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Graptolites with Associated Sedimentary Grooving

Published online by Cambridge University Press:  01 May 2009

J. D. D. Smith
J. D. D. Smith
Affiliation:
Geological Survey and Museum, Exhibition Road, London, S.W. 7.
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Abstract

Two graptolites with associated grooving in the sediment are recorded; these structures are thought to be caused by the thecae grooving the sediment during movement of the graptolite by a flow of overlying mud.

Type
Articles
Information
Geological Magazine , Volume 94 , Issue 5 , October 1957 , pp. 425 - 428
Copyright
Copyright © Cambridge University Press 1957

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References

REFERENCES

Bulman, O. M. B., 1957. Annotated Bibliography of Marine Paleoecology—Graptolites. Mem. Geol. Soc. Amer., Mem. 67, vol. 2, 987–991.Google Scholar
Hundt, R., 1938. Eine biostratomisch interessante Graptolithenplatte. Zentralblatt für Min, u.s.w., Abt. B, no. 7, 269–271.Google Scholar
Kuenen, P. H., 1950. Turbidity currents of high density. Rep. 18th Int. Geol. Cong., viii, 44–52.Google Scholar
Kuenen, P. H., and Menard, H. W., 1952. Turbidity currents, graded and non-graded deposits. Journ. Sed. Pet., xxii, 83–96.Google Scholar
Lamplugh, G. W., Kitchin, F. L., and Pringle, J., 1923. The Concealed Mesozoic Rocks in Kent. Mem. Geol. Surv.Google Scholar