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Tetragonostomina Mikhalevich 1975

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Tetragonostomina ( Spanish; Castilian )

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Tetragonostomina es un género de foraminífero bentónico de la subfamilia Textulariinae, de la familia Textulariidae, de la superfamilia Textularioidea, del suborden Textulariina[1]​ y del orden Textulariida.[2]​[3]​[4]​ Su especie tipo es Tetragonostomina rhombiformis. Su rango cronoestratigráfico abarca el Holoceno.

Clasificación

Tetragonostomina incluye a la siguiente especie:[5]​[6]​[7]​

Bibliografía

  1. ↑ Loeblich, A.R., Jr. y Tappan, H. (1987). Foraminiferal genera and their classification. Van Nostrand Reinhold Company (ed.), 2 vol., 1-970, 1-212 + 847 láminas.
  2. ↑ Loeblich, A.R., Jr. y Tappan, H. (1992). Present Status of Foraminiferal Classification. Studies in Benthic Foraminifera en Benthos'90, Sendai (1990), Tokai University Press, 93-102.
  3. ↑ Sen Gupta, B.K. (2002). Systematics of modern Foraminifera, In: Barun K. Sen Gupta (Hrsg.), Modern Foraminifera. Springer Netherlands (Kluwer Academic), ISBN 978-1-4020-0598-5, S. 23.
  4. ↑ Kaminski, M.A. (2004). The Year 2000 Classification of the Agglutinated Foraminifera. En: Bubík, M. & Kaminski, M.A. (eds), Proceedings of the Sixth International Workshop on Agglutinated Foraminifera. Grzybowski Foundation Special Publication, 8: 237-255.
  5. ↑ Encyclopedia of the Life, en http://eol.org/
  6. ↑ World Modern Foraminifera Database, en http://www.marinespecies.org/foraminifera/index.php
  7. ↑ Classifications Browser en http://www.ubio.org/browser/classifications.php?conceptID=13894357&expand=1&namebankID= Página 1 de 134
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Tetragonostomina: Brief Summary ( Spanish; Castilian )

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Tetragonostomina es un género de foraminífero bentónico de la subfamilia Textulariinae, de la familia Textulariidae, de la superfamilia Textularioidea, del suborden Textulariina​ y del orden Textulariida.​​​ Su especie tipo es Tetragonostomina rhombiformis. Su rango cronoestratigráfico abarca el Holoceno.

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Diagnosis

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Test free, flaring, and spatulate to rhomboidal in outline, flattened to diamond shaped in section, with broad, low, biserially arranged chambers, and thickened and elevated sutures that form a peripheral keel and a median ridge along the zigzag suture; wall agglutinated, with quartz and calcium carbonate particles in a fine-grained ground mass and with very small micropores opening at the surface; aperture a high quadrangular opening at the base of the final chamber face, with a distinct bordering ridge on three sides, the lateral borders of the aperture being slightly constricted. Holocene; Nigeria; Liberia; Ivory Coast. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification)

Reference

Loeblich, A. R.; Tappan, H. (1987). Foraminiferal Genera and their Classification. Van Nostrand Reinhold Company, New York. 970pp.

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