Published online by Cambridge University Press: 01 May 2009
The series of fossil plants from the Tertiary strata of New South Wales and Tasmania, to which these remarks relate, were sent to Mr. R. Etheridge, jun., at the British Museum, for examination partly by Prof. Liversidge, of Sydney University, and by Mr. C. S. Wilkinson, F.G.S., Government Geologist for New South Wales, whilst the remainder already formed a portion of the National Collection.
page 154 note 1 Johnston, R. M.—Regarding the Composition and Extent of certain Tertiary Beds in and around Launceston. Proc. R. Soc. Tas. for 1873, pp. 34–48.Google Scholar
page 154 note 2 Johnston R. M. The Launceston Tertiary Basin; Second Paper. Ibid, for 1874, pp. 29 and 53–62.
page 154 note 3 Johnston, R. M.. Note on the Discovery of Spondylostrobus Smythii (v. Mueller) and other Fossil Fruits in the Deep Lead Drift at Brandy Creek Gold Field.Google ScholarIbid, for 1879, pp. 29–41.
page 154 note 4 Johnston R. M. Notes on the Relations of the Yellow Limestone (Travertin), of Geilston Bay, with other Fluviatile and Lacustrine Deposits in Tasmania and Australia, ogether with Descriptions of the two New Fossil Helices. Ibid, for 1879, pp. 81–90.
page 155 note 5 Johnston R. M. Notes showing that the Estuary of the Derwent was occupied by a Fresh-Water Lake during the Tertiary Period. Ibid. 1881, pp. 1–21.
page 156 note 1 For an enumeration of the species known, previous to the researches of Baron Ettingshausen, see the Catalogue of Australian Fossils, by E. Etheridge, jun.