Two further places where sedimentary rock may be exposed are roadcuts and quarries, even though the solid rocks nearby are covered with glacial deposits and soil. Fossil collectors are opportunistic. Some of the best fossils are found where weather and well-beaten paths have not had a chance to degrade them; fresh exposures are most often the best. Limestone (calcium carbonate) and shale (fine-grained, layered rocks formed from clay and silt) and sandy silicates often replace the hard parts of ancient animals so well that the original shapes and structures survive many years of exposure. The advent of "acid rain" is certain to do more damage than centuries of normal weathering. ![]()
PHYLLUM:
BRYOZOA - Colonies of these tiny animals underwent extensive development during the Ordovician period. There are approximately as many living species (c.3000) as extinct. BRACHIOPODA - They have shells of unequal valves, and the plane of symmetry runs through the valves rather than between them. About 15,000 species are extinct, but over 200 survive to recent times. MOLLUSCA: ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ANNELIDA - Segmented worms originated in the Cambrian period. Around 36,000 species are living today, while about 1,000 are extinct. ARTHROPODA - Subphylum Trilobitomorpha includes trilobites and related forms, all of which are extinct. Of the entire class other than insects, the ratio is 58,600 living to 4,400 extinct species. ECHINODERMATA - Subphylum Pelmatozoa, Class Crinoidea called "sea lilies" are animals dating from Ordovician times to recent. Of the crinoids, some 800 are living and 5,000 are extinct. |