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Johnson, G. A. L. (1957) The Goniatite Girtyoceras cf. weetsense Moore from the shales above the Jew Limestone, Northumberland. Geological Magazine, 94 (3) 229-234 doi:10.1017/s001675680006859x

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Reference TypeJournal (article/letter/editorial)
TitleThe Goniatite Girtyoceras cf. weetsense Moore from the shales above the Jew Limestone, Northumberland
JournalGeological Magazine
AuthorsJohnson, G. A. L.Author
Year1957 (June)Volume94
Issue3
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s001675680006859x
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Mindat Ref. ID248666Long-form Identifiermindat:1:5:248666:0
GUID0
Full ReferenceJohnson, G. A. L. (1957) The Goniatite Girtyoceras cf. weetsense Moore from the shales above the Jew Limestone, Northumberland. Geological Magazine, 94 (3) 229-234 doi:10.1017/s001675680006859x
Plain TextJohnson, G. A. L. (1957) The Goniatite Girtyoceras cf. weetsense Moore from the shales above the Jew Limestone, Northumberland. Geological Magazine, 94 (3) 229-234 doi:10.1017/s001675680006859x
In(1957, June) Geological Magazine Vol. 94 (3) Cambridge University Press (CUP)
Abstract/NotesAbstractA new Yoredale goniatite locality in the shales above the Jew Limestone (Lower Carboniferous) at Temon, near Greenhead, Northumberland, has yielded a fauna including Girtyoceras cf. weetsense Moore; a lower P2 age (Bollandian) is indicated. The fauna and lithology of the goniatite-bearing shale is described and the lateral correlation of the Jew Limestone discussed. It is suggested that the base of the Jew (= Hardraw = Oxford) Limestone is the most satisfactory horizon for the P1–P2 boundary in the northern Pennines.


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