MODERN BOTANY - P. RAVEN - 1990
Appendix B. Geological Eras
Class="center">Era1 |
Period1 |
Epoch1 |
Life Forms |
Climate and Major Geological Events |
Cenozoic (65) |
Quaternary (2) Tertiary (65) |
Recent, or Holocene (0.01) Pleistocene (2) Pliocene (5.1) Miocene (24.6) Oligocene (38) Eocene (54.9) Paleocene (65) |
Age of humans. Extinction of many large mammals and birds Aridification, desert formation; climates become diverse. First appearance of Australopithecines Spread of grasslands as forests shrink. Herbaceous mammals, higher primates Herbivorous mammals, ape-like primates; appearance of many modern plant genera Widespread adaptive radiation of mammals and birds; beginning of grassland formation Early insectivorous mammals and primates |
Fluctuations from cold to mild. More than two dozen glacial advances and retreats, final uplift of many mountain ranges Colder. Intensive mountain-building processes; extensive glaciation in the Northern Hemisphere. Uplift of the Isthmus of Panama, connecting North and South America Temperate. Extensive glaciation begins again in the Southern Hemisphere Uplift of the Alps and Himalayas. South America separates from Antarctica. Volcanoes in the Rocky Mountains Mild to distinctly tropical. Australia separates from Antarctica; Hindustan connects with Asia Mild to cool. Extensive shallow continental seas largely disappear |
Mesozoic (248) |
Cretaceous (144) Jurassic (213) Triassic (248) |
Appearance and dominance of many groups of angiosperms and insects. Age of reptiles. Dinosaur extinction at the end of the period Gymnosperms, especially cycads. Appearance of birds Forests of gymnosperms and ferns. Appearance of dinosaurs and mammals |
Climate universally tropical or subtropical. Africa and South America separate Mild. Lowland continents with vast areas covered by seas Mountainous continents joined into a supercontinent. Extensive arid regions |
|
Paleozoic (590) |
Permian (286) Carboniferous: Pennsylvanian (320) and Mississippian (360) subperiods Devonian (408) Silurian (438) Ordovician (505) Cambrian (590) |
Appearance of conifers, cycads, and ginkgos; earlier types of forests disappear. Increasing diversity of reptiles Amphibians move onto land; forests appear and become dominant. Emergence of insects and reptiles. Age of amphibians Age of Fishes. Spread of land plants; extinction of primitive vascular plants The period begins with an intensive organismal extinction. First fossil plants. First jawed fishes The period begins with the first large-scale organismal extinction. Oldest fossil crustaceans. Increased diversity of Mollusks. Possible migration of plants onto land. First Fungi Emergence of external skeletons in animals. Explosive evolution of phyla and divisions. Appearance of Chordates. |
Extensive glaciation in the Southern Hemisphere. Uplift of the Appalachians. Widespread aridity Warm, with minor seasonal fluctuations; lowland, swampy land; formation of coal deposits Most of the continents covered by seas, mountains are rare Mild. Continents mostly flat Mild. Shallow seas, continents mostly flat; seas cover a significant part of the modern USA Mild. Territories of modern continents occupied by vast seas |
|
Precambrian (4500) |
Origin of life (at least 3.5 billion years ago), eukaryotes (at least 1.5 billion years ago), Multicellular animals (about 700 million years ago) |
Formation of the Earth's crust and the onset of continental drift |
1 The number following the name of a geological time interval indicates how many millions of years ago it began
Last update: 07/08/2026
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