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In Siluria sirR. Murchison everywhere assumes that the same or related breeds lived onthe face of the Earth at the same time. In Russia, in Bohemia, in the UnitedThe States, in South America, strata are classed as belonging to one oranother part of the Silurian system only on the grounds that they containsimilar fossils themselves; it is sufficient that they are two ora known quantity of the same or related between themselves breedsthey belong to the same epoch, in whatever area these layers are nowere is a matter of undoubted In Russia the relative positionlayers is determined on the basis of the fact that, together with someunlocking forms you find an instance of Pentamerus oblongus.Based on the fact that one form of crustaceans, known under the nameeurypterid is a distinguishing feature of the upper sadlowski mountainbreed, the author observes that "eurypterid fall into the so-called blacktraumatolog shale in Westmorland in Onatsko County new York, shale,which, in all probability, will be the corresponding upper sadlowskithe breed". It is "in all probability" shows us to what extent the strongconfidence in widespread distribution of the same organisms in one andthe same era, and at the same time provides us with the example of the ease with which thisconfidence begets of itself any evidence in advancepreparing the minds to find an identity in a time where fossil rocksbe the same. Sir R. Murchison interprets not onlyformations of Russia, England and America, but extends the same welcome and the antipodesFossils found in the colony of Victoria, he is with the quartermaster,sent from the government, klassificeret as belonging to the lowerlandamerica or Silurian age, in other words, it takesthe undoubted fact that at the time when the famous breed of crustaceans andmollusks lived in Wallis, breed similar crustaceans and mollusks were living inAustralia.
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