Animals and plants go extinct for many different reasons, but human activities in the last two centuries have had the greatest impact. Since the industrial revolution, the human population has grown exponentially. As a consequence, habitats have been destroyed, fragmented, or polluted, while ecosystems have been injured by climate change, pollution, and invasive species. Poaching, illegal hunting, and trade in exotic wildlife have contributed to the downward spiral of vulnerable species.
To be sure, other factors contribute to extinction, and many of these are natural events that would happen even if humans did not populate the Earth. Fossil records show that some species followed a path of evolution to a point in which new life forms emerged and transformed habitats. The original species did not adapt to the new conditions and so vanished. Species may also go extinct due to natural disasters, natural climate change cycles, competition, and overspecialization. Any extinction caused by things other than a natural event is called a premature extinction, because it occurs at a faster rate than would naturally take place. Premature extinctions occur mainly because of the following five human-related factors:
- habitat loss, destruction, or fragmentation
- invasive species
- human population growth and expansion
- pollution
- overharvesting (overhunting, overfishing, poaching)
The above factors plus natural events cause three different types of extinction: local, ecological, and biological. A local extinction may occur when a species no longer inhabits a certain area, even though it can be found in other parts of the world. Ecological extinction means that so few members of a species remain, the species can no longer play its normal role in ecosystems. Finally, biological extinction occurs when a species no longer exists on Earth.
Animal extinctions that have taken place in human history have mirrored the migration of humans from Africa and Asia to Europe, and then to the Americas. Some of the species known to have disappeared during humans’ westward migration are the following: the dodo, great auk, passenger pigeon, dusky seaside sparrow, Carolina parakeet, Steller’s sea cow, and aepyornis (elephant bird).
Scientists estimate 99.9 percent of all species that have ever existed are now extinct. Some animals succumbed to mass extinctions, which occur periodically over a course of millions of years. Other extinctions take place more frequently, about every few to several centuries, and are called extinction spasms, such as the disappearance of dinosaurs. Most biodiversity experts agree on extinction rates of between 0.1 percent and 1 percent per year throughout the world. To put these numbers in perspective, at 0.1 percent, Earth loses 14,000 species per year if there are a total of 14 million species; at 1 percent, Earth loses 140,000 species of the 14 million. Furthermore, at a rate of 1 percent lost per year, at least onefifth of the world’s plants and animals could be gone by 2030 and half by 2100. Perhaps most troubling of all, an extinction rate of 0.1 to 1 percent may be a conservative estimate, which means the extinction rate could be significantly faster. Edward O. Wilson has pointed out perhaps the main obstacle to finding a true extinction rate: “The vast majority of species are not monitored at all.” Scientists clearly cannot study things that they do not know exist.
Fossil records help fill in the gaps regarding species that have disappeared. Fossils consist of mineralized sections of things that once lived: bones, teeth, entire skeletons, shells, leaves, or seeds. Sometimes the biological matter has degraded and only an impression in sediment remains, but these impression fossils are valuable because they show what an animal or plant looked like millions of years ago. In addition fossil structures compared with skeletons of present-day animals or plants shed light on how a species may have evolved.
Fossil studies have drawbacks that make them useful only as complements to other technologies. First, some species may have left no fossil records, or, second, their fossils have not yet been discovered. Third, many fossils decompose to a condition that yields little information about the creature that had lived millions of years ago. Despite these disadvantages fossil records have been used to show the following animals became extinct in prehistoric eras: mastodon, mammoth, wooly rhinoceros, saber-tooth cat, and dire wolf.
Three additional technologies supplement the information from fossil examinations. The first technique is radioisotope dating. An isotope is a form of an atom that spontaneously emits an alpha or beta particle or gamma rays. American chemist Willard Libby of the University of Chicago won the 1960 Nobel Prize in chemistry for developing radioisotope
dating, which measures the isotopes emitted by fossils. Libby devised a method based on the radioisotope carbon-14, which the atmosphere makes continuously when neutrons from the Sun bombard nitrogen molecules. In one reaction, a Sun neutron displaces a neutron from nitrogen and emits carbon-14 and a proton (N is nitrogen, C is carbon, and H is
hydrogen):

A small portion of Earth’s carbon is carbon-14, which, when it decays, returns to 7N14 by emitting an electron. Carbon dating makes use of these reactions plus the two following pieces of information: carbon-14 decay has a half-life of 5,730 years, and living organisms contain a constant amount of carbon-14 (about 1 atom of carbon-14 per 1012 atoms of normal carbon-12) in their cells. When an organism dies, it no longer metabolizes carbon, and its carbon-14 content gradually decays. Carbon-14 degrades at a known rate of 693 disintegrations/hour/gram of total carbon, so an estimate of the age of an object becomes

where ln is a natural logarithm, Nf/No is the percent of carbon-14 in the sample compared with that in living cells, and t1/2 is the half-life of carbon- 14. When it is put all together in the following example, a fossil containing
5 percent of its total carbon as carbon-14 can be dated as follows:

A second method used in dating fossils involves deoxyribonucleic acid (DNA) analysis. Analysts compare the DNA recovered from a fossil with the DNA from a similar present-day organism, and they use the assumption that mutations occur in DNA over time at a constant rate. By this method, scientists have estimated the age of Siberian permafrost to be 50,000–100,000 years old.
The third method of dating ancient life is done by core sampling of glacial ice. This technique has helped scientists correlate the depth of the core sample to the number of years ago in which the ice formed. The U.S. Geological Survey’s (USGS) National Ice Core Laboratory has recovered cores from polar sites that date to at least 100,000 years.