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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