From Charles James Fox Bunbury to Charles Lyell 3 February 18661
Barton,
February 3rd, ’66.
My dear Lyell
I thank you much for sending me Madame Agassiz’s letter to Mary, which I have read with much curiosity and interest.2 The variety of new fish and other novelties which Agassiz has discovered are not half so astonishing to me as the rapid growth of that country.3 How completely Brazil seems to be revolutionized by the one single agency of steam. Madame Agassiz speaks of the voyage from Para to the Barra de Rio Negro taking five days;4 when the botanist Spruce explored that country, no longer ago than 1850, the voyage from Para to Santorin, which is little more than half way to the Barra, often required a month. 5 Still, I should have more confidence in observations made by men who have been a long time stationary in chosen spots, like Bates and Wallace and Spruce, than in those made at steam pace.6
Agassiz’s observation on “glacial phenomena,” in Brazil are certainly very astonishing indeed; so astonishing that I have very great difficulty in believing them.7 They shake my faith in the glacial system altogether;—or perhaps they ought rather to shake the faith in Agassiz. They seem to threaten a reductio ad absurdum of the whole theory. If Brazil was ever covered with glaciers, I can see no reason why the whole earth should not have been so. Probably the whole terrestrial globe was once “one entire and perfect icicle.”8 Seriously,—to answer your questions;—there is nothing in the least northern, nothing that is not characteristically Brazillian, in the flora of the Organ mountains.9 I did not myself ascend any of the peaks, but Gardner did, and made very rich collections, of which he has given an account in Sir W. Hooker’s Journal, and more compendiously in his volume of Travels.10 The vegetation consists of very curious dwarfish forms of those families and genera which are characteristic of tropical America, and especially of Brazil; together with representatives of some other groups which are widely diffused, but by no means northern. So also the vegetation of the table lands has many peculiar forms, but is composed mainly of under-shrubby and herbaceous species, of the same families and genera which in the forests appear as trees and tall climbers.11
Certainly, IF Brazil was ever covered with glaciers it seems to me certain that the whole of the tropical flora must have come into existence since. I also think it clear, on the same IF, that the absence of “glacial action” from Southern Europe must be due to some other cause than climate.12
Again, to answer your last question.— Brazil (I speak not merely of the small part which I saw, but of what I have read of, and I have read a good many books of travels in that country), seems to be very deficient in lakes, with the exception of lagoons (“broads” they would be called in Norfolk), on the coast; of these there are plenty, but they are evidently formed in the same way as the Norfolk broads, by the natural damming up of the outfall of the abundant waters. Where I travelled, in the higher lands of the interior, the running streams were absolutely innumerable, but scarcely so much as a permanent pond to be seen.13
Many thanks to dear Mary for her kind message.14 With much love to her, believe me ever
Your affectionate friend | Charles J. F. Bunbury
I think Joseph Hooker will be as sceptical as myself about the glaciation of Brazil.15
Footnotes
Bibliography
Allan, Mea. 1967. The Hookers of Kew, 1785–1911. London: Michael Joseph.
Bates, Henry Walter. 1863. The naturalist on the River Amazons. A record of adventures, habits of animals, sketches of Brazilian and Indian life, and aspects of nature under the equator, during eleven years of travel. 2 vols. London: John Murray.
Columbia gazetteer of the world: The Columbia gazetteer of the world. Edited by Saul B. Cohen. 3 vols. New York: Columbia University Press. 1998.
Dean, Warren. 1995. With broadax and firebrand: the destruction of the Brazilian Atlantic forest. Berkeley, Calif., and London: University of California Press.
Gardner, George. 1843. Contributions towards a flora of Brazil. II. Plants from the Organ Mountains. London Journal of Botany 2: 329–55.
Imbrie, John and Imbrie, Katherine Palmer. 1979. Ice Ages: solving the mystery. London and Basingstoke: Macmillan Press.
Lurie, Edward. 1960. Louis Agassiz: a life in science. Chicago: University of Chicago Press.
Lyell, Charles. 1867–8. Principles of geology or the modern changes of the earth and its inhabitants considered as illustrative of geology. 10th edition. 2 vols. London: John Murray.
Marcou, Jules. 1896. Life, letters, and works of Louis Agassiz. 2 vols. London and New York: Macmillan and Co.
Origin: On the origin of species by means of natural selection, or the preservation of favoured races in the struggle for life. By Charles Darwin. London: John Murray. 1859.
Rudwick, Martin John Spencer. 1969. The glacial theory. History of Science 8: 136–57.
Spruce, Richard. 1908. Notes of a botanist on the Amazon & Andes, being records of travel … during the years 1849–1864. Edited by Alfred Russel Wallace. 2 vols. London: Macmillan and Co.
Wallace, Alfred Russel. 1853. A narrative of travels on the Amazon and Rio Negro, with an account of the native tribes, and observations on the climate, geology, and natural history of the Amazon valley. London: Reeve.
Summary
Discusses Louis Agassiz’s theory of the glaciation of Brazil.
Letter details
- Letter no.
- DCP-LETT-4995F
- From
- Charles James Fox Bunbury, 8th baronet
- To
- Charles Lyell, 1st baronet
- Source of text
- F. J. Bunbury ed. 1891–3, Later life 1: 134–6.
Please cite as
Darwin Correspondence Project, “Letter no. 4995F,” accessed on 26 September 2022, https://www.darwinproject.ac.uk/letter/?docId=letters/DCP-LETT-4995F.xml
Also published in The Correspondence of Charles Darwin, vol. 14