Published online by Cambridge University Press: 01 May 2009
The Inferior Oolite and contiguous deposits of the neighbourhood of Doulting have been described in detail in my paper on “The Inferior Oolite and Contiguous Deposits of the Bath-Doulting District”; but since that paper appeared, through the courtesy of the Urban District Council, I have had the loan of the John-Phyllis. Collection of Inferior-Oolite fossils that are housed in the Shepton-Mallet Museum.
page 509 note 1 Quart. Journ. Geol. Soc., 1907, vol. lxiii, pp. 383–444.Google Scholar
page 510 note 1 At first I thought the clay-bed might come below the Striatulum-Bed, making it pre-striatuli, but then an alternative explanation suggested itself, which was graphically represented on p.392 of my main paper. Unfortunately, however, the statement of the earlier view (lines 15–17 from bottom of p. 391) escaped the necessary qualification.
page 511 note 1 The statement in my main paper (p. 420)—“but how thick it was, or whether it rests directly upon the ‘grit’, or was separated therefrom by the Upper Coral-Bed …”—was inadvertently transcribed from notes made before I had satisfied myself about the correct position of the Upper Coral-Bed and should be erased.
page 511 note 2 Quart. Journ. Geol. Soc., 1893, vol. xlix, p. 484.Google Scholar