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From the very beginning of the dispute the arguments of the disputing parties revolved around thoseevidence of the gradual improvement of organicforms that we see in the rising number of our sedimentary formations. Onehand, those who contend that higher organisms evolved from lower ones,as proponents of the view that the progressive higher organisms werecreated consistently in later periods, indicate the testimony ofthe paleontological facts, speaking in favor of their views. On the otherhand, the uniformitarian, who not only reject the hypothesis of development, butdeny the fact that modern life forms are higher formslast, argue that the paleontological evidence currentlystill very incomplete, that, although we have not found still the remnants of creatures withthe highest organization in layers the most ancient times, it does not givewe claim that such creatures did not exist at the timewhen these layers are settled, and that, in all probability, geologicalthe study will eventually open the desired substance. It is impossible not to admit that so far the evidence be in favor ofthe latest instalment. Every year geological discoveries show how littleall you can give prices negative facts. The belief that in ancientlayers are no traces of higher organisms was not due to the lack ofsuch residues, but due to incomplete research. In this exampleincompleteness of sir Charles Lyell, on page 460 of his Leadership to the elementaryof Geology, leads the list. From this list it appears that in 1709 notknew of the existence of fish in the strata of the underlying Permian system. In 1793G. they were found in the underlying Carboniferous system, in 1828 in the Devonian,in 1840 in the upper Silurian. About the reptiles, we read that in 1710 gfound in the lower Permian system, in 1844 - in the Carboniferous, in1852 in the upper Devonian. On the other hand, a list of mammalsshows that in 1798 was not yet opened any mammal belowthe middle Eocene; but in 1818. they were discovered in the lower oolitic, in1847 in the upper Trias.
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