The Spring Hill and Central Leads Company, near Smeaton, in the sinking of their main shaft, which work is being carried on, discovered, at a depth of 295 feet from the surface, in hydrothermal deposit and basaltic boulders, a petrified bone, which was exhibited at the office of the manager (Mr JJ. H. Dill). Subsequently it was forwarded to the Minister of Mines, who submitted it to Mr C. W. De Vis, Palaeontologist of the Queensland Museum, Brisbane. Mr De Vis has sent the following communication regarding it, a copy of which Mr Dill received yesterday morning:-
Queensland Museum,
Brisbane, 30th June, 1896.
To Honorable the Minister of Mines, Victoria. Sir, - You do me the honor to ask in your letter numbered S96 | 3657 in the margin my opinion of the sample accompanying it. Beyond question it is part of a fossil bone. Its mode and state of preservation, in which respects it is identical with the majority of Queensland fossils of the earlier Nototherian period (generally assumed to be post-tertiary, but very possibly tertiary), lead me to refer it without hesitation to that period. The bone is pronouncedly reptilian in character, but it is not from one of the great land lizards of its age, nor is it from a chelonian. It has the general aspect of the upper portion of a tibia (shank-bone) of a crocodilian, and is in fair agreement with the corresponding parts of the tibia of the living crocodile (crocodilus povosus); but at the same time its distinctness is very patent. As at the present time but one post-tertiary crocodilian is known, the alligator, pallymnarchus pollens. I conclude provisionally that it belonged to that animal. I purpose, with permission, to retain the specimen for a time in the hope that other parts of the skeleton may be found in the same deposit. - Yours &c.,
(Signed) C. W. De Vis.