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Taxonomy:
Distinguishing features:
Parent taxon (B. morionum group): Spine low, globular, height<2x width
This taxon: Small rhabdoliths with relatively low, hollow, sacculiform spines. Spine broadens from base and is capped by curving upper surface that appears to be constructed from two parts (XPL); spine usually slightly wider than coccolith. Coccolith rim appears to be narrow, and only one cycle has been observed
Farinacci & Howe catalog pages: C. mericii *
Size:
LITHS: planolith, elliptical, CA: ca_disjunct, grill, process, |
Lith size: 2->4µm; Data source notes: lith size (spine height) from OD & Bown 2005 |
Geological Range:
Last occurrence (top): within NP15b subzone (44.12-45.49Ma, top in Lutetian stage). Data source: Bown 2005
First occurrence (base): within NP12 zone (50.50-53.70Ma, base in Ypresian stage). Data source: Varol, 1989
Plot of occurrence data:
Bown, P. R. (2005d). Palaeogene calcareous nannofossils from the Kilwa and Lindi areas of coastal Tanzania (Tanzania Drilling Project 2003-4). Journal of Nannoplankton Research. 27(1): 21-95. gs O Dunkley Jones, T., Bown, P. R. & Pearson, P. (2009). Exceptionally well preserved upper Eocene to lower Oligocene calcareous nannofossils (Prymnesiophycidae) from the Pande Formation (Kilwa Group), Tanzania. Journal of Systematic Palaeontology. 7(4): 359-411. gs Varol, O. (1989c). Palaeocene calcareous nannofossil biostratigraphy. In, Crux, J. A. & van Heck, S. E. (eds) Nannofossils and their applications: Proceedings of the 2nd INA Conference, London 1987. British Micropalaeontological Society Publication Series . 265-310. gs Varol, O. (1989b). Eocene calcareous nannofossils from Sile (northwest Turkey). Revista Española de Micropaleontología. 21: 273-320. gs Young, J. R. (2023). Some proposed changes to the systematics of Cenozoic and Mesozoic nannoplankton. Journal of Nannoplankton Research. 41(1): 15-25. gs References:
Blackites mericii compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 26-1-2025
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