Psammosiphonella cylindrica ( Glaessner, 1937 )

Benedetti, A, 2017, Eocene / Oligocene deep-water agglutinated foraminifers (DWAF) assemblages from the Madonie Mountains (Sicily, Southern Italy), Palaeontologia Electronica 20 (1), pp. 1-66 : 20

publication ID

https://doi.org/ 10.26879/660

persistent identifier

https://treatment.plazi.org/id/03B7056B-2B5E-0A26-FF3B-FEFBFEF7FBDC

treatment provided by

Felipe

scientific name

Psammosiphonella cylindrica ( Glaessner, 1937 )
status

 

Psammosiphonella cylindrica ( Glaessner, 1937) View in CoL

Figure 12.4-5 View FIGURE 12

1937 Rhabdammina cylindrica ; Glaessner, p. 354, pl. 1, fig. 1.

1952 Psammosiphonella cylindrica (Glaessner) ; Avnimelech, p. 65.

1992 Rhabdammina cilindrica ; Glaessner; Morlotti and Kuhnt, p. 223, pl. 2, fig. 1.

2005 Psammosiphonella cylindrica (Glaessner) ; Kaminski and Gradstein, p. 119, pl. 5/6, fig. 9- 13.

2009 Rhabdammina cylindrica (Glaessner) ; Kender, Kaminski and Jones, p. 492, pl. 1, fig. 1.

Material. 238 specimens from 21 samples.

Description. Test tubular with circular section. Wall thick, composed of quartz grains dispersed in siliceous cement. Surface rough, aperture a simple terminal opening. Against the light is clearly visible the central siphon.

Distribution. Known in flysh-type deposits from the Cretaceous.

Remarks. Psammosiphonella cylindrica differs from Rhabdammina discreta Brady, 1884 in the absence of constrictions, and in having smoother surface. Psammosiphonella linearis is smaller and thinner, and has a more evident siphon.

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