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The Ammonite Zones of the Lias

Published online by Cambridge University Press:  01 May 2009

Extract

The increasing diversity of interpretation of the Jurassic Record is proving very troublesome to teachers and students alike. “To-day, hardly a subdivision of the Jurassic is free of controversy as to its exact scope and nomenclature,” wrote S. W. Muller in a recent laudable attempt to reconcile the differing opinions. More is involved, however, than a mere reconciliation of conflicting views. Our knowledge of the Jurassic Record is as yet far less complete than many geologists realize. For while some of the subdivisions of Jurassic time are in general use by all stratigraphers and have stood the test of time, others are in dispute because they are still based on too local and often defective material, or on too incomplete information; a number remain as much surmises as when they were originally introduced. Any scheme put forward at the present day cannot thus be regarded as the final word in the subdivision of the Jurassic, but merely as a contribution towards an ultimate, ideal, “Standard.”

Type
Articles
Copyright
Copyright © Cambridge University Press 1942

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References

1942Standard of the Jurassic System, Bull. Geol. Soc. America, 52, 1941, 1428.Google Scholar

2Vol. v, 1925, pp. 75–8; vol. vi, 1930, pp. 37–41.Google Scholar

3 On the Grouping of some Divisions of so-called “Jurassic” Time. Quart. Journ. Geol. Soc., 54, 1898, table i, to p. 450.Google Scholar

4The fuller paper already mentioned gives the reasons why apyrenum, S. Buckman, 1911, is used for the lower spinatum zone instead of bechteri, Frentzen, 1934 (accepted by Muller).Google Scholar

5The Ammonites of the Blue Lias. Proc. Geol. Ass., xxxv, 1924, 187–8.Google Scholar