Daughter taxa (time control age-window is: 0-800Ma)![]() | ||||
![]() | ![]() | Lophodolithus acutus Large Lophodolithus with an asymmetric wing at one end and a distinctive angular ‘corner’ at the other end, where the rim side and end meet. Central area with disjunct, complex, tranverse bar. | ||
Lophodolithus luntii Bilaterally symmetrical Lophodolithus without a bar | ||||
![]() | Lophodolithus mochlophorus Large Lophodolithus with a broad, near-symmetric wing at one end and central area spanned by a disjunct tranverse bar. Rim is narrowly elliptical at the opposite end to the wing. | |||
![]() | ![]() | ![]() | ![]() | Lophodolithus mytiliformis Strongly asymmetric Lophodolithus with prominent wing and wide bar |
![]() | Lophodolithus nascens Large, slightly asymmetric Lophodolithus with a narrow, asymmetric wing at one end; central area with disjunct tranverse bar. | |||
Lophodolithus reniformis Lophodolithus with kidney-shaped ouline. | ||||
![]() | Lophodolithus rotundus Large to very large, broadly elliptical to subcircular Lophodolithus with a very broad (~half the length of the rim), near-symmetric wing at one end. No central area structures observed. Wing elements clearly visible in LM. | |||
Lophodolithus sp. Specimens which cannot be assigned to any established species |
Taxonomy:
Distinguishing features:
Parent taxon (Zygodiscaceae): Muroliths with rim formed from well-developed V- and variably developed R-units, with opposite imbrication directions, and central area structures that include disjunct transverse bars and diagonal crosses. R-units vestigial or not observed in several genera (Chiphragmalithus, Isthmolithus, Neococcolithes).
This taxon: Modified muroliths with high walls (higher at one end and forming an asymmetric flange) and wide central area usually spanned by a disjunct, complex tranverse bar.
Farinacci & Howe catalog pages: Lophodolithus *
Search data:
LITHS: murolith, asymmetric, elliptical, CA: ca_disjunct, bar, CROSS-POLARS: rim-bicyclic, V-prominent, R-prominent, |
Lith size: 8->23µm; |
Geological Range:
Last occurrence (top): at top of NP16 zone (100% up, 40.4Ma, in Bartonian stage). Data source: Total of ranges of the species in this database
First occurrence (base): within NP6 zone (58.97-59.54Ma, base in Selandian stage). Data source: Total of ranges of species in this database
Plot of occurrence data:
Deflandre, G. & Fert, C. (1954). Observations sur les coccolithophoridés actuels et fossiles en microscopie ordinaire et électronique. Annales de Paléontologie. 40: 115-176. gs Perch-Nielsen, K. (1981). New Maastrichtian and Paleocene calcareous nannofossils from Africa, Denmark, and USA and the Atlantic, and some Paleocene lineages. Eclogae Geologicae Helvetiae. 74(3): 831-863. gs OReferences:
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Lophodolithus compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 10-12-2023
Short stable page link: https://mikrotax.org/Nannotax3/index.php?id=829 Go to Archive.is to create a permanent copy of this page - citation notes |
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