Daughter taxa (time control age-window is: 0-800Ma) | ||||
Pseudoplanomalina cheniourensis | ||||
Pseudoplanomalina sp. Specimens which cannot be assigned to established species |
Taxonomy
Original description: Test planispiral, bi-evolute, microperforate, periphery of chambers not rounded as in Globigerinelloides but subangular, with a distinct break in the peripheral round, better marked on the first chambers of the last whorl by a concentration of perforation cones giving it a peripheral pseudo-keel.
Entries in the Catalog of original descriptions: Pseudoplanomalina
Geological Range:
Last occurrence (top): at top of H. planispira zone (100% up, 111.8Ma, in Albian stage). Data source: Total of ranges of the species in this database
First occurrence (base): within L. cabri zone (119.05-120.55Ma, base in Aptian stage). Data source: Total of ranges of species in this database
Plot of range and occurrence data:
Moullade, M., Bellier, J. -P. & Tronchetti, G. (2002). Hierarchy of criteria, evolutionary processes and taxonomic simplification in the classification of Lower Cretaceous planktonic foraminifera. Cretaceous Research. 23(1): 111-148. gsReferences:
Pseudoplanomalina compiled by the pforams@mikrotax project team viewed: 3-11-2024
Short stable page link: https://mikrotax.org/pforams/index.php?id=110462 Go to Archive.is to create a permanent copy of this page - citation notes |
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Comments (2)
original description Moullade, M.; Bellier, J.-P.; Tronchetti, G. (2002). Hierarchy of criteria, evolutionary processes and taxonomic simplification in the classification of Lower Cretaceous planktonic foraminifera. Cretaceous Research. 23(1), 111-148., available online at https://doi.org/10.1006/cres.2002.0304
page(s): pp. 133-134
thanks, i've added that