Henry Fairfield Osborn

Summary

Henry Fairfield Osborn 1911 Encyclopædia Britannica, Volume 20… (1911)

In order to illustrate the grateful services which palaeontology through restoration may render to the related earth sciences let us imagine a vast continent of the past wholly unknown in its physical features, elevation, climate, configuration, but richly represented by fossil remains. All the fossil plants and animals of every kind are brought from this continent into a great museum
Source: Wikisource

Henry Fairfield Osborn 1911 Encyclopædia Britannica, Volume 20… (1911)

The mutual relations of palaeontology and embryology and comparative anatomy as means of determining the ancestry of animals are most interesting. In tracing the phylogeny, or ancestral history of organs, palaeontology affords the only absolute criterion on the successive evolution of organs in time as well as of (progressive) evolution in form. From comparative anatomy alone it is possible to arrange a series of living forms which, although structurally a convincing array because placed in a graded series, may be, nevertheless, in an order inverse to that of the actual historical succession.
Source: Wikisource

Henry Fairfield Osborn 1911 Encyclopædia Britannica, Volume 20… (1911)

It should be remembered that palaeontology is the most unfavourable field of all for observation and demonstration of sudden salutations or mutations of character, because of the limited materials available for comparison and the rarity of genetic series. It should be borne in mind, first, that wherever a new animal suddenly appears or a new character suddenly arises in a fossil horizon we must consider whether such appearance maybe due to the non-discovery of transitional links with older forms, or to the sudden invasion of a new type or new organ which has gradually evolved elsewhere.
Source: Wikisource

Get perspective with Kwize: daily news enlightened by great literature