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Miscellany

Erratum

This article refers to:
Gastropods and tergomyans from the Upper Ordovician (Viru–Harju) of the Fågelsång area, Scania, southern Sweden

Ebbestad, J. O. R., Högström, A. E. S. & Frisk, Å. M. 2013. Gastropods and tergomyans from the Upper Ordovician (Viru–Harju) of the Fågelåsng area, Scania, southern Sweden. Journal of Systematic Palaeontology, 11, 295–336.

The authors have noted the following errors in their article. Taylor & Francis apologises for these errors.

P. 297, : revised figure (see below)

Figure 2. Stratigraphy of the uppermost Middle Ordovician and Upper Ordovician of the Fågelsång area, showing lithology and fossil ranges. Chitinozoan zonation is based on Nõlvak & Grahn (1993), Bergström et al. (2000), Vandenbroucke (2004) and Grahn & Nõlvak (2007a). Graptolite zonation is based on Bergström & Nilsson (1974), Nilsson (1977) and Bergström et al. (2000). Conodont zonation is based on Bergström (1971, 2007a, b), Bergström & Nilsson (1974), and Bergström et al. (2000). The sections and lithostratigraphy are based on Lindström (1953), Glimberg (1961), Jaanusson (1964), Bergström & Nilsson (1974), Nilsson (1979), Bergström et al. (1999, 2002), Bergström (2007a). Major recognized K-bentonites are marked in the Koängen section (Gr = Grimstorp complex, K = Kinnekulle, S = Sinsen, GB = Grefsen). Note that the facies of the various sections are simplified, and only a few key beds are included.

Figure 2. Stratigraphy of the uppermost Middle Ordovician and Upper Ordovician of the Fågelsång area, showing lithology and fossil ranges. Chitinozoan zonation is based on Nõlvak & Grahn (1993), Bergström et al. (2000), Vandenbroucke (2004) and Grahn & Nõlvak (2007a). Graptolite zonation is based on Bergström & Nilsson (1974), Nilsson (1977) and Bergström et al. (2000). Conodont zonation is based on Bergström (1971, 2007a, b), Bergström & Nilsson (1974), and Bergström et al. (2000). The sections and lithostratigraphy are based on Lindström (1953), Glimberg (1961), Jaanusson (1964), Bergström & Nilsson (1974), Nilsson (1979), Bergström et al. (1999, 2002), Bergström (2007a). Major recognized K-bentonites are marked in the Koängen section (Gr = Grimstorp complex, K = Kinnekulle, S = Sinsen, GB = Grefsen). Note that the facies of the various sections are simplified, and only a few key beds are included.

P. 299, paragraph 4, line 4 should read:

Frisk and Harper (2011) have shown that Sericoidea can occupy a wider range of environments, in Tvären, Sweden where large concentrations are found in shallower water settings. Generally Sericoidea is not mixed with the deeper distinctive Foliomena fauna.

P. 305, paragraph 3, line 14: (Harper & Stewart 2007) should read (Harper & Stewart 2008).

P. 329, : revised figure (see below)

Figure 15. A–O, Straparollina? norvegica (Koken in Koken & Perner, 1925). A–B, lectotype (PMO 20274), Royal palace in Oslo, Norway. C, D, paralectotype (PMO 36993), Hovindsholm on Helgøya, Mjøsa district, Norway. E–J, internal mould (LO 11303t), Koängen drill core, Fågelsång, Sweden, 32.77–32.82 m. K, partial specimen (LO 11304t), Koängen drill core, Fågelsång, Sweden, 29.90–29.91 m. L–O, Palaeomphalus sp. (PMO 72798), Cephalopod Limestone Member, Elnes Formation (Uhaku), Hovindsholm, Mjøsa district, Norway; figured by Yochelson (1963, pl. 4, figs 3, 6, 9). Scale bars: A–I, K–N = 5 mm; J, O = 1 mm.

Figure 15. A–O, Straparollina? norvegica (Koken in Koken & Perner, 1925). A–B, lectotype (PMO 20274), Royal palace in Oslo, Norway. C, D, paralectotype (PMO 36993), Hovindsholm on Helgøya, Mjøsa district, Norway. E–J, internal mould (LO 11303t), Koängen drill core, Fågelsång, Sweden, 32.77–32.82 m. K, partial specimen (LO 11304t), Koängen drill core, Fågelsång, Sweden, 29.90–29.91 m. L–O, Palaeomphalus sp. (PMO 72798), Cephalopod Limestone Member, Elnes Formation (Uhaku), Hovindsholm, Mjøsa district, Norway; figured by Yochelson (1963, pl. 4, figs 3, 6, 9). Scale bars: A–I, K–N = 5 mm; J, O = 1 mm.

P. 329, heading Straparollina? norvegica (Koken in Koken & Perner, 1925): (A–K)

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