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Flashcards covering major geological periods, life origins, biological milestones, and the five major mass extinctions as detailed in the Earth History overview lecture.
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Archaean
The geological eon spanning from 4.0−2.5 billion years ago (BYA) involving the origin of life and the appearance of the first microfossils.
Microstromatolites
The first microfossils dating from 3.5 billion years ago (BYA) which consist of photosynthetic bacteria.
Proterozoic
The eon from 2.5 billion years ago (BYA) to 539 million years ago (MYA) characterized by an oxidative atmosphere, glaciation periods, eukaryotes, and multicellularity.
Palaeoproterozoic
The era from 2.5−1.6 billion years ago (BYA) that included the Great oxygenation event and the origin of eukaryotes around 2 billion years ago (BYA).
Great oxygenation event
A massive increase in oxygen levels (105 fold) occurring roughly 2.5−1.6 billion years ago (BYA), likely caused by photosynthesis from cyanobacteria.
Huronian glaciation
A mass extinction event triggered by the Great oxygenation event during the Palaeoproterozoic era.
Primary endosymbiosis
The process occurring around 2 billion years ago (BYA) that led to the origin of eukaryotes.
Mesoproterozoic
The era from 1.6−1 billion years ago (BYA) involving sexual reproduction, diversification of unicellular organisms, and secondary endosymbiosis.
Secondary endosymbiosis
An event in the Mesoproterozoic era that gave rise to the first glaucophytes, red algae, and green algae.
Neoproterozoic
The era from 1000−539 million years ago (MYA) featuring major glaciation, the formation of the ozone layer, and the split of major animal lineages.
Snowball Earth
A condition during the Cryogenian period (720 million years ago) where Earth was probably almost fully covered by ice.
Ediacaran
A period around 635 million years ago (MYA) providing clear fossil evidence of multicellular life forms.
Ozone layer
A protective layer formed in the Neoproterozoic that blocks UV radiation, enabling the colonisation of land.
Phanerozoic
The current eon from 539 million years ago (MYA) to the present, divided into the Palaeozoic, Mesozoic, and Cenozoic eras.
Cambrian
The period from 539−487 million years ago (MYA) where all modern animal phyla were represented and trilobites were abundant.
Burgess Shale
The source of many Cambrian fossils that show all major animal groups were already present during that period.
Ordovician
The period from 487−443 million years ago (MYA) characterized by many invertebrates and armoured fishes.
Gnathostomes
The first jawed fishes, which appeared during the Silurian period between 443−419 million years ago (MYA).
Devonian
The period from 419−359 million years ago (MYA) involving the first terrestrial vertebrates (amphibians), teleosts (bony fishes), sharks, and insects.
Carboniferous
The period from 359−299 million years ago (MYA) featuring the first reptiles with cleidoic eggs, winged insects, and a peak in oxygen levels.
Permian
The period from 299−252 million years ago (MYA) involving the diversification of insects (the first beetles) and the separation of reptile lineages.
Triassic
The period from 252−201 million years ago (MYA) characterized by the first dinosaurs, turtles, and flies.
Jurassic
The period from 201−143 million years ago (MYA) where dinosaurs were the dominant terrestrial megafauna and the first mammals and birds appeared.
Cretaceous
The period from 143−66 million years ago (MYA) characterized by the evolution of angiosperms and the first bees and ants.
Cenozoic
The era from 66 million years ago (MYA) to now, known as the 'Age of mammals,' including the radiation of angiosperms and grasses.
Ordovician-Silurian Mass Extinction
An extinction occurring 445−440 million years ago (MYA) caused by a massive ice age and sea level drop of 70−100m.
Late Devonian Mass Extinction
An extinction occurring 375−359 million years ago (MYA) caused by temperature drop and oxygen depletion in oceans.
Permian-Triassic Mass Extinction
A major extinction 252 million years ago (MYA) resulting in the loss of >90% of species due to fast temperature rise.
Triassic-Jurassic Mass Extinction
An extinction 201 million years ago (MYA) caused by volcanic eruptions and falling sea levels.
Cretaceous-Palaeogene Mass Extinction
An extinction occurring 66 million years ago (MYA) caused by an asteroid impact, resulting in the loss of non-avian dinosaurs and ammonites.