The Medals of Creation, Volumes 1 and 2: First Lessons in Geology and the Study of Organic RemainsMantell, Gideon Algernon
Science
The Medals of Creation, Volumes 1 and 2: First Lessons in Geology and the Study of Organic Remains
Mantell, Gideon Algernon
Geology -- England -- Guidebooks; Paleontology
As in the more recent forms, these Cidarites are separable into
two groups or families; one in which the spiniferous tubercles are
imperforate as in the Echinus (_Palæchinidæ_ of M'Coy); the other
with numerous small secondary tubercles and a few large primary
ones, perforated for the ligament of the spine as in Cidaris (the
_Archæocidaridæ_ of M'Coy).[301]
[301] Prof. Sedgwick's "British Palæozoic Fossils," p. 124.
Clypeastridæ.--The shell in this family of sea-urchins, is oblong or
rounded; the mouth is of an angular form, and situated in the middle
of the base or inferior face; it is furnished with well-developed
dental organs. The outlet is distant from the summit. The tubercles
are mere granulations, and the spines proportionally small. This group
is subdivided into two tribes: the Galeritidæ (_helmet-like_), and the
Clypeideæ (_buckler-like_).
Galerites albo-galerus. _Lign. 104._--The tribe of which this genus is
the type has the shell inflated, orbicular, oblong, or pentangular.
The ambulacra are simple, never petaloid; the poriferous zones extend
uninterruptedly from the summit to the mouth.
In the species figured _Lign. 104, fig. 1_, the shell is of a
conical form, in some varieties subpentagonal; narrowest at the hinder
part. The mouth is of a decagonal shape, and armed with teeth: it is
situated in the centre of the base (_Lign. 104, fig, 1a_); the outlet
is near the posterior margin of the base. The surface of the shell
is covered with granulations irregularly distributed. This species,
which received the name of _albo-galerus_, from its fancied resemblance
to the white conical caps of the priests of Jupiter, occurs in great
numbers and perfection in the Kentish chalk; it is less common in that
of Sussex. Siliceous casts of the shell are constantly found among the
drift and gravel, and on the ploughed lands of chalk districts; they
are popularly termed "_sugar-loaves_." The specimens obtained from the
chalk, when filled with flint, yield exquisite casts, if the shell be
dissolved in dilute hydrochloric acid; by this means the form of the
plates, and casts of the minutest ambulacral pores are obtained.
[Sidenote: ECHINITES FROM THE CHALK.]
[Illustration: Lign. 104. Echinites from the Chalk. _Lewes._
Fig. 1.--Galerites albo-galerus: _nat._
1_a_.--Base of the same, with the five teeth.
2.--Ananchytes ovatus: 1/2 _nat._
2_a_.--Base of the same.
]
[Illustration: Lign. 105. Holectypus (_Galerites_) inflatus.
_Kimmeridge Clay, Switzerland._
The left-hand figure shows the summit; the middle figure a profile; and
the right hand, a view of the base, with the mouth in the centre, and
the outlet towards the margin. (_M. Agassiz_).]
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