Distinguishing features: Cretarhabdids with central area net that often includes axial cross bars.
Daughter taxa (time control age-window is: 0-800Ma)![]() | ||||
![]() | ![]() | ![]() | Cretarhabdus conicus Medium to very large (7-15 µm) cretarhabdid coccoliths with a distinct central area axial cross and net. | |
![]() | ![]() | Cretarhabdus inaequalis Small (3-6 µm) Cretarhabdus with an irregular central grill. The bars of the grill are distinctly birefringent in XPL. | ||
![]() | ![]() | ![]() | Cretarhabdus madingleyensis Medium to large (7-12 µm) with relatively wide central area and multiple lateral bars (~4 in each quadrant). | |
![]() | ![]() | Cretarhabdus striatus Large to very large (9-15 µm) Cretarhabdus with distinctive wide central net that includes narrow axial cross bars and multiple narrow lateral bars. The bars of the net are birefringent. | ||
![]() | ![]() | ![]() | Cretarhabdus sp. Specimens not identified to species level |
Taxonomy:
Farinacci & Howe catalog pages: Cretarhabdus + + * , Allemanites * , Cretarhabdella * , Polypodorhabdus * , Stradneria *
Distinguishing features: Cretarhabdids with central area net that often includes axial cross bars.
Search data:Tags | LITHS: placolith, elliptical, CA: cross-axial, ca_disjunct, grill, process, CROSS-POLARS: rim-unicyclic, R-prominent, |
Metrics | Lith size: 3->15µm; Data source notes: size range of included species |
Geological Range:
Last occurrence (top): at top of Maastrichtian Stage (100% up, 66Ma, in Maastrichtian stage). Data source: Total of range of species in this database
First occurrence (base): at base of Oxfordian Stage (0% up, 163.5Ma, in Oxfordian stage). Data source: Total of range of species in this database
Plot of occurrence data:
Black, M. (1971a). Coccoliths of the Speeton Clay and Sutterby Marl. Proceedings of the Yorkshire Geological Society. 38: 381-424. gs Bown, P. R. & Cooper, M. K. E. (1998). Jurassic. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series. 34-85. gs Bramlette, M. N. & Martini, E. (1964). The great change in calcareous nannoplankton fossils between the Maestrichtian and Danian. Micropaleontology. 10(2): 291-322. gs Burnett, J. A. (1998). Upper Cretaceous. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series. 132-199. gs V O Grün, W. & Allemann, F. (1975). The Lower Cretaceous of Caravaca (Spain): Berriasian Calcareous Nannoplankton of the Miravetes Section (Subbetic Zone, Prov. of Murcia). Eclogae Geologicae Helvetiae. 68: 147-211. gs V O Lambert, B. (1987). Nannofossiles calcaires de l'Albien supérieur et du Vraconnien du Cameroun méridional. Cahiers de Micropaléontologie. 2(2): 33-60. gs V O Young, J. R. & Bown, P. R. (2014). Some emendments to calcareous nannoplankton taxonomy. Journal of Nannoplankton Research. 33(1): 39-46. gs V OReferences:
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Cretarhabdus compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 28-2-2021
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