Taxonomy:
Distinguishing features: Elliptical and with <12 slits in the distal shield
Farinacci & Howe catalog pages: E. ovata * , R. pacifica * , S. gartneri *
Morphology: Coccoliths similar to P. lacunosa but elliptical and with <12 slits in the distal shield.
Tags | LITHS: placolith, elliptical, CA: ca_conjunct, grill, vacant, CSPH: equant, monomorphic, CROSS-POLARS: rim-unicyclic, R-prominent, |
Metrics | Lith size: 3->6µm; |
Geological Range:
Notes: Very abundant in Late Pliocene
Last occurrence (top): within NN19 zone (0.44-1.93Ma, top in Ionian stage). Data source: Young 1998
First occurrence (base): within NN14 zone (3.92-4.13Ma, base in Zanclean stage). Data source: Young 1998
Plot of occurrence data:
Bukry, D. (1973c). Coccolith stratigraphy, eastern equatorial Pacific, Leg 16, Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project. 16: 653-711. gs V O Lourens, L. J., Hilgen, F. J., Shackleton, N. J., Laskar, J. & Wilson, D. (2004). The Neogene Perion. In, Gradstein, F. M., Ogg, J. G. & Smith, A. (eds) A Geologic Time Scale. Cambridge University Press, Cambridge 409-440. gs Matsuoka, H. & Okada, H. (1989). Quantitative analysis of Quaternary nannoplankton in the subtropical Northwestern Pacific Ocean. Marine Micropaleontology. 14: 97-118. gs Nishida, S. (1979). Atlas of Pacific Nannoplanktons. News of Osaka Micropaleontologists, Special Paper. 3: 1-31. gs Varol, O. (2004). Salisia n.g. – a new Pliocene-Pleistocene coccolith genus. Neues Jahrbuch für Geologie und Paläontologie, Monatshefte. 2004(2): 119-128. gs Young, J. R. (1990). Size variation of Neogene Reticulofenestra coccoliths from Indian Ocean DSDP cores. Journal of Micropalaeontology. 9: 71-86. gs V O Young, J. R. (1998). Neogene. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series. 225-265. gs V OReferences:
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Pseudoemiliania ovata compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 7-3-2021
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