Hostname: page-component-78c5997874-fbnjt Total loading time: 0 Render date: 2024-11-15T07:47:55.294Z Has data issue: false hasContentIssue false
  • English
  • Français

V.—On Concretionary Nodules with Plant-Remains found in the Old Bed of the Yarra at S. Melbourne; and their Resemblance to the Calcareous Nodules known as ‘Coal-Balls.’

Published online by Cambridge University Press:  01 May 2009

Frederick Chapman
Frederick Chapman
Affiliation:
Palæontologist to the National Museum, Melbourne.
Get access Rights & Permissions [Opens in a new window]

Extract

Although many of the nodular bodies met with in sedimentary rocks which were formerly held to be concretions or simple aggregations of mineral matter have since been found to be due to the work of minute animals or plants, there is yet a more numerous class of true concretions which were undoubtedly formed by chemical reaction in the surrounding water and sediments; the resulting precipitation being often deposited upon nuclei of organic origin, as fish, woody fragments, or shells. Occasionally these nodules were of subsequent formation to the deposit in which they occur. In nodules which include organic remains, the segregation was accelerated by the partial decay of the included organic fragments.

Type
Original Articles
Information
Geological Magazine , Volume 3 , Issue 12 , December 1906 , pp. 553 - 556
Copyright
Copyright © Cambridge University Press 1906

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

page 554 note 1 1 Mr. Spry has also shown me portions of branches of gum-trees, one of which has been charred by fire. These he found at the bottom of a sewer manhole at the corner of McGowan and Power Streets, at 14 feet from the surface and about 4 to 6 feet below the present low-water mark. Prehistoric bush-fires must have been of frequent occurrence, and may be ascribed to the action of lightning. At the time of writing this note there is a paragraph in the Argus, February 14th, 1906, reporting several bush-fires having been started by lightning at Chetwynd and Kadnook in Western Victoria. An interesting feature connected with the above occurrence of drifted wood was a bank of marine shells 7 inches thick, left behind the logs by the retreating tide. See also the reference to charred wood in coal-seam nodules by A. C. Seward (“Fossil Plants,” vol. i, p. 88).

page 555 note 1 See Cash, & Hick, : Proc. Yorkshire Geol. and Polytech. Soc., vol. vii (1878-1881), p. 73.CrossRefGoogle Scholar Also Seward, : “Fossil Plants,” vol. i (1898), p. 85.Google Scholar

page 555 note 2 Report, 1892, p. 13. See also Scott, D. H.: “Studies in Fossil Botany,” 1900, p. 11.Google Scholar

1 Whilst writing these notes I have received a valuable and suggestive paper by Douvillé, M. H., “Les ‘Coal-balls’ du Yorkshire,” from the Bull. Soc. Géol. France, sér. iv, vol. v, pp. 154–156Google Scholar, pl. vi, in which that author records the association of large numbers of Goniatites (Gastrioceras), Nautilus, Orthoceras, Aviculopecten, and other marine shells, with the coal-balls and their vegetable contents.