Distinguishing features: Typical small to medium Zeugrhabdotus - used as default identification by many workers - a modern name would be Z. howei
Taxonomy:
Farinacci & Howe catalog pages: Z. elegans + *
Distinguishing features: Typical small to medium Zeugrhabdotus - used as default identification by many workers - a modern name would be Z. howei
Search data:Tags | LITHS: |
Metrics | Lith size: 0->0µm; |
Geological Range:
Last occurrence (top): within Maastrichtian Stage (66.04-72.05Ma, top in Maastrichtian stage). Data source: [JRY rough estimate]
First occurrence (base): within Cretaceous Period (66.04-145.01Ma, base in Berriasian stage). Data source: [JRY rough estimate]
Plot of occurrence data:
Gale, A. S., Kennedy, W. J., Burnett, J. A., Caron, M. & Kidd, B. E. (1996). The Late Albian to Early Cenomanian succession at Mont Risou, near Rosans (Drôme, SE France): an integrated study (ammonites, inoceramids, planktonic foraminifera, nannofossils, oxygen and carbon isotopes). Cretaceous Research. 17: 515-606. gs Gartner, S. (1968). Coccoliths and related calcareous nannofossils from Upper Cretaceous deposits of Texas and Arkansas. University of Kansas Paleontological Contributions, Articles. 48 (Protista 1): 1-56. gs V O Kennedy, W. J. et al. (2000). Integrated stratigraphy across the Aptian-Albian boundary in the Marnes Bleues, at the Col de Pre _-Guittard, Arnayon (Drome), and at Tartonne (Alpes-de-Haute-Provence), France: a candidate Global Boundary Stratotype Section and Boundary Point for the base of the Albian Stage. Cretaceous Research. 21: 591-720. gs Roth, P. H. & Thierstein, H. R. (1972). Calcareous nannoplankton: Leg 14 of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project. 12: 546-559. gs V OReferences:
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Zeugrhabdotus elegans compiled by Jeremy R. Young, Paul R. Bown, Jacqueline A. Lees viewed: 5-3-2021
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