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Dusenburyina Bermúdez & Key 1952

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Dusenburyina ( Spanish; Castilian )

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Dusenburyina es un género de foraminífero bentónico de la familia Dusenburyinidae, de la superfamilia Hormosinoidea, del suborden Hormosinina[1]​ y del orden Lituolida.[2]​ Su especie tipo es Clavulina procera. Su rango cronoestratigráfico abarca el Holoceno.

Discusión

Clasificaciones previas incluían Dusenburyina en el suborden Textulariina del orden Textulariida[3]​ o en el orden Lituolida sin diferenciar el suborden Hormosinina.[4]​

Clasificación

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

Bibliografía

  1. ↑ 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.
  2. ↑ Sen Gupta, B.K. (1999). Systematics of modern Foraminifera. En: Sen Gupta, B.K. (Ed.), Modern Foraminifera. Kluwer Academic Publishers, 7–36.
  3. ↑ 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.
  4. ↑ 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.
  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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Dusenburyina: Brief Summary ( Spanish; Castilian )

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Dusenburyina es un género de foraminífero bentónico de la familia Dusenburyinidae, de la superfamilia Hormosinoidea, del suborden Hormosinina​ y del orden Lituolida.​ Su especie tipo es Clavulina procera. Su rango cronoestratigráfico abarca el Holoceno.

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Diagnosis

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Test elongate, uniserial, rectilinear to slightly arcuate, chambers numerous, increasing slowly in size as added; wall thick, coarsely agglutinated, commonly of calcareous particles; aperture terminal, semicircular in the early stage, later with a distinct tooth projecting from the flattened margin of the aperture, which always represents the outer curve of the test. Holocene; Atlantic; Caribbean; ?N. Pacific: Philippines. (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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