Neolenticulina variabilis (Reuss)

Hanagata, S & Nobuhara, T, 2015, Illustrated guide to Pliocene foraminifera from Miyakojima, Ryukyu Island Arc, with comments on biostratigraph, Palaeontologia Electronica (Cambridge, England) 33 (8), pp. 1-142 : 32

publication ID

https://doi.org/ 10.26879/444

persistent identifier

https://treatment.plazi.org/id/A029445F-E93E-FF9B-4A07-BE347059A5D5

treatment provided by

Felipe

scientific name

Neolenticulina variabilis (Reuss)
status

 

Neolenticulina variabilis (Reuss) View in CoL

Figures 11.16, 11.17 View FIGURE 11

1850 Cristellaria variabilis Reuss , p. 369, pl. 46, figs. 15, 16.

1866 Cristellaria peregrina Schwager , p. 245, pl. 7, fig. 89.

1903 Cristellaria variabilis Reuss — Millett (part XIV), pp. 256, 257, pl. 5, fig. 1.

1913 Cristellaria variabilis Reuss — Cushman, p. 70, pl. 36, figs. 1—3.

1938 “ Cristellaria ” peregrina Schwager — Asano (a), pl. 29, figs. 6, 7, 11.

1956 Lenticulina peregrina (Schwager) — Asano (a), p. 7, pl. 3, figs. 9, 17, 18.

1964 Lenticulina peregrina (Schwager) — LeRoy, p. F22, pl. 4, figs. 5, 6.

1968 Lenticulina peregrina (Schwager) — Huang, p. 58, pl. 13, fig. 35.

1977 Neolenticulina chathamensis McCulloch , p. 8, pl. 94, fig. 12.

1994 Neolenticulina variabilis (Reuss) — Jones, p. 80, pl. 68, figs. 11—16.

1994 Neolenticulina peregrina (Schwager) — Loeblich and Tappan, p. 69, pl. 124, figs. 1—11.

Remarks. Jones (1994) demonstrated that N. variabilis has precedence over L. peregrina ; we adopt this view.

Occurrence. Abundant in the Oura Formation, rare in the Onogoshi and Minebari formations.

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