A century of science in America : $b with special reference to the American Journal of Science, 1818-1918
History
A century of science in America : $b with special reference to the American Journal of Science, 1818-1918
American journal of science; Science -- United States -- History
│Upper or Silurian │Ludlowian (Murchison
Silurian Period. │ (Murchison, restricted, │ 1839).
│ 1835). │
„ │ „ │Wenlockian (Murchison
│ │ 1839).
„ │ „ │Landoverian (Murchison).
─────────────────┼──────────────────────────┼──────────────────────────
„ │Middle or Ordovician │Caradocian (Murchison
│ (Lapworth 1879). │ 1839).
„ │ „ │Landeilian (Murchison
│ │ 1839).
„ │ „ │Arenigian (Sedgwick 1847).
─────────────────┼──────────────────────────┼──────────────────────────
│Lower or Cambrian │
„ │ (Sedgwick, restricted, │Potsdamian (Emmons 1838).
│ 1835). │
„ │ „ │Menevian (Salter and Hicks
│ │ 1865).
„ │ „ │Georgian (Hitchcock 1861).
Regarding this period, which, by the way, is not very unlike that of
Barrande, Renevier remarks that it is “as important as the Cretaceous or
the Jurassic. Lapworth even gives it a value of the first order equal to
the Protozoic era.”
In the above there is an obvious objection in the double usage of the
term Silurian, and this difficulty was met later on in Lapparent’s
Traité by the proposal to substitute Gothlandian for Silurian. Of this
change Geikie remarks: “Such an arrangement ... might be adopted if it
did not involve so serious an alteration of the nomenclature in general
use.” On the other hand, if diastrophism and breaks in the stratigraphic
and faunal sequence are to be the basis for geologic time divisions, we
cannot accept the above scheme, for it recognizes but one period where
there are at least four in nature.
_Conclusions._—We have arrived at a time when our knowledge of the
stratigraphic and faunal sequence, plus the orogenic record as
recognized in the principle of diastrophism, should be reflected in the
terminology of the geologic time-table. It would be easy to offer a
satisfactory nomenclature if we were not bound by the law of priority in
publication, and if no one had the geologic chronology of his own time
ingrained in his memory. In addition, the endless literature, with its
accepted nomenclature, bars our way. Therefore with a view of creating
the least change in geologic nomenclature, and of doing the greatest
justice to our predecessors that the present conditions of our knowledge
will allow, the following scheme is offered:
Silurian period. Llandovery to top of Ludlow in Europe.
Alexandrian-Cataract-Medina to top of Manlius in America.
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