History of Life on Earth Notes
How Old is Earth?
- Estimated age: 4.5 billion years old.
- Alexander Ivanovich Oparin: Proposed early Earth's reactive atmosphere and "primordial soup" oceans.
Origin of Life
- Stanley Miller and Harold Urey: Experiment simulating early atmosphere with hydrogen, methane, ammonia, and water, yielding amino acids.
- Microscopic cell-like structures appeared 200-300 million years ago.
- Protenoid microspheres: Selectively permeable membrane; simple energy storage/release.
- Possible locations:
- Soil surfaces
- Interstellar space
- Atmosphere
- Oceans (though less likely due to high sodium and chlorine content)
Origin of Eukaryotic Cells
- Endosymbiosis: Organism lives inside another.
- Endosymbiotic theory: Eukaryotic cells formed symbiotic relationships with prokaryotic organisms.
Paleontology
- Study of the history of life, including the origin and extinction of different groups.
- Focuses on fossil remains, ecologies of the past, and organism evolution.
- Example: Archaeopteryx lithographica shows dinosaur ancestry of birds
Geology
- The study of rocks and Earth's materials
Geologic Time Scale
- Calendar of Earth's history arranged chronologically.
- Developed by studying rock layers and index fossils.
- Divisions: Eon, Era, Period, Epoch.
Divisions of Geologic Time Scale
- Eons: Largest divisions (hundreds of millions of years).
- Phanerozoic: Organisms with skeletons or hard shells.
- Proterozoic: First multicellular organisms; mass extinction.
- Archaeozoic: First single-celled organisms.
- Hadean: Earth's formation from dust and gases.
- Precambrian Time: Proterozoic, Archaeozoic, and Hadean eons (almost 90% of Earth’s history).
- Eras: Smaller time intervals within eons.
- Phanerozoic divided into Paleozoic, Mesozoic, and Cenozoic.
Eras
- Paleozoic: Marine organisms
- Mesozoic: Age of Reptiles/Dinosaurs, appearance of flowering plants.
- Cenozoic: Age of Mammals
Periods
- Subdivisions of eras.
- Proterozoic: Vendian/Ediacaran (soft-bodied underwater life).
- Paleozoic: Cambrian, Ordovician, Silurian, Devonian, Carboniferous, Permian.
Periods Explained
- Cambrian: Hard body parts evolved; most animal phyla appeared.
- Ordovician and Silurian: Early cephalopods.
- Devonian: Plants adapted to land; Age of Fishes.
- Carboniferous and Permian: Reptiles evolved from amphibians.
- Mesozoic: Cretaceous, Jurassic, and Triassic periods (age of dinosaurs).
Mesozoic Periods
- Triassic: Dinosaurs appeared (e.g., Coelophysis).
- Jurassic: Dinosaurs dominated land; Archeopteryx appeared.
- Cretaceous: Reptiles were dominant; new dinosaurs evolved; meteorite-caused mass extinction.
Cenozoic Era
- Divided into Tertiary and Quaternary periods.
- Tertiary: Warm climate; flowering plants and grasses flourished.
- Quaternary: "Age of Man"; ice ages; Homo sapiens evolved.
Epochs
- Finer subdivisions (Cenozoic and parts of Mesozoic eras).
- Geologic timescale is used to identify past organisms.