Geological facts; or, the crust of the earth, what it is, and what are its uses — John Shaqi
Geological facts; or, the crust of the earth, what it is, and what are its usesBarrett, W. G. (William Garland)
Religion
Geological facts; or, the crust of the earth, what it is, and what are its uses
Barrett, W. G. (William Garland)
Geology
Now with regard to the hard names to which we have just made
allusion—names that, apart from their etymology, which is nothing more
than “sending vagrant words back to their parish,” are enough to startle
any one; names such as heterocercal, homocercal, cephalaspis,
pterichthys, coccosteus, osteolepis, &c. &c.—why, they will all
presently become plain, and, we hope, familiar to our readers. “They
are,” says Hugh Miller, “like all names in science, unfamiliar in their
aspect to mere English readers, just because they are names not for
England alone, but for England and the world. I am assured, however,
that they are all composed of very good Greek, and picturesquely
descriptive of some peculiarity in the fossils they designate.”[41]
The rest of this chapter will be occupied with an account of the four
most remarkable and characteristic fishes of this formation, to
understand which a few preliminary remarks are necessary. Cuvier divided
all fish into two groups, the _bony_ and the _cartilaginous_; and these
two groups he subdivided into two divisions, characterised by
differences in their _fins_, or organs of locomotion, one of which he
called Acanthopterygian,[42] (thorny-finned,) and the other,
Malacopterygian,[43] (or soft-finned.) This concise arrangement did not,
however, meet all the wants of the fish-students, and it was often
practically difficult to know under which class to arrange particular
specimens. More recently M. Agassiz has arranged fish, not according to
their _fins_, but according to their _scales_; and simple as this
classification may seem, it is one of the greatest triumphs of genius in
modern times, inasmuch as all fishes extinct and existing, that have
inhabited or are inhabiting the “waters under the earth,” may be grouped
easily under the following four divisions:—
[Illustration:
1. GANOID SCALE; as bony pike.[44]
]
[Illustration:
2. PLACOID SCALE.[45]
]
[Illustration:
3. CTENOID SCALE; as sole or perch.[46]
]
[Illustration:
4. CYCLOID SCALE; as herring.[47]
]
One more preliminary remark, and we will proceed to look at the four
fishes already alluded to. Neither the teacher nor the student of any
science can skip definitions, axioms, postulates, and so on; they must
just be mastered, and their mastery is a real pleasure. In addition to a
marked difference in the _fins_, a difference was observed also in the
_tails_ of fossil (extinct) and living pieces of fish. This difference
between the tails of fish has been happily described in two words,
heterocercal and homocercal, of which the figures below will give a
better idea than a lengthened description.
[Illustration:
1. HETEROCERCAL.
]
[Illustration:
2. HOMOCERCAL.
]
[Illustration:
3. HOMOCERCAL.
]
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