The topography and geology of the Fayum province of EgyptBeadnell, H. J. L. (Hugh John Llewellyn)
Science
The topography and geology of the Fayum province of Egypt
Beadnell, H. J. L. (Hugh John Llewellyn)
Geology -- Egypt
In this connection it is interesting to notice the observation of
so eminent a palæontologist as Prof. H. F. Osborn. In two recent
addresses[83] to the New York Academy of Sciences he pertinently
points out his belief that the African continent has been a great
centre of radiation of certain groups of the mammalia, and especially
mentions the Proboscidea as likely to have been evolved in the
Ethiopian region. Our discoveries in the Fayûm and Andrews’s
determinations, made subsequently to these addresses, so completely
confirm this view, at any rate with regard to the elephants, that it
may not be out of place to give here a somewhat lengthy extract of his
“_Theory of Successive Invasions of an African Fauna into Europe_”
(op. cit. pp. 56-58). “In Europe there are in the Upper Eocene two
classes of animals, first those which have their ancestors in the older
rocks; second, the class including certain highly specialized animals
which have no ancestors in the older rocks, among these, perhaps,
are the peculiar flying rodents or _Anomaluridæ_, now confined to
Africa, and secondly the highly specialized even-toed ruminant types
the anoplotheres, xiphodonts and others, the discovery of which in the
gypse near Paris Cuvier has made famous. It is tempting to imagine
that these animals did not evolve in Europe but that they represent
what may be called the first invasion of Europe by African types from
the Ethiopian region.
“It is a curious fact that the African continent as a great
theater of adaptive radiation of Mammalia has not been sufficiently
considered. It is true that it is the dark continent of palæontology
for it has no fossil mammal history; but it by no means follows that
the Mammalia did not enjoy there an extensive evolution.[84]
“Although it is quite probable that this idea has been advanced
before, most writers speak mainly or exclusively of _the invasion
of Africa by European types_. Blanford and Allen, it is true, have
especially dwelt upon the likeness of the Oriental and Ethiopian
fauna, but not in connection with its antecedent cause. This cause
I believe to have been mainly an invasion from south to north,
correlated with the northern extension of Ethiopian climate and
flora during the Middle Tertiary. It is in a less measure due to a
migration from north to south. Let us therefore clearly set forth
the hypothesis of _the Ethiopian region or South Africa as a great
center of independent evolution_ and as the source of successive
northward migrations of animals, some of which ultimately reached
even the extremity of South America, I refer to the Mastodons. This
hypothesis is clearly implied if not stated by Blanford in 1876 in
his paper upon the African element in the fauna of India.
Public-domain text, read in full here on John Shaqi.
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