Lithraphidites acutus subsp. eccentricus


Classification: Mesozoic -> Nannoliths inc sedis -> Microrhabdulaceae -> Lithraphidites -> Lithraphidites acutus -> Lithraphidites acutus subsp. eccentricus
Sister taxa: L. acutus subsp. acutus, L. acutus subsp. eccentricus,

Distinguishing features: Lithraphidites with four narrow, triangular processes projecting orthogonally from a position ⅔ to ¾ along the main rod.


Taxonomy:

Citation: Lithraphidites acutus subsp. eccentricus Watkins in Watkins & Bowdler, 1984
Rank: Sub-species
Synonyms:

Farinacci & Howe catalog pages: L. acutum eccentricum *

Distinguishing features: Lithraphidites with four narrow, triangular processes projecting orthogonally from a position ⅔ to ¾ along the main rod.


Morphology remarks: Lithraphidites acutus eccentricus and Lithraphidites acutus acutus were thought to be palaeobiogeographic variants by Watkins & Bowdler (1984).

Corbett & Watkins (2014), however, argue that eccentricus and acutus are separate species with overlapping ranges but with eccentricus only occuring during the lower part of thw range of  acutus (their text-fig.3). They also suggest redefining the difference between the taxa based on size (eccentricus > ca 10 µm vs. acutus < ca 10 µm) and/or lath structure (bilamellar in eccentricus vs monolamellar in acutus). Lath structure is probably not a good criterion since Janin (1998) presented strong evidence that all Lithraphidites nannoliths have bilamellar structure.

Search data:
TagsLITHS: nannolith-other, rod-shaped, CA: process, CROSS-POLARS: T-prominent,
MetricsLith size: 15->30µm; Segments: 4->4;
Data source notes: original description
The morphological data given here can be used on the advanced search page. See also these notes

Geological Range:
Last occurrence (top): within UC3c subzone (94.79-95.02Ma, top in Cenomanian stage). Data source: Corbett & Watkins 2014
First occurrence (base): within UC3a subzone (95.93-96.16Ma, base in Cenomanian stage). Data source: Corbett & Watkins 2014

Plot of occurrence data:

References:

Applegate, J. L. & Bergen, J. A. (1988). Cretaceous calcareous nannofossil biostratigraphy of sediments recovered from the Galicia Margin, ODP Leg 103. Proceedings of the Ocean Drilling Program, Scientific Results. 103: 293-348. gs V O

Bown, P. R. (2005c). Early to Mid-Cretaceous Calcareous Nannoplankton from the Northwest Pacific Ocean, Leg 198, Shatsky Rise. Proceedings of the Ocean Drilling Program, Scientific Results. 198: 1-82. gs V O

Corbett, M. J. & Watkins, D. K. (2014). Cenomanian through basal Coniacian Calcareous Nannofossil biostratigraphy of the Mancos Shale reference section, Mesa Verde National Park, CO. Stratigraphy. 11(1): 97-108. gs

Janin, M. -C. (1998). Remarques sur l'ultrastructure et les affinities biologiques des Lithraphidites, nannofossiles calcaires du Crétacé. Revue de Micropaléontologie. 41(4): 281-296. gs

Watkins, D. K. & Bowdler, J. L. (1984). Cretaceous calcareous nannofossils from Deep Sea Drilling Project Leg 77, southeast Gulf of Mexico. Initial Reports of the Deep Sea Drilling Project. 77: 649-674. gs V O


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Lithraphidites acutus subsp. eccentricus compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 29-9-2020

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