Life on the Earth was
pushed to the edge of extinction at least five times. The worst happened about 250 million years
ago (mya) when 90 percent of life was wiped out. However, our Deep Ancestors survived the
Great Dying of the Permian Period to repopulate the Earth. We, the Living today, are the result of their
endurance, and ability to change.
Our Deep Ancestors are
more than simply interesting animals.
They may seem far removed from us, but we carry Them inside of ourselves,
as a part of our DNA. We would do well
to listen and gain wisdom from Them especially on how to adapt to the changing
times.
NOTES:
Tracing
Ancestors: The
tracing of human ancestry, from prehistory to the present, is not a linear
process. At present, the fossil records
are incomplete to accomplish this.
Instead, paleontologists will zigzag from known fossils to known fossils,
and guess at the gaps in-between.
Mass Extinction: A
mass extinction event occurs when there is a sharp decrease in the diversity
and abundance of life on earth. This
usually happens when undue stress is placed on living things because of a
changing environment. The “official
zoological definition” is the decrease of two to five taxa such as Classes or
Orders. Generally, this means that at
least ten percent of all families, forty percent of all genera (genus), and
seventy percent of all species die out at one time.
Major Mass Extinction Events: There were five major extinction
events in the earth’s history. The most
severe was the Permian-Triassic Event (258 mya). Known as “The Great Dying”, 57 percent of all
families, 83 percent of all general, and at least 90 percent of all species
died out. In addition, this extinction
event ended the primacy of mammal-like reptiles and ushered in the Age of
Dinosaurs.
The second worst extinction event was the
Ordovician-Silurian Event (443 mya), when 27 percent of all families and 57
percent of all genera died out. The only
mass extinction of insects occurred at this time. After this event came the diversification of
land species and new ecosystems.
The other extinction events were the Late Devonian Event (19
percent families, 50 percent genera, and 70 percent species, 354 mya) when the
trilobites disappeared. The
Triassic-Jurassic Event (23 percent families and 48 percent genera, 206 mya)
saw the end of large amphibians and many mammal-like reptiles. The well-known Cretaceous-Paleogene
(Tertiary) Event (17 percent families, 50 percent genera, and 75 percent
species, 65 mya) wiped out the dinosaurs and gave rise to the Age of Mammals.
WORKS
USED:
Haines, Tim and
Paul Chambers, “The Complete Guide to
Prehistoric Life”, Firefly: Ontario, 2006.
Pianka, Eric and
Laurie Vitt, “Lizards: Windows to the
Evolution of Diversity”, University of California, Berkeley, 2003.
Turner, Alan, “National Geographic Prehistoric Mammals”,
National Geographic Society, Washington D.C., 2004.
Various, “Prehistoric Life”, Dorling Kindersley,
New York, 2009.
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