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Published online by Cambridge University Press: 01 May 2009
page 419 note 2 Being an abstract of a paper read before the Eleventh Session of the Int. Geol. Congress, Stockholm, August, 1910.
page 420 note 1 See Trans. Tenth Int. Geol. Cong., Mexico, vol. i, pp. 437–82, 1906.Google Scholar
page 420 note 2 Bull. Geol. Soc. Am., vol. xix, pp. 347–69, 11, 1908Google Scholar. See also Davis, ibid., vol. xvii, p. 414, August, 1906.
page 420 note 3 Chamberlin, & Salisbury, , Geology, ii, p. 273.Google Scholar
page 420 note 4 Manual, 4th ed., p. 484.
page 420 note 5 Chamberlin & Salisbury, ii, p. 656.
page 421 note 1 Chamberlin & Salisbury, ii, p. 672.
page 421 note 2 Neumayr held that there were climatic zones in Jurassic and Cretaceous times; see Blanford, W. T., Address to Geol. Soe., 1890, p. 55.—ED. Geol. Mag.Google Scholar
page 422 note 1 There is an apparently zonal distribution of the very much mixed groups of Pliocene life which may have resulted from a similar di-tribution of temperatures, but exceptional conditions warn us against too implicit an acceptance of this conclusion.
page 422 note 2 See Trans. Tenth Int. Geol. Cong., Mexico, vol. i, pp. 349–405, 1906.Google Scholar
page 423 note 1 Professor David, , Trans. Tenth Int. Geol. Cong., Mexico, vol. i, pp. 481–2, 1906.Google Scholar