Taxonomy
Original description: Stout test having well developed early planispirally enrolled test. The primary stage is followed by a biserial one consisting of two to (rarely) tree pairs of chambers. Chambers subglobular to globular, sometimes slightly dorso-ventrally flattened. Sutures straight to slightly depressed. Wall finely perforate. Test surface is smooth, unornamented, lacking any trace of striae. Primary aperture, a low arch at the base of the last formed chamber, is bordered by a narrow imperforate lip.
Entries in the Catalog of original descriptions: Heterohelix olssoni
Character matrix
test outline: | Subtriangular | chamber arrangement: | Biserial | edge view: | Compressed | aperture: | Interiomarginal |
sp chamber shape: | Globular | coiling axis: | N/A | periphery: | N/A | aperture border: | Thin lip |
umb chbr shape: | Globular | umbilicus: | N/A | periph margin shape: | Broadly rounded | accessory apertures: | N/A |
spiral sutures: | Flush | umb depth: | N/A | wall texture: | Smooth | shell porosity: | |
umbilical or test sutures: | Flush | final-whorl chambers: | 2.0-2.0 | N.B. These characters are used for advanced search. N/A - not applicable |
Geological Range:
Last occurrence (top): within T. reicheli zone (95.94-96.08Ma, top in Cenomanian stage). Data source: [copied from Chronos database]
First occurrence (base): within T. reicheli zone (95.94-96.08Ma, base in Cenomanian stage). Data source: [copied from Chronos database]
Plot of range and occurrence data:
Georgescu, M. D. (2000). Late Albian-Turonian planktonic foraminifera in the Romanian western Black Sea offshore. Revista Española de Micropaleontología. 32: 157-173. gsReferences:
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Planoheterohelix olssoni compiled by the pforams@mikrotax project team viewed: 25-3-2023
Short stables page link: https://mikrotax.org/pforams/index.php?id=110403 Go to Archive.is to create a permanent copy of this page - citation notes |
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