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Geological Time Scale
A system used to organize Earth's history into Eons, Eras, Periods, and Epochs based on significant events
Eons
The longest divisions of geological time spanning hundreds of millions of years
Phanerozoic Eon
The most recent eon that began about 500 million years ago
Eras
Subdivisions within eons
Three eras of the Phanerozoic Eon
Paleozoic, Mesozoic, and Cenozoic
Periods
Subdivisions within eras that vary in length
Paleozoic periods
Permian, Carboniferous, Devonian, Silurian, Ordovician, and Cambrian
Earth formed
About 4.6 billion years ago
Earth's crust solidified
About 4 billion years ago
First life appeared in oceans
About 3.5 billion years ago
Oldest micro-organism fossils found
Western Australia
Prokaryotes dominated Earth
From 3.5 billion to 2 billion years ago
Two groups that diverged from prokaryotes
Bacteria and Archaea
Oxygen started accumulating in atmosphere
About 2.5 billion years ago due to cyanobacteria
Oceans contained significant oxygen
About 2 billion years ago
Oldest eukaryotic fossils
About 1.5 billion years ago
First cells with nuclei
Appeared about 1.5 billion years ago
Oldest animal fossils
About 600 million years ago
First multicellular organisms
About 700 million years ago
Cambrian Explosion
Rapid diversification of animal life about 540 million years ago
Colonization of land by plants, fungi, and animals
About 450 million years ago
First land plants with xylem vessels
Appeared about 450 million years ago
Largest mass extinction
About 250 million years ago killing 99% of life
Age of Dinosaurs began
About 250 million years ago
Supercontinent began breaking apart
About 180 million years ago
Dinosaurs became extinct
About 65 million years ago
Percentage of life lost in dinosaur extinction
About 70%
Mammals evolved
About 200 million years ago
First proto-humans
Appeared in Africa about 4 million years ago
First ancestors of Homo sapiens
About 200 000 years ago
Recorded human history began
About 5 000 years ago
Cambrian Explosion definition
A short period where most major animal groups suddenly appeared in the fossil record
Duration of Cambrian Explosion
Lasted about 20 million years
Platyhelminthes
Flatworms
Nematoda
Worms
Annelida
Segmented worms
Mollusca
Slugs, snails, and shelled organisms
Arthropoda
Invertebrates with exoskeletons and jointed limbs
Echinodermata
Marine invertebrates
Chordata
Vertebrates with skeletons
Fish evolved
About 500 million years ago
Amphibians evolved
About 370 million years ago
Reptiles evolved
About 340 million years ago
Birds evolved
About 150 million years ago
Mammals evolved from primitive forms
About 200 million years ago
Humans evolved
About 200 000 years ago
Mass extinction
A period where many species die out in a relatively short time
First mass extinction
Ordovician extinction caused by climate change
Ordovician extinction effect
Extinction of many trilobites
Second mass extinction
Devonian extinction caused by ice ages and global cooling
Third mass extinction
Permian extinction caused mainly by volcanic eruptions
Most severe mass extinction
Permian extinction
Fourth mass extinction
Triassic extinction caused by acid rain and low ocean oxygen
Fifth mass extinction
Cretaceous extinction caused by asteroid impact
Current possible sixth mass extinction
Caused by human activities
Human causes of sixth extinction
Illegal veld fires, habitat destruction, and hunting
Environmental disaster theory
Mass extinctions caused by meteors, volcanism, radiation, or diseases
Failure to adapt theory
Organisms become extinct because they cannot adapt to environmental changes
Fossil
Preserved remains or traces of organisms from long ago
Paleontologist
Scientist who studies fossils
Paleoanthropologist
Scientist who studies human ancestors through fossils
Petrification
Process where organic remains are replaced by minerals and become stone-like
Sedimentary rock
Rock formed from layers of sediment in aquatic environments
Transitional fossil
Fossil showing features of ancestral and descendant groups
Step 1 of fossil formation
Organism buried by sediment
Step 2 of fossil formation
More sediment accumulates and minerals replace organic matter
Step 3 of fossil formation
Tectonic movement lifts sediments closer to surface
Step 4 of fossil formation
Erosion exposes fossils
Relative dating
Estimating fossil age by comparing with other fossils or events
Radiometric dating
Determining exact age using radioactive isotopes
Examples of fossils
Bones, shells, footprints, coprolites, petrified wood, leaf imprints
Coprolites
Hardened fossilized faeces
Examples of fossils preserved in unusual conditions
Woolly mammoths in ice and sabre-toothed cats in tar
Organic molecules
Molecules mainly made of carbon, hydrogen, and oxygen
Inorganic compounds
Compounds that usually do not contain carbon
Micronutrient
Element needed in small amounts
Macronutrient
Element needed in large amounts
Main organic compounds in cells
Carbohydrates, lipids, proteins, nucleic acids, enzymes, and vitamins
Main inorganic compounds in cells
Water and mineral salts
Percentage of water in cells
70-95%
Water as universal solvent
Dissolves many substances for transport and reactions
Water function in plants
Maintains turgidity
Water function in organisms
Removes waste products
Macro-nutrients
Essential minerals needed in large amounts
Micro-nutrients
Essential minerals needed in small amounts
Sodium function in animals
Water-salt balance and nerve and muscle function
Sodium deficiency symptom
Muscular cramps
Potassium function in plants
Forms proteins and enzymes
Potassium function in animals
Water-salt balance and heart, muscle, and nerve function
Potassium deficiency in plants
Slow growth
Potassium deficiency in animals
Muscle weakness and irregular heartbeat
Calcium function in plants
Root development and cell wall formation
Calcium function in animals
Bone and teeth formation and muscle function
Calcium deficiency in plants
Chlorosis
Calcium deficiency in animals
Rickets and weak bones and teeth
Phosphorus function in plants
Root development
Phosphorus function in animals
Bone and teeth formation
Phosphorus deficiency in plants
Brown leaves
Phosphorus deficiency in animals
Bone and teeth weakness, nerve and muscle malfunctioning
Magnesium function in plants
Formation of chlorophyll