This paper explores the origins of the analytical definition of simple substance, a concept whose central importance in the new chemistry of Lavoisier and his colleagues is now widely recognized. I argue that this notion derived from the practical activities of metallurgists and mineral assayers, and that the theoretical elaboration necessary for the analytical concept to be understood as relevant to chemistry was inspired by the efforts of enlightened rulers in Sweden and Germany to turn chemical science to the benefit (...) of mining—and thus of the various state treasuries. The involvement of chemically-literate mineralogists in the mining industry led them to adopt the principle that analytically-determined composition was a far more essential aspect of minerals than any mere congeries of properties. The same men who pioneered the analytical notion of simple substance also inaugurated the attempt to define a nomenclature for chemistry based exclusively on composition, as determined in the laboratory. -/- . (shrink)

In his comprehensive survey of the work of William Herschel, published in the Annuaire du Bureau des Longitudes for 1842, Dominique Arago argued that the life of the great astronomer ‘had the rare privilege of forming an epoch in an extended branch of astronomy’. Arago also noted, however, that Herschel's ideas were often taken as ‘the conceptions of a madman’, even if they were subsequently accepted. This fact, commented Arago, ‘seems to me one that deserves to appear in the history (...) of science’. From the time Herschel published his first paper in the Philosophical transactions in 1781, he was subjected to the suggestion of lunacy. His patron and friend William Watson, told him that after his claims for the extraordinary power of his telescopes, ‘your prognosis that some would think you fit for Bedlam has been verified’. On learning of Herschel's supremely accurate new micrometer, the astronomer Alexander Aubert exclaimed to Herschel that ‘we would go to Bedlam together’: Aubert wrote to Herschel in January 1782 that he should ‘mind not a few jealous barking puppies: a little time will clear up the matter, and if it lays in my power you would not be sent to Bedlam alone, for I incline much to be of the party’. (shrink)

Beginning the nineteenth-century and continuing down to the present, many authors writing on the history of geology and paleontology have attributed the theory that fossils were inorganic formations produced within the earth, rather than by the deposition of living organisms, to the ancient Greeks and Romans. Some have even gone so far as to claim this was the consensus view in the classical period up through the Middle Ages. In fact, such a notion was entirely foreign to ancient and medieval (...) thought and only appeared within the manifold of ‘Renaissance episteme,’ the characteristics of which have often been projected backwards by some historians onto earlier periods. This paper endeavors to correct this error, explain the development of the Renaissance view, describe certain ancient precedents thereof, and trace the history of the misinterpretation in the literature. -/- . (shrink)