The 5 Major Mass Extinctions
Animals & Nature
A History of Mass Extinctions
Throughout the 4.6 billion years of history the Earth has been
around, there have been five known major mass extinctions that wiped out
an overwhelming majority of all species living at that time. These five
major mass extinction events include the Ordovician Mass Extinction,
Devonian Mass Extinction, Permian Mass Extinction, Triassic-Jurassic
Mass Extinction, and Cretaceous-Tertiary (or the K-T) Mass Extinction.
All of these major mass extinction events varied in size and causes, but
all of them completely devastated the biodiversity found on Earth at
the times that they happened.
Defining Mass Extinctions
Before diving into these different mass extinction events in depth,
it is important to understand what can be classified as a mass
extinction event and how mass extinction shape the evolution of species
that happen to survive these extreme catastrophes. A “mass extinction”
can be defined as a time period in which a large percentage of all
known species living at the time goes extinct, or is completely wiped
out. There are several causes for mass extinctions such as climate change,
geologic catastrophes (such as large amounts of volcanic eruptions), or
even meteor strikes on the Earth’s surface. There is even evidence to
suggest that microbes may have sped up or contributed to some of the
mass extinctions that are known throughout the Geologic Time Scale.
Mass Extinctions and Evolution
So how do mass extinction events contribute to evolution? Usually,
after a very large mass extinction event, there is a very rapid period
of speciation among the few species that do survive. Since so many
species die off during these catastrophic events, there is so much more
room for the surviving species to spread out and so many niches in the
environments that need to be filled. As populations separate and move
away, they adapt over time to the new environmental conditions and
eventually are reproductively isolated
from the original populations of the species. At that point, they can
be considered a brand new species and biodiversity expands rather
quickly. The rate of evolution is significantly increased because of all
of the roles and spaces that need to be filled by individuals that
managed to survive. There is less competition for food, resources,
shelter, and even mates, allowing the “leftover” species from the mass
extinction event to thrive and reproduce rapidly. More offspring and
more generations tend to favor an increased rate of evolution.
The First Major Mass Extinction - The Ordovician Mass Extinction
When: The Ordovician Period of the Paleozoic Era (about 440 million years ago)
Size of the Extinction: Up to 85% of all living species at the time were eliminated
Suspected Cause or Causes: Continental Drift and subsequent climate change
The mass extinction event that happened during the Ordovician Period
of the Paleozoic Era on the Geologic Time Scale is the first known major
mass extinction. At this time in the history of life on Earth, really,
life was in its early stages. The first known life forms appeared about
3.6 billion years ago. By the Ordovician Period, however, larger aquatic
life forms had come into existence. There were also even some land
species at this time. The cause is thought to be due to the shift in the
continents and the drastic climate change. It happened in two different
waves. The first wave was an ice age that encompassed the entire Earth.
Sea levels were lowered and many land species could not adapt fast
enough to survive the harsh, cold climates. It was not all good news,
however, when the ice age ended. It ended so suddenly that the ocean
levels rose too fast to keep enough oxygen in them to keep the species
that had survived the first wave alive. Again, species were too slow to
adapt before extinction took them out completely. It was then up to the
few aquatic autotrophs that had survived to increase the oxygen levels
so new species could evolve.
05
of 09
The Second Major Mass Extinction - The Devonian Mass Extinction
When: The Devonian Period of the Paleozoic Era (about 375 million years ago)
Size of the Extinction: Nearly 80% of all living species at the time were wiped out
Suspected Cause or Causes: Lack of oxygen in the oceans, quick cooling of air temperatures, possibly volcanic eruptions and/or meteor strikes
The second major mass extinction in the history of life on Earth
happened during the Devonian Period of the Paleozoic Era. This major
mass extinction event actually followed the previous Ordovician Mass
Extinction event relatively quickly. Just as life on Earth began to
rebound and flourish as the climate stabilized and species adapted to
the new environments, almost 80% of all living species, in both the
water and on land, were wiped out.
There are several hypotheses as to why this second mass extinction
occurred at that time in Geologic History. The first wave, which dealt a
major blow to aquatic life, may have actually been caused by the quick
colonization of land. Many aquatic plants adapted to live on land,
leaving fewer autotrophs to create oxygen for all of the sea life. This
led to a mass death in the oceans. The quick moving on to the land of
plants also had a major effect on the carbon dioxide available in the
atmosphere. By removing so much of the greenhouse gas relatively
quickly, the temperatures plummeted. Land species had trouble adapting
to these changes in climate and also went extinct. The second wave is
more of a mystery. It could have included mass volcanic eruptions and
some meteor strikes, but the exact cause of the second wave is still
considered unknown.
The Third Major Mass Extinction - The Permian Mass Extinction
When: The Permian Period of the Paleozoic Era (about 250 million years ago)
Size of the Extinction: An Estimated 96% of all species living on Earth at the time
Suspected Cause or Causes: Unknown - Possibly asteroid strikes, volcanic activity, climate change, and microbes.
The third major mass extinction was during the last period of the
Paleozoic Era called the Permian Period. This is the largest of all
known mass extinctions with a whopping 96% of all species on Earth
completely lost. It is no wonder this major mass extinction has been
dubbed “The Great Dying”. It seems as if nothing was safe from this
massive extinction event. Aquatic and terrestrial life forms alike
perished relatively quickly as the event took place.
It is still pretty much a mystery as to what set off this greatest of
the mass extinction events. Several hypotheses have been thrown around
by scientists who study this time span of the Geologic Time Scale. Some
believe it may be a chain of events that led to so many species
disappearing. It could have been massive volcanic activity paired with
asteroid impacts that sent deadly methane and basalt into the air and
across the surface of the Earth. These could have caused a decrease in
oxygen that suffocated life and brought about a very quick climate
change. Newer research points to a microbe from the Archaea domain that
flourishes when methane is high. These extremophiles may have “taken
over” and choked out the life in the oceans, as well. Whatever the
cause, this biggest of the major mass extinctions ended the Paleozoic
Era and ushered in the Mesozoic Era.
07
of 09
The Fourth Major Mass Extinction - The Triassic-Jurassic Mass Extinction
When: At the end of the Triassic Period of the Mesozoic Era (about 200 million years ago)
Size of the Extinction: More than half of all known species living at the time
Suspected Cause or Causes: Major volcanic activity with basalt flooding, global climate change, and changing pH and sea levels of the oceans.
The fourth major mass extinction event was actually a combination of
many, smaller extinction events that happened over the last 18 million
years of the Triassic Period during the Mesozoic Era. Over this long
time span, about half of all known species on Earth at that time
perished. The causes of these individual small extinctions can be
attributed to volcanic activity with basalt flooding for the most part.
The gases spewed into the atmosphere from the volcanoes also created
climate change issues that changed sea levels and possibly even pH
levels in the oceans.
08
of 09
The Fifth Major Mass Extinction - The K-T Mass Extinction
When: At the end of the Cretaceous Period of the Mesozoic Era (about 65 million years ago)
Size of the Extinction: Nearly 75% of all known species living at the time
Suspected Cause or Causes: Extreme asteroid or meteor impact
The fourth major mass extinction is perhaps the most well-known mass
extinction event. The Cretaceous-Tertiary Mass Extinction (or K-T
Extinction) became the dividing line between the final period of the
Mesozoic Era, the Cretaceous Period, and the Tertiary Period of the
Cenozoic Era. This one, even though it is not the biggest, is the most
well known because it is the mass extinction when the dinosaurs died
off. Not only the dinosaurs went extinct, however, up to 75% of all
known living species died during this major mass extinction event. It is
pretty well documented that the cause of this mass extinction was a
major asteroid impact. The huge space rocks hit the Earth and sent
debris into the air, effectively producing an “impact winter” that
drastically changed the climate all over the Earth. Scientists study the
large craters left by the asteroids and can date them back to this
time.
The Sixth Major Mass Extinction - Happening Now?
Is it possible we are in the midst of the sixth major mass
extinction? Many scientists believe we are. Many known species have been
lost since humans have evolved. Since these mass extinction events can
take millions of years, it is possible we are witnessing the sixth major
mass extinction event. Will humans survive? That is yet to be
determined.
Nenhum comentário:
Postar um comentário
Observação: somente um membro deste blog pode postar um comentário.