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Hudson, R. G. S. (1944) On the Carboniferous Corals: Zaphrentites shunnerensis sp. nov. Geological Magazine, 81 (1) 45-48 doi:10.1017/s0016756800073842

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Reference TypeJournal (article/letter/editorial)
TitleOn the Carboniferous Corals: Zaphrentites shunnerensis sp. nov
JournalGeological Magazine
AuthorsHudson, R. G. S.Author
Year1944 (February)Volume81
Issue1
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800073842
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Mindat Ref. ID247366Long-form Identifiermindat:1:5:247366:0
GUID0
Full ReferenceHudson, R. G. S. (1944) On the Carboniferous Corals: Zaphrentites shunnerensis sp. nov. Geological Magazine, 81 (1) 45-48 doi:10.1017/s0016756800073842
Plain TextHudson, R. G. S. (1944) On the Carboniferous Corals: Zaphrentites shunnerensis sp. nov. Geological Magazine, 81 (1) 45-48 doi:10.1017/s0016756800073842
In(1944, February) Geological Magazine Vol. 81 (1) Cambridge University Press (CUP)
Abstract/NotesThe Shunner Fell Limestone is one of a group of calcareous shales and impure limestones, in all about fifteen feet thick, occurring in beds of Namurian age and Millstone Grit facies exposed on Shunner Fell, Wensleydale. The presence of Anthracoceras glabrum s.l. Bisat in these beds (Chubb and Hudson, 1925, p. 262) assigns them to the Arnsbergian (Upper Eumorphoceras Age, E2, Hudson and Cotton, 1943). Other fossils include small cornute corals, trilobites, gastropods such as Bellerophon and Euphemus, and brachiopods such as Athyris, Chonetes, Lingula, Schizophoria, Spirfer, and the spinose Productids. The occurrence of these beds and some of their fossils has been recorded by Goodchild (in Dakyns and others, 1891, p. 145), King (1914), and Chubb and Hudson (1925).


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