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When for a long period of slowly settling the mainland inferiorplace the wide ocean with a few miles of depth, the bottom of which is notmay form sediments, brought by rivers or washed from the shores, andwhen, after another vast period of time, the bottom of this oceanagain begins to slowly rise and become a place of formation of newlayers, not obvious that fossils contained in these newstrata will, in all likelihood, have very little in common with fossilthe remnants of the layers lying under them? Take for example the Northern part of theOf the Atlantic ocean. We have already mentioned the fact that between England andUnited States the ocean floor is covered by Cretaceous sedimentary layer, beginningthis process dates back, in all probability, even to the time whenthere was a great subsidence of the earth's crust, which appearedThe Atlantic ocean in the distant geological epoch. This chalk consists oftiny shells mnogogrannyj shells (Forammifera), whichmixed with the remains of small crustaceans Magnolia (Ento mostraca) andin all probability, a small number of pteropod shells (Pteropoda), althoughthe probe so far has not brought a single copy of the latest Suchthis way, this new Cretaceous formation in higher organic formsis perfect space. Rarely is the bones of somethe polar bear off the ice, could fall to the seabed ordead rotting whale could similarly leave traces. Butsuch remains must be so rare that, even assumingthis new chalk formation is available to immediate observation, the whole STOyears can pass before they will open it But suppose now thatafter a few million years the floor of the Atlantic ocean will rise up and over the topit is overlain by strata of the coastal or estuary precipitation, precipitation of these will containthe remnants of flora and fauna, before from falling inthe underlying layers, making them very easy to take over the newly created shape. So, we see that near continuity of life on the earth's surfacenot only can, but must exist a lot of breaks in the chain of fossilresidue, that's why these breaks cannot be considered asthe arguments that speak against the theory of gradual development. We have to address another common doctrine, and this doctrinemore than any other influences relevant to the question of gradual development.
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