Daughter taxa (time control age-window is: 0-800Ma)![]() | |||||
sides convex to weakly indented | |||||
![]() | ![]() | Micrantholithus breviradiatus Small to large Micrantholithus with shallowly indented sides and rounded apices. | |||
![]() | ![]() | Micrantholithus cosoviciae Very small (<3 µm), without indentations | |||
![]() | ![]() | Micrantholithus disculus Simple, elevated Micrantholithus with rounded outline and elliptical side views. | |||
![]() | ![]() | Micrantholithus flos Micrantholithus with relatively straight edges, sutures often raised | |||
![]() | ![]() | ![]() | ![]() | Micrantholithus triquetra Relatively large (typically >5 µm), triangular-shaped nannoliths that thicken along the longer sides and exhibit low birefringence in XPL. | |
sides deeply indented | |||||
![]() | ![]() | ![]() | Micrantholithus astrum Medium sized Micrantholithus with deeply indented sides and rounded apices. | ||
![]() | Micrantholithus entaster Medium sized Micrantholithus with deeply indented sides and elevated central star | ||||
![]() | ![]() | ![]() | ![]() | Micrantholithus excelsus Large, elevated Micrantholithus with deeply indented sides and gracile, long rays. The height of the pentalith results in a ragged LM appearance. | |
![]() | ![]() | ![]() | ![]() | Micrantholithus hebecuspis Large Micrantholithus with deeply indented sides and blunt, flat-ended apices. | |
![]() | ![]() | ![]() | ![]() | Micrantholithus minimus A small (typically <4 µm) Micrantholithus with raised ridges along the line of the segment sutures that give the appearance of a deeply indented pentalith. Many specimens, however, have thin calcite between the raised, birefringent areas. | |
![]() | ![]() | Micrantholithus pinguis Medium sized Micrantholithus with deeply indented sides and elevated structure. | |||
Micrantholithus vesper Stellate Micrantholithus with deeply indented sides | |||||
very deeply indented sides | |||||
![]() | ![]() | ![]() | Micrantholithus attenuatus Stellate Micrantholithus with deeply indented sides and gracile, long rays. | ||
![]() | Micrantholithus mirabilis Micrantholithus with thickened central area and long extensions formed typically by single segments. | ||||
ornate species | |||||
Micrantholithus angulosus Arms end in a trilobate termination. most specimens thin with narrow arms. | |||||
![]() | ![]() | ![]() | Micrantholithus bramlettei Stellate pentalith with pointed rays and double indented sides. | ||
![]() | ![]() | ![]() | Micrantholithus bulbosus Micrantholithus with relatively straight edges and raised ridges around the sutures that widen at their ends. | ||
![]() | ![]() | ![]() | ![]() | Micrantholithus crenulatus Micrantholithus with crenulate edges. | |
Micrantholithus tinus Micrantholithus with bifurcate ray-like extension from each segment (sutures do not go along arms). Resembles a discoaster but evidently shows the birefringence of a pentalith and a specimen of M. concinnus with short rays is illustrated from the same sample so the identification seems well-founded. | |||||
![]() | ![]() | ![]() | ![]() | Micrantholithus sp. Specimens which cannot be assigned to established species |
Taxonomy:
Distinguishing features:
Parent taxon (Braarudosphaeraceae): Coccospheres pentagonal dodecahedra formed of five pentagonal plates
This taxon: Pentaliths with sutures emerging through corners; edge often indented giving stellate outline
Farinacci & Howe catalog pages: Micrantholithus * , Citrocalculus *
Morphology:
Ecology & Biogeography
See also: Micrantholithus - the genus also occurs in the Mesozoic;
Search data:LITHS: nannolith-radiate, pentagonal, CA: process, |
Lith size: 3->30µm; Segments: 5->5; Liths per sphere: 12->12 |
Geological Range:
Notes: Predominantly Palaeogene but it has been sporadically recorded in the Miocene - e.g. Moshkovitz & Ehrlich 1981
Last occurrence (top): at top of Sarmatian Paratethyan stage (100% up, 11.6Ma, in Tortonian stage). Data source: Total of ranges of the species in this database
First occurrence (base): within Paleocene Epoch (55.96-66.04Ma, base in Danian stage). Data source: Total of ranges of species in this database
Plot of occurrence data:
Bown, P. R., Rutledge, D. C., Crux, J. A. & Gallagher, L. T. (1998). Lower Cretaceous. In, Bown, P. R. (ed.) Calcareous Nannofossil Biostratigraphy. British Micropalaeontological Society Publication Series . 86-131. gs O Deflandre, G. & Fert, C. (1954). Observations sur les coccolithophoridés actuels et fossiles en microscopie ordinaire et électronique. Annales de Paléontologie. 40: 115-176. gs Deflandre, G. (1950a). Observations sur les Coccolithophoridés, à propos d'un nouveau type de Braarudosphaeridé, Micrantholithus, à éléments clastiques. Comptes rendus hebdomaire de l'Académie des sciences, Paris. 231: 1156-1158. gs Moshkovitz, S. & Ehrlich, A. (1981). Biostratigraphical problems of the Middle Miocene calcareous nannofossils and the palaeoecological significance of the Braaruudosphaerids in the coastal plain and offshore of israel. Geological Survey of Israel Current Research. 198: 43-47. gsReferences:
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Micrantholithus compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 28-4-2025
Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=855 Go to Archive.is to create a permanent copy of this page - citation notes |
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