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IV.—On the Systematic Position of the Upper Cretaceous Dinosaur Titanosaurus
Baron Francis Nopcsa
Published online by Cambridge University Press:

01 May 2009, p. 261
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Being prevented by other work from continuing at present my work on the Danian (Laramie) Dinosaurs of Transylvania, I wish briefly to draw attention to the fact that the Upper Cretaceous Titanosaurus, as known from the Montagne Noire in France and from the Cretaceous formation of Argentina, and perhaps also from East Africa (as already pointed out by Fraas), has nothing to do with the Sauropoda, but belongs to the Trachodontid Orthopods, as proved by the abundant Transylvanian material at my disposal.

III.—Some Tertiary Dykes of the Clyde Area
G. W. Tyrrell, A.R.C.Sc., F.G.S.
Published online by Cambridge University Press:

01 May 2009, pp. 350-356
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Leidleite and Inninmorite.—Typical rocks of these groups are as yet unknown in the Clyde area. A N.N.W. dyke at Barrassie Sands, near Troon (Ayrshire), has points in common with leidleite. It shows anorthite phenocrysts in a subvariolitic groundmass of acicular felspar and augite, enveloped in a partially devitrified glassy base. A north–south dyke at the north end of Loch Fad, Bute, may perhaps be regarded as a doleritic end-variety of leidleite (see Anderson & Radley, 1916, fig. 2b, p. 208). A pitchstone-like dyke from the Smurig Burn in the south of Arran has all the characters of leidleite, except that it carries rather abundant granular augite, instead of acicular crystals.

Geological Magazine