Earth's Geological Eras and Paleontological Insights
Classified in Geology
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Understanding Earth's Ancient History
Key Concepts in Paleontology
Paleobiogeography: Species Distribution and Migration
- Defining the largest possible precision divergence geographic areas of species and fossil groups.
- Understanding their migrations.
Barriers to Migration
- Weather patterns
- Prevailing winds
- Ocean currents
- Differences in temperature and salinity
- Presence of rivers
- Areas of dense vegetation
- Mountain ranges
Paleontological Basis: Evolution Through Time
- Variation of organisms over time.
- Intermediate or transitional forms.
- Synthetic forms.
- Progressive vestigial organs.
Stratigraphic Paleontology: Fossils and Strata
- Characteristic fossils in specific strata.
- Fast-moving species.
- Wide area dispersion.
- Abundance in the layers.
Earth's Geological Eras: A Timeline
Cenozoic Era (0-65 Million Years Ago)
- Glaciations.
- Quaternary and Tertiary periods.
Mesozoic Era (65-225 Million Years Ago)
- Separation of Pangea.
- Age of Reptiles.
- Flowering plants emerge.
- Periods: Cretaceous, Jurassic, Triassic.
Paleozoic Era (225-570 Million Years Ago)
- Collision of the Americas to form Pangea.
- Periods: Permian, Carboniferous, Devonian, Silurian, Ordovician, Cambrian.
Precambrian Era (570-4600 Million Years Ago)
- Characterized by igneous and metamorphic rocks.
- 100% marine life.
Detailed Eras and Evolutionary Milestones
Precambrian Era: Earth's Earliest Beginnings
- Formation of the planet and primitive atmosphere.
- Impacts of meteorites and volcanic activity.
- Modification of the primitive atmosphere.
- Appearance of photosynthesis.
- High temperatures.
- Earliest evidence of life (potentially extraterrestrial or chemical origin, thermophilic or hyperthermophilic environment).
- Certainties: Unicellular, heterotrophic, anaerobic life forms.
- Increase in atmospheric oxygen.
- Emergence of eukaryotic cells.
- Appearance of the Metazoan group.
Paleozoic Era: Diversification of Life
- Existence of Pangea.
- Greater development of life forms.
- Explosive radiation of marine animals without a spinal column.
- Evolution of the skeleton.
Early Paleozoic: Marine Invertebrates (Cambrian-Silurian)
- Dominance of invertebrate marine organisms.
Late Paleozoic: Conquest of Land (Devonian-Permian)
- Conquest of the terrestrial environment.
- Cambrian: Appearance of jawless fish (agnathans) and the spine.
- Devonian: Jawed fish evolve, amphibian evolution begins.
The Conquest of Land: Key Adaptations
- Body fully supports its weight.
- Efficient breathing mechanisms.
- Adaptations to avoid dehydration.
- Permian: First appearance of reptiles.
Evolution of Plants
- Silurian: Plants had no leaves, stem photosynthesis, reproductive structures at the apex.
- Devonian: Gymnosperms, ferns, mosses appear.
- Cretaceous: Angiosperms emerge.
Evolution of Insects
- Silurian: First appearance of insects.
- Cretaceous: Significant proliferation of insects.
Mesozoic Era: Age of Reptiles and Fragmentation
- Beginning of the fragmentation of Pangea.
- Starts and ends with mass extinctions.
- Increase in biodiversity.
- Significant development of cephalopods.
- Great development of ferns and gymnosperms.
- Onset of warm-blooded organisms.
Cenozoic Era: Age of Mammals and Modern Life
- Age of mammals.
- Diversification of angiosperms and decline of gymnosperms.
- Abundance of insects.
- Evolution of humankind.