An Introduction to Paleobotany - download pdf or read online

By Chester A. Arnold

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Extra resources for An Introduction to Paleobotany

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Numerous other examples of imperfects might be cited, although their importance is relatively slight. The fossil record has thrown no light on the problem of the evolution Morphological studies of recent fungi indicate or origin of the fungi. is polyphyletic, different groups having developed from various algal types through the loss of chlorophyll and the resulting inability to sustain themselves independent of previously synthesized that the class organic material. Therefore, it is probably useless to look for a common Different ones originated starting point in the time series for all fungi.

These are lateral There is no evidence structures produced along the sides of the stem. The archegonia that they are axillary, although they may replace leaves. are sessile, but the spore capsules are borne on basal stalks about 3 mm. A "perianth" of four lobes develops around the base of the archegonium. The mature sporophyte is a globular body less than 1 mm. 00 microns in long. diameter. The entire plant was attached by slender rhizoids. Naiadita was originally supposed to be a monocotyledon allied to Naias.

Crystals may, however, form in cavities such as knotholes, stem hollows, or large cracks in otherwise tissues in their original form. well-preserved logs. amethyst crystals Amethyst Mountain received its name from in the silicified logs scattered over the slopes. the Among the cryptocrystalline types agate is frequently present, and splendid examples are found in the Eden Valley petrified forest, of Eocene age, in western Wyoming. Chalcedony characterises the logs in the Petrified In Forest National Monument of Arizona, and jasper is frequent.

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An Introduction to Paleobotany by Chester A. Arnold


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