Ceratolithus cristatus HET

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Cenozoic Taxa

Ceratolithus cristatus HET

Ceratolithus cristatus Kamptner 1950 HET

Description: Circular heterococcoliths with a single shield and open central area, surrounded by a collar/tube. Formed of a single cycle of crystal-units with sub-vertical c-axes (Young et al. 1998).

Original description:

Neosphaera coccolithomorpha 020365.jpgNeosphaera coccolithomorpha 020366.jpg

Cer_HET_CSF0146.JPGCer_HET_166-06.JPGCer_HET_113-22.JPGCer_HET_114-96.JPG modern
5-21coccolithomorpha.JPG5-26coccolithomorpha.JPG5-27coccolithomorpha.JPGCerHet201 (471-0) 23NN14-15.JPG fossil

Remarks (relation to ceratoliths): A succesion of observations (Alcober & Jordan 1997, Young et al. 1998, Cros et al. 2000, and Sprengel & Young 2000) have shown that these heterococcoliths are formed during an alternate life-cycle stage of Ceratolithus cristatus and so should not be regarded as a discrete species.

Synonyms:

  • Neosphaera Lecal-Schlauder 1950
  • Craspedolithus Kamptner 1963

Variants: three different forms can be identified in the modern plankton (Kleijne 1993), and may represent discrete species, although given the life-cycle complexities it is simpler to place them all in C. cristatus.

  1. large coccolithomorpha type: 6-10 µm across, opening 0.4-0.5x total diameter [= Neosphaera coccolithomorpha Lecal-Schlauder 1950].
  2. small coccolithomorpha type: 4-5 µm across, opening 0.35-0.45x total diameter.
  3. nishidae type: 4-7 µm across, opening 0.15-0.3x total diameter [=Neosphaera coccolithomorpha var. nishidae Kleijne 1993].

Geological Time Data
Notes on occurrence information: 
Quite common in the Quaternary and has been observed back to at least the mid Pliocene, but is not routinely recorded since it is difficult to sperate from Umbilicosphaera in the LM. NB The first occurrence does seem to approximately conicide with that of Ceratolithus ceratoliths, but there is no obvious reason why this should be the case since the ancestor of Ceratolithus (Triquetrorhabdulus?) might be precidited to have formed heterococcoliths.
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