Page:Geology and Mineralogy considered with reference to Natural Theology, 1837, volume 1.djvu/385

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This third great change in the vegetable kingdom is considered to supply another argument in favour of the opinion, that the temperature of the Atmosphere, has gone on continually diminishing from the first commencement of life upon our globe.

The number of species of plants in the various divisions of the Tertiary strata, is as yet imperfectly known. In 1828, M. Ad. Brongniart considered the number then discovered, but not all described, to be 166. Many of these belonging to Genera at that time not determined. The most striking difference between the vegetables of this and of the preceding periods is the abundance in the Tertiary series, of existing forms of Dicotyledonous Plants and large trees, e. g. Poplars, Willows, Elms, Chestnuts, Sycamores, and many other Genera whose living species are familiar to us.

Some of the most remarkable accumulations of this vegetation are those, which form extensive beds of Lignite and Brown-coal. In some parts of Germany this Brown-coal occurs in strata of more than thirty feet in thickness, chiefly composed of trees which have been drifted, apparently by fresh water, from their place of growth, and spread forth in beds, usually alternating with sand and clay, at the bottom of then existing lakes or estuaries.

The Lignite, or beds of imperfect and stinking Coal near Poole in Dorset, Bovey in Devon, and Soissons in France, have been referred to the first, or Eocene period of the Tertiary formations. To the same period probably belongs the Surturbrand of Iceland, (see Henderson's Iceland, vol. ii. p. 114.) and the well-known examples of Brown-coal on the Rhine near Cologne and Bonn, and of the Meisner mountain, and Habichtswald near Cassel. These formations occasionally contain the remains of Palms, and Professor Lindley has lately recognised, among some specimens