Scarcely any palæontological discovery is more striking than the fact, that the forms of life change almost simultaneously throughout the world. Thus our European Chalk formation can be recognised in many distant
→parts of the world,
under the most different climates, where not a fragment of the mineral chalk itself can be found;
in North America, in equatorial South America, in Tierra del Fuego, at the Cape of Good Hope, and in the peninsula of India. For at these distant points, the organic remains in certain beds present an unmistakeable
resemblance to those of the Chalk. It is not that the same species are met with; for in some cases not one species is identically the same, but they belong to the same families, genera, and sections of genera, and sometimes are similarly characterised in such trifling points as mere superficial sculpture.
other forms, which are not found in the Chalk of
but which occur in the formations either above or below,
→occur in the same order
at these distant points of the world. In the several successive palæozoic formations of Russia, Western
and North America, a similar parallelism in the forms of life has been observed by several
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