Summary

John Allen Howe 1911 Encyclopædia Britannica, Volume 20… (1911)

The divisions in the fossil record having been thus established, they must for convenience remain, but their artificially cannot be too strongly emphasized, for the broad stratigraphical gaps and lithological groups which made the divisions sharp and clear to the earlier geologists are proved to be absent in other regions, and fossils which were formerly deemed characteristic of the Palaeozoic era are found in some places to commingle with forms of strongly marked Mesozoic type.
Source: Wikisource

John Allen Howe 1911 Encyclopædia Britannica, Volume 20… (1911)

Cambrian, Ordovician, Silurian, Devonian, Carboniferous and Permian. The fact that fossils found in the rocks of the three earlier epochs—Cambrian, Ordovician, Silurian—have features in common, as distinguished from those in the three later epochs has led certain authors to divide this era into an earlier, Protozoic (Proterozoic) and a later Deuterozoic time. The rocks of Palaeozoic age are mainly sandy and muddy sediments with a considerable development of limestone in places.
Source: Wikisource

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