Geologic Time Table Flashcards
Involves vast amounts of times - millions or billions of years
Magnitude of geologic time
Describes the processes in the geologic time
Gradual
The basis of the division of the time scale
Life-forms
Geologic time divisions called
Geochronological units
Most life-forms found as
Fossils
Divisions in the geologic time scale
Eons, eras, periods, epochs
Longest subdivision; based on the abundance of certain fossils
Eons
The four geologic eons
Phanerozoic, Proterozoic, Archaean, Hadean
The four geologic eons collectively called
Precambrian
Percentage that the Precambrian encompasses in the geologic time
about 88%
Next to the longest subdivision; marked by major changes in the fossil record
Eras
Three geologic eras
Paleozoic, Mesozoic, Cenozoic
The basic unit of geologic time
Period
Large interval units of time that encompasses smaller intervals of time
Periods
Paleozoic meaning
Old Life
Mesozoic meaning
Middle Life
Cenozoic meaning
New Life
Began with the breakup of one supercontinent and the formation of another; plants became widespread; vertebrate animals colonized the land; abundant ocean-dwelling organisms that required oxygen to live
Paleozoic era
Six divisions of the Paleozoic era
Permian, Carboniferous, Devonian, Silurian, Ordovician, and Cambrian
Major extinction; reptiles diversify
Permian period
First reptiles, trees, seed ferns
Carboniferous period
First amphibians; fish diversify
Devonian
First vascular plants
Silurian
Major diversification of animal life
Ordovician
First fish, first chordates (animal with backbone)
Cambrian
Pangaea stars to separate into
Laurasia and Gondwana
Began approximately 250 million years ago after a major mass extinction
Mesozoic era
3 subdivisions of the Mesozoic era
Triassic, Jurassic, Cretaceous
Major event of the Mesozoic era
Breakup of Pangaea
When Mesozoic era ended with a major mass extinction
66 million years ago
Life forms that dominated the Triassic
Gymnosperms and ferns
Seed-bearing plant that bears its seeds on the surface of cones
Gymnosperm
Conifers and cycad forests dominate such as
Mosses and liverworts, gingkoes, palm-like cycads
Reptiles in the Triassic
Icthyosaurs (4.5-9 m); Plesiosaurs (15 m); Pliosaurs (4-15 m)
Dinosaurs dominate such as
Allosaurs, Diplodocus, Brachiosaurus, Stegasaurus
Tiny animal of the mid-Jurassic; ancestor of placental mammals
Juramia
Indicates that mammals evolved much earlier than previously thought
Juramia
The breakup of Pangaea into separate continents was underway.
Cretaceous period
The Cretaceous period dated back
135 million years ago
Complete separation of Laurasia and Gondwana
Cretaceous period
In the first half of the Cretaceous,
warm temperatures, low seasonality, and high global sea levels
At the end of the Cretaceous,
severe climate changes, lowered sea levels, and high volcanic activity
Dinosaurs that dominated in the Cretaceous
T.rex (carnivore), Triceratops (horned); Trachadon (duck-billed)
Plants in the Triassic
Gingko, cycad, and conifer
66 million years ago, a 10-km wide meteorite struct the Earth near what is now Mexico.
Meteorite impact theory
The impact caused
Shock waves, tidal waves, a tremendous amount of dust into the atmosphere
As the dust re-entered the Earth’s atmosphere, it would have instantly heated the atmosphere which caused
forest fires
Age of the mammals
Cenozoic era
Cenozoic era dated when
65,000,000 years ago until the present
Two periods of the Cenozoic era
Tertiary, quaternary
The other term used to refer to the Cenozoic era
“Era of recent life”
The time that the world took on its modern form
Cenozoic era
Reptiles in the Cenozoic era
Rattlesnake, chameleon, desert tortoise, turtle, American alligator
The epoch determined by its warm climate
Eocene epoch
The oldest known fossils of the modern order of mammals appeared during this time period.
Eocene epoch
Types of plants that became dominant in the Eocene epoch
Gymnosperms and angiosperms
Major boundaries between geological divisions corresponded to
Extinction events in the fossil record
O2 began accumulating in the atmosphere and rusting iron-rich terrestrial rocks.
2.7 billion years ago
From 2.7 to 2.3 billion years ago, caused the extinction of many prokaryotic groups
:“Oxygen revolution”
Groups adapted using
Cellular respiration