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Pyropilus ( Spanish; Castilian )

provided by wikipedia ES

Pyropilus es un género de foraminífero bentónico de la subfamilia Cymbaloporinae, de la familia Cymbaloporidae, de la superfamilia Planorbulinoidea, del suborden Rotaliina[1]​ y del orden Rotaliida.[2]​ Su especie tipo es Pyropilus rotundatus. Su rango cronoestratigráfico abarca el Holoceno.

Clasificación

Pyropilus incluye a la siguiente especie:[3][4][5]

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. Encyclopedia of the Life, en http://eol.org/
  4. World Modern Foraminifera Database, en http://www.marinespecies.org/foraminifera/index.php
  5. Classifications Browser en http://www.ubio.org/browser/classifications.php?conceptID=13894357&expand=1&namebankID= Página 1 de 134
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Pyropilus: Brief Summary ( Spanish; Castilian )

provided by wikipedia ES

Pyropilus es un género de foraminífero bentónico de la subfamilia Cymbaloporinae, de la familia Cymbaloporidae, de la superfamilia Planorbulinoidea, del suborden Rotaliina​ y del orden Rotaliida.​ Su especie tipo es Pyropilus rotundatus. Su rango cronoestratigráfico abarca el Holoceno.

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Diagnosis

provided by World Register of Marine Species
Test trochospirally enrolled in the early stage, chambers later added irregularly to form an elongate mass, all chambers visible on the spiral side, only the final series visible around the umbilical depression of the opposite side, sutures depressed, periphery rounded; wall calcareous, coarsely perforate, with thin organic lining, surface smooth; on the umbilical side of the test, one or more rows of large apertural pores occur along the sutures of all chambers of the final whorl, as in Cymbaloporella, and additional pores may occur at the umbilical end of the final chamber. Holocene; Pacific: Rangiroa Atoll. (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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Tomas Cedhagen [email]