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Meanwhile, this theory is hardly better off first. We don't haveany Foundation with the confidence to believe that formations containingthe same organic remains, synchronous in its origin. Exactlyalso it would be too bold to assert that the formations containing variousorganic remains, certainly different and at the time of their origin.These provisions are, no doubt, will strike most readers, but theyof course, accepted the highest authority. Sir Charles Lyellrecognizes that organic remains should rely "withsame restrictions as on the mineral characteristics". Sir Henry de LaBech, which makes the various examples in confirmation of this truth,specifies the way to a sharp difference that should exist betweenfossil remains of our coal seams and remains of sealayers formed during the same period. But despite the fact that in the abstractreasoning clearly admits the danger of basing positive conclusions ondata submitted to us by the fossil remains, in practice, do littlepay attention to the danger. The generally accepted conclusion regardingdegrees of antiquity seams a little taking it in consideration; and many geologistsapparently, absolutely not even suspect its existence.
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