^{page 146 note 1} Leriche, , “Observations sur les Terrains tertiaires des environs de Reims et d' Epernay”: Ann. Soc. géol. Nord, vol. xxxvi, 1907, p. 367.Google Scholar

^{page 146 note 2} Compare Lemoine, Géologie du Bassin de Paris, 1911, p. 200.Google Scholar

^{page 146 note 3} Leriche, , “Sur les Horizons paléontologiques du Landénien marin du Nord de la France”: Ann. Soc. géol. Nord, vol. xxxii, 1903, p. 239.Google Scholar

^{page 148 note 1} Leriche, , Bull. Soc. géol. France, sét. iv, vol. xii, 1912, pls. xxiii–xxvii.Google Scholar

^{page 148 note 2} Prestwich, , Quart. Journ. Geol. Soc., vol. xliv, 1888, pp. 98–9.Google Scholar

^{page 148 note 3} Stamp, and Priest, , “Geology of the Swanscombe Eocene Outlier”: Proc. Geol. Assoc., vol. xxxi, 1920, p. 187.CrossRefGoogle Scholar

^{page 148 note 4} Stamp, , “On the Beds at the Base of the Ypresian in the Anglo-Franco-Belgian Basin”: read at the meeting of the Geologists' Association, 07 2, 1920. GEOL. MAG., Vol. LVII, 1920, p. 380 (in the Press).Google Scholar

^{page 149 note 1} In most cases the megalospheric and microspheric forms of each species of Nummulites have been described under different names. In this paper the double name is given on the first occasion of reference to the species, but, for the sake of brevity, the more usual name is generally used.

^{page 149 note 2} Leriche, , op. cit., 1912, p. 700 (with references).Google Scholar

^{page 149 note 3} Leriche, , op. cit., 1912, pl. xxv.Google Scholar

^{page 151 note 1} Dollfus, , “Excursion to Paris”: Proc. Geol. Assoc., vol. xxi, 1909, p. 12. The writer is indebted to M. Dollfus for further unpublished information on this question.Google Scholar

^{page 151 note 2} Dollfus, , “On the Classification of the Beds of the Paris Basin”: Proc. Geol. Assoc., vol. xxi, 1909, pp. 107–12.Google Scholar

^{page 151 note 3} Leriche, , “Observations sur la Classification des Assises paléocènes et éocènes du Bassin de Paris”: Ann. Soc. géol. Nord, vol. xxxiv, 1905, p. 391.Google Scholar

^{page 151 note 4} Boussac, , “La Limite de l' Eoc`ene et de l' Oligoène”: Bull. Soc. géol. France, s´er. iv, vol. vii, 1907, p. 400.Google Scholar

^{page 151 note 5} Von, Koenen, “Ueber diie Parallelisrung des norddeutschen, englischen, Und französischen Oligocäns”: Zeitsch. d. deutsch. geol. Gesells., 1867, pp. 23–32.Google Scholar

^{page 151 note 6} White, , Geology of the Country near Lymington and Portsmouth (Mem. Geol. Surv.), 1915, p. 43. More recently White has adopted the correlation of Dollfuss (1909), Handb. Reg. Geol., Band iii, i Abt.: The British Isles, p. 272 (1917).Google Scholar

^{page 152 note 1} Leriche, , op. cit., 1905, p. 391.Google Scholar

^{page 152 note 2} Dollfus, , op. cit., 1909, p. 107.Google Scholar

^{page 152 note 3} Reid, Quart. Journ. Geol. Soc., vol. lii, 1896, p. 490; ibid., vol. liv, 1898, p. 234.

^{page 153 note 1} Parent, , “Notes sur lea Terrains Tertiaires du Pays de Caux”: Ann. Soc. géol. Nord, vol. xxii, 1894, p. 9.Google Scholar

^{page 154 note 1} White, , op. cit., 1915, p. 11.Google Scholar

^{page 154 note 2} Meyer, ,“On the Lower Tertiary Deposits recently exposed at Portsmouth”: Quart. Journ. Geol. Soc., vol. xxvii, 1871, p. 74.CrossRefGoogle Scholar

^{page 155 note 1} White, , loc. cit., p. 11.Google Scholar

^{page 155 note 2} Leriche, , “Observations sur la Géologic de l'^lle de Wight”: Ann. Soc.géol. Nord, vol. xxxiv, 1905, p. 16.Google Scholar

^{page 155 note 3} White, , loc. cit., p. 20.Google Scholar

^{page 155 note 4} Fisher, , “On the Bracklesham Beds of the Isle of Wight Basin”: Quart. Journ. Geol. Soc., vol. xviii, 1862, p. 65.CrossRefGoogle Scholar

^{page 155 note 5} White, , “Geology of the Country around Bournemouth,” 2nd ed. (Mem. Geol. Surv.), 1917, p. 29. The Bournemouth Freshwater Series is situated in the upper part of the Bagshot Sands.Google Scholar

^{page 156 note 1} Boussac, , “Observations sur la faune des couches supérieures de Bracklesham à Nummulites variolarius”: Ann. Soc. géol. Nord, vol. xxxvi, 1907, p. 360.Google Scholar