[{113}] The paragraph which ends here is difficult to interpret. In spite of obscurity it is easy to recognize the general resemblance to the discussion on the importance of subsidence given in the Origin, Ed. i. pp. 290 et seq., vi. pp. 422 et seq.
[{114}] See Note 3, p. 27.
[{115}] Compare Origin, Ed. i. p. 298, vi. p. 437. “We shall, perhaps, best perceive the improbability of our being enabled to connect species by numerous, fine, intermediate, fossil links, by asking ourselves whether, for instance, geologists at some future period will be able to prove that our different breeds of cattle, sheep, horses, and dogs have descended from a single stock or from several aboriginal stocks.”
[{116}] The sudden appearance of groups of allied species in the lowest known fossiliferous strata is discussed in the Origin, Ed. i. p. 306, vi. p. 446. The gradual appearance in the later strata occurs in the Origin, Ed. i. p. 312, vi. p. 453.
[{117}] Compare Origin, Ed. i. p. 307, vi. p. 448.
[{118}] I have interpreted as Sandstone a scrawl which I first read as Sea; I have done so at the suggestion of Professor Judd, who points out that “footprints in the red sandstone were known at that time, and geologists were not then particular to distinguish between Amphibians and Reptiles.”
[{119}] This refers to Cuvier's discovery of Palæotherium &c. at Montmartre.
[{120}] This simile is more fully given in the Origin, Ed. i. p. 310, vi. p. 452. “For my part, following out Lyell’s metaphor, I look at the natural geological record, as a history of the world imperfectly kept, and written in a changing dialect; of this history we possess the last volume alone, relating only to two or three countries. Of this volume, only here and there a short chapter has been preserved; and of each page, only here and there a few lines. Each word of the slowly-changing language, in which the history is supposed to be written, being more or less different in the interrupted succession of chapters, may represent the apparently abruptly changed forms of life, entombed in our consecutive, but widely separated formations.” Professor Judd has been good enough to point out to me, that Darwin’s metaphor is founded on the comparison of geology to history in Ch. i. of the Principles of Geology, Ed. i. 1830, vol. i. pp. 1-4. Professor Judd has also called my attention to another passage,—Principles, Ed. i. 1833, vol. iii. p. 33, when Lyell imagines an historian examining “two buried cities at the foot of Vesuvius, immediately superimposed upon each other.” The historian would discover that the inhabitants of the lower town were Greeks while those of the upper one were Italians. But he would be wrong in supposing that there had been a sudden change from the Greek to the Italian language in Campania. I think it is clear that Darwin’s metaphor is partly taken from this passage. See for instance (in the above passage from the Origin) such phrases as “history ... written in a changing dialect”—“apparently abruptly changed forms of life.” The passage within [ ] in the above paragraph:—“Lyell’s views as far as they go &c.,” no doubt refers, as Professor Judd points out, to Lyell not going so far as Darwin on the question of the imperfection of the geological record.
[{121}] On rarity and extinction see Origin, Ed. i. pp. 109, 319, vi. pp. 133, 461.
[{122}] In the Origin, Ed. i. p. 346, vi. p. 493, the author begins his discussion on geographical distribution by minimising the effect of physical conditions. He lays great stress on the effect of barriers, as in the present Essay.