Anomalinoides glabratus (Cushman)

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 : 113

publication ID

https://doi.org/ 10.26879/444

persistent identifier

https://treatment.plazi.org/id/A029445F-E953-FFF6-48B5-BDF370B3A12E

treatment provided by

Felipe

scientific name

Anomalinoides glabratus (Cushman)
status

 

Anomalinoides glabratus (Cushman)

Figures 33.1, 33.2 View FIGURE 33

1924 Anomalina glabrata Cushman , p. 39, pl. 12, figs. 5—7.

1941 Anomalina glabrata Cushman — LeRoy (Part 2), p. 88, pl. 3, figs. 16—18; LeRoy (Part 3), p. 119, pl. 2, figs. 19—21.

1944 Anomalina glabrata Cushman — LeRoy (Part 2), p. 92, pl. 6, figs. 16—18.

1959 Anomalina glabrata Cushman — Graham and Militante, p. 115, pl. 19, fig. 8.

1964 Anomalina glabrata Cushman — LeRoy, p. F43, pl. 6, figs. 8—10.

1966 Anomalina glabrata Cushman — Belford, p. 177, pl. 32, figs. 1—7.

1989 Anomalina glabrata Cushman — Ōki, pl. 21, fig. 4.

Remarks. The genus Anomalina is problematic because d'Orbigny did not assign a holotype for its type species, A. punctulata , no specimens from the type area can be located, and d'Orbigny's original figures were not clear. Hansen and Rögl (1980) suggested that the use of this genus be suppressed, and we follow their convention here.

Occurrence. Common in the Onogoshi and Minebari formations, rare in the Yonahama Formation.

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