Essay on the Theory of the EarthCuvier, Georges, baron
Science
Essay on the Theory of the Earth
Cuvier, Georges, baron
Geology; Paleontology
(PART 2 of 2)
+----------------+-------------+
| | Number of |
| | Species |
| NAMES OF +------+------+
|CLASSES, ORDERS,|In the|In the|
| OR FAMILIES. |living|fossil|
| |state.|state.|
| | | |
| | | |
+----------------+------+------+
|Polyparia, | 527 | 414 |
|Stellaridæ, | 76 | 4 |
|Echinidæ, | 95 | 112 |
|Annulosa, | 17 | 29 |
|Serpulacea, | 36 | 69 |
|Cirripeda, | 50 | 17 |
|Tubicolæ, | 11 | 16 |
|Pholadaria, | 12 | 4 |
|Bivalve shells, | 1009 | 1104 |
|Univalve shells,| 1945 | 1544 |
|Genera little | | 5 |
| known, | | |
|Crustacea, | | 54 |
|Pisces, | | 183 |
|Mammifera & | | 89 |
| Cetacea, | | |
|Aves, | | 3 |
|Reptilia, | | 23 |
|Insecta, | | |
|Vegetabilia, | | |
+----------------+------+------+
(a) The fossil remains of birds being very difficult to be
recognized, the number of genera in that state is undoubtably much
more considerable.
THE END.
FOOTNOTES:
[1] See Note A, at the end of this Essay.
[2] See Note B.
[3] The opinion maintained by some geologists, that certain strata
have been formed in the inclined position in which they are now
found, admitting it true with regard to some particular strata
which might have been crystallized, as Mr Greenough supposes, like
the deposit which encrusts the inside of vessels, in which water
containing gypsum has been boiled, cannot at least apply to those
which contain shells or rolled stones, which could not have waited,
so suspended, the formation of the cement by which they were to be
agglutinated.
[4] See Note C.
[5] The conjecture of the Marquis de la Place, that the materials of
which the globe is composed, have perhaps existed at first in the
elastic form, and have successively assumed a liquid consistence on
cooling, and have at length been solidified, is well supported by the
recent experiments of M. Mitscherlich, who has composed, of all sorts
of substances, and crystallized by the heat of intense furnaces,
several of the mineral species which enter into the composition of
primitive mountains.--Note D.
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