What is life? What does life require? How did life begin?
Transition from protobionts to single-celled eukaryotes
The evolution of multicellularity
Diversification of multicellular eukaryotes
Life is a dynamic system that:
Composed of elements that self-organize
Responds to the environment
Capable of replication
Energy: Fuels metabolism for survival, growth, and reproduction
Materials (Elements): Used for constructing biomass
Information: Facilitates organization, response to stimuli, and replication
Homeostasis: Maintenance of a stable internal environment
Organization: Structured arrangement of components
Metabolism: Chemical processes to maintain life
Adaptation: Evolutionary adjustments to environment
Response to stimuli: Reacting to external changes
Reproduction: Ability to produce offspring
Energy, materials, and information are essential for each feature
Formation of Earth: About 4.5 billion years ago
Created from a cloud of matter following the formation of the sun
First life: Approximately 3.5 billion years ago
Spontaneous Generation (Abiogenesis): Idea that life arises from inanimate matter
Aristotle: Observations, e.g., mice from hay
Francesco Redi (1668): Experiment disproving spontaneous generation with meat and flies
Primordial Soup Theory:
Mid-19th Century: Darwin suggested a "warm little pond" with essential chemicals fostering life
Mid-20th Century: J.B.S Haldane proposed oceans as a "hot dilute soup"
Abiotic synthesis of small organic molecules (amino acids, nucleotides)
Joining small molecules into macromolecules (proteins, nucleic acids)
Packaging of molecules within membranes (protobionts)
Self-replication (origin of RNA)
Simulated early Earth atmosphere to create organic compounds
Materials used: Water (H2O), methane (CH4), ammonia (NH3), hydrogen (H2)
Exposed to sparks to replicate lightning
Found 22 amino acids
Protobionts: clusters of molecules, precursors to prokaryotes
Form spontaneously; resemble phospholipid bilayers
Maintain different internal and external environments
Capable of simple replication and metabolism
Protobiont: not a true cell
Prokaryote: Fully functional cellular structure without a nucleus
Lived in an oxygen-poor environment (3.5 billion years ago)
Relied on photosynthesis for energy
Major oxygen (O2) production from photosynthetic bacteria
O2 accumulation began around 2.7 billion years ago
Oxygen-rich atmosphere led to both challenges and opportunities for life
Eukaryote fossils date back 2.2 billion years
Characterized by membrane-bound organelles and a nucleus
Arise from infolding of cellular membranes
Endosymbiosis Theory (1967): Chloroplasts and mitochondria evolved from small prokaryotes living inside larger host cells
Similar inner membrane structure/function between organelles and prokaryotes
Organelles' cell division resembles prokaryotic fission
Chloroplasts and mitochondria can transcribe and translate their own DNA
Ribosomes of organelles resemble prokaryotic ribosomes
Eukaryotic cell evolution led to a greater diversity of unicellular forms
Multicellularity evolved to produce algae, plants, fungi, and animals
Multicellular eukaryotes emerged around 1.2 billion years ago; early forms were colonial
Fungi, plants, and animals started land colonization around 500 million years ago
Arthropods and tetrapods became widespread land animals
Tetrapods evolved from lobe-finned fishes approximately 365 million years ago
1.2 billion years ago: First multicellular eukaryotes
2.1 billion years ago: First eukaryotes (single-celled)
3.5 billion years ago: First prokaryotes (single-celled)
535–525 million years ago: Cambrian explosion (diversification of animal forms)
500 million years ago: Land colonization by fungi, plants, and animals