Hostname: page-component-6bf8c574d5-vmclg Total loading time: 0 Render date: 2025-02-20T05:21:29.409Z Has data issue: false hasContentIssue false
  • English
  • Français

Factors controlling the availability of sediment-bound lead to the estuarine bivalve scrobicularia plana

Published online by Cambridge University Press:  11 May 2009

Samuel N. Luoma  and
G. W. Bryan
Samuel N. Luoma
Affiliation:
U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California, U.S.A.
G. W. Bryan
Affiliation:
The Laboratory, Marine Biological Association, Citadel Hill, Plymouth
Rights & Permissions [Opens in a new window]

Extract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Concentrations of lead in the soft tissues of the deposit-feeding bivalve Scrobicularia plana have been compared with the physicochemical characteristics of sediments in 20 estuaries in southern and western England and one in north-west France. The results indicate that the biological availability of lead in the sediment is controlled mainly by the concentration of iron, and that the concentration of lead in the bivalve may be predicted from the Pb/Fe ratio in 1 N hydrochloric acid extracts of surface sediments.

Type
Research Article
Information
Journal of the Marine Biological Association of the United Kingdom , Volume 58 , Issue 4 , November 1978 , pp. 793 - 802
Copyright
Copyright © Marine Biological Association of the United Kingdom 1978

References

REFERENCES

Bryan, G. W. & Hummerstone, L. G., 1973. Brown seaweed as an indicator of heavy metals in estuaries in south-west England. Journal of the Marine Biological Association of the United Kingdom, 53, 705–720.CrossRefGoogle Scholar
Bryan, G. W. & Hummerstone, L. G., 1978. Heavy metals in the burrowing bivalve Scrobicularia plana from contaminated and uncontaminated estuaries. Journal of the Marine Biological Association of the United Kingdom, 58, 401–419.CrossRefGoogle Scholar
Bryan, G. W. & Uysal, H., 1978. Heavy metals in the burrowing bivalve Scrobicularia plana from the Tamar Estuary in relation to environmental levels. Journal of the Marine Biological Association of the United Kingdom, 58, 89–108.CrossRefGoogle Scholar
Chao, T. T., 1972. Selective dissolution of manganese oxides from soils and sediments with acidified hydroxylamine hydrochloride. Proceedings. Soil Science Society of America, 31, 764–768.CrossRefGoogle Scholar
Hem, J., 1970. Study and interpretation of the chemical characteristics of natural water. U.S. Geological Survey Water Supply, paper no. 1473, 2nd edition, 362 pp.Google Scholar
Jenne, E. A., 1968. Controls on Mn, Fe, Co, Ni, Cu and Zn concentrations in soils and water: the significant role of hydrous Mn and Fe oxides. In Trace Inorganics in Water (ed. Gould, R. F.), pp. 337–379. Washington, D.C.: American Chemical Society.CrossRefGoogle Scholar
Jenne, E. A. & Luoma, S. N., 1977. The forms of trace elements in soils, sediments and associated waters: an overview of their determination and bioavailability. In Biological Implications of Metals in the Environment (ed. Drucker, H. and Wildung, R. E.), pp. 110–143. U.S. NTIS, CONF–750929. Springfield, Va.Google Scholar
Luoma, S. N. & Jenne, E. A., 1977. The availability of sediment-bound cobalt, silver and zinc to a deposit-feeding clam. In Biological Implications of Metals in the Environment (ed. Drucker, H. and Wildung, R. E.), pp. 213–231. U.S. NTIS, CONF-750929. Springfield, Va.Google Scholar
Schwertmann, W. Z., 1964. Differentiation of the iron oxides of the soil by extraction with ammonium-oxalate solution. Bodenkunde und Pflanzenernährung, 105, 194–201.CrossRefGoogle Scholar