If you think of parrots as birds that live in lush, tropical jungles, you may be surprised to learn that the United States used to have its own native parrot. The Carolina parakeet lived in the American southeast until the early 20th century. These brightly colored, noisy birds were a nuisance. They ate fruits, vegetables and grains, and they traveled in large, noisy, crop-destroying flocks. This made them a favorite target of hunters, who wanted to protect the food supply and sell the birds' vivid feathers. If you want to see a Carolina parakeet today, you have to look for it in illustrations or stuffed museum displays -- it has died out completely due to hunting and habitat loss and was declared extinct in 1939.
Hundreds of years passed between the influx of European settlers on the coasts of North America and the extinction of the Carolina parakeet. But not all modern extinctions have been so slow in coming. Arctic explorers first made note of Stellar's sea cow, which looked like an extra large, wrinkly manatee, in 1741. By 1768, less than 30 years later, excessive hunting led to the sea cow's extinction.
These are just two of the life forms that have died out since mankind started keeping records. But today's research suggests that these extinctions may be part of a bigger trend -- a human-caused mass extinction that could rival prehistoric events that destroyed most life on Earth. The most famous of these was the mass extinction that killed the dinosaurs, although other events were far more devastating.
Whether they're big or small, extinctions change the world. And while extinctions themselves are all about change, the study of extinction is all about uncertainty. Anything that lives can become extinct, but how do scientists know when it happens? How is it possible to figure out how quickly species are disappearing when no one really knows how many species live on Earth in the first place? This article will delve into what happens when species disappear, from dinosaurs to dodos, and explore the question of how new life can arise from widespread extinction.
It's easy to think of extinction as a big, dramatic event, the product of an asteroid collision or the invasion of new, aggressive species. But extinctions happen even without the aid of natural disasters or widespread slaughter. Researchers estimate that between 1 and 4 billion species have lived on Earth during its history. All but about 50 million of those are gone today. Less than a third of those billions of extinct life forms died out during mass extinctions [source: Newman].
The rest died as part of an ongoing process. They were part of the background rate of extinction, or the average number of extinctions that happen over millions of years. According to scientists' estimates, the background rate of extinction is somewhere between one and five species per year [source: Ward].
You'll notice that these are all averages and approximations. That isn't just because they involve large numbers and long time spans. These numbers are approximate because of several unavoidable difficulties that are part of studying extinction:
- Only a fraction of the species that have lived on Earth appear in the fossil record, or all the discovered and analyzed fossils on the planet. This means that you can't painstakingly count all the known fossils and expect to get a good idea of the number of species that have lived.
- Fossilization happens only in very specific conditions. It's highly unlikely that the very last member of a species will become a fossil when it dies. For this reason, species usually disappear from the fossil record before they disappear from the planet -- sometimes millions of years before.
- The fossil record isn't a linear timeline of what has happened on Earth. Instead, it's a collection of rock layers that hold fossils from different periods of the Earth's history.
- No one knows exactly how many species are alive on Earth today, and it can be hard to tell exactly when -- or whether -- a species dies out.
Because of all this, a lot of the study of extinction can seem like it has more to do with math than with real, living beings. Researchers use the number of known fossils to estimate the number of species that have ever existed. They use estimates called confidence intervals to analyze how likely it is that a particular species became extinct at a particular time. And they use equations and algorithms to try to make up for the holes in the available data and to make accurate predictions of how, when and why species have become extinct.
Researchers can also apply mathematical analysis to the plants, animals and microscopic organisms that are alive today. For example, with math, researchers can estimate how many of a particular plant or animal are alive on the planet. Math also helps researchers figure out a species' minimum viable population, or the point at which it's sure to become extinct, even though there are a few left. All of this mathematical work can help scientists figure out whether a single species is endangered and how to help protect it.
But extinction isn't all about math. In the next two sections, we'll look at the practical aspects of extinction on large and small scales. You'll find out about the world's most devastating mass extinction. You'll also learn why a butterfly, regardless of whether it can create a storm with the flapping of its wings, can cause the extinction of numerous other species if it disappears.
The Extinction of a Species
Every once in a while, a species that hasn't gone extinct will disappear from the fossil record. Sometimes, this is because a life form has evolved into a new species -- this is known as pseudoextinction. Life forms can also disappear from the fossil record and reappear later. These Lazarus species may have experienced a dip in population, or they may not have died in conditions that lead to fossilization.
But most of the time, when a species disappears from the fossil record -- or from the face of the planet today -- it's because it's on its way to extinction. Typically, these small-scale extinctions happen because of some kind of change in the environment where a life form lives. While some species can adapt to the changes, others die, and if enough die, the species becomes extinct. These are some of the biggest factors in the extinctions of particular species:
- Habitat loss
- Competition with new species
- Human hunting
- Contaminants in the environment, such as pesticides
The loss of one species can also lead to the loss of many others. For example, flowering plants rely on pollinators, like bees and butterflies, to reproduce. If the pollinators disappear, the flowering plants can die, too. The same is true with changes in the food chain. If an animal relies on a specific plant for food and that plant becomes extinct, the animal will soon follow unless it's able to change its diet. A good example is the extinctions that happened at the end of the last ice age, about 11,000 years ago. Small mammals began to go extinct, probably because of climate change and changes in geography. This caused the extinction of bigger animals, like saber-tooth cats, which lost their food source.
Typically, little changes like this happen all over the world all the time, leading to the extinction of a few interrelated species. But sometimes the stress on an ecosystem is so large that not many life forms survive. Next, we'll look at some of the world's biggest extinctions.
Volcanoes, Asteroids, Acid and Mass Extinctions
It's easy to think of mass extinctions as events that suddenly, instantly destroy most life on Earth. In reality, most mass extinctions take place over millions of years. Lots of plants, animals and microscopic organisms gradually die as a result of a massive stress on the ecosystem. This eventually leads to the extinction of many life forms.
When studying these extinctions, researchers look at life forms in groups using scientific classifications. These classifications organize life forms according to traits they have in common. From biggest to smallest, these groups are domain, kingdom, phylum, class, order, family, genus and species. Researchers usually examine how mass extinctions affected families and genera to determine the extent of the extinction.
Researchers disagree about exactly how many mass extinctions have struck the planet. However, most agree that there have been five primary mass extinctions:
- The Ordovician extinction took place about 490 million years ago. Glacier formation caused sea levels to drop, which led to the extinction of about half of all animal families.
- The cause of the late Devonian extinction is still under debate. Because of it, about a quarter of marine families and more than half of marine genera became extinct. The late Devonian extinction took place about 360 million years ago.
- The Permian-Triassic extinction was the biggest mass extinction of all. Nearly 85 percent of marine genera and 70 percent of all land species became extinct. This extinction happened 250 million years ago, and there are numerous theories about its cause.
- Volcanoes were the likely culprit in the end-Triassic extinction, which killed about 20 percent of marine families and half of marine genera 200 million years ago.
- The most famous mass extinction is the Cretaceous-Tertiary event, also known as the K-T event. This is the extinction that led to the end of the dinosaurs 65 million years ago. The current hypothesis is that an asteroid impact off the coast of what is now Mexico either caused or contributed heavily to the K-T event.
In each of these mass extinctions, some type of event placed extreme stress on the world's ecosystems. Large groups of animals died, making room for new life. After each mass extinction, new species arose. Survivors of the extinction also thrived, taking advantage of the newly available room and resources. It's because of these extinctions that life on Earth looks like it does today.
However, the Earth might not look this way for long. Next, we'll look at how extinctions are affecting the world today and whether humans are the cause of a sixth major mass extinction.
Based on analysis of the fossil record, researchers estimate that most species on Earth have an overall life span of about 10 million years. It's an ongoing cycle of plants, animals and microscopic organisms appearing in the fossil record, remaining for about 10 million years and disappearing. Most likely, this is the natural state of life on Earth, regardless of exactly what species are alive.
However, live forms are dying out much faster today than they appear to at any point in the fossil record. As we discussed earlier, the background rate of extinction is somewhere between one and five species per year. But today, the extinction rate appears to be anywhere from 100 to 1,000 times greater than that [source: Holsinger]. Exact numbers are hard to pin down. No one knows exactly how many species are alive on Earth today. On top of that, it can be difficult to impossible to determine whether a plant or animal has died out. Even after exhaustive searches, researchers have declared some animals extinct only to find new specimens later.
The major cause of these extinctions isn't global warming or acid rain -- it's habitat loss. As the human population grows and more of the planet becomes industrialized, natural habitats for plants and animals disappear. As species that lived in these habitats die, the level of biodiversity decreases. The loss of plant and animal species can lead to everything from food shortages to poor soil quality. The loss of microscopic organisms can also play a role. For example, one theory about the Permian-Triassic extinction is that helpful marine bacteria became extinct, and the bacteria that flourished as a result produced hydrogen sulphide and caused acid rain.
Human behavior is also causing other ecosystem stresses, such as pollution, which could threaten species with extinction. Global changes,such as global warming, play a role in extinction as well. In theory, addressing these issues might slow the rate of extinction, but it's unclear how long it might take animal and plant populations to return to normal.
Regardless of whether a mass extinction is looming, researchers agree that the loss of biodiversity has a negative impact on ecosystems. To learn more about whether to expect a mass extinction in the near future, read Will we soon be extinct? If you'd like to know more about biodiversity, conservation and related topics, see the links on the next page.
Related HowStuffWorks Articles
More Great Links
- Brashares, Justin S. "Ecological, Behavioral and Life-history Correlates of Mammal Extinctions in West Africa." Conservation Biology. Vol. 17, no. 3, June 2003.
- Bryant, Peter J. "Biodiversity and Conservation." University of California, Irvine. (2/27/2007) http://darwin.bio.uci.edu/~sustain/bio65/Titlpage.htm#Table%20of%20contents
- Dunn, Robert R. "Modern Insect Extinctions, the Neglected Majority." Conservation Biology. Vol. 19, no. 4. August 2005.
- Eklof, Anna and Bo Ebenman. "Species Loss and Secondary Extinctions in Simple and Complex Model Communities." Journal of Animal Ecology. Vol. 75. 2006.
- Holloway, Marguerite. "When Extinct Isn't." Scientific American. 8/8/2005. (2/27/2007) http://www.sciam.com/article.cfm?id=when-extinct-isnt
- Holsinger, Kent. "Patterns of Biological Extinction." University of Connecticut. 9/4/2007. (2/27/2007) http://darwin.eeb.uconn.edu/eeb310/lecture-notes/extinctions/extinctions.html
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- State Museum of Illinois. "Late Pleistocene Extinctions." (2/27/2007) http://www.museum.state.il.us/exhibits/larson/lp_extinction.html
- UCMP Berkley. "The Ordovician." (2/27/2007) http://www.ucmp.berkeley.edu/ordovician/ordovician.html
- Ward, Peter Douglas. "The Call of Distant Mammoths." Springer. 10/9/1998. (2/27/2007)
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