Ammobaculites agglutinans ( d’Orbigny, 1846 )

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 : 41

publication ID

https://doi.org/ 10.26879/660

persistent identifier

https://treatment.plazi.org/id/03B7056B-2B65-0A1D-FF37-F9D9F828FE37

treatment provided by

Felipe

scientific name

Ammobaculites agglutinans ( d’Orbigny, 1846 )
status

 

Ammobaculites agglutinans ( d’Orbigny, 1846) View in CoL

Figure 19.11 View FIGURE 19

1846 Spirolina agglutinans ; d’Orbigny, p. 137, pl. 7,

figs. 10-12. 2005 Ammobaculites agglutinans (d’Orbigny) ;

Kaminski and Gradstein, p. 324, pl. 70, figs. 1-

8. Material. Two specimens from two samples. Description. Test free, robust, initially planispiral involute coil, becoming uniseriate in the last chambers. The coiled portion consists of 4–5 chambers in the last whorl, separated by straight and depressed sutures. The uniseriate stage is rectilinear, composed of low, circular in section, chambers separated by indistinct sutures. Aperture terminal at the end of the ultimate chamber. Wall medium to coarse agglutinated.

Distribution. Late Cretaceous–Recent ( Kaminski and Gradstein, 2005).

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