arrayname: original
Daughter taxa (time control age-window is: 0-800Ma)![]() | ||||
Syracosphaera mediterranea Typical form, medium sized; BCs 3-4 µm, coccospheres 12-20 µm | ||||
![]() | ![]() | ![]() | Syracosphaera maxima Like C. mediterranea but larger; BCs 4-6 µm, coccospheres 25-40 µm; CFCs more elliptical. | |
Syracosphaera sp. Y Similar to S. mediterranea but wall is narrower and higher, lacking clear inner cycle and with small central spine. |
Taxonomy:
The synonymy with Zygosphaera and Syracolithus is based on life-cycle associations.
Distinguishing features:
Parent taxon (Syracosphaera): Coccospheres usually dithecate. Exothecal coccoliths (XCs) highly variable. Endothecal coccoliths are muroliths with 1, 2 or 3 flanges, the forms with 2 flanges are often placolith-like.
This taxon: BCs muroliths with imbricate wall, bipartite axial structure. No XCs (formerly Coronosphaera)
Farinacci & Howe catalog pages: Coronosphaera * , Laminolithus * , Zygosphaera + * , Syracolithus + *
Morphology:
Body coccoliths - flangeless muroliths; rims formed of an outer cycle of strongly imbricate (anticlockwise) elements and an inner cycle of vertical elements. Central area with plaque formed of two plates.
Circum Flagellar Coccoliths - similar but slightly smaller, with low spine.
Distinguishing features of this set of species from other Syracosphaera species
Number of lath vs. rim elements. As noted by Gaarder & Heimdal (1977) there are more radial laths than rim elements. This is unusual as in other Syracosphaeraceae there is one lath per rim unit. Young et al. (2003) stated that there were 2 lath elements per rim elements, however, counts on several specimens indicate that typically there are 45-55 lath elements and 30-36 rim elements, ie. a ratio of 1.5:1 on modern S. mediterranea. Moreover, on Miocene fossil Coronosphaera from the Paratethys (material described by Galovic & Young 2012) there is one lath element per rim element. So although rim element number does appear to be consistently lower than lath element number in modern Coronosphaera this is not an ancestral character. [my obs. JRY 2015]
LITHS: murolith, elliptical, CA: ca_disjunct, plate, grill, CSPH: equant, CFC, CROSS-POLARS: V-prominent, R-prominent, |
Lith size: 2.5->6µm; Coccosphere size: 13->53µm; |
Geological Range:
Last occurrence (top): Extant. Data source: Total of ranges of the species in this database
First occurrence (base): within Miocene Epoch (5.33-23.03Ma, base in Aquitanian stage). Data source: Total of ranges of species in this database
Plot of occurrence data:
Gaarder, K. R. & Heimdal, B. R. (1977). A revision of the genus Syracosphaera Lohmann (Coccolithineae). “Meteor” Forschungsergebnisse. 24: 54-71. gs O Galovic, I. & Young, J. R. (2012). Revised taxonomy of some Middle Miocene calcareous nannofossils in the Paratethys. Micropaleontology. 58(4): -. gs Triantaphyllou, M. et al. (2016). Coccolithophore combination coccospheres from the NE Mediterranean Sea: new evidence and taxonomic revisions. Micropaleontology. 61 [2015](6): 457-472. gs Young, J. R., Geisen, M., Cros, L., Kleijne, A., Probert, I. & Ostergaard, J. B. (2003). A guide to extant coccolithophore taxonomy. Journal of Nannoplankton Research. S1: 1-132. gs Young, J. R., Arapov, J., Skejic, S., Bakrac, A., Buzancic, M. & Triantaphyllou, M. (2020). Verification of the life-cycle of Helicosphaera pavimentum, and discussion of the identity of Syracolithus dalmaticus. Journal of Nannoplankton Research. 30(1): 41-47. gs References:
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SY mediterranea group compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 19-4-2025
Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=361 Go to Archive.is to create a permanent copy of this page - citation notes |
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