Ceratolithus cristatus

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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.

Ceratolithus cristatus

Ceratolithus cristatus Kamptner, 1950 CER

Description: Horseshoe-shaped strongly birefringent ceratolith, with c-axis perpendicular to length. Arms variable in length and in degree of keel development.

Remarks: As noted in the generic description, ceratoliths show very consistent morphology in terms of asymmetry and pattern of development of ridges and teeth. Nonetheless, individual ceratoliths are highly variable in size and degree of ornamentation which has lead to discrimination of several “species”. In particular the forms telesmus and simplex appear to be simply more and less ornate forms of cristatus whilst rugosus appears to be an irregular variant as a result of poor preservation. The rostratus type of ceratolith is a highly ornate form common in modern assemblages.

NB The heterococcolith stage - Ceratolithus cristatus Kamptner, 1950 HET is described on a separate page.

Original description:

Ceratolithus cristatus 030148.jpgCeratolithus cristatus 030149.jpgCeratolithus cristatus 030150.jpgCeratolithus cristatus 030151.jpgCeratolithus cristatus 030152.jpg

10-20telesmus.JPGCeratolithusB.JPGCeratolithusA.JPGCer-crist_132-3.JPGCer cristatus 129-07Cer-rost181-89.JPGCeratolithusE.JPG

Synonyms/Variants

  • Ceratolithus rugosus Bukry and Bramlette, 1968 - ceratolith with thick arms and irregular form. These are almost certainly simply overgrown C. cristatus specimens. They are mostly recorded from the Pliocene but, as argued by Bergen (1984), this is probably a function of preservation being worse in older sediments.
  • Ceratolithus simplex Bukry, 1979 - small, smooth form. This morphotype occurs throughout the range of C. cristatus and in modern assemblages.
  • Ceratolithus separatus Bukry, 1979 - both arms slightly extended beyond the arch, a moderately ornamented form. This morphotype occurs in modern assemblages and is not obviously discrete from normal C. cristatus.
  • Ceratolithus cristatus var. telesmus (Norris, 1965) Jordan and Young, 1990 [Cr. telesmus] - variety with long sinuous arms. Range: NN16 to 21, but possibly becomes more common in younger samples.
  • Ceratolithus cristatus forma rostratus Borsetti & Cati 1976 [NB this form was not given a formal description and so is invalid]. Ceratolith with high keels and with the rodded keel of the right hand arm extended into an apical beak/rostrum.
Geological Time Data
Geological Time Periods: 
Biblio Reference: 
Young, JR.  1998.  Neogene. Calcareous nannofossil biostratigraphy. :225-265.
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