Distinguishing features:
Parent taxon (Nephrolithus): Reniform; central-area net with two to numerous pores
This taxon: Central area with 2-15 perforations each surrounded by neat rings of rhombic elements
Sub-taxa & variants (time control age-window is: 0-800Ma)![]() | ||||
Nephrolithus frequens subsp. frequens Forms of N. frequens, with >2 holes in the central area (usually larger than N. frequens miniporus) | ||||
![]() | Nephrolithus frequens subsp. miniporus Reniform to elliptical subspecies of N. frequens with only two holes within the central area. |
Taxonomy:
Farinacci & Howe catalog pages: N. frequens + * , N. gorkae * , N. furcatus * , N. trientis * , N. barbarae *
Distinguishing features:
Parent taxon (Nephrolithus): Reniform; central-area net with two to numerous pores
This taxon: Central area with 2-15 perforations each surrounded by neat rings of rhombic elements
Search data:
LITHS: placolith, asymmetric, CA: closed, plate, pores, ca_disjunct, CROSS-POLARS: R-prominent, V-prominent, rim-bicyclic, |
Lith size: 4->8µm; Data source notes: range of sub-species |
Geological Range:
Notes: FAD highly diachronous, occurring UCboreal20b in N. Europe; at base UC17 in the Tethyan Province; and in UC15e in the "extreme Tethyan province (Burnett 1998). Its regional FAD can be a valuable marker within the Maastrichtian but needs to be used with caution, Watkins et al. 1996, Pospichal & Wise 1990.
Last occurrence (top): within Late Maastrichtian Substage (66.04-70.10Ma, top in Maastrichtian stage). Data source: Burnett 1998
First occurrence (base): in mid part of UC15d subzone (50% up, 76.3Ma, in Campanian stage). Data source: Burnett 1998
Plot of occurrence data:
Åberg, M. (1966). Electron microscope studies on Nephrolithus (Coccolithophoraceae). Stockholm Contributions in Geology. 13: 63-67. gs Bown, P. R. & Young, J. R. (1997). Mesozoic calcareous nannoplankton classification. Journal of Nannoplankton Research. 19(1): 21-36. gs Bralower, T. J. & Siesser, W. G. (1992). Cretaceous calcareous nannofossil biostratigraphy of Sites 761, 762, and 763, Exmouth and Wombat Plateaus, northwest Australia. Proceedings of the Ocean Drilling Program, Scientific Results. 122: 529-556. gs Burnett, J. A. (1998). Upper Cretaceous. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series . 132-199. gs O Górka, H. (1957). Les Coccolithophoridés du Maestrichtien supérieur de Pologne. Acta Palaeontologica Polonica. 2: 239-284. gs Perch-Nielsen, K., Sadek, A., Barakat, M. G. & Teleb, F. (1978). Late Cretaceous and Early Tertiary Calcareous nannofossil and Planktonic foraminifera zones from Egypt. Actes du VI Colloque Africain de Micropaléontologie - Tunis 1974. Annales des Mines et de la Géologie Tunissienne. 28: 337-403. gs Pospichal, J. J. & Wise, S. W. (1990). Maestrichtian calcareous nannofossil biostratigraphy of Maud Rise ODP leg 113 sites 689 and 690, Weddell Sea. Proceedings of the Ocean Drilling Program, Scientific Results. 113: 465-487. gs Sissingh, W. (1977). Biostratigraphy of Cretaceous calcareous nannoplankton. Geologie en Mijnbouw. 65(1): 37-65. gs Watkins, D. K., Wise, S. W., Pospichal, J. J. & Crux, J. (1996). Upper Cretaceous calcareous nannofossil biostratigraphy and paleoceanography of the Southern Ocean. In, Moguilevsky, A. & Whatley, R. (eds) Microfossils and Oceanic Environments. University of Wales, Aberystwyth Press 355-381. gs References:
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Nephrolithus frequens compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 15-5-2025
Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=10798 Go to Archive.is to create a permanent copy of this page - citation notes |
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