The Principles of Stratigraphical GeologyMarr, J. E. (John Edward)
Science
The Principles of Stratigraphical Geology
Marr, J. E. (John Edward)
Geology, Stratigraphic
The Palæontological evidence in favour of destruction of ancient
continental areas and their replacement by the sea is more
satisfactory than that which is based on physical grounds. The
distribution of the Glossopteris flora of the Permo-Carboniferous
period points to the former existence of a great southern continent,
including the sites of Australia, India, South Africa and South
America,--the Gondwanaland of Prof. E. Suess[124].
[Footnote 124: On this question and that of the other destroyed
continental areas noted here, see W. T. Blanford's _Presidential
Address_, _loc. cit._]
Again, a study of Jurassic and Cretaceous faunas has led
palæontologists to conclude that there was a connexion betwixt S.
Africa and India in Mesozoic times across a portion of the area now
occupied by the Indian Ocean, and also between S. Africa and S.
America, and these inferences are supported by study of the
distribution of existing forms.
The sudden appearance of the Dicotyledonous Angiosperms in Upper
Cretaceous rocks has also been used as evidence of destruction of
considerable tracts of land subsequently to Upper Cretaceous times,
and there is a certain amount of evidence in favour of the existence
of this land in the north polar region, in an area now largely
occupied by water, though relics of it are left, as the Faroe Isles,
Spitsbergen, Novaya Zembla and Franz Josef Land.
I cannot conclude the consideration of the question of permanence of
oceans and continents more fitly than by quoting from Dr Blanford's
address. He says, "There is no evidence whatever in favour of the
extreme view accepted by some physicists and geologists that every
ocean-bed now more than 1000 fathoms deep has always been ocean, and
that no part of the continental area has ever been beneath the deep
sea. Not only is there clear proof that some land-areas lying within
continental limits have at a comparatively recent date been submerged
over 1000 fathoms, whilst sea-bottoms now over 1000 fathoms deep must
have been land in part of the Tertiary era, but there are a mass of
facts both geological and biological in favour of land-connexion
having formerly existed in certain cases across what are now broad and
deep ocean[125]."
[Footnote 125: _Loc. cit._, _Proc._ p. 107.]
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