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Deep-Sea taxon detailsClavulina d'Orbigny, 1826
 409586 (urn:lsid:marinespecies.org:taxname:409586)
accepted
Genus
marine,
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. 268 [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Clavulina d'Orbigny, 1826. Accessed through: Glover, A.G.; Higgs, N.; Horton, T. (2025) World Register of Deep-Sea species (WoRDSS) at: https://www.marinespecies.org/DeepSea/aphia.php?p=taxdetails&id=409586 on 2025-05-07
Glover, A.G.; Higgs, N.; Horton, T. (2025). World Register of Deep-Sea species (WoRDSS). Clavulina d'Orbigny, 1826. Accessed at: https://www.marinespecies.org/DeepSea/aphia.php?p=taxdetails&id=409586 on 2025-05-07
Date action by 2009-07-20 12:27:37Z created db_admin
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. 268 [details] basis of record GulfBase, available online at http://www.gulfbase.org [details] additional source GulfBase, available online at http://www.gulfbase.org [details]  Present Inaccurate Introduced: alien Containing type locality
From editor or global species database
Diagnosis Test elongate, early stage triserial and triangular in section, later stage uniserial and rectilinear, with angular to rounded section; wall agglutinated, with considerable calcareous cement, in at least some species addition of a new chamber results in addition of an imperforate floor to the new chamber, so that the septa are secondarily doubled; wall canaliculate, fine canaliculi bifurcating within the wall, openings of the canaliculi sealed internally by an inner organic lining, and externally by the imperforate surface layer of the wall; aperture interiomarginal in the early triserial stage, terminal and rounded in the adult, with imperforate bordering rim and an imperforate apertural toothplate obstructing part of the aperture, reducing it to a semilunate form, then extending inward from the aperture through the chamber to attach to that preceding, successive toothplates oriented 120¡ apart, reflecting the original triseriality. Paleocene to Holocene; cosmopolitan. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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