British palaeontologist (born 1951)
Simon Conway Morris (born 6 November 1951) is a British paleontologist, who became noted for his studies of the Burgess Shale fossils. He is Professor of Evolutionary Palaeobiology in the Department of Earth Sciences at the University of Cambridge.
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Conway Morris
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It was G.K. Chesterton who trenchantly reminded us that, if one was going to preach, then it was more sensible to expend one's energies on addressing the converted rather than the unconverted. It was the former, after all, that were—and even more so are—in constant danger of missing the point and sliding away from the Faith into some vague sort of syncretistic, gnostic, gobbledegook. Chesterton, as ever, was right and should you think this is just another of his tiresome paradoxes may I urge you to re-read him: his prescience concerning our present situation and, worse, where we are heading is astounding.
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The underlying reason for convergence seems to be that all organisms are under constant scrutiny of natural selection and are also subject to the constraints of the physical and chemical factors that severely limit the action of all inhabitants of the biosphere. Put simply, convergence shows that in a real world not all things are possible.
Gould's arguments on the quirkiness of human intelligence are not only presented as part of an evolutionary argument, but also I believe to buttress an ideological viewpoint. In brief, his assessment of Man as an evolutionary accident is to lead us into a libertarian attitude whereby, by virtue of a cosmic accident, we, and we alone, have no choice but to take responsibility for our own destiny and mould it to our desire.
The long history of mankind is studded with convergences, perhaps most notably in social systems and the use of artefacts and technology. But for human history, set in the arrow of time, there appears to be one intolerable stumbling-block. This is the catastrophic failure in human values and decency.
Perhaps a suitable analogy to explain the short-falls of Dawkins's account of evolution is to think of an oil painting. In this analogy Dawkins has explained the nature and range of pigments; how the extraordinary azure colour was obtained, what effect cobalt has, and so on. But the description is quite unable to account for the picture itself. This view of evolution is incomplete and therefore fails in its side-stepping of how information (the genetic code) gives rise to phenotype, and by what mechanisms. Organisms are more than the sum of their parts, and we may also note in passing that the world depicted by Dawkins has lost all sense of transcendence.