| Typical specimen | Genus | Range | Distinguishing features |
| |
Reticulofenestra | Eocene-Recent | Elliptical, central area open or closed |
| |
Cyclicargolithus | Eocene-NN | Circular with narrow central area |
| |
Pseudoemiliania | NN14-19 | Numerous slits in distal shield |
| |
Gephyrocapsa | NN14-21 | Bridge over central area |
| |
Emiliania | NN21 | Slits between all distal shiled elements |
| |
Noelaerhabdus | NN10-11 | Paratethyan endemic wth large spine |
| Bekelithella | NN10-11 | Paratethyan endemic wth circlet of spines |
Coccolith structure: Coccoliths are placoliths with Reticulofenestra-type
structure, i.e. V-unit vestigial, R-unit forms proximal shield, distal
shield, inner andouter tube-cycles, grill and any central-area
structures; strongly birefringent. In the SEM characteristic features
include; grill in central area, anti-clockwise imbrication of inner
tube elements, and monocyclic proximal shield. References: Young
(1989), Young et al. (1994).
Genera included:
Life-cycles and culture studies: Emiliania huxleyi and Gephyrocapsa oceanica have been cultured extensively and their life-cycle is well worked out (Klaveness 1972, Green et al 1996, Houdan et al. 2003). The dominant phase is diploid, non-motile and usually heterococcolith-bearing (= C-cells), although naked mutants often occur inculture (= N-cells). The alternate phase is haploid, scale-bearing and motile(= S-cells). There is no holococcolith stage.
Fossil Record: The Noelaerhabdaceae dominate most Neogene nannofossil assemblages with the dominant genera being succesively Cyclicargolithus (NN1-6), Reticulofenestra (NN6-16), Pseudoemiliania (NN16-19), Gephyrocapsa (NN19-20) and Emiliania (NN21). The last occurrences of various larger forms provide excellent highly synchronous biostatigraphic events - particularly LO large R. pseudoumbilicus (end NN10A), LO R. pseudoumbilicus (end NN15), LO large Gephyrocapsa (NN19), LO P. pseudoemiliania (end NN19).
Synonym: Gephyrocapsaceae Black, 1971
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