Foraminifera taxon details

Ercumentina sayqensis Serra-Kiel & Vicedo, 2016 †

1312518  (urn:lsid:marinespecies.org:taxname:1312518)

accepted
Species
marine, brackish, fresh, terrestrial
fossil only
Serra-Kiel, J.; Vicedo, V.; Razin, P.; Grélaud, C. (2016). Selandian-Thanetian larger foraminifera from the lower Jafnayn Formation in the Sayq area (eastern Oman Mountains). <em>Geologica Acta.</em> 14(3): 315-333.
page(s): p. 321, figs. 5.1-5.9 (holotype fig. 5.1). [details] Available for editors  PDF available [request]
Original description Diagnosis. Shells with porcelaneous wall and multiple apertures. Microspheric forms unknown. Flexostylic megalosphere...  
Original description Diagnosis. Shells with porcelaneous wall and multiple apertures. Microspheric forms unknown. Flexostylic megalosphere followed by chambers with planispiral, involute arrangement. Alveolar exoskeleton composed of several beams and one generation of rafters. Endoskeleton restricted to slight ridges. Ridges fused with beams at the proximal part of the chamber. Multiple foramina distributed in two rows and aligned from one chamber to the next. Foramina of the lower row regularly alternated with ridges. Additional foramina irregularly distributed in a second upper row.
(Serra-Kiel et al. (2016)). [details]
Hayward, B.W.; Le Coze, F.; Vachard, D.; Gross, O. (2025). World Foraminifera Database. Ercumentina sayqensis Serra-Kiel & Vicedo, 2016 †. Accessed at: https://marinespecies.org/foraminifera/aphia.php?p=taxdetails&id=1312518 on 2026-04-15
Date
action
by
2018-12-01 11:50:27Z
created

original description Serra-Kiel, J.; Vicedo, V.; Razin, P.; Grélaud, C. (2016). Selandian-Thanetian larger foraminifera from the lower Jafnayn Formation in the Sayq area (eastern Oman Mountains). <em>Geologica Acta.</em> 14(3): 315-333.
page(s): p. 321, figs. 5.1-5.9 (holotype fig. 5.1). [details] Available for editors  PDF available [request]
From editor or global species database
Original description Diagnosis. Shells with porcelaneous wall and multiple apertures. Microspheric forms unknown. Flexostylic megalosphere followed by chambers with planispiral, involute arrangement. Alveolar exoskeleton composed of several beams and one generation of rafters. Endoskeleton restricted to slight ridges. Ridges fused with beams at the proximal part of the chamber. Multiple foramina distributed in two rows and aligned from one chamber to the next. Foramina of the lower row regularly alternated with ridges. Additional foramina irregularly distributed in a second upper row.
(Serra-Kiel et al. (2016)). [details]
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