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Due to the slow changes inthe direction of the earth's axis of these extremes are gradually softened. By the end of 10 500years achieved the opposite, moderately hot, longsummer gives way to warm and short winter. Currentlythe predominance of sea in the southern hemisphere contributes significantlyto mitigate those extremes faced this hemisphere due toastronomical terms. On the other hand, the large predominance ofcontinent in the Northern hemisphere contributes to the difference, whichexists on this hemisphere between summer and winter; so at the present timethe climate of both hemispheres are not very dramatically different from each other. But afterten thousand years the Northern hemisphere will have a much strongest annualtemperature fluctuations, than at present. In the latest edition of his Essays on astronomy, sir John Herschel admitsthis circumstance is an important element in geological processes and considersit is highly probable that it partly influenced the climatic changes onwhich indicate monuments of the past of the Earth. To this circumstance playedan important role in the most dramatic changes in the climate, indicatedus the actual data, it is hardly likely, as we have reason to think thatthese changes were much slower and lasted longer; but that itcould result in a rhythmic or most extreme moderationclimates due to other causes, seems to us to be unquestionable fact.Equally undeniable is the us and the fact that, in accordance with thesechanges in climate have occurred and known changes in rhythmicthe distribution of organisms, and these rhythmic changes we would liketo draw the reader's attention, as one of the reasons for the smaller breaks,notice in the succession of fossil remains.
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