Geologic Timescale
Precambrian
Precambrian is the oldest and longest part of Earth's history, lasting from 4.6 billion to 541 million years ago.
Precambrian period lasted from about 4.6 billion years ago to the beginning of the Cambrian Period, 541 million years ago, setting the stage for the explosion of life.
The first multicelled animals appeared in the fossil record almost 600 million years ago. Known as the Ediacarans, these bizarre creatures bore little resemblance to modern life forms. They grew on the seabed and lacked any obvious heads, mouths, or digestive organs
Cambrian
Cambrian period saw the emergence of the first predators like Anomalocaris and the first eyes in trilobites.
Permian
Permian period was the last and longest of the Paleozoic Era, lasting 47 million years and ending in a cataclysmic extinction event.
Paleozoic
Paleozoic Era was a time of amazing changes and diversity in life on Earth, from the first animals to the first reptiles and plants.
Ordovician
Ordovician period had mostly barren land with some algae, fungi, and primitive plants, and the only continent was Gondwana.
Triassic
Triassic period is the first period of the Mesozoic Era, starting 252 million years ago and ending 201 million years ago.
Four Eras
Precambran
Paleozoic
Mesozoic
Cenozoic
Paleozoic Era
Paleozoic Era began 541 million years ago with the Cambrian explosion and ended about 252 million years ago with the end-Permian extinction, a significant event in Earth's history.
Cambrian Explosion
Cambrian Explosion occurred about 545 million years ago, leading to a sudden diversity in life forms and the creation of major animal groups.
Mesozoic Era
Mesozoic Era, the age of dinosaurs, lasted almost 180 million years from approximately 250 to 65 million years ago, including the Triassic, Jurassic, and Cretaceous periods.
Triassic Period
Triassic period began 252 million years ago and ended 201 million years ago, marked by the supercontinent of Pangea and the rise of marine reptiles.
Jurassic Period
Jurassic period succeeded the Triassic period, with major landmasses forming Pangea and the rise of marine reptiles and corals.
plate tectonic activity picked up, and a period of continental rifting began. On the margins of the continents, shallow seas, which had dwindled in area at the end of the Permian, became more extensive
sea levels gradually rose, the waters of continental shelves were colonized for the first time by large marine reptiles and reef building corals of modern aspect.
Cretaceous Period
Cretaceous period was the last and longest segment of the Mesozoic Era, lasting approximately 79 million years and marked by the development of flowering plants.
The oldest angiosperm fossil that has been found to date is Archaefructus liaoningensis found by Ge Sun and David Dilcher in China
Cenozoic era
Cenozoic Era, known as the Age of Mammals, is the most recent era, but the diversity of life during this time is wider
Geologic Time scale
Late Proterozoic
First skeletal elements
first soft-bodies metazoans
First animal traces
Cambrian
First fishes
First Chordates
Ordovician
Sudden diversification of metazoan families
Silurian
First vascular land plants
Devonian
First amphibians
Jawed fishes diversify
Pennsylvanian
First reptiles
Mississippian
Scale trees
seed ferns
Permian
Major extinctions
Reptile diversify
Triassic
First mammals
First dinosaurs
Jurassic
First birds
Dinosaurs diversify
Cretaceous
Extinction of dinosaurs
first primatees
first flowering plants
Paleogene/Neogene
Mammals diversify
Quaternary
Evolution of humans
Iba pa
Cyanobacteria
First Bacteria
Anomalocaris
First Predator
Alfred Wegener
Continental Drift
Pangea became gondwana and laurasia
Ediacaran