Ridley Chapter 1
History of evolutionary ideas --- Part 1, before Darwin
Part 2, History of evolutionary ideas after Darwin
510 index page
Evolution is a theory with a bumpy history. That history brings with it much baggage, in the form of ideas, words, and controversies that continue to shape discussion of evolution today. So we begin by looking at that history, not just out of respect for the workers that have gone before but because understanding that history can illuminate important current difficulties.
BRIEF OUTLINE (hyperlinks to expanded outline; use "back" button to return)
EXPANDED OUTLINE
The "new" science of geology
- Nicolaus Steno's laws (1669).
These may seem like simple, obvious ideas, but they were basic to reconstructing the history of the earth and creating the need for a theory to explain differences between past and present life.
- Law of Superposition
"At the time when any given stratum was being formed, all the matter resting upon it was fluid, and, therefore, at the time when the lowest stratum was being formed, none of the upper strata existed."
- Law of Original Horizontality
Undisturbed bedding planes are nearly horizontal.
- Law of Concealed Stratification.
As originally deposited, edges are never visible.
- James Hutton's (1795), Theory of the Earth contained the famous phrase describing Earth's history, "No vestige of a beginning, no prospect of an end." Here is how Hutton's life is described by James Burke (Scientific American, October 1998, p. 132):
"...Hutton was a great example of the Scottish Renaissance man... He studied humanities, physics, geography, law, medicine and chemistry and qualified as a doctor. Then, in the manner of such eclectic people, he became a farmer. Why not? It may have been his consequent landowner's interest in rocks and soil that got him into geology. In 1764 he began a series of trips to stonier parts of the British Isles, tapping and chipping away... Well, all the hammering must have been really productive, because in 1785 Hutton penned the outline of a modest work, eventually published under the modest title of Theory of the Earth, and blew everybody away with his description of a great, cyclical process: land degradation by erosion, resultant deposits washed into the sea, sedimentary layers settling over millions of years, ultimately to be thrown up again, to be eroded once more and so on. And, as Hutton said, if this process had taken as long in the past as it seemed to take in the modern world, then the planet was humongously ancient, never mind the Bible. It would be this particular bit of Hutton's geologic uniformitarianism ... that would in time inspire Darwin."
- William Smith (1815), was a mine surveyor and canal builder, employed on behalf of the emerging industrial revolution to supply coal for steam engines and factories.
"And I presume to think, that the accurate surveys and examinations of the strata ... to which I have devoted the whole period of my life ... have enabled me to prove that there is a great degree of regularity in the position and thickness of all these strata ... and that each stratum is also possessed of properties peculiar to itself, has the same exterior characters and chemical qualities, and the same extraneous or organized fossils throughout its course. I have ... collected specimens of each stratum, and of the peculiar extraneous fossils, organic remains, and vegetable impressions, and compared them with others from very distant parts of the island ... and have arranged them in the same order as they lay in the earth; which arrangement must readily convince every scientific or discerning person, that the earth is formed ... according to regular and immutable laws, which are discoverable by human industry and observation, and which form a legitimate and most important object of science" (W. Smith, as quoted in Geology Illustrated).
- Meanwhile, Georges Cuvier (1813), founder of comparative anatomy, earned a reputation for interpreting past life from fossil bones. Cuvier mustered evidence for extinction, especially of giant animals. [As the world of the 18th and 19th centuries became ever more thoroughly explored, the possibility of large fossil animals (dinosaurs, mammoths) being discovered alive faded, although mastodon remains in the eastern United States led Thomas Jefferson to entertain thoughts that Lewis and Clark's expedition might find mastodons still living in the great western wilderness.] Cuvier believed in discontinuity (and catastrophism) rather than the scala naturae, and thought progressive evolutionism was inconsistent with the evidence.
- Finally, Charles Lyell is famous for the concepts of uniformitarian geology. What shaped the past is the same as what acts in the present. His Principles of Geology (1830-33) inspired Darwin, who read his books while on board the Beagle. But Lyell never accepted the transformation of species.
Charles Darwin, of course, introduced our modern view of evolution with his Origin of Species in (1859). We shall consider the evidence, ideas and arguments that led Darwin to his theory when we discuss Chapter 3 and Chapter 4 in upcoming classes.
Continued in Chapter 1, part 2 , History of evolutionary ideas after Darwin
510 index page
Recent items of relevance to this chapter:
- Stephen Jay Gould, "A division of worms / The use and disuse of Lamarck", Natural History, February 1999 (to be continued in the March issue).
- An extended essay on Lamarck's contributions, going well beyond the standard textbook caricature.
- Richard Milner, "Charles Darwin and Associates,Ghostbusters", Scientific American, October 1996.
- An interesting article on the fad of spiritualism in Britain in the late 1800s, discussing Darwin's and Wallace's opposite roles.
- Stephen Jay Gould, "Writing in the margins", Natural History, November 1998, and "Capturing the center", Natural History, December 1998.
- A two-part essay on Antoine-Laurent Lavoisier and geology in the late 1700s, shortly before the French Revolution in which he was executed. Lavoisier, you will recall from high school chemistry, was the great French chemist who discovered oxygen. Here we learn about Lavoisier's important contributions to geology as well.
510 index page
Readable references: (also note end-of-chapter references in Ridley)
- John A. Moore (1993) Science As a Way of Knowing. The Foundations of Modern Biology. Harvard University Press.
- An elegantly written book on the nature of science, with sections on ancient worldviews and evolution (relevant here) as well as genetics and development.
- Loren Eiseley (1958)  Darwin's Century: Evolution and the Men Who Discovered It. Doubleday.
- A scholarly but eloquent discussion of people and ideas associated with evolution in the 1800s.
- Ernst Mayr (1982) The Growth of Biological Thought. Diversity, Evolution, and Inheritance. Harvard University Press
- A thorough, insider's view of the history of some central ideas in biology. Discusses diversity, evolution and genetics both before and after Darwin.
- John McPhee (1998) Annals of the Former World.
- About geology rather than evolution, including commentary on the history of ideas relating to the earth's history. Elegant, entertaining prose by a much-acclaimed writer. This volume is a compiliation of several earlier works, In Suspect Terrain, Basin and Range, Rising from the Plainsand Assembling California. Reviewed in Science 282:885 (30 October 1998).
510 index page
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