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Ashbrookia ( espagnol ; castillan )

fourni par wikipedia ES

Ashbrookia es un género de foraminífero bentónico de la subfamilia Ashbrookinae, de la familia Placentulinidae, de la superfamilia Discorboidea, del suborden Rotaliina[1]​ y del orden Rotaliida.[2]​ Su especie tipo es Ashbrookia ornata. Su rango cronoestratigráfico abarca el Holoceno.

Clasificación

Ashbrookia incluye a las siguientes especies:[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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Ashbrookia: Brief Summary ( espagnol ; castillan )

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Ashbrookia es un género de foraminífero bentónico de la subfamilia Ashbrookinae, de la familia Placentulinidae, de la superfamilia Discorboidea, del suborden Rotaliina​ y del orden Rotaliida.​ Su especie tipo es Ashbrookia ornata. Su rango cronoestratigráfico abarca el Holoceno.

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Diagnosis ( anglais )

fourni par World Register of Marine Species
Test planoconvex, low trochospiral coil of approximately two whorls, about three strongly overlapping chambers per whorl, without a tubular undivided second chamber like that of Patellina, chambers low and crescentic and sutures strongly curved as seen from the convex spiral side, final chamber occupying well over half the periphery and umbilical side, outer margin of the chambers with short radial septula, umbilical margin of the final chamber projecting at the center, and with a curved reentrant at each end; wall calcareous, hyaline, finely punctate; aperture umbilical in position but without the columella structure of the Patellinidae. Holocene; Philippine Islands; China: Zhongsha Islands. (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]