The geologic time scale divides the 4.6 billion years of Earth
history into several units. Each time unit represents a particular
stage in the development of the climate, life forms and landscapes
of the planet. By studying sequences of superimposed rock strata
in different parts of the globe, scientists have been able to divide
geologic time into a certain number of periods of very long duration.
Every layer of rock corresponds to a specific time in the history
of the formation of the Earth.
[D] Click for larger version, 99 KB Superposed layers of rock, Victoria Island, Northwest Territories
Geological
time is divided into a complex hierarchy of time periods. This note
gives some of the most basic and best known. The longest units of
time, referred to as eons, are called the Archean, Proterozoic and
Phanerozoic.
The first two eons comprise the Precambrian, the most ancient period
of time, which accounts for over five-sixths of all geologic ages.
The Precambrian, began with the formation of the Earth (at least
four billion years ago) and ended approximately 570 000 000 years
ago. It corresponds to the time before the appearance of complex
life forms. As a result, fossils are rare in Precambrian rocks.
As well, these rocks are highly deformed and difficult to trace
from one region to another. Consequently, Precambrian time has not
been subdivided to the same degree of precision as more recent times.
In Canada, Precambrian has two major subdivisions: the lower Precambrian
or Archean, and the upper Precambrian or Proterozoic.
Rocks that formed during more recent periods and eras are better
preserved than those dating from the Precambrian and it is therefore
possible to differentiate their ages more readily. A result, increasingly
recent time units are more numerous and more precise and hence represent
increasingly shorter periods of time.
The Precambrian is followed by the Phanerozoic, which is divided
into three eras: the Paleozoic, Mesozoic and Cenozoic eras. Each
of these eras is divided into periods, the periods into epochs and
the epochs into ages.
- The Paleozoic began 570 000 000 years ago. It consists of six
periods which, from oldest to most recent are: Cambrian, Ordovician,
Silurian, Devonian, Carboniferous and Permian.
- The Mesozoic began 225 000 000 years ago and is divided into
three periods which, from oldest to most recent are: Triassic,
Jurassic and Cretaceous.
- Finally, the Cenozoic, or most recent era, covers the past 65
000 000 years. It is divided into several relatively short periods.
The older, and much longer, is the Tertiary. The Tertiary is subdivided
into five periods: Paleocene, Eocene, Oligocene, Miocene and Pliocene.
The Quaternary, which follows the Tertiary, is made up of the
Pleistocene, which was a time of cooling temperatures in the Northern
Hemisphere, and the Holocene, which dates from the end of the
most recent glaciation, approximately 10 000 years ago, to the
present day.
Scientists have been able to establish the fact that the Pleistocene
began approximately 1 500 000 years ago. During that time, alternating
periods of cold and warm temperatures generated four successive
glacial epochs, during which ice sheets covered vast areas of North
America, Europe and Asia. Each of these glaciations is believed
to have lasted 100 000 years. Various studies have shown that climate
during the interglacials was sometimes warmer than it is today.
How are geologic time divisions determined?
Throughout the world, sediments are continually being deposited and, over time, they become rock. Layers of rock build up on top of each other as they form, with the oldest on the bottom. Each layer contains the remains of animals or plants that lived during the time the sediments were deposited. Once buried, these animals and plants were preserved and became fossils after the sediments were lithified. The appearance and disappearance of certain life forms provide clues that can be used to reconstruct the past. In addition, certain fossils are indicative of a specific time.
[D] Click for larger version, 45 KB Cambrian trilobite from Newfoundland
[D] Click for larger version, 29 KB Cretaceous ammonite fossil
The various types of fossils deposited during a given time period
have similar counterparts in other areas of the continent. As a
result, it is possible to correlate between locations and compensate
for problems encountered in areas where specific rock strata are
missing or have been shifted out of sequence as a result of sudden,
strong folding events.
In addition to the findings of paleontological studies (i.e. of
fossils), isotopic dating methods are used to determine the time
divisions. The duration of the various periods can be calculated
on the basis of the proportions of potassium and argon isotopes.
An isotope is an element (like potassium, carbon, argon, etc.) that
has lost one or more neutrons. These dating methods are based on
the principle that by losing neutrons, elements undergo isotopic
decay slowly, at a known rate. Therefore, the greater the quantity
of a given element that has undergone such decay, the more time
has elapsed, and the older the rock containing the element must
be.
[D] Click for larger version, 28 KB Fossilized pollens are indicators of the past environment. Microscopic samples of ancient pollens.
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