Note on<i>Campophyllum flexuosum</i>(Goldfuss)

Hill, Dorothy; Jull, R. K.

doi:10.1017/s001675680005322x

Cited by 5 publications

(1 citation statement)

References 7 publications

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“…Skolekophyllum Fomichev, 1953 is a cyathopsid with prominent lateral dissepiments and an amplexoid early stage. Originally, it was described as a subgenus of Campophyllum Milne-Edwards and Haime, 1850; the morphology of that genus was not well understood before the revision of Hill and Jull (1965). Similar features shared with Preisingerella are: occurrence in accumulations, minor septa short, well-developed lateral dissepiments.…”

Section: Systematic Paleontologymentioning

confidence: 99%

Large-sized Early Permian “caninioid” corals from the Karavanke Mountains, Slovenia

2016

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A new monospecific “caninioid” genus, Preisingerella n. gen., from the lower Permian of the Karavanke Mountains (Southern Alps, Slovenia) is erected. The type species is Preisingerella stegovnikensis n. sp. The new taxon can be differentiated from other Caninia-type genera by its specific ontogeny and features of its dissepimentarium. Corals with such morphology had a wide distribution during the Carboniferous and early Permian, occurring in mostly shallow-water carbonate rocks. The phylogenetic relationships within this group are mostly unclear due to similarities in the adult stages. The earlier stages reveal the main distinguishing features that are decisive for a generic assignment, but these have rarely been well preserved and properly considered. The new taxon is compared with related genera of the Cyathopsidae and species of Caninella Gorskiy, 1938 characterized by lateral dissepiments. Large numbers of specimens of the new species, representing a monospecific assemblage, have been collected from the Born Formation at Mt. Stegovnik. Sedimentological and microfacies characteristics, as well as macro- and microfossil assemblages, underline this correlation. The fusulinoidean assemblage of the Born Formation, with Sphaeroschwagerina carniolica (Kahler and Kahler, 1937), as the predominant species, corresponds to the time span between the Sphaeroschwagerina moelleri-Schwagerina fecunda and Pseudofusulina moelleri zones, indicating a late Asselian to early Sakmarian age in the Southern Urals.

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Section: Systematic Paleontologymentioning

confidence: 99%

Large-sized Early Permian “caninioid” corals from the Karavanke Mountains, Slovenia

2016

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Late Devonian (Famennian) rugose coral fauna of the Percha Shale of southwestern New Mexico

Sorauf

1992

J. Paleontol.

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Solitary rugose corals (Cnidaria, Rugosa) are common to abundant in the calcareous Box Member of the late Famennian Percha Shale (Lower expansa Zone) of southwestern New Mexico; the Box is best developed in the western part of the Percha outcrop belt. The corals include a number of forms characteristic of Strunian faunas throughout the world. Recognized here are Gorizdronia sp. cf. G. tenuis Rozkowska, Campophyllum? ursinum n. sp., Caninia cooperi n. sp., Siphonophyllia? folia n. sp., S.? corbicula n. sp., “Bothrophyllum” argenteum n. sp., “B.” argenteum argenteum n. subsp., “B.” argenteum bilateralis n. subsp., “B.” argenteum dibunophylloides n. subsp., Arachnolasmella elytra n. sp., and Cyathoclisia sp. A. This fauna is clearly ancestral to Carboniferous genera and species. Percha species, where represented by large populations, are seen to be remarkably variable, especially in axial structure.

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Givetian rugose corals from the northern margin of the Burdekin Basin, north Queensland

Zhen

1994

Alcheringa: An Australasian Journal of Palaeontology

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Note onCampophyllum flexuosum(Goldfuss)

Cited by 5 publications

References 7 publications

Large-sized Early Permian “caninioid” corals from the Karavanke Mountains, Slovenia

Large-sized Early Permian “caninioid” corals from the Karavanke Mountains, Slovenia

Late Devonian (Famennian) rugose coral fauna of the Percha Shale of southwestern New Mexico

Givetian rugose corals from the northern margin of the Burdekin Basin, north Queensland

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