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Septotextularia ( espagnol ; castillan )

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

Clasificación

Septotextularia incluye a las siguientes especies:[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. (1999). Systematics of modern Foraminifera. En: Sen Gupta, B.K. (Ed.), Modern Foraminifera. Kluwer Academic Publishers, 7–36.
  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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Septotextularia: Brief Summary ( espagnol ; castillan )

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

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Diagnosis ( anglais )

fourni par World Register of Marine Species
Test free, large, up to 2 mm in length, stout, biserial throughout, the lower margin of each chamber deeply incised just anterior to the septa, and with about four backward directed projections on each chamber that overlap the sutures, chamber lumen subdivided by four to six vertical radial partitions that extend nearly to the center of the test; sutures slightly arched, septa thick, particularly in the vicinity of the aperture; wall agglutinated, canaliculate, thick, coarser grained near the exterior and somewhat fined grained toward the test interior; aperture a low arch at the base of the apertural face. Holocene: Pacific. (Loeblich & Tappan, 1987, Foraminiferal Genera and Their Classification)

Référence

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

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Tomas Cedhagen [email]