Chilostomelloidea

Chilostomelloidea is a superfamily of foraminifera in the order Rotaliida.[1] They are found in sediments of Early Cretaceous (Barremian) to the present.[2]

Chilostomelloidea
Temporal range: Early Cretaceous - Present
(Barremian - present)
Scientific classification
Clade: SAR
Phylum: Foraminifera
Class: Globothalamea
Order: Rotaliida
Superfamily: Chilostomelloidea
Brady, 1881
Families

See text

Synonyms

Chilostomellacea

The test, or shell, may be trochospiral to planispiral throughout, or just in the early part with the later part uncoiled. Chambers may be somewhat enveloping, and attached forms may uncoil in the adult. In coiled forms, the aperture is interiomarginal, or terminal in uncoiled forms. The test wall is of perforate hyaline (glassy) oblique calcite, appearing optically granular.

Subtaxa

The superfamily Chilostomelloidea consists of the following families:[1]

  • Alabaminidae Hofker, 1951
  • Anomalinidae Cushman, 1927
  • Chilostomellidae Brady, 1881
  • Coleitidae Loeblich & Tappan, 1984
  • Gavelinellidae Hofker, 1956
  • Globorotalitidae Loeblich & Tappan, 1984
  • Karreriidae Saidova, 1981
  • Lublinidae Gawor-Biedowa, 1989
  • Quadrimorphinidae Saidova, 1981
  • Svratkinidae Bugrova, 1989
  • Trichohyalidae Saidova, 1981
gollark: I'm not sure it fixes much though. You still have to keep giant timezone databases around, and extra transitional logic, on top of the new ones.
gollark: More so than utter UTC, yes.
gollark: Oh no.
gollark: A bunch of places will have to switch. Timezone databases will need updating, as will basically all signs and stuff. A UTC migration would have the same sign-updating things, but no timezone-database issues and much less ambiguity there.
gollark: It still has almost exactly the same problems plus fun new ones.

References


This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.