Published online by Cambridge University Press: 01 May 2009
The two Cephalopods—an Ammonoid and a Belemnoid—referred to in the present note were obtained in the summer of 1907 by Dr. A. P. Young from the Tarntaler Köpfe, an isolated mountain-mass in Tyrol, to the north of the Tuxer Alps, and about 20 kilometres south-east of Innsbruck. The Ammonoid was found “at a height of nearly 2500 metres above sea-level, on the surface of a scree-cone which has accumulated under the high hanging valley known as the Lower Tarntal”, and the Belemnoid was found “somewhat lower on the slope of the same cone”. They are the fossils referred to by Dr. A. P. Young on p. 342 of his paper on the Structure and Physiography of the Tarntal Mass, published in the August number of this Magazine (pp. 339–346), where a photograph of the scree-cone is given (Pl XVII, Fig. 5), and now form part of the National Collection.
Published by permission of the Trustees of the British Museum.
page 443 note 3 British Museum (Natural History), register number C. 12113.
page 444 note 1 Parona, C. F., “Contribuzione alla conoscenza delle Ammoniti liasiche di Lombardia,” pt. iii, Ammoniti del calcare nero di Moltrasio, Careno, Civate nel Bacino lariano (Mém. Soc. Pal. Suisse, vol. xxv, 1898), p. 11, pl. xv, fig. 5Google Scholar (Arietites ( Arnioceras) Arnouldi).
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page 445 note 2 British Museum (Natural History), register number C. 12114.
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page 445 note 4 Pichler, Adolf, “Beiträge zur Geognosie Tirols”: Zeitschr. des Ferdinandeums für Tirol und Vorarlberg, 1859, Folge iii, Heft viii.Google Scholar
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page 446 note 2 The trivial name radians has been applied by different authors to various Toarcian and Bajocian species of Ammonites. For synopsis of these species see Buckman, S. S., Mon. Inf. Ool. Amm. (Pal. Soc.), pt. iv, 1890, pp. 188–90.Google Scholar
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