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Relatively organic bodies, namely, the formations formedcurrently, the rule it is equally true, if notmore. Even along the same coast, a short distanceorganic forms are significantly different. But they differmuch more on the coast, distant from each other. This is added tothe fact that very different organisms livingalong next to the same shore, do not leave their residues inthe same sedimentary layers. For example, at the bottom of the Adriatic sea,where, depending on the prevailing currents, precipitation in some places consist ofTina, in others of calcareous substances, it is known that variousthe types of shells, existing together, are buried in one, then another of theseformations. From our own shores the sea remains, we find inseveral miles from the shore, in the shallows, where fish, other than thoselocated near the shore, where only littoral species.A significant part of marine organisms has such a device body,which does not allow them to go into a state fossils; betweenthe rest most destroyed upon the death of different species of predators.
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