Hostname: page-component-6d856f89d9-4thr5 Total loading time: 0 Render date: 2024-07-16T04:24:06.345Z Has data issue: false hasContentIssue false
  • English
  • Français

The Muds of the Clyde Sea Area. III. Chemical and Physical Conditions; Rate and Nature of Sedimentation; and Fauna

Published online by Cambridge University Press:  11 May 2009

Hilary B. Moore
Hilary B. Moore
Affiliation:
Assistant Naturalist at the Marine Station, Millport
Get access Rights & Permissions [Opens in a new window]

Extract

A Preliminary survey of the area with regard to the distribution of the total nitrogen and phosphate content of the muds was described in a previous paper (Moore, 5). A number of stations were worked, and these were further examined for nature and distribution of particles, water content, and density, and as a result of this survey certain stations were chosen as suitable for more extensive work. At the same time it became evident that the layers in which the greatest and most important changes were taking place were those within a few centimetres of the surface, and these were therefore studied most intensively.

Type
Research Article
Information
Journal of the Marine Biological Association of the United Kingdom , Volume 17 , Issue 2 , September 1931 , pp. 325 - 358
Copyright
Copyright © Marine Biological Association of the United Kingdom 1931

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

REFERENCES

1Atkins, W. R. G.The Phosphate Content of Fresh and Salt Waters in its relationship to the Growth of Algal Plankton. Journ. Mar. Biol. Assoc., N.S., Vol. XIII, 1923, p. 119.CrossRefGoogle Scholar
2Clark, W. M.The determination of hydrogen ions. Bailliére, Tindale and Cox, London, 1928.Google Scholar
3 International Society of Soil Science. Commission 2. Leningrad, July 1930. Report of the Committee on Soil Measurements as adopted at the Second International Soil Congress.Google Scholar
4Lloyd, B.Muds of the Clyde Sea Area, II. Journ. Mar. Biol. Assoc., N.S., Vol. XVII, No. 2, 1931.Google Scholar
5Moore, H. B.The Muds of the Clyde Sea Area, I. Phosphate and Nitrogen Content. Journ. Mar. Biol. Assoc, N.S., Vol. XVI, No. 2, 1930.Google Scholar
6Moore, H. B., and Neill, R. G.An Instrument for Sampling Marine Muds. Journ. Mar. Biol. Assoc., N.S., Vol. XVI, No. 2. 1930.Google Scholar
7Moore, H. B.The specific identification of Faecal Pellets. Journ. Mar. Biol. Assoc., N.S., Vol. XVII, No. 2, 1931.Google Scholar
8Ostenfeld, C. H.Report Danish Biol. Station. XVI, 1908.Google Scholar
9Petersen, C. G. J.Valuation of the sea. I. Animal life on the sea, bottom; its food and quantity. Rept. Danish Biol. Station. XX, 1911.Google Scholar
10Schokalsky, J.L'Expédition océanographique de la Mer Noire. C. R. Acad. Sci. Paris, CLXXXVI, 1928, pp. 1707–1709.Google Scholar