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VI.—Blind Trilobites

Published online by Cambridge University Press:  01 May 2009

Extract

The majority of fossiliferous beds in the Cambrian are of anargillaceous nature, and limestones are comparatively rare, but weneed not here enter into a discussion as to the causes of their rarity.When, however, we come to the Ordovician, we find calcareous bedsmuch developed, and since we find in them, as well as in the slatesand shales, these blind genera, and as far as we know not lessabundantly, it appears as if the physical conditions of sedimentationhad but little to do with the existence and perpetuation of theseforms.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1898

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References

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