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
A tooth from the Fife coal-field, drawn
for one of the woodcuts in a popular elementary manual, was also
named megalichthys; an error perpetuated through every edition till
the last, where the tooth has been restored to its true owner--the
holoptychius. In truth, no two organisms have ever been so maltreated;
and if the reader will kindly bear with me a little further, it will
not be difficult to show him that the holoptychius had peculiarities
of its own quite as distinct as those that have come before us in the
megalichthys, and that each animal has a full and legitimate claim to a
separate and independent niche in the gallery of fossil fishes.
[Footnote 45: See Agassiz, _Poiss. Foss._, tom. ii. Part 2, p. 89 _et
seq._]
The word _holoptychius_ means, as I have said, "wrinkled or folded
all over,"--a name truly expressive of the peculiar style of ornament
displayed by every part of the exterior of the animal's body. The
head-plates, which are of great size, exhibit a fine corrugated
shagreen-like surface, roughened into knobs, and wavy lines of
confluent tubercules, that remind one disposed to be fanciful, of a
frosty December moon with its isolated peaks, and confluent mountain
chains. The scales are of a rounded or oval form, and vary from less
than half an inch to fully four or even five inches in diameter.
Their upper side consists of two parts, one of which with a crescent
shape lay beneath, the over-lapping scales, while the other passed
outwards to form a portion of the outer visible surface. The part
that was hidden by the overlapping scale was smooth, with a finely
striated surface. The exposed portion displayed the usual corrugated
sculpturing, many of the little tubercules having striated sides, and
showing, in consequence, no little resemblance to the star-like knobs
on the dermal covering of the Old Red Sandstone asterolepis. The inner
surface of the scales was concave, with a central prominent oblong
point surrounded by encircling scaly ridges, and forming what is called
the centre of ossification.[46]
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