Heterocoenia inflexa

Baron-Szabo, Rosemarie Christine, Tschanz, Karl & KÜrsteiner, Peter, 2022, Scleractinian corals from the Lower Cretaceous of the Alpstein area (Anthozoa; Vitznau Marl; lower Valanginian) and a preliminary comparison with contemporaneous coral assemblages, Swiss Journal of Palaeontology (3) 141 (1), pp. 1-61 : 33

publication ID

https://doi.org/10.1186/s13358-021-00238-8

persistent identifier

https://treatment.plazi.org/id/0390879F-3871-FF87-2E07-FE05E470F973

treatment provided by

Felipe

scientific name

Heterocoenia inflexa
status

 

Heterocoenia inflexa ( Eichwald, 1865 –69)

Figs. 10A–B View Fig

*1865–69 Stereopsammia inflexa m.: Eichwald, vol. 2, p. 164, Pl. 11, Fig. 2a–b View Fig .

1888 Latusastraea provincialis, d’Orb. sp.: Solomko, Geyer 1954 p. 76–77.

1907 Latusastraea? inflexa Eichw. : Karakash, p. 262. 2002 Latusastraea exigua Fromentel, 1862 : Kuzmicheva, p. 126, Pl. 8, Fig. 3. View Fig

v2018 Heterocoenia cf. inflexa ( Eichwald, 1865 –69): Baron-Szabo, p. 84, Pl. 12, Fig. G.

v2021 b Heterocoenia inflexa ( Eichwald, 1865 –69): Baron-Szabo, p. 77, Pl. 13, Fig. F.

Dimensions of skeletal elements. Great diameter of corallites: 1–1.8 mm, up to around 3 mm when wall exceptionally thick (around 0.5 mm or larger); great diameter of corallites (lumen): 0.8–1.8 mm; septa/corallite: 1–12; distance of corallite centers: 1.2– 3 mm, in areas of intense budding around 1 mm.

Description. Small submassive to subramose colony; corallites plocoid to cerio-plocoid, cerioid when crowded, oval to irregularly shaped in outline, regularly disposed over the colony; septa arranged bilaterally; in some corallites, septal arrangement in 3 systems present; one major septum present; remaining septa highly irregularly developed including very thin and half the length of major septum, or very short, spine-like; axial end of major septum rhopaloid or cuneiform; costae short and thin, up to twice the number of septa.

Type locality of species. Valanginian–lower Hauterivian of Ukraine .

Distribution. Upper Berriasian (upper Őhrli Formation [= Oerfla Formation]) of western Austria, lower Valanginian of northeastern Switzerland (Vitznau Marl, Wart; this paper), Valanginian–lower Hauterivian of Ukraine, upper Barremian–lower Aptian of western Austria (Schrattenkalk Formation, Vorarlberg), lower Aptian of southern Germany (Upper Schrattenkalk, Bavaria).

Material. NMSG Coll. PK–2.10.31d (= 2.10.32b).

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