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Fig. 6 | Swiss Journal of Palaeontology

Fig. 6

From: Evolutionary prospection in the Neogene planktic foraminifer Globorotalia menardii and related forms from ODP Hole 925B (Ceara Rise, western tropical Atlantic): evidence for gradual evolution superimposed by long distance dispersal?

Fig. 6

Mean radius of the upper osculating circle (R up) in keel view (μm) per sample through time (Ma) at Hole 925B for G. menardii (a), G. limbata (b), and G. multicamerata (c). In d means of R up of the three groups are compared to each other. See Fig. 5 for explanation of symbols. For explanation of the radius of the upper osculating circle R up refer to Fig. 4. Measurements and statistics can be read from Tables 4a–c and 5a–c in the electronic supplementary materials

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