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Hyalinea ( espagnol ; castillan )

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Hyalinea es un género de foraminífero bentónico de la familia Planulinidae, de la superfamilia Planorbulinoidea, del suborden Rotaliina[1]​ y del orden Rotaliida.[2]​ Su especie tipo es Nautilus balthicus. Su rango cronoestratigráfico abarca desde el Pleistoceno hasta la Actualidad.

Clasificación

Hyalinea 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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Hyalinea: Brief Summary ( espagnol ; castillan )

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Hyalinea es un género de foraminífero bentónico de la familia Planulinidae, de la superfamilia Planorbulinoidea, del suborden Rotaliina​ y del orden Rotaliida.​ Su especie tipo es Nautilus balthicus. Su rango cronoestratigráfico abarca desde el Pleistoceno hasta la Actualidad.

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Diagnosis ( anglais )

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Test discoidal, very low trochospiral to nearly planispiral, semievolute on both sides, about two slowly enlarging whorls, eight to twelve chambers in the final whorl, umbilical margin of the chambers with a small umbilical flap or folium, sutures radial, slightly curved, limbate, elevated, the thickened sutures grading into the broad imperforate peripheral carina, periphery angular; wall calcareous, optically radial, finely perforate, surface smooth, except for the elevated imperforate septa and keel and occasional pustules in the umbilcal region; aperture a low equatorial and interiomarginal arch, bordered above by a narrow lip, a low slit continuing laterally beneath the folium in the umbilical region and around the spiral suture on both sides of the test, chamber lumen communicating with the exterior through a small rounded opening beneath the folium, apertures remaining open for a few chambers before being closed by lamellar thickening. Pleistocene to Holocene; Atlantic; Pacific; Mediterranean; Europe; USA. (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]