Topics covered in this section:
The origin of the solar system
The beginning of life
The earliest life forms
Evolution into multicellular life
Life transitioning onto land
General timelines of animal and human evolution
A PBS NOVA video titled "Where Did We Come From?" is recommended for streaming.
Additional resources for viewing:
YouTube link
Amazon rental option for $2.99
Early Earth had a substantially different atmosphere:
Lack of oxygen and ozone
High UV radiation exposure
Rich in methane, ammonia, water, and hydrogen
Frequent meteorite impacts and volcanic eruptions
Presence of electrical storms and lightning
1950s experiments simulating early Earth conditions (prebiotic simulation):
Mixed gases present in early Earth and added energy sources (electricity, UV light, or heat)
Resulted in the formation of organic molecules within days.
Organic molecules = building blocks of life.
Continued experiments support the hypothesis that:
Simple organic molecules combined to create complex structures leading to the earliest cells.
This process took nearly a billion years for the initial life forms to emerge.
Simple precursor chemicals in a watery environment ("soup")
CO₂, H₂, H₂O, NH₃ present
Formation of small organic molecules
Chemical reactions produce amino acids and lipids.
Joining of monomers into polymers
Formation of polypeptides and nucleic acids.
Genetic material encodes proteins
Lipids create membrane-bound structures.
Formation of protocells
Self-replicating systems encapsulated in membranes.
The idea of "Panspermia":
Suggests life may have originated from extraterrestrial conditions, supported by findings of organic molecules in meteorites.
Current conditions on Earth differ significantly from early Earth:
Reduced volcanic activity and electrical storms
Presence of predatory microbes would hinder the formation of new organic compounds.
Earth formed ~4.5 billion years ago.
Life developed over almost a billion years, with oldest fossils (~3.5 billion years) being prokaryotes (primitive bacteria).
The first prokaryotes thrived in ocean environments, competing for organic molecules.
After a few hundred million years, photosynthetic prokaryotes emerged:
Utilized sunlight for energy, creating an ecological advantage.
Photosynthesis produced oxygen (O₂), essential for the development of Earth’s atmosphere.
Significant oxygen levels appeared ~2 billion years ago, leading to major evolutionary shifts.
The rise in O₂ levels allowed the evolution of aerobic metabolism:
Aerobic organisms harvest significantly more energy compared to anaerobic (prokaryotic) organisms.
Increased energy levels led to competition, enhancing natural selection and contributing to the evolution of complex eukaryotic cells.
The increase of O₂ and protection from UV rays led to greater biodiversity.
The last common ancestor of all current living organisms appeared ~3 billion years ago.
Evolution towards larger cells provided advantages:
Larger cells could capture and consume smaller cells.
However, there were disadvantages regarding diffusion of gases and nutrients.
Solution: evolution of multicellular organisms allowing for specialization of cells.
Multicellular life emerged ~1.2 billion years ago, starting with algae in oceanic environments.
Specialization of cells provided various ecological advantages.
Life began to transition onto land approximately 475 million years ago with the first plants.
Animals followed roughly 400 million years ago.
Land organisms faced several challenges:
Need to support own weight versus buoyancy in water.
Searching for water sources.
Protecting reproductive gametes from dehydration.
Plant life slowly expanded from shallow waters to shores, gaining advantages:
Photosynthesis more efficient outside water.
Access to nutrient-rich soil versus nutrient-limited seawater.
Initial absence of land-based predators.
Early lobefin fishes adapted to terrestrial life, enabling movement across land during dry conditions.
Lobefins evolved into amphibians, requiring proximity to water for reproduction and hydration.
Some amphibians adapted to drier environments, leading to the evolution of reptiles, which developed:
Waterproof reproductive eggs.
Scaly skins to retain moisture.
Improved lung functionality.
As climate shifted, reptiles became dominant on land, leading to the rise of diverse dinosaur groups.
Dinosaurs thrived for over 150 million years alongside numerous smaller reptiles and amphibians.
Evolutionary adaptations to retain heat:
Feathers in some reptiles led to the emergence of birds.
Hair in others led to early mammals.
The earliest primates appeared 55 million years ago, exhibiting key traits:
Opposable thumbs, flat nails, and enhanced binocular vision.
Hominins (humans and their extinct relatives) emerged approximately 6 million years ago, with a complex evolutionary history.
The genus Australopithecus arose about 4 million years ago, containing several extinct species recorded in the fossil record.
Genus Homo branched from australopithecines ~2.5 million years ago, with noticeable increases in body and brain size.
Further species discoveries are ongoing within the Homo lineage.
Homo erectus, first hominin to leave Africa, ventured into Asia but went extinct for unknown reasons.
Neanderthals inhabited Europe ~300-400 thousand years ago and became extinct ~30 thousand years ago.
Genetic analysis shows a close relation between Neanderthals and modern humans.
Homo sapiens originated in Africa ~150,000 years ago, with genetic and fossil analysis tracing modern human migration around the globe.
The oldest known modern human fossils outside Africa date back 90,000-120,000 years.
Dinosaurs thrived for ~164 million years before extinction; modern humans have existed for only a few million years.
Research indicated that populations outside of Africa exhibit less genetic diversity compared to African populations, supporting the founder effect hypothesis.
Globally, humans share ~99.9% genetic similarity, highlighting our common ancestry despite diverse appearances.
Additional viewing resources on the subject are provided, particularly the PBS NOVA videos.