Cave Hunting: Researches on the evidence of caves respecting the early inhabitants of EuropeDawkins, William Boyd
History
Cave Hunting: Researches on the evidence of caves respecting the early inhabitants of Europe
Dawkins, William Boyd
Antiquities, Prehistoric -- Europe; Caves -- Europe; Europe -- Antiquities; Prehistoric peoples -- Europe
_Sorex moschatus._
_S. vulgaris._
_Talpa Europæa._
_Trogontherium Cuvieri._
_Castor fiber._
_Ursus spelæus._
_U. arvernensis._
_Canis lupus._
_C. vulpes._
_Machairodus._
_Cervus megaceros._
_C. capreolus._
_C. elaphus._
_Cervus Polignacus._
_C. carnutorum._
_C. verticornis._
_C. Sedgwickii._
_Bos primigenius._
_Hippopotamus major._
_Sus scrofa._
_Equus caballus._
_Rhinoceros etruscus._
_R. megarhinus._
_Elephas meridionalis._
_E. antiquus._
_E. primigenius._
From the examination of this list, the peculiar mixture of pleiocene
and pleistocene species is evident. The _Ursus arvernensis_, _Cervus
Polignacus_, _Hippopotamus major_, _Rhinoceros etruscus_, and _R.
megarhinus_, the horse, _Elephas meridionalis_, and _E. antiquus_
were living in the pleiocene age in France and Italy, and probably in
Norfolk. The cave-bear, the wolf, fox, mole, beaver, Irish elk, roe,
stag, urus, wild-boar, and the mammoth have not as yet been discovered
in the continental pleiocenes, as judged by the standards offered by
the Val d’Arno and Southern France. They are more or less abundant in
the late pleistocene age. This singular association seems to me to
imply that the fauna of the forest-bed is intermediate between the two,
and, from the fact that only three out of the whole series, viz. _Ursus
arvernensis_, _Rhinoceros etruscus_, and _Cervus Polignacus_, are
peculiar to the continental pleiocene, that it is more closely allied
to the pleistocene than to the pleiocene.
It is also very probable that this early pleistocene age was of
considerable duration; for in it we find at least two forms (and the
number will probably be very largely increased) which are unknown in
continental Europe, although pleiocene and pleistocene strata have
been diligently examined in France and Germany. The very presence of
the _Cervus Sedgwickii_ and _C. verticornis_ implies that the lapse
of time was sufficiently great to allow of the evolution of forms of
animal life hitherto unknown, and which disappeared before the middle
and late pleistocene stages. The _Trogontherium_ also, as well as the
_Cervus carnutorum_, both of which occur in the forest-bed and in the
gravel-beds of St. Prest, near Chartres, and which are peculiar to this
horizon, point to the same conclusion.
The deer of the forest-bed, in this list, do not represent
approximately the number of species: there are at least five, and
perhaps six, represented by a series of antlers, which I do not venture
to quote, because I have not been able to compare them with those of
the pleiocenes of the Val d’Arno, of Marseilles, or of Auvergne.
Public-domain text, read in full here on John Shaqi.
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