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From Charles Lyell   17 June 1856

Summary

CD forgets an author [CD himself in Coral reefs] "who, by means of atolls, contrived to submerge archipelagoes (or continents?), the mountains of which must originally have differed from each other in height 8,000 (or 10,000?) feet".

CL begins to think that all continents and oceans are chiefly post-Eocene, but he admits that it is questionable how far one is at liberty to call up continents "to convey a Helix from the United States to Europe in Miocene or Pliocene periods".

Will CD explain why the land and marine shells of Porto Santo and Madeira differ while the plants so nearly agree?

Author:  Charles Lyell, 1st baronet
Addressee:  Charles Robert Darwin
Date:  17 June 1856
Classmark:  DAR 146: 475
Letter no:  DCP-LETT-1905

Matches: 2 hits

  • J.  D. Hooker 1857 ). CD’s reply indicates that he thought Lyell referred to Raoul …
  • Hooker described as the same as that of New Zealand in J.  D. Hooker 1853–5 , 1: vii, or to Raoul Island, in the Kermadec group, which also possesses a New Zealand flora but is some 600 miles from New Zealand. Hooker wrote a paper on the botany of Raoul Island in 1857 ( …

From Charles Lyell   [16 January 1857]

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Summary

Enumerates fossil mammals known in Secondary strata.

Lack of angiosperm plants in rocks older than Chalk is no reason to anticipate rarity of warm-blooded quadrupeds.

Author:  Charles Lyell, 1st baronet
Addressee:  Charles Robert Darwin
Date:  [16 Jan 1857]
Classmark:  DAR 205.9: 394
Letter no:  DCP-LETT-2039

Matches: 1 hit

  • … 2: 238–9). See also letter to J.  D. Hooker, 17 January [1857] . The fossil molar teeth of …
Document type
letter (2)
Author
Lyell, Charlesdisabled_by_default
Addressee
Correspondent
Date
1856 (1)
1857 (1)