The Story of a Boulder; or, Gleanings from the Note-book of a Field GeologistGeikie, Archibald
Science
The Story of a Boulder; or, Gleanings from the Note-book of a Field Geologist
Geikie, Archibald
Geology; Petrology
But while this continued the general type on which the encrinites
were constructed, it received many minor modifications. These were
effected chiefly on the form and arrangement of the cup-shaped body
and its appendages, and form now the basis of our classification
into genera and species. Thus, in the genus known as _Platycrinus_,
the lower part of the cup consists of two rows of large hexagonal or
polygonal plates fitting closely into each other, while the upper part
rises into a dome-like elevation formed of smaller polygonal plates,
which have often a mammillated exterior. The arms sprang from the
widest part of the body where the large pieces of the lower cup were
succeeded by the small pieces of the upper. In an Irish species (_P.
triacontadactylus_), the arms subdivided into thirty branches, each
fringed with minuter pinnules and folding round the central elevated
spire, as the petals of a crocus close round its central pistil. In
another encrinite (_Poteriocrinites conicus_), the cup was shaped like
an inverted cone, the point being affixed to the summit of the stalk,
and the broad part throwing out from its edges the lateral arms. The
_Woodocrinus macrodactylus_ had such gigantic arms as well-nigh to
conceal the position of the cup, which relatively was very small in
size. They sprang from near the base of the cup, five in number, but
soon subdivided each into two, the ten arms thus produced being closely
fringed with the usual jointed calcareous pinnules.
The size and arrangement of the joints of the stalk also differed in
different genera. The Woodocrinus and many others had them alternately
broad and narrow, like a string of buttons of unequal sizes; others had
all the joints of the same relative diameter (Fig. 19 _b_), so that the
stalk tapered by a uniform line from base to point. I may add, that
on some specimens of both these kinds of stems, we can notice small,
solitary _areolæ_, or scars, which may mark the points of attachment
of cirri, or little tentacles, like those on the stem of the existing
Pentacrinite. But though each of these varieties of stem is peculiar to
a certain number of genera, there is often so little distinction among
the detached fragments, that it becomes difficult, indeed impossible,
to assign each to its appropriate individual. We may say, that certain
encrinal stalks could not have belonged to a poteriocrinus, and others
could never have fitted on to the cup of an actinocrinus; but we cannot
often say positively to what species they actually would have fitted.
There can, however, be no doubt about their being encrinites, and so
we have in them a safe and evident test for the origin of the rock in
which their remains occur. But to this I shall afterwards revert.
Public-domain text, read in full here on John Shaqi.
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