Paleozoic Earth ] Back | Next >

Location
 Earth orbit
 260 million years ago

Mean atmospheric O2
 115% of modern level

Mean atmospheric CO2
 3x pre-industrial level

Mean temperature
 2C above modern level

 

Paleozoic Earth - Ring arcs over the Permian Earth, tektites - Space Art/Natural History Illustration Geologic Time Scale 

 Era: Paleozoic
  Period: Permian
   Epoch: Lopingian
    Age: Wuchiapingian

     
 

Ring arcs over the Permian Earth

A dusty ring arc orbits four thousand miles above Earth's equator 260 million years ago. The massive continent below is Pangea and the ocean is Panthalassa. This is how the Earth may have appeared during the end of the Permian period, a time just prior to the appearance of the dinosaurs, when continental drift was pulling Pangea apart into the seven continents we know today.

Earth may have been host to ring arcs composed of debris thrown into  orbit by a collision with a large meteorite or comet. The debris consisted of tiny pebbles that were once molten droplets of ejecta, long since cooled in the vacuum of space. The orbit of the ring arc would eventually decay, returning the debris back to Earth as a shower of meteorites. This debris is found on Earth's surface today in the form of dark, glassy objects known as tektites.

 

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Copyright Walter B. Myers. All rights reserved.

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