Trochamminoides velascoensis Cushman, 1926

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 : 35

publication ID

https://doi.org/ 10.26879/660

persistent identifier

https://treatment.plazi.org/id/03B7056B-2B6F-0A17-FF39-FB43FD6FF944

treatment provided by

Felipe

scientific name

Trochamminoides velascoensis Cushman, 1926
status

 

Trochamminoides velascoensis Cushman, 1926 View in CoL

Figure 18.4 View FIGURE 18

1926 Trochamminoides velascoensis ; Cushman, p. 583, pl. 15, fig. 2a, b.

2005 Trochamminoides velascoensis (Cushman) ; Kender, Kaminski, and Cieszkowski, p. 264, fig. 12K.

Material. Three specimens from three samples.

Description. Test free, subcircular in outline, planispirally coiled. Numerous subrectangular and flattened chambers (10 in the last whorl). Suture few evident.

Distribution. Trochamminoides velascoensis was firstly described from the Velasco Formation of Mexico ( Cushman, 1926), and recently signaled from the Eocene of Carpathians ( Kender et al., 2005).

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