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V SEMSTER ZOOLOGY GEOLOGICAL TIME SCALE Era Period Epoch Million Organisms evolved Years Coenozoic Quaternary Holocene 0.01-0 Dominance of man. Domestication of animals and agriculture. Modern genera and species evolved. Last ice age 30-40 thousand years ago. Woolly mammoth extinct. Pleistocene 1.5-0.1 Mass extinction. Huge floods. Ice age. Many large mammals extinct. Mastodons and woolly mammoth extinct. Prehistoric man evolved. Cave paintings. Tertiary Pliocene 6-1.5 Dry climate. Oceans shrink. Mammals increase specialization. Mountains rise. First hominids appear. First orchids. Miocene 23-6 Ice age. First man-like apes. Evolution of apes, monkeys, horse, elephant. Radiation of grazing mammals. Huge grasslands. All grass subfamilies distinct. Oligocene 37-23 Archaic mammals attain their maximum diversity. Creodonts (archaic carnivores) appear. First apes. Origin of grasslands. Eocene 53-37 Forests of monocotyledons and flowering plants appear. Ancestors of horse, camel, elephant appear. First bats. Paleocene 65-53 Climate warm. Vegetation abounds. Ancestors of most modern mammals appear. Insectivores abundant. First grasses, Rhododendrons, whales and rodents. 1 Mesozoic Cretaceous Mass extinction. 60% of tetrapod families extinct. 135-65 Himalayas, Andes, Alps arise. Dinosaurs and Ammonites extinct. First monocotyledons. First marsupials and placental mammals (Pantotheres). First flowering plants. Climate cool. Angiosperms radiate. Jurassic 205-135 First bird, Archaeopteryx. Dominance of dinosaurs. Earliest mammals. Dicotyledons and conifers common. Continents become high. Origin of insect pollinators. Triassic 250-205 Mass extinction. 80% of tetrapod families extinct. Continental drift begins. Arid conditions. Gymnosperms dominate. First dinosaurs. Mammal- like reptiles. First teleosts, first crocodiles and first flying reptiles. Palaeozoic Permian 290-250 Mass extinction. 70% of tetrapod families extinct. Single land mass, Pangaea and single ocean. Continents rise. Glaciations set in. Expansion of reptiles, origin of Cotylosauria and Therapsida. Last trilobites. Carbonife- Pennsylva- 290 Warm and humid climate. Swamps abundant. First rous nian modern soils. First reptiles. Sharks abundant. First mammal-like reptiles. Earthworms. Mississipp- Forests of ferns and gymnosperms. Foraminiferans ian 350 and shell-crushing sharks abound. First winged insects. Radiation of amphibians. Little seasonal variations. Devonian 410-350 Mass extinction. Arid climate. First gymnosperm forests. First amphibians (Labyrinthodonts). First spiders. Dominance of fishes. First ferns. First vascular plants. First insects. Silurian 440-410 Algae dominate. Land plants definite. Trilobites decline. First scorpions and millipedes appear. First fishes, ostracoderms and placoderms appear. 2 Ordovician 510-438 Land submerged. Warm climate. Algae abound. Plants invade land. First corals. First vertebrates. Cephalopods and snails. First Agnatha. Cambrian 600-510 Mass extinction. Mild climate. Marine algae. Many invertebrates. Trilobites. Brachiopods. Sponges. Molluscs. Explosion after mass extinction. Proterozoic 3,500-600 Primitive aquatic algae and fungi. Annelid burrows. Protozoa. Oxygenation of atmosphere. Prokaryote radiation. Skeleton of sponges. Archeozoic 4,600-3,500 Calcareous deposits by algae. Origin of life. Fossils of cyanobacteria. Solar 5,000-4,600 Formation of Solar system. Strong solar wind. Formation of primitive atmosphere on earth. Cosmic 20,000-5,000 Big Bang and matter synthesis. 3
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