Hostname: page-component-cd9895bd7-dk4vv Total loading time: 0 Render date: 2024-12-24T16:34:38.340Z Has data issue: false hasContentIssue false

Eustatic Control of Major Cyclic Changes in Jurassic Sedimentation

Published online by Cambridge University Press:  01 May 2009

A. Hallam
Affiliation:
Grant Institute of Geology, University of Edinburgh.

Abstract

Evidence is sought to prove, with reference to five examples, that major cyclic changes in Jurassic sedimentation have been controlled by eustatic rises and falls of sea level. Abrupt variations suggestive of pronounced deepening of the sea in areas of marine sedimentation in Europe are correlated with extensive marine transgressions in widely separated parts of the world. A connection is recognized between eustatic movements and evolution and migration of the invertebrate fauna, and relationships between eustatic and local, epeirogenic movements outlined.

Type
Articles
Copyright
Copyright © Cambridge University Press 1963

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

Aldinger, H., 1957. Eisenoolithbildung und rhythmische schichtung in süddeutschen Jura. Geol. Jb., 74, 8796.Google Scholar
Arkell, W. J., 1933. The Jurassic System in Great Britain. Oxford.Google Scholar
Arkell, W. J., 19511958. A monograph of English Bathonian ammonites. Pal. Soc. Lond.Google Scholar
Arkell, W. J., 1956. Jurassic Geology of the World. London and Edinburgh.Google Scholar
Donovan, D. T., 1958. The ammonite zones of the Toarcian (Ammonitico Rosso Facies) of Southern Switzerland and Italy. Ecl. Geol. Helvet., 51, 3360.Google Scholar
Dubar, G., 1925. Études sur le Lias des Pyrénées francaises. Mém. Soc. géol. Nord, 9, 1332.Google Scholar
Fairbridge, R. W., 1961. Eustatic changes of sea level. In Physics and Chemistry of the Earth, 4, 99185. New York, Oxford, London, Paris; Pergamon Press.Google Scholar
Frebold, H., 1925. Über cyklische Meeressedimentation. Leipzig.Google Scholar
Frebold, H., 1957. The Jurassic Fernie Group in the Canadian Rocky Mountains and Foothills. Geol. Surv. Canada Mem. 287.Google Scholar
Frebold, H., 1960. The Jurassic faunas of the Canadian Arctic: Lower Jurassic and lowermost Middle Jurassic ammonites. Geol. Surv. Canada Bull. 59.Google Scholar
Hallam, A., 1961. Cyclothems, transgressions and faunal changes in the Lias of North-West Europe. Trans. Edinburgh Geol. Soc., 18, 125174.Google Scholar
Hudson, J. D., 1962. The stratigraphy of the Great Estuarine Series (Middle Jurassic) of the Inner Hebrides. Trans. Edinburgh Geol. Soc. 19, 139165.Google Scholar
Klüpfel, W., 1917. Über die Sedimente de Flaschee im Lothringer Jura. Geol. Rdsch., 7, 97109.CrossRefGoogle Scholar
Kuenen, P. H., 1950. Marine Geology. New York.Google Scholar
Le Calvez, Y., and Lefavrais-Raymond, A., 1961. Le Charmouthien du Lot. C.R. Socs. sav.-Chambery 1960. Colloque sur le Lias en France, 793802.Google Scholar
Lieb, F., 1951. Die Ammonitenhorizonte der Murchisonaeschichten des nordschweizerischen Juragebirges. Ecl. Geol. Helvet., 44, 450458.Google Scholar
Theobald, N., and Maubeuge, P. L., 1949. Paléogéographie du Jurassique inférieur et moyen dans le nord-est de la France et le sud-ouest de l'allemagne. Ber. naturf. Ges. Freiburg., 39, 249320.Google Scholar
Wells, A. J., 1960. Cyclic sedimentation: a Review. Geol. Mag., 97, 389403.Google Scholar