1. Introduction: Three extinct species
Meet Brachiosaurus. This enormous ancient herbivore lived in North America about 156 – 145 million years ago. It was between 18 and 21 meters long. It’s estimated to have weighed between 28 and 58 metric tons (128,000 pounds).
To the left is a fossil of a trilobite. These animals were arthropods: relatives of insects, spiders, and crabs. They lived from 521 million years ago until about 252 million years ago.
Trilobites make up a clade with over 20,000 recognized species. They ranged in size from a few millimeters (think of a ladybug) to about the size of a crab. However, one species was 72 centimeters long. Most crawled, but some swam. Some were scavengers. Others were predators. Trilobites were so numerous (and they were so easily fossilized) that you can buy a 500 million year old trilobite fossil for less than $20.
Here’s a reconstruction of Archaeopteryx. This transitional species had features of both dinosaurs (jaws with sharp teeth, a three fingers with claws, a long bony tail) and birds (feathers and flight). Archaeopteryx lived in Europe about 150 million years ago.
These are three extinct species. The total number of such species could be 5 billion.
2. Extinction is the flip side of speciation
There are as many as 8.7 million species alive on Earth today. But that number is a tiny fraction of all of the species that have lived during life’s 3.8 billion year history. It’s estimated that as many as 5 billion species have inhabited the Earth at one point in time or another. 99.9% of these species are extinct.
Extinction happens when a species can no longer exploit its ecological niche. That might be because of an environmental change that alters the niche, or because of a competitor that’s better adapted to exploit that niche. In some cases, a newly arrived predator or parasite might cause a species to decline.
True extinction— the death of the last member of a species — is final and forever. However, there are a few intermediate conditions along the road to extinction.
- A species can become locally extinct. In that case, it’s gone from a particular area, but continues to live elsewhere. For example, the African Rhinoceros used to exist over most of Sub Saharan africa. Now, it’s limited to a few small refuges. While efforts are underway to reintroduce it to areas that were once part of its range, the species continues to be in overall decline. Similarly, the Grizzly bear — the state emblem of California — has been extinct in California since 1924 (though it continues to exist elsewhere).
- A species can become extinct in the wild when there are only a few individuals remaining, and all of the rest are in captivity (in zoos, wildlife parks, etc.). Sometimes, these species can be successfully reintroduced into the wild. You can see a list of such species on Wikipedia.
- A functionally extinct species has become so reduced that, while a few individuals might continue to exist, they no longer constitute a viable population. Their ultimate demise is only a matter of time.
3. The Extinction Vortex
Species in decline can enter into what’s called an extinction vortex. A whirlpool above a drain is an example of a vortex. In the same way that a whirlpool pulls water down a drain, an extinction vortex pulls species toward extinction. The vortex works like this:
- Ecological disturbances make it difficult for a species to successfully exploit its niche. As a result, there’s a decrease in the population size.
- This lowered size decreases genetic variability.
- Decreased variability makes the population less resilient and less fertile.
- Additional disturbances lead to further population decline.
Because the system is a positive feedback loop, species that enter the vortex often quickly decline toward extinction.
4. The background level of extinction
Looking at Earth’s history, it’s possible to calculate a background extinction rate. This is how often extinctions normally occur. This background rate of extinction is in contrast with the rate of extinction during periods of widespread environmental change. These periods are called mass extinctions (and we’ll address them below).
A widely quoted benchmark for the background extinction is 1 extinction per million species per year. Thus, if there are 8.7 million species on Earth, then we’d expect 8 species to become extinct each year. However, a 2014 study funded by the Society for Conservation Biology, estimated that this benchmark might be too high: in fact the background level of extinction might be as low as 0.1 extinctions/million species/year.
Another way to talk about background extinction rate is to talk about species lifespans, or species survival rates. In the same way that we can talk about the average lifespan of a dog or a human being, it’s possible by looking at fossil data to determine how long a species can be expected to survive before becoming extinct. This varies for different taxa.
Here are a few species survival rates (source: wikipedia)
- All invertebrates: 11 million years
- Mammals: 1 million years
- Echinoderms (sea stars, sea urchins, sand dollars, etc): 6 million years.
5. Mass extinction
Extinction is a normal part of the history of life on Earth. If the rate of speciation and the rate of extinction are equal, then overall species diversity remains constant. However, there have been periods in Earth’s history when geological and even astronomical forces cause environments throughout much of the planet to significantly change. This alters many species’ niches to the point where they can no longer survive. Because the change occurs on a widespread (and even a planetary scale), no migration to a place of refuge is possible. This leads to a mass die-off called a mass extinction.
The Y axis on this graph is extinction intensity. Extinction intensity, in this graph, is the percentage of genera (plural of “genus”) that were present at one period of time, but don’t exist afterward (because they became extinct). For example, find number 3 on the graph. The value is above 50%. What this indicates is that over 50% of the genera that were present at this time became extinct. Note that each genus can contain many species. This mass extinction, known as the Permian extinction, wiped out up to 95% of marine species and 70% of terrestrial species.
Two additional things to note about this graph:
- The values on this graph are based on marine species, because these organisms are the ones with the best fossil record.
- There were two mass extinctions that occurred about 500 million years ago. These are marked with an asterisk because this was very close to “Cambrian explosion” of animal diversity, and the fossil record at that point is poorly developed. Hence, these two mass extinctions aren’t usually counted among the other five.
What causes these mass extinctions? Let’s just look at two.
- Number 3 is called the Permian extinction. As the greatest of all mass extinctions, it’s sometimes referred to as the Great Dying. There’s no complete consensus on its cause. In fact, there might have been several factors that coincided to alter both marine and terrestrial environments in such a way that wiped out a huge swath of Earth’s species (including the trilobites described above). These factors include
- Massive releases of carbon dioxide: In what’s currently Siberia (eastern Russia), a series of enormous volcanic eruptions released significant quantities of carbon dioxide into the air. These eruptions might have ignited sediments rich in coal and petroleum: that released additional carbon dioxide into the air. This carbon dioxide acted as a greenhouse gas, trapping heat and causing the planet’s temperature to become significantly warmer, altering environments and disrupting food chains around the globe.
- Poisoning of the oceans: Increased ocean temperatures reduced the amount of dissolved oxygen in the oceans. This reduction in oxygen, along with higher temperatures, would have stressed marine organisms. On top of that, the reduction of oxygen could have led to a bloom of sulfate-reducing bacteria. These bacteria release hydrogen sulfide (H2S), a poisonous gas. The release of this gas would have killed off both marine and terrestrial species.
- Number 5 is the Cretaceous-Tertiary extinction (confusingly abbreviated as the K-T extinction). The cause of this extinction, which wiped out the dinosaurs, is clear. About 65.5 million years ago, an asteroid about 10 kilometers in diameter (the size of Mount Everest) struck Earth in what’s now the Gulf of Mexico. This impact caused a variety of climate-related effects that disrupted terrestrial and marine food chains. In one account of the disaster (recounted in a fabulous episode of Radiolab called “Dinopocalypse”), debris from the impact flew into space and then rained down upon the Earth. The subsequent meteor shower superheated the Earth’s atmosphere, cooking the dinosaurs alive. Within a few hours, a clade that had dominated the Earth for hundreds of millions of years was wiped out. The only terrestrial species that would have survived would have been those with nests or burrows underground.
The 1998 movie Deep Impact is built around the premise of a similar impact occurring in modern times. The impact scene in the movie depicts how an oceanic asteroid strike would generate a tsunami that would devastate any nearby landmass. Two favors, please, before you watch a two minute clip of the movie. 1) I suspect that this clip might get taken down for copyright violation. If so, would you let me know? 2) If you’re in class, ask your teacher if it’s okay to watch. Here’s the link (it’ll open in a new tab).
6. What happens after mass extinctions?
You wouldn’t want to be around during a mass extinction. However, you are around because of a mass extinction. Here’s why.
The graph to the left shows species diversity before, during and after a mass extinction event. Number “1” shows the number of taxa before the event. At “2,” you can see diversity plummet, reaching the bottom at “3.”
After “3,” the environment begins to recover. As a result, the survivors begin to diversify into the newly empty ecological niches. The result is an amplification of species diversity (shown by the rising line at “4”), ending in a new equilibrium between speciation and the background level of distinction (at “5”).
The graph to the right tells a similar story. “1” shows phylogenetic diversification leading up to a mass extinction, which occurs at “2.”
You can see how the mass extinction extinguishes most lineages. But some survive, such as the lineage shown at “4.” During the subsequent eons, the survivors get to experience their own adaptive radiation, which occurs during time period “3.”
Let’s apply this to the Cretaceous extinction, the one caused by the asteroid impact 65 million years ago. Among the lineages that came to an end were all the dinosaurs, as well as their marine cousins, like mosasaurs and plesiosaurs. But the mammals (which in this case would be the lineage at “4”) survived. With a few million years, all of the modern mammal clades (for example, the whales, dogs, bears, rodents, horses, bats, and primates) came into being.
Had the dinosaurs not been wiped out, our primate clade would have never emerged. That means that apes wouldn’t have emerged, and hominids wouldn’t have emerged either. That doesn’t mean that sapient, conscious beings wouldn’t have emerged on this planet: it just means that they wouldn’t have been beings like you or me. We both owe our existence to that asteroid that wiped out the dinosaurs. Every other mammal should be similarly appreciative.
The takeaway? Mass extinctions are terrifying. But they also set the stage for new diversification of life.
7. Conclusion, and Checking Understanding
It’s widely agreed that a sixth mass extinction is in progress, and that we humans are to blame. We’ll cover that in a later module about human impact on biodiversity. But for now, consolidate your understanding by taking the quiz below.
[qwiz qrecord_id=”sciencemusicvideosMeister1961-Extinction” style=”width: 600px !important;”]
[h] Understanding Extinction
[q] Extinction happens when a species can no longer exploit its ecological [hangman]. This might be because of a change in the [hangman], or the arrival of a better adapted [hangman].
[q] The rhinoceros isn’t entirely extinct: just [hangman] extinct in much of its former range.
[q] The positive feedback loop in which ecological disturbance lowers a population’s size to the point where it has less genetic variability, becomes less adaptable, which further lowers the population’s size is known as an extinction [hangman].
[q] The rate at which extinctions normally occur is called the [hangman] level of extinction.
[q multiple_choice=”true”] It’s estimated that _________ of the species that have ever existed are now extinct.
[q multiple_choice=”true”] The average lifespan of a species is closest to
[q] Periods of significant, global environmental change can lead to [hangman] extinctions
[q multiple_choice=”true”] Which of the following statements about point “3” is correct.
[q] In the graph below, which number indicates the mass extinction that wiped out the dinosaurs?
[q] In the graph below, which number indicates the mass extinction that’s known at the “Great Dying.”
[q] In the graph below, which number indicates a mass extinction?”
[q] In the graph below, which number indicates adaptive radiation following a mass extinction?”
[q] The graph below indicates how following a [hangman] [hangman] (at “2”), survivors (such as the one shown at “4”) can undergo [hangman] [hangman] as their descendants diversify into the ecological space vacated by the organisms that became extinct.
[q] In the graph below, which number indicates a lineage that wasn’t wiped out by a preceding mass extinction.
[q] In the graph below, which number indicates the mass extinction.
[q] In the graph below, which number indicates an adaptive radiation that follows a mass extinction.