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References
Paratype, BM(NH) No. ZF. 2369, illustrated in Brady, H. B., Rep. Voy. Challenger, 9 (Zool.), Pl. 84, Fig. 8 (1884); cf. S. dehiscens dehiscens, lectotypified by Banner and Blow, Contr. Cushman Found., 11, 35, Pl. 7, Fig. 3 (1960).
Forms referred (auctt.) to G. multicamerata from Recent seas are referable to G. cultrata (s.1.) et al.
Banner, F. T., and Blow, W. H., Nature, 207, 1351 (1965).
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G. sicanus de Stefani, Plinia, 3, 9 (1952) is regarded as a synonym of G. bisphericus Todd, Amer. J. Sci., 252, 681 (1954).
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‘Globigerina wilsoni bolivariana Petters’, Contr. Cushman Found., 5, 39 (1954) is represented by a single specimen (holotype) in the U.S. National Museum; our examination of this specimen has shown it to be so similar to Globorotalia opima opima Bolli, 1957, that we suspect that its supposed provenance from the Middle Eocene is incorrect; if the two taxa prove to be synonymous, bolivariana is the senior species-name, but more specimens would be necessary to establish this, because the holotype may be an atypical homoeomorph. In our work, the species G. opima opima is maintained for nomenclatorial stability.
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Globigerina sellii does not occur below Zone P.19, but it is known to persist to within Zone N.3.
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Series named by Papp, A., Mitt. Geol. Ges. Wien, 56, 240 (1963); zonation after Kapounek, J., et al., Sond. Erdoel-Erdgas-Zeitschr., 8, 109 (1965).
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Described by Gignoux, M., Ann. Univ. Lyon, 36, 35 (1913), as typical of his Calabrian stage as proposed in C.R. Acad. Sci., Paris, 150, 841 (1910).
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BANNER, F., BLOW, W. Progress in the Planktonic Foraminiferal Biostratigraphy of the Neocene. Nature 208, 1164–1166 (1965). https://doi.org/10.1038/2081164a0
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DOI: https://doi.org/10.1038/2081164a0
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