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Vast swampy forests were a marked feature of the Tertiary period, appearing in many of the low-lying land areas that emerged as a result of extensive mountain-folding. To give themselves additional support, conifers grew long prop roots, while the lower trunks of deciduous trees became cone-shaped (see Figure 26). As the original carbon-containing material of the forests became buried, it was subjected to enormous pressure. With the Tertiary swamp deposit, the carbonization process only went to the stage of lignite, or brown coal. This contains much
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less carbon than the earlier Carboniferous deposits, which themselves vary in grade from bituminous (soft) coal to anthracite (hard coal). The appearance of grasses, which belongs to the angiosperm class of monocot, changed the Tertiary landscape as well as the diversity of animals. |