Taxonomy:
Subdivision: The large number of described species have been variously subdivided into sub-groups by different workers (e.g. Theodoridis 1984, Aubry 1990, Young 1998). The subdivision followed here is based on Young (1998) which followed previous work. The main Paleogene and Neogene groups are respectively the lophota and carteri groups. The recta group is an additional well-separated Oligo-Miocene lineage. Finally the walbersdorfensis and ampliaperta groups include some distinctive Miocene species, although the separation from the carteri group is somewhat subjective.
Alternative taxonomy: Aubry & Bord (2009) proposed an alternative taxonomy for the species conventionally included in Helicosphaera on the basis that there is "morphostructural evidence" that Helicosphaera carteri evolved from Pontosphaera in the Late Oligocene, rather than from other Helicosphaera species such as H. intermedia or H. euphratis. The nature of this morphostructural evidence is not explained, however, the proposal seems extremely unlikely to us since Helicosphaera is a distinctive and unique set of species. In particular the spiral coiling of the shield in Helicosphaera is a unique feature within the coccolithophores and is essentially identical in all species conventionally included in Helicosphaera. Moreover intermediates occur between the species H. euphratis, H. intermedia and H. carteri, indeed in the Early Miocene it is often dificult to separate these species. Hence we regard it as highly unlikely that Helicosphaera is polyphyletic and this further means that the genera Helicosphaerella, and Helicosphaeroides, are unnecessary. They could, of course, still be used - for respectively the H. recta group and the H. lophota group as recognised here. However, the proposed names are confusingly similar so using them does not seem advantageous.
Distinguishing features:
Parent taxon (Helicosphaeraceae): Varimorphic; liths placolith-like but with helical shield structure; arranged in spiral on coccosphere
This taxon: Coccoliths with helical flange; arranged spirally on the coccosphere
Farinacci & Howe catalog pages: Helicosphaera + * , Helicopontosphaera * , Helicosphaerella * , Helicosphaeroides *
Morphology:
Various sub-groups can be recognised based on presence/absence of a disjunct bar, bar orientation, degree to which the blanket (R-units) covrs the flange (V-units), termintion of the flange, etc. (see e.g. Theodoridis 1984, Perch-Nielsen 1985b, Aubry 1990, Young 1998).
There is however also signifiant variation within all species, notably in degree of development of the wing. In modern Helicosphaera carteri this can be seen to be relsted to position on the coccosphere, with the coccoliths around the flagellar opning typiclly having especially wel-devloped wings.
LITHS: placolith, asymmetric, CSPH: elongated, monomorphic, CROSS-POLARS: V-prominent, R-prominent, rim-bicyclic, |
Lith size: 4->22µm; |
Geological Range:
Last occurrence (top): Extant. Data source: Total of ranges of the species in this database
First occurrence (base): within NP12 zone (50.50-53.70Ma, base in Ypresian stage). Data source: Total of ranges of species in this database
Plot of occurrence data:
Aubry, M. -P. & Bord, D. (2009). Reshuffling the cards in the photic zone at the Eocene/Oligocene boundary. In, Koeberl, C. & Montanari, A. (eds) The Late Eocene Earth—Hothouse, Icehouse, and Impacts. Geological Society of America, Special Papers . 452: 279-301. gs Aubry, M. -P. (1990). Handbook of Cenozoic calcareous nannoplankton. Book 4: Heliolithae (Helicoliths, Cribriliths, Lopadoliths and others). Micropaleontology Press, American Museum of Natural History, New York. 1-381. gs Jafar, S. A. & Martini, E. (1975). On the validity of the calcareous nannoplankton genus Helicosphaera. Senckenbergiana Lethaea. 56: 381-397. gs Kamptner, E. (1954). Untersuchungen über den Feinbau der Coccolithen. Archiv für Protistenkunde. 100: 1-90. gs Perch-Nielsen, K. (1985). Cenozoic calcareous nannofossils. In, Bolli, H. M., Saunders, J. B. & Perch-Nielsen, K. (eds) Plankton Stratigraphy. Cambridge University Press, Cambridge (1): 427-555. gs Theodoridis, S. (1984). Calcareous nannofossil biostratigraphy of the Miocene and revision of the helicoliths and discoasters. Utrecht Micropaleontological Bulletin. 32: 1-271. gs O Young, J. R. (1998). Neogene. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series . 225-265. gs Young, J. R., Henriksen, K. & Probert, I. (2004b). Structure and morphogenesis of the coccoliths of the CODENET species. In, Thierstein, H. R. & Young, J. R. (eds) Coccolithophores - From molecular processes to global impact. Springer, Berlin 191-216. gs OReferences:
Helicosphaera compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 7-12-2024
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