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Foraminifera taxon detailsValdanchella Canérot & Moullade, 1971 †
 739369 (urn:lsid:marinespecies.org:taxname:739369)
accepted
Genus
Simplorbitolina miliani Schroeder, 1968 † accepted as Valdanchella miliani (Schroeder, 1968) † (type by original designation)
marine,
fossil only
feminine
Canérot, J.; Moullade, M. (1971). Le Valanginien à faciès marin dans le Maestrazgo (Provinces de Castellon, Tarragona, Teruel-Espagne) : étude particulière des Orbitolinidae : Valdanchella n. gen., Paracoskinolina pfenderae n. sp. <em>Archives des Sciences, Genève.</em> 24: 207-219., available online at https://doi.org/10.5169/seals-739700
page(s): p. 214 [details] Available for editors  [request]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2024). World Foraminifera Database. Valdanchella Canérot & Moullade, 1971 †. Accessed at: https://www.marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=739369 on 2024-06-20
Date action by
original description
Canérot, J.; Moullade, M. (1971). Le Valanginien à faciès marin dans le Maestrazgo (Provinces de Castellon, Tarragona, Teruel-Espagne) : étude particulière des Orbitolinidae : Valdanchella n. gen., Paracoskinolina pfenderae n. sp. <em>Archives des Sciences, Genève.</em> 24: 207-219., available online at https://doi.org/10.5169/seals-739700
page(s): p. 214 [details] Available for editors [request] From editor or global species database
Diagnosis Test conical, megalospheric generation with apically located two-or three-chambered simple embryonic apparatus indicated by external sutures, as septa may be secondarily resorbed; later with broad, low rectilinear chambers that increase rapidly in diameter as added, marginal zone of chambers subdivided by numerous fine radial exoskeletal beams, of constant thickness throughout, the somewhat longer major beams alternate with shorter secondary ones, outermost part of the chambers with a single layer of horizontal rafters that together with the numerous beams subdivide the marginal zone into a reticular network, central zone occupied by vertical endoskeletal pillars that thicken toward both chamber floor and roof, where there is a slight tendency to anastomose, pillars narrowest slightly above the floor and appear triangular in axial section; wall of imperforate microgranular calcite; aperture not observed, probably a series of pores on the central part of the final septum. L. Cretaceous (Valanginian); Spain. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification) [details]
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