File:Geological magazine (1882) (14595448077).jpg

Identifier: geologicalmagazi29wood (find matches)
Title: Geological magazine
Year: 1882 (1880s)
Authors: Woodward, Henry, 1832-1921, ed
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Publisher: London (etc.) Cambridge University Press
Contributing Library: Harvard University, Museum of Comparative Zoology, Ernst Mayr Library
Digitizing Sponsor: Harvard University, Museum of Comparative Zoology, Ernst Mayr Library

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established themselves uponit. Not only did it do this, but it carried off part of the oldermoraine and incorporated this into its own, the lower part of this, inwhich chalk is plentiful, being largely made up of the older morainereconstructed, and sheets of the old moraine thus carried oif are atDimlington and near the site of the Talbot Inn to be seen alternatingwith sheets of the newer moraine in the lower part of the latter. So far from what Mr. Lamplugh had to show invalidating myassertion that the shells lived where they occur, his descriptionsappear to me in the fullest way, as far as they go, to confirm notonly this assertion, but the whole process which I have traced.February 6, 1882. Seakles V. WoOD. Errata in the February Number, 1882. p. 94, line 10 from bottom,/or Upper White Lias, 7-ead Upper Lias.p. 96, for Transactions of the Bath Literary and Philosophical Association, readProceedings of the Bath Natural History and Antiquarian Field Club. DECADE II.VOL .IX. PLATE V.
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OxfordiaxL and Lower Oolite Gasteiopoda, Iforkshire. G-.M.WoodbWocrol/ oLel. efcUtJi.. West.Kawmooi. a.C?im.p. THE GEOLOGICAL MAGAZINE, NEW SERIES. DECADE II. VOL. IX. No. v.—MAY, 1882. I.—Contributions to the Paleontology of the Yorkshire Oolites. By Wilfrid H. Hudleston, M.A., F.G.S. President Geologists Association. (Continued from page 151.) (PLATE V.) Genns Fusus, Lamarck, 1799. THE number of fossil species of Fusus is considerable, but theydo not date back from a very high antiquity. None areenumerated by Tate and Blake from the Lias of Yorkshire. Certainforms from the Upper Lias of Normandy, referred by Deslong-champs to Fusus, have not been accepted as such, and the first ofthe genus admitted by DOibigny is Fusus noclulosus, Desl., from theGreat Oolite of Langrune. Even this almost comes within the genusBrachytrema of Lycett (Ool. Moll. p. 24), instituted to include somesmall turbinated forms with highly ornamented whorls and a shortoblique canal. Fusus multicostatus, M. a

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