Ennucula aegeensis ( Forbes, 1844 )
publication ID |
https://doi.org/ 10.11646/zootaxa.4186.1.1 |
publication LSID |
lsid:zoobank.org:pub:029B675F-776C-4CD6-9992-FA05AEADFA7B |
DOI |
https://doi.org/10.5281/zenodo.6082129 |
persistent identifier |
https://treatment.plazi.org/id/03C587A5-FFCA-F97B-FF3B-FE8263F9FA9A |
treatment provided by |
Plazi |
scientific name |
Ennucula aegeensis ( Forbes, 1844 ) |
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Ennucula aegeensis ( Forbes, 1844) View in CoL
Fig. 2 View FIGURE 2. a – b c–e
Nucula aegeensis Forbes, 1844 View in CoL (p. 192).
Nucula aegeensis Forbes—Jeffreys 1879 View in CoL (p. 581).
Lionucula tenuis aegeensis ( Forbes, 1843) — Nordsieck 1969 (p. 3, pl. 1, fig. 00.02).
Nucula tenuis aegeensis (Forbes) View in CoL — Di Geronimo & Panetta 1973 (p. 92, pl. 3, fig. 2).
Nucula (Leionucula) tenuis aegeensis Forbes—Di Geronimo 1974 (p. 153, pl. 5, figs. 1,4).
Nuculoma aegeensis Forbes, 1844 — Cossignani et al. 1992 (fig. 256).
Nucula aegeensis Forbes, 1844 View in CoL — Poppe & Goto 1993 (p. 38, pl. 1, fig. 19).
Ennucula aegeensis ( Forbes, 1844) View in CoL — Salas 1996 (p. 38, figs. 16–18); La Perna 2003 (p. 23, pl. 1, fig. 3); Repetto et al. 2005 (p. 282, mid left fig.); Mastrototaro et al. 2010 (fig. 5 k).
Ennucula aegensis [sic] ( Forbes, 1844)— Giannuzzi-Savelli et al. 2001 (p. 48, figs. 26–28).
Ennucula aegeensis (Forbes) View in CoL —Rosso et al. 2010 (fig. 11 D).
Diagnostic characters. Suboval outline; inner ventral margin not crenulated; low weak commarginal cords, more evident on later growth stages. Prodissoconch: shell type ST-1B; P-1: length about 290 µm; ellipsoidal outline; convex, slightly asymmetrical profile; smooth surface except for the cicatrix area; transition to the nepioconch well marked.
Occurrence. Box-corer samples BC04 (7 specimens), BC05 (5), BC11 (1), BC66 (5), BC71 (5), BC72 (94); cores BC04 (4), BC05 (22), BC21 (33), BC51 (33), BC67 (1), BC72 (30). Maximum length: 5 mm.
Distribution and habitat. Ennucula aegeensis is an almost exclusively Mediterranean species, with some citations from the Lusitanian province; it occurs on mud and coral debris from the circalittoral zone to over 2800 m depth ( Nordsieck 1969; Poppe & Goto 1993; Pons-Moyà & Pons 1999). It was regarded as an exclusive characteristic taxon of VP (bathyal mud) biocoenosis (Di Geronimo 1979[a]; Di Geronimo et al. 1982) and characterizes the Abra-Nucula biocoenosis in the bathyal of Taranto ( Di Geronimo & Panetta 1973). In the Santa Maria di Leuca CWC biotope, it was found on the muddy bottoms around the coral colonies (Mastrototaro et al. 2010), being abundant in mollusk mud, and common in coral rubble and foraminifer mud thanatofacies (Rosso et al. 2010).
Fossil record. Pliocene of Italy ( Tabanelli 2008); probably also Pleistocene of the Mediterranean ( La Perna 2003).
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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Ennucula aegeensis ( Forbes, 1844 )
Negri, Mauro Pietro & Corselli, Cesare 2016 |
Nucula aegeensis Forbes—Jeffreys 1879
Forbes-Jeffreys 1879 |
Nucula aegeensis
Forbes 1844 |
Nuculoma aegeensis
Forbes 1844 |
Nucula aegeensis
Forbes 1844 |
Ennucula aegeensis (
Forbes 1844 |
Lionucula tenuis aegeensis (
Forbes 1843 |