Hostname: page-component-74656f9884-skzmx Total loading time: 0 Render date: 2026-11-06T07:51:05.756Z Has data issue: false hasContentIssue false

A Model for the Division of Semiotic Labor in Scientific Argument: The Interaction of Words and Images

Published online by Cambridge University Press:  08 November 2011

Alan G. Gross*
Affiliation:
University of Minnesota
Rights & Permissions [Opens in a new window]

Argument

A growing cross-disciplinary literature has acknowledged the importance of verbal-visual interaction in the creation and communication of scientific texts. I contend that the proper understanding of these texts must flow from a hermeneutic model that takes verbal-visual interaction seriously, one that is firmly grounded in cognitive constraints and affordances. The model I propose has two modules, one for perception, derived from Gestalt psychology, the other for cognition, derived from Peirce's semiotics. I apply this model to an important but largely neglected text in the history of nineteenth-century science, Charles Lyell's The Geological Evidences of the Antiquity of Man, and to two accounts by well-respected historians of science, both of the same key discovery in quantum physics. In doing so, I hope to demonstrate the advisability of incorporating the exegetical practices my model entails into the everyday practices of historians of science.

Information

Type
Research Article
Copyright
Copyright © Cambridge University Press 2011
Figure 0

Fig. 1. Section of a gravel pit containing flint implements at St. Acheul, near Amiens, observed in July, 1860 (Lyell 1863, 135). Layer 1 is vegetable soil and made ground, two to three feet thick. Layer 2 is brown loam with some angular flints, in parts passing into ochreous gravel, filling up indentations on the surface of layer 3, three feet thick. Layer 3 is white silicious sand with layers of chalky marl, and included fragments of chalk, for the most part unstratified, – nine feet. Layer 4 is flint-gravel, and whitish chalky sand, flints subangular, average size of fragments, three inches diameter, but with some large unbroken chalk flints, intermixed, cross stratification in parts. Bones of mammals, grinder of elephant at b, and flint implement at c, – ten to fourteen feet. Layer 5 is chalk with flints. a. is part of an elephant's molar, eleven feet from the surface; b is entire molar of E. primigenius, seventeen feet from surface; c is position of flint hatchet, eighteen feet from surface; d is a projecting ridge consisting of gravel cemented or frozen together.

Figure 1

Fig. 2. Elephas primigenius. Penultimate molar, lower jaw, right side, approximately one-half natural size, Post-pliocene. Coexisted with man (Lyell 1863, 133).

Figure 2

Fig. 3. Flint implement from post-pliocene drift of Abbeville and Amiens. a. Oval-shaped flint hatchet from Mautort, near Abbeville, approximately size of original, which is five-and-a-half inches long, from a bed of gravel underlying the fluvio-marine stratum. b. Same seen edgewise. c. Shows a recent fracture of the edge of the same at the point a, or near the top. This portion of the tool, c, is drawn approximately twice the natural size, the black central part being the unaltered flint, the white outer coating, the layer which has been formed by discoloration or bleaching since the tool was made.

Figure 3

Fig. 4. Two unknown men, one pointing to Prestwich and Evans's discovery of an Old Stone Age flint tool. The inset shows a similar tool. The actual tool has since been identified. Taken on Wednesday, April 27, 1859 (Gamble, “Breaking the Time Barrier”).

Figure 4

Fig. 5. Map showing the supposed course of the ancient and now extinct glacier of the Rhone, and the distribution of the erratic blocks and drift conveyed by it to the great valley of Switzerland (Lyell 1863, 299).

Figure 5

Fig. 6. Map of the moraines of extinct glaciers extending from the Alps into the plains of the Po near Turin. Legend: A. crest or watershed of the Alps; B. snow-covered Alpine summits which fed the ancient glaciers; C. moraines of ancient or extinct glaciers (Lyell 1863, 306).

Figure 6

Fig. 7. Side view of human brain (from Gratiolet) namely, that of the bush-woman called the Hottentot Venus. Showing the backward extension of the cerebrum A at d; beyond the cerebellum C at e; f is the fissure of Sylvius (Lyell 1863, 483).

Figure 7

Fig. 8. Distorted side view of brain of Chimpanzee (from Schroeder van der Kolk and Vrolik) showing at e the extension of the disputed cerebellum C beyond the cerebrum at A at d (Lyell 1863, 482).

Figure 8

Fig. 9. Correct side view of Chimpanzee's brain (from Gratiolet) showing the backward extension of the cerebrum A at d; beyond the cerebellum C at e; f is the fissure of Sylvius (Lyell 1863, 482).

Figure 9

Fig. 10. Mass spectrum showing the existence of J. Results from two spectrometer settings are plotted showing that the peak is independent of spectrometer currents. The run at reduced current was taken two months later than the normal run (Aubert et al. 1974, 1405).