NB This site is under active development, current content in the main database is primarily from Bolli et al 1994, Hayward et al. 2012, Holbourn et al. 2013, Holbourn and Kaminski 1997, Alegret & Thomas 2001, and Katz et al. 2003. It is intended to expand and develop this to provide rather comprehensive coverage of Mesozoic and Cenozoic deep-sea benthic foraminifera.
Daughter taxa (time control age-window is: 0-800Ma)![]() | ||||
![]() | Aschemocella grandis | |||
Aschemocella sp. |
Catalog entries: Aschemocella
NB These concise distinguishing features statements are used in the tables of daughter-taxa to act as quick summaries of the differences between e.g. species of one genus.Search data:
Final whorl chambers: ->0 |
Geological Range:
Last occurrence (top): within (-Ma, top in "Holocene" stage).
First occurrence (base): within (-Ma, base in "Holocene" stage).
Plot of occurrence data:
NB The ranges given for genera and higher taxa are the total ranges of species included in that taxon in this database - so the true total range of the taxon will usually be longer
Vyalov, O. S. (1966). О крупных кремнистых фораминиферах Silicinifera из верхнемелового флиша Карпат - [Large siliceous foraminifer Silicinifera from the Upper Cretaceous flysch of the Carpathians]. Paleontologicheskii Sbornik, Lvovskogo Geologicheskogo Obshchestva. 3(2): 27-36. gsReferences:
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Aschemocella compiled by the bforams@mikrotax project team viewed: 13-7-2025
Short stable page link: https://mikrotax.org/bforams/index.php?id=2001554 Go to Archive.is to create a permanent copy of this page - citation notes |
bforams@mikrotax has been supported by US IODP Science Support Program and by the Geologic TimeScale Foundation![]() ![]() |