^{page 351 note 1} These arguments have been recently renewed by Mr. Seeley, but without the support of any additional observations, and in the face of the facts brought forward by Dr. Barrois and myself.

^{page 352 note 1} Ann. Philos. ser. ii. vol. viii. pp. 365 and 458.Google Scholar

^{page 352 note 2} Quart. Journ. Geol. Soc. vol. i. p. 77.Google Scholar

^{page 353 note 1} Notes on the Geology and Chemical Composition of the Various Strata in the Isle of Wight, London, 1849.

^{page 353 note 2} Journ. Roy. Agric. Soc. ser. i. vol. ix. p. 56.Google Scholar

^{page 354 note 1} Quart. Journ. Geol. Soc. vol. iv. p. 257.Google Scholar

^{page 355 note 1} Proc. Geol. Soc. vol. iv. p. 169.Google Scholar

^{page 355 note 2} Brit. Assoc. Rep. Trans. Sec. 144.

^{page 355 note 3} Brit. Assoc. Rep. 1843, Trats. Sec. p. 69.

^{page 356 note 1} Notes, etc., on the Strata of the Isle of Wight, London, 1849.

^{page 356 note 2} Quart. Journ. Geol. Soc. vol. iv. pp. 257 and 262.Google Scholar

^{page 357 note 1} Pal. Soc. Mem. 1852, p. 114.

^{page 357 note 2} Quart. Journ. Geol. Soc., vol. xxvii. p. 98.Google Scholar

^{page 357 note 3} Geol. Mag. 12. II. Vol. I. p. 196.Google Scholar

^{page 357 note 4} Quart. Journ. Geol. Soc. vol. xxx. p. 369.Google Scholar

^{page 358 note 1} See Barrois, , Sur l'age des couches de Blackdown, Ann. Soc. Geol. du Nord, torn. iii. p. 7.Google Scholar

^{page 358 note 2} Quart. Journ. Geol. Soc, vol. xxxi. p. 272.Google Scholar

^{page 358 note 3} The fact of the entire absence of the characteristic fossils of the Warminster beds in the Cambridge Greensand is sufficient proof that these beds were never deposited in that area, loc. cit., pp. 272, 273.

^{page 358 note 4} Proc. Geol. Assoc, vol. iii.Google Scholar

^{page 359 note 1} Recherches sur le Terrain Crétacé supérieur de l'Angleterre et de l’Ireland, pur Ch. Barrois, D.Sc. Lille, 1876.

^{page 361 note 1} Proc. Geol. Assoc. vol. iv. p. 8.Google Scholar