Published online by Cambridge University Press: 06 July 2012
The original specimen of the stem with secondary wood, to which the name Palæopitys Milleri was given by M'Nab in 1870, was found by Hugh Miller in a nodule half disinterred by the sea near Cromarty; its age was shown by the remains of Coccosteus decipiens in other nodules of the deposit, and by scales of Diplacanthus in the nodule containing the wood.
page 409 note * p. 124, 2nd ed.
page 409 note † Pp. 191–9, figs. 64, 65, 20th ed.
page 409 note ‡ Pp. 11, 436–7, fig. 3, 1st ed.
page 409 note § Trans. Bot. Soc. Edin., vol. x, p. 312.
page 409 note ║ Footprints of the Creator, fig. 64.
page 410 note * See Mem. Geol. Survey, Scotland, “The Geology of the Lower Findhorn and Lower Strathnairn, including part of the Black Isle near Fortrose,” 1923, Appendix I, p. 113, published while this paper was in the press.
page 415 note * Salter, , Q. J. Geol. Soc., vol. xiv, p. 72.Google ScholarPeach, , Trans. Geol. Soc. Edin., 1877, p. 148.Google Scholar
page 415 note † Salter, , loc. cit., pl. v, fig. 1a, 1c.Google Scholar
page 415 note ‡ Abh. d. k. preuss. geol. Landesanstalt, 1896, p. 63.
page 415 note § The scalariform pitting of the secondary wood of Völkdia refracta is described by Solms, (Zeitsch. für Bot., vol. ii (1910), p. 534)Google Scholar as being distributed on all sides of the tracheides.