XIII. Analysis of Coprolites and other Organic Remains imbedded in the Limestone of Burdiehouse near Edinburgh

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Abstract
It is not my intention to enter into any detailed description of the external characters of the several interesting organic remains which are found imbedded in the limestone of Burdiehouse, that being a task which belongs to their distinguished discoverer Dr Hibbert.As little do I mean to describe the geological relations of the limestone bed, that being equally the province of Dr Hibbert. It will be sufficient to state generally, that it forms one of the lowest members of the carboniferous group, being inferior in position even to the Encrinal mountain limestone of its immediate vicinity; and that besides its numerous animal remains, some of which will be mentioned in the sequel, it contains throughout its entire mass numerous impressions of land and fresh-water tropical plants.

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