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
Pentremites pyriformis (_Pear-shaped angular Encrinite_). _Lign.
91, fig. 2._--The column of this remarkable crinoid is short, and
formed of cylindrical, perforated ossicula, with radiated surfaces,
and has irregular side-arms. The receptacle is composed of polygonal
plates, divided by five perforated grooves or furrows, which are of
an elongated petalous form, and converge in a rosette on the summit.
The marginal longitudinal rows of minute pores are not however for the
passage of soft membranous feelers, as in the ambulacra of echinoderms,
as was formerly conjectured, but are channels for the transit of
vessels that supply an infinite number of delicate simple tentacula,
composed of extremely minute calcareous ossicula, as in the other
Crinoidea, but not subdivided as in the Pentacrinites and Encrinites.
These articulated tentacula are arranged close together in longitudinal
rows on the ambulacral spaces; there being two rows, each consisting
of fifty tentacula, on every space. They are directed upwards towards
the vertex of the receptacle, and appear to be the instruments for the
capture and conveyance of food to the mouth.[287]
[287] See Dr. Fred. Röemer on jointed tentacles found on the ambulacral
spaces of _Pentremites_, "Geol. Journal," vol. v. p. 8.
There are several species of Pentremites, some of which swarm in the
cherty limestones of Kentucky. Mr. Say, to whom we are indebted for the
first satisfactory investigation of these fossils, mentions that such
is their abundance, that he has observed, on a piece of rock not larger
than three inches by two-and-a-half, above twenty specimens lying in
relief
Cystidea.--In the ancient fossiliferous strata there occurs a
remarkable family of crinoideans, which is supposed to be restricted
to the palæozoic ages; these fossils have been named by Von Buch,
_Cystideæ_, from the body of the animal being wholly inclosed in a
cyst, or box. The receptacle is of a spherical form, and composed of
polygonal plates, articulated to each other; it has distinct apertures
for the mouth, vent, and oviduct; the orifice of the latter is closed
by valves. It has a short pedicle, but no arms have been discovered,
and the Cystideæ are generally described as Crinoids without appendages
of this kind. But in some members of this group, there are not only
arms and tentacula, but likewise certain organs connected with the
plates, which Prof E. Forbes terms, "pectinated rhombs," the functions
of which are not obvious. The arms more closely resemble those of
the Ophiuridæ than of the Crinoidea.[288] This order comprises several
genera, and is the type under which the Crinoidea first appear in
the natural records of our planet, according to the present state of
our knowledge, and which becomes extinct before the advent of the
Pentacrinites.
[288] See a memoir on the British Cystidea, by Prof. Ed. Forbes; in the
Mem. Geological Survey, vol. ii.
[Sidenote: MARSUPITES MILLERI.]
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