or foraminal tubes, later chambers and chamberlets of a single chamber connected by radial stolons or tubes and may also have annular stolons or tangential tubes, so-called because of their position, Y-shaped supplementary stolons occur at the distal tip of the secondary septula in the median plane, smaller connections occur between the chamber lumen and peripheral canals of the final whorl and spiralling canals of the underlying whorl and may also lead to the intraseptal canals, canal system opens through small branches or trabeculae into the relatively large pores or openings of the marginal, septal and secondary septal canals and to the exterior; wall calcareous, finely perforate, chambers and stolons with organic lining but none present in the canal system, up to six interseptal pillars present on the lateral chamberlet walls; openings of the canal system along the periphery may serve for ingestion of nutrients, waste excretion, and exit of the protoplasm from the test at the time of sexual reproduction; live individuals have endosymbiotic diatoms whose photosynthesis provides nutrition for the host; asexual reproduction by multiple fission of protoplasm that earlier had streamed outside the test, producing 100 to over 1,000 young that obtain symbionts from the parent protoplasm, rarely some residual protoplasm remains in the parent cell, continues to grow, and later reproduces a second time; at gamogony thousands of 120 µm ovoid biflagellate gametes are produced. U. Eocene to Holocene; cosmopolitan, tropical to temperate Atlantic, Pacific, and Indian Oceans. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]