Damonella grandiensis Tomé et al., 2014
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publication ID |
https://doi.org/ 10.11646/zootaxa.5159.4.4 |
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publication LSID |
lsid:zoobank.org:pub:D3D2D54E-4B22-45FC-9904-FBB8BEF2E601 |
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DOI |
https://doi.org/10.5281/zenodo.6794802 |
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persistent identifier |
https://treatment.plazi.org/id/31296775-CE7E-FFFF-86B7-F8EA9DFDFAC4 |
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treatment provided by |
Plazi |
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scientific name |
Damonella grandiensis Tomé et al., 2014 |
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Damonella grandiensis Tomé et al., 2014
Fig. 3P–R View FIGURE 3
1992 Mantelliana (?) sp.—Colin et al., p. 368, plate 3, fig. 1.
1999 Ostracode 207—Neumann, p. 93, figs. 2–4.
2002 Ostracode 207— Coimbra et al., p 691, plate IV, fig. 31.
2006 Candona sp —Ramos et al., p. 344, fig. 4.
2010 Damonella sp. — Tomé & Lima Filho, p. 63, plate. 2 (a–c).
2013 Candona ? sp.—Do Carmo et al., p. 95 and 103, fig. 5, nº.12–14.
2014 Damonella grandiensis —Tomé et al., p. 163, fig.10 A–D.
Non 2014 Damonella grandiensis —Tome et al., p. 163, fig. 10 (D–F) and 167, fig. 10 (G–M).
Non 2015 Damonella aff. grandiensis —Trabelsi et al., p. 10, fig. 5D, 1–3.
2017 Damonella grandiensis —Souza et al., p. 9, fig. 1, G–I.
Non 2021 Damonella grandiensis —Araripe et al., p. 6, fig. 5 (M–P).
2022 Damonella grandiensis —Araripe et al., p. 7, fig. 5 (10a–b).
Illustrated material. Adult shell, Nº. DGEO-CTG-UFPE-1513. Illustrated material from the Santo Antonio section (2.65 m).
Dimension. Nº. DGEO-CTG-UFPE-1513 ( Fig. 3 P–R View FIGURE 3 ); L= (LV) 0.576 / ( RV) 0.611 mm, H= 0.325 mm, and W= 0.245 mm.
Comparison. Material compared to D. grandiensis (Nº DGEO-CTG-UFPE-1157 and Nº-DGEO-CTG-UFPE- 1158) described and deposited by Tomé et al. (2014) in the Ivan de Medeiros Tinoco Microfossils Collection. The comparison was satisfactory, with the exception of the specimen Nº. DGEO-CTG-UFPE-1157, since they presented identical outlines and posterodorsal and ventral overlapping.
Occurrence and associated fauna. It was recorded in the Santo Antonio section, in all depths and associated with all species. It is the only species that occurs associated with the nannofossils Thoracosphaera sp. and Biscutum sp. (Araripe at al. 2022).
Observations. Tomé et al. (2014) emphasize the sexual dimorphism of this species and describe the male form, however in the present study these forms are described as distinct species, mainly due to the different outlines, since both specimens are smooth.
Stratigraphic distribution. In Africa, it has been commonly recorded in the d’Hama-Koussou Basin, Lower Cretaceous (Aptian) ( Colin et al. 1992). In Brazil, it has been recorded in the Araripe Basin, Crato Formation (Neumann 1999), Aptian; Grajaú Basin, Codó Formation, lower Aptian ( Ramos et al. 2006); Cedro Basin, Crato Formation, upper Aptian (Tomé 2007; Tome & Lima Filho 2010); Potiguar Basin, Alagamar Formation, Aptian ( Do Carmo et al. 2013). In the Sergipe / Alagoas Basin, Krommelbein & Weber (1971) observed the occurrence of this species and called it Ostracode 207 (Nº SMF Xe-22592), which is stored in slide PIA-3-AL (obtained from a depth of 900 to 930 m) in Frankfurt ( Tomé et al. 2014). Additionally found in the Jatobá Basin, Serra Negra Formation, in the strata correlated to the Crato Formation, upper Aptian ( Tomé et al. 2014), and this study in the Araripe Basin, Romualdo Formation, upper Aptian and lower Albian.
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Collection of Leptospira Strains |
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