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.

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