Plato Profile Directory 05

War was now inevitable; but the incapacity of Sp. Postumius Albinus, who arrived to conduct it (B.C. 110), and still more that of his brother Aulus, whom he left to command in his absence, when called away to hold the elections at Rome, proved as favorable to Jugurtha as the corruption of their predecessors. Aulus, having penetrated into the heart of Numidia, suffered himself to be surprised in his camp; great part of his army was cut to pieces, and the rest only escaped a similar fate by the ignominy of passing under the yoke. But Jugurtha had little reason to rejoice in this success, great as it might at first appear; for the disgrace at once roused all the spirit of the Roman people; the treaty concluded by Aulus was instantly annulled, immense exertions made to raise troops, and one of the Consuls for the new year (B.C. 109), Q. Caecilius Metellus, hastened to Numidia to retrieve the honor of the Roman arms. But this did not satisfy the people. The scandalous conduct of so many of the Nobles had given fresh life to the popular party; and the Tribune C. Mamilius carried a bill for the appointment of three Commissioners to inquire into the conduct of all of those who had received bribes from Jugurtha. Scaurus, though one of the most guilty, managed to be put upon the Commission. But he dared not shield his confederates. Many men of the highest rank were condemned, among whom were Bestia, Albinus, and Opimius. The last named was the Opimius who acted with such ferocity toward Caius Gracchus and his party. He died in exile at Dyrrhachium some years afterward, in great poverty.

This period produced the great beds of coal we use to-day. But the vegetation of the coal period would present strange features to our eyes. The vegetation commenced with the lowest orders of flowerless plants, such as sea-weeds; but, before it was brought to a close, there was a wonderful variety and richness of plants of the flowerless or Cryptogamic division. In some of the warmest portions of the globe, we have to-day tree-ferns growing four or five feet high. During the closing part of the Paleozoic time, there were growing all over the temperate zone great tree-ferns thirty feet or so in height. Some varieties of rushes in our marshes, a foot or two in height, had representatives in the marshes of the coal period standing thirty feet high, and having woody trunks.<7> Near the close of the Paleozoic time, vegetation assumed a higher form of life. Flowering plants are represented. Pines were growing in the coal measures.

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