The Edinburgh New Philosophical Journal, Vol. XLIX: April-October 1850Various
Science
The Edinburgh New Philosophical Journal, Vol. XLIX: April-October 1850
Various
Science -- Periodicals
"IV. _Jurassic Period._--This period is one of the most extensive by
the formations which it comprehends, and the variety of different
special epochs of vegetation which it embraces; although we cannot
refuse to comprehend, under a common title, epochs during which very
analogous forms have succeeded each other. It thus comprehends from
the Keuper inclusively, up to the Wealdean formations. In fact, we
find the Pterophyllum of the Keuper appear anew, with slight specific
differences in the Wealdean formations. The _equisetites_ of the
Keuper extend to the mean oolithic formation; the _baiera_ of the Lias
likewise recurs in the Wealdean beds of the north of Germany; the
Sagenopteris and the Camptopteris likewise appear in the Keuper, Lias,
and Oolite.
"Yet these common characters, which indicate a great analogy between
the Floras of each of these epochs of formation, do not prevent each
of them having characters of its own, and often an assemblage of
species, almost all peculiar to each particular epoch. We ought,
therefore, to distinguish here those various subdivisions, the number
of which will perhaps be afterwards multiplied, when we become better
acquainted with the vegetables of each of the stages of the Jurassic
formations.
"_Keupric Epoch._--M. Brongniart then gives an enumeration of the
vegetables of the Keupric epoch, which, in regard to the Amphigenous
cryptogams, consist of Algæ; in regard to the Acrogenous cryptogams,
of Ferns and Equisetaceæ; in the case of the Gymnospermous
dicotyledons of Cycadeæ and Coniferæ; lastly, of two doubtful
monocotyledons (_Palæoxyris_ and _Preisleria_.)
"On comparing this Flora with that of the variegated sandstone of the
Vosges, and with that of the Lias, we perceive that it has nothing in
common with the first except the palæoxyris, which appears very nearly
related to that of the variegated sandstone; on the contrary, it
resembles the Flora of the Lias or Oolite in the ferns, many of which
are specifically identical, or nearly allied in the _Nilsonia_ and
_Pterophyllum_, which are likewise either identical, or very nearly
connected specifically with the Lias.
"_Lias Epoch._--The Liasic epoch furnishes Amphigenous cryptogams,
consisting of Algæ, mushrooms, and lichens; Acrogenous cryptogams,
such as Ferns, Marsileaceæ, Lycopodiaceæ, and Equisetaceæ;
Gymnospermous dicotyledons, represented by the Cycadeæ and Coniferæ;
finally, doubtful monocotyledons, consisting of _Proacites_ and
_Cyperites_.
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