. Darwinism : an exposition of the theory of natural selection, with some of its applications. Natural selection; Evolution. 364 DARWINISM pared with the enormous areas of sea-bottom, over Avhich the atmospheric dust must have been scattered, render it in the highest degree improbable that the maximum limit either of size of particles, or of distance from land has been reached. Let us, however, assume that the quartz grains, found by Mr. Murray in the deep-sea ooze 700 miles from land, give us the extreme limit of the power of the atmosphere as a carrier of solid particles, and let us compare
. Darwinism : an exposition of the theory of natural selection, with some of its applications. Natural selection; Evolution. 364 DARWINISM pared with the enormous areas of sea-bottom, over Avhich the atmospheric dust must have been scattered, render it in the highest degree improbable that the maximum limit either of size of particles, or of distance from land has been reached. Let us, however, assume that the quartz grains, found by Mr. Murray in the deep-sea ooze 700 miles from land, give us the extreme limit of the power of the atmosphere as a carrier of solid particles, and let us compare with these the weights of some seeds. From a small collection of the seeds of thirty. species of herbaceous plants sent me from Kew, those in the above table were selected, and small portions of eight of them carefully weighed in a chemical balance.^ By counting these portions I was able to estimate the number of seeds weighing one grain. The three very minute species, whose numbers are marked ^Yith. an asterisk (*), were estimated by the comparison of their sizes with those of the smaller weighed seeds. If now Ave compare the seeds with the quartz grains, Ave ^ I am indebted to Professor R. Meldola of the Finsbiiry Technical Institute, and Rev. T. D. Titmas of Charterhouse for furnishing me with the weights Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Wallace, Alfred Russel, 1823-1913. London : Macmillan
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