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Published online by Cambridge University Press: 01 May 2009
The nine specimens of Phyllopodous Crustacea about to be noticed are, with one exception (that from Lanarkshire), all from the undoubted Carboniferous Limestone series, East Kilbride, a locality already well known to local geologists as having yielded a very rich series of Carboniferous forms.
page 482 note 1 Records of General. Science, by Dr. R. D. Thomson, 1835, vol. i. p. 136.
page 482 note 2 Probably the other half of the carapace has been folded beneath it, as the posterior margin seems to be doubled.
page 484 note 1 See Murchison's “Siluria,” 4th edition, 1867, p. 236, fig. 66, and footnote. See also Geol. Mag., 1865, Vol. II. p. 401, Pl. XI. Fig. 1.
page 484 note 2 For “anterior” read posterior.
page 484 note 3 For “posterior” read anterior.
page 485 note 1 Not deeply emarginated, as in D. Scouleri, M'Coy.
page 485 note 2 M'Coy, Carb. Foss. Ireland, p. 163, pl. xxiii. fig. 2. There seems no reason to doubt that this species is synonymous with D. testudineus, with which it should now be merged.