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Loeblichopsis Hofker 1969

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Loeblichopsis ( Spanish; Castilian )

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Loeblichopsis es un género de foraminífero bentónico de la subfamilia Hormosininae, de la familia Hormosinidae, de la superfamilia Hormosinoidea, del suborden Hormosinina[1]​ y del orden Lituolida.[2]​ Su especie tipo es Reophax cylindrica. Su rango cronoestratigráfico abarca el Holoceno.

Discusión

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

Clasificación

Loeblichopsis incluye a las siguientes especies:[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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Loeblichopsis: Brief Summary ( Spanish; Castilian )

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Loeblichopsis es un género de foraminífero bentónico de la subfamilia Hormosininae, de la familia Hormosinidae, de la superfamilia Hormosinoidea, del suborden Hormosinina​ y del orden Lituolida.​ Su especie tipo es Reophax cylindrica. Su rango cronoestratigráfico abarca el Holoceno.

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Diagnosis

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Test uniserial and rectilinear, may be up to 10 mm in length, chambers somewhat pyriform, with successive chambers overlapping previous ones so that sutures are obscure externally and the test is nearly cylindrical; wall thick, agglutinated of more than a single layer of fine quartz grains and tests of small foraminifers, may be only partially cemented, thickest where the new chamber overlaps that preceding, with an inner proteinaceous lining; aperture terminal, central, round. Holocene; N. Atlantic from 100 m to 4,066 m; Indian Ocean at 3,140 m. (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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