The Student's Elements of GeologyLyell, Charles, Sir
Science
The Student's Elements of Geology
Lyell, Charles, Sir
Geology
Relation of the Fauna of the Crag to that of the recent Seas.—By far
the greater number of the recent marine species occurring in the
several Crag formations are still inhabitants of the British seas; but
even these differ considerably in their relative abundance, some of the
commonest of the Crag shells being now extremely scarce—as, for
example, _Buccinum Dalei_—while others, rarely met with in a fossil
state, are now very common, as _Murex erinaceus_ and _Cardium
echinatum._ Some of the species also, the identity of which with the
living would not be disputed by any conchologist, are nevertheless
distinguishable as varieties, whether by slight deviations in form or a
difference in average dimensions. Since Mr. Searles Wood first
described the marine testacea of the Crags, the additions made to that
fossil fauna have not been considerable, whereas we have made in the
same period immense progress in our knowledge of the living testacea of
the British and arctic seas, and of the Mediterranean. By this means
the naturalist has been enabled to identify with existing species many
forms previously supposed to be extinct.
In the forthcoming supplement to the invaluable monograph communicated
by Mr. Wood to the Palæontographical Society, in which he has completed
his figures and descriptions of the British crag shells of every age,
list will be found of all the fossil shells, of which a summary is
given in the table, p. 202.
To begin with the uppermost or Chillesford beds, it will be seen that
about 9 per cent only are extinct, or not known as living, whereas in
the Norwich, which succeeds in the descending order, seventeen in a
hundred are extinct. Formerly, when the Norwich or Fluvio-marine Crag
was spoken of, both these formations were included under the same head,
for both at Bramerton and Thorpe, the chief localities where the
Norwich Crag was studied, an overlying deposit occurs referable to the
Chillesford age. If now the two were fused together as of old, their
shells would, according to Mr. Wood, yield a percentage of fifteen in a
hundred of species extinct or not known as living.
NUMBER OF KNOWN SPECIES OF MARINE TESTACEA IN THE CRAG.
CHILLESFORD AND ALDEBY BEDS Total
number Not known
as living Percentage of
Shells not known
as living Bivalves 61 4 9·5 Univalves 33 5
Brachiopods 0 0 NORWICH OR FLUVIO-MARINE CRAG Bivalves
61 10 17·5 Univalves 64 12 Brachiopods 1 0
RED CRAG
_(Exclusive to many derivative shells)_ Bivalves 128 31 25·0
Univalves 127 33 Brachiopods 1 1 CORALLINE CRAG
Bivalves 161 47 31·5 Univalves 184 60 Brachiopods
5 3
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