Syracosphaeraceae

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Cenozoic Taxa

Coronosphaera

Coronosphaera Gaarder in Gaarder & Heimdal 1977

Description: Coccospheres - Monothecate, dimorphic, motile. 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 two radial laths per rim element and central plaque formed of two plates. Circum Flagellar Coccoliths similar but slightly smaller, with low spine.

Cor_med_134-35.JPGCor_med_114-62b.JPGCor_med_N15U2.JPGCor_bin_103-33.JPGCor_bin_103-32.JPGCor_bin_103-34.JPG

Remarks: Coronosphaera is usually placed in the family Syracosphaeraceae, but has also been considered a genus incertae sedis within the order Syracosphaerales. It is distinguished from Syracosphaera by

  • the strong imbrication of the rim elements
  • the occurrence of two laths per rim
  • Absence of flanges
  • Absence of exothecal coccoliths

References: Gaarder & Heimdal (1977) - morphology; Geisen et al. (2002) - holococcolith associations; Houdan et al. (2004) - culture observations.

Type species: C. mediterranea.

LM: Isolated body coccoliths typically show a narrow rim with high birefringence and strongly curved isogyres. The central area is weakly birefringent and shows tangential orientation (so blue and yellow sectors show the opposite to normal disposition) and two central elements.

Original description:

Coronosphaera genus 030051.jpg

Syracosphaeraceae

Family SYRACOSPHAERACEAE (Lohmann 1902) Lemmerman 1903

Description: Motile, coccospheres typically elaborate, often showing dithecatism (development of distinct inner and outer layers of coccoliths) and/or modified polar coccoliths. The endothecal (inner layer) coccoliths are normally relatively conservative in form, typically muroliths with a well-developed central-area lath-cycle and variable inner central-area (coccoliths with this structure have been termed caneoliths). Exothecal coccoliths are much more variable, including planolith, murolith and dome-shaped forms (the planoliths have been termed cyrtoliths).

Remarks: These coccoliths are typically delicate and only rarely preserved. The recent tendency, following Jordan & Young (1990), has been to include most species forms in the single genus Syracosphaera. The main exception is a set of genera with highly modified circum-flagellar and/or antapical coccoliths forming appendages, instead of exothecal coccoliths.

The fossil record of the family is poor but extends back into the Paleogene; fossil specimens are normally assigned to Syracosphaera.

Key references: Okada & McIntyre (1977) - many new spp.; Gaarder & Heimdal (1977) - detailed descriptions of several species; Inouye & Pienaar (1988) - detailed description of S. pulchra cytology and coccolith structure; Kleijne (1993) - illustration and notes on most spp. and many undescribed forms; Cros (2000) - analysis of exothecal coccoliths; Cros et al (2000) - holococcolith-heterococcolith combinations; Cros & Fortuño (2002) - detailed description of most species; Young et al. (2003), identification notes and illustration of most species; Young et al. (2004) description of coccolith structure.

Original description:

Syracosphaera genus 090244.jpg

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