Page:Geology and Mineralogy considered with reference to Natural Theology, 1837, volume 1.djvu/372

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368
FLORA OF THE SECONDARY SERIES.

relative numbers of other families of plants, in each of the successive geological epochs, which are thus connected with our own, by a new and beautiful series of links, derived from one-of the most important tribes of the vegetable kingdom.




SECTION III.


VEGETABLES IN STRATA OF THE SECONDARY SERIES.[1]


Fossil Cycadeæ.

The Flora of the Secondary Series[2] presents characters of an intermediate kind between the Insular vegetation of the Transition series, and the Continental Flora of the Tertiary formations. Its predominating feature consists in the abundant presence of Cycadeæ, (see Pl. 1, Figs. 33, 34, 35,) together with Coniferæ,[3] and Ferns.[4] (See Pl. 1, Figs. 37, 38, 39.),

M. Ad. Brongniart enumerates about seventy species of

  1. See Pl. 1, Figs. 31 to 39.
  2. M. Ad. Brongniart, in his arrangement of fossil plants, has formed, a distinct group out of the few species which have been found in the Red sandstone formation (Gres bigarré) immediately above the Coal. In our division of the strata, this Red-sandstone is included, as an inferior member, in the Secondary series. Five Algæ, three Calamites, five Ferns, and five Coniferæ, two Liliaceæ, and three uncertain Monocotyledonous plants form the entire amount of species which he enumerates in this small Flora.

    See also Jaeger uber die Pflanzenversteinerungen in dem Bausandstein von Stuttgart, 1827.

  3. We again refer to Witham's Account of Conifer: from the Lias, in his observations on Fossil Vegetables, 1833.
  4. A very interesting account, accompanied by figures, showing the internal structure of the stems of fossil arborescent Ferns of the Secondary period, is given in Cotta's Dendrolithen, Dresden, 1832; these appear to be chiefly from the New red sandstone of Chemnitz near Dresden.