What theory explains the extinction of dinosaurs and other plants and animals that ended the?

A small coelurosaur, a feather-tailed dinosaur that lived 99 million years ago, approaches a resin-coated branch on the forest floor in an illustration.

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Why did the dinosaurs go extinct?

Learn about the mass extinction event 66 million years ago and the evidence for what ended the age of the dinosaurs.

ByVictoria Jaggard

Published July 31, 2019

6 min read

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Abundant fossil bones, teeth, trackways, and other hard evidence have revealed that Earth was the domain of the dinosaurs for at least 230 million years. But so far, not a single trace of dinosaur remains has been found in rocks younger than about 66 million years. At that point, as the Cretaceous period yielded to the Paleogene, it seems that all nonavian dinosaurs suddenly ceased to exist.

Along with them went fearsome marine reptiles such as the mosasaurs, ichthyosaurs, and plesiosaurs, as well as all the flying reptiles known as pterosaurs. Ancient forests seem to have flamed out across much of the planet. And while some mammals, birds, small reptiles, fish, and amphibians survived, diversity among the remaining life-forms dropped precipitously. In total, this mass extinction event claimed three quarters of life on Earth.

3:32

Dinosaurs 101

Over a thousand dinosaur species once roamed the Earth. Learn which ones were the largest and the smallest, what dinosaurs ate and how they behaved, as well as surprising facts about their extinction.

Piecing together what happened has been a massive effort for paleontologists, and theories for what killed the dinosaurs and the rest of the planet’s Cretaceous inhabitants have ranged from the plausible to the downright zany. For now, two leading ideas are battling it out within the scientific community: Were dinosaurs victims of interplanetary violence, or more Earthly woes?

Death from above

One of the most well-known theories for the death of the dinosaurs is the Alvarez hypothesis, named after the father-and-son duo Luis and Walter Alvarez. In 1980, these two scientists proposed the notion that a meteor the size of a mountain slammed into Earth 66 million years ago, filling the atmosphere with gas, dust, and debris that drastically altered the climate.

Their key piece of evidence is an oddly high amount of the metal iridium in what’s known as the Cretaceous-Paleogene, or K-Pg, layer—the geologic boundary zone that seems to cap any known rock layers containing dinosaur fossils. Iridium is relatively rare in Earth's crust but is more abundant in stony meteorites, which led the Alvarezs to conclude that the mass extinction was caused by an extraterrestrial object. The theory gained even more steam when scientists were able to link the extinction event to a huge impact crater along the coast of Mexico’s Yucatán Peninsula. At about 93 miles wide, the Chicxulub crater seems to be the right size and age to account for the dino die-off.

In 2016, scientists drilled a rock core inside the underwater part of Chicxulub, pulling up a sample stretching deep beneath the seabed. This rare peek inside the guts of the crater showed that the impact would have been powerful enough to send deadly amounts of vaporized rock and gases into the atmosphere, and that the effects would have persisted for years. And in 2019, paleontologists digging in North Dakota found a treasure trove of fossils extremely close to the K-Pg boundary, essentially capturing the remains of an entire ecosystem that existed shortly before the mass extinction. Tellingly, the fossil-bearing layers contain loads of tiny glass bits called tektites—likely blobs of melted rock kicked up by the impact that solidified in the atmosphere and then rained down over Earth.

Volcanic fury

However, other scientists maintain that the evidence for a massive meteor impact event is inconclusive, and that the more likely culprit may be Earth itself.

Ancient lava flows in India known as the Deccan Traps also seem to match nicely in time with the end of the Cretaceous, with massive outpourings of lava spewing forth between 60 and 65 million years ago. Today, the resulting volcanic rock covers nearly 200,000 square miles in layers that are in places more than 6,000 feet thick. Such a vast eruptive event would have choked the skies with carbon dioxide and other gases that would have dramatically changed Earth’s climate.

Proponents of this theory point to multiple clues that suggest volcanism is a better fit. For one, some studies show that Earth’s temperature was changing even before the proposed impact event. Other research has found evidence for mass die-offs much earlier than 66 million years ago, with some signs that dinosaurs in particular were already in a slow decline in the late Cretaceous. What’s more, volcanic activity is frequent on this planet and is a plausible culprit for other ancient extinctions, while giant meteor strikes are much more rare. This all makes sense, supporters say, if ongoing volcanic eruptions were the root cause of the world-wide K-Pg extinctions.

Why not both?

Increasingly, scientists trying to unravel this prehistoric mystery are seeing room for a combination of these ideas. It’s possible the dinosaurs were the unlucky recipients of a geologic one-two punch, with volcanism weakening ecosystems enough to make them vulnerable to an incoming meteor.

pThis nearly whole, deep-black skull belongs to the most complete specimen of iTyrannosaurus rex/i on display in Europe, an individual nicknamed Tristan Otto. With 170 of its 300-odd bones preserved, this scientifically important but privately owned skeleton is currently at the Museum für Naturkunde in Berlin, Germany. Discovered in 2010 in Montana’s famed Hell Creek Formation of the late Cretaceous, the 40-foot-long fossil took four years to excavate and prepare./p

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pA closeup shows the spine and tail bristles on an incredibly well-preserved fossil of the herbivorous dinosaur iPsittacosaurus mongoliensis/i, on display at the Senckenberg Museum in Frankfurt, Germany. These bristles are likely related to the feathers found on other dinosaurs and may have been used for communication and display. The dark material seen here is the preserved remains of soft tissue, such as skin./p
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iSinosauropteryx prima/i, from China’s northeastern province of Liaoning, was found in 1996 and is recognized as the first known feathered dinosaur. The discovery of downy plumage – seen here as dark fuzz surrounding the fossil – shook the foundations of paleontology; many dinosaur experts were already convinced that birds descended from dinosaurs, but here was the feathery proof turned to stone. More than 50 other species of dinosaur have been found with impressions or other evidence of feathers in the past few decades.br

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The fossil deposits of Liaoning, China, not only preserve dinosaurs, but also early birds, such as these delicate and beautiful specimens of the 120- to 125-million-year-old species iConfuciusornis sanctus/i. This bird – noted for its two long, ribbon-like tail feathers – is one of the most commonly discovered animals in the Yixian and Jiufotang formations of the early Cretaceous, with many hundreds of specimens now in Chinese museums. This means researchers can ask questions about variation within the population, an unusual opportunity in a fossil species.br

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At about 200 million years old, the dainty carnivore iCoelophysis bauri/i was one of the earliest dinosaurs to live in the U.S. Southwest. This late Triassic species, which is the state fossil of New Mexico, reached up to 9.8 feet in length but weighed just 33 to 44 pounds. This specimen has its head twisted back over its spine in what is known as the “death pose” – a common position for fossilized dinosaurs that is possibly caused by the contraction of muscles and ligament after death.

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These eggs belonged to sauropods, giant long-necked dinosaurs that grew to be the largest land animals that ever lived. While sauropod eggs have been found across the world, from Spain and France to Argentina and the United States, these particular specimens still embedded in rock hail from China. Dinosaur eggs are usually found in groups and would have been laid in depressions in the ground. They come in a variety of shapes and sizes, depending on the species, but sauropod eggs are typically round and about the size of a grapefruit.

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A skull of the late Jurassic predatory dinosaur iAllosaurus fragilis/i remains encased in rock in the Quarry Exhibit Hall of the Dinosaur National Monument in Jensen, Utah. The apex carnivore of its time, iAllosaurus/i terrorized the western United States about 150 to 155 million years ago.

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iProtoceratops andrewsi/i, an early relative of the horned dinosaur iTriceratops/i, is seen on display at CosmoCaixa Barcelona as part of an exhibit of dinosaurs from Mongolia’s Gobi desert. Sheep-size iProtoceratops/i was a major prey animal for the turkey-size iVelociraptor mongoliensis/i, and remarkable fossils of the two have sometimes been found locked in combat.

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Exhibition workers put the finishing touches on an anatomically precise, life-size reconstruction of a iSpinosaurus aegypticus/i skeleton created from digital models of the fossil bones. The 50-foot-long model went on display at the National Geographic Museum in Washington, D.C., in September 2014 as the centerpiece of the “Spinosaurus: Lost Giant of the Cretaceous” exhibition.br

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This closeup shows the formidable teeth and jaws of a female iTyrannosaurus rex/i known as ‘Trix,” which is on display at the Natural History Museum of Leiden in the Netherlands. Excavated in 2013 in Montana by museum scientists, the fossil skeleton is more than 80 percent complete, ranking it among the top iT. rex/i specimens in the world.

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pThis picture shows armored plates on the spectacularly complete fossil of an ankylosaur named iBorealopelta markmitchelli/i; the lighter bands represent more flexible tissue between this dinosaur’s tough defensive exterior. Discovered in 2011 at an oil sands mine in the Canadian state of Alberta, the fossil bears a crack from the impact of a tractor shovel. Thankfully, it was rescued from the mining machinery before more damage occurred. After six years and 7,000 hours of preparation, it is now on display at the Royal Tyrell Museum./p
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This unusual skull comes from a relative of iTriceratops/i named iKosmoceratops richardsoni/i. This rhino-size ceratopsian dinosaur lived on the late Cretaceous landmass of Laramidia, which is today the western part of North America. iKosmoceratops/i means “ornamented horned face,” and the species has 15 horns and frills on its skull, which were likely used to attract mates or battle rivals rather than defend against predators.br

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Two sets of footprints at the Moenkopi Dinosaur Tracks in Arizona were likely left by a mother and a young iDilophosaurus wetherilli/i about 193 million years ago – an evocative record of dinosaur behavior from the early Jurassic period. These narrow, three-toed footprints are typical of carnivorous theropod dinosaurs.

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As winds and rain pound surface layers of sediment, they slowly expose any dinosaur fossils encased within, which are made of more hardy material. Here, a two-foot-long section of the tail of a duck-billed hadrosaur emerges from sandstone. Some of the world’s best fossil-hunting locales are badlands, where surface sediments are rapidly eroded by weathering.br

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This cast of iTriceratops horridus/i resides at the Royal Tyrell Museum in Alberta, Canada. iTriceratops/i was the first known horned dinosaur, or ceratopsian, described in 1889. More than 80 other species of ceratopsians have now been described, the vast majority from western North America, and new finds are revealed every year.br

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A close-up shows the tail region of the early Cretaceous Chinese dinosaur, iSinornithosaurus millenii/i. This feathered dromaeosaur relative of iVelociraptor/i had ossified tendons in its tail anchored by its vertebrae or backbones. These narrow bony rods stiffened the tail, improving balance and aiding maneuverability for this fleet-footed, predatory species.

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A set of dinosaur tracks crosses the Valley of the Dinosaurs in Sousa, northeastern Brazil. While fossilized dinosaur bones tell us about the anatomy of these long-extinct animals, so-called ichnofossils such as footprints, teeth marks, nest scrapes, and coprolites (dung) give us important clues to the behavior and lives of ancient species.br

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This skull of the dinosaur iVelociraptor mongoliensis/i comes from the early Cretaceous formations in Mongolia’s Gobi desert. Made famous by the 1993 movie iJurassic Park/i, these dromaeosaurs were much smaller in real life than what’s been depicted in the film and its sequels, reaching just 1.6 feet high and likely weighing little more than about 33 pounds.

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The name of this species, iMei long/i, comes from the Chinese for “soundly sleeping dragon,” reflecting the fact that this remarkable fossil captures a rare and peaceful moment of dinosaur behavior. Seen here from underneath, this troodontid is tucked up in the roosting position familiar from modern birds, with its head nestled under its forearm. The folded-up feet and legs run right-left in this image, with the tail wrapped across the top.br

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pStitched together from a number of images, this panorama shows the massive reconstruction of a titanosaur sauropod installed at the American Museum of Natural History in New York in January 2016. This 122-foot behemoth may be the largest dinosaur that ever lived and was described as a new species dubbed iPatagotitan mayorum/i in 2017, based on a number of fossils excavated from the Chubut region of Patagonia in Argentina./p
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A detail shows the feet and claws of a near-complete specimen of iTyrannosaurus rex/i dubbed Tristan Otto, which is on display at the Museum für Naturkunde in Berlin, Germany. In life these claw bones would have been covered with keratin sheaths, akin to the claws of a cat, but much larger and capable of inflicting far more significant damage.

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This cast of the extravagantly crested duck-billed hadrosaur iParasaurolophus walkeri/i is on display at the Senckenberg Museum in Frankfurt, Germany. The nasal passages and forehead of this species extend to the rear of its head, forming a six-foot-long hollow, bony crest. This is thought to have been used as a resonance chamber, akin to a wind instrument such as a trombone or trumpet, likely allowing the species to produce loud calls that carried over great distances.

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This highly ornamented dinosaur, featured on the December 2007 cover of National Geographic magazine, was originally described as a new species called iDracorex hogwartsia/i, or “dragon king of Hogwarts” after the wizarding school in the iHarry Potter/i booksi. /iHowever, subsequent research from several teams suggests that this unusual skull covered in spikes and knobs belongs to a juvenile form of the dome-headed dinosaur iPachycephalosaurus./i

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<p>This nearly whole, deep-black skull belongs to the most complete specimen of <i>Tyrannosaurus rex</i> on display in Europe, an individual nicknamed Tristan Otto. With 170 of its 300-odd bones preserved, this scientifically important but privately owned skeleton is currently at the Museum für Naturkunde in Berlin, Germany. Discovered in 2010 in Montana’s famed Hell Creek Formation of the late Cretaceous, the 40-foot-long fossil took four years to excavate and prepare.</p>

This nearly whole, deep-black skull belongs to the most complete specimen of Tyrannosaurus rex on display in Europe, an individual nicknamed Tristan Otto. With 170 of its 300-odd bones preserved, this scientifically important but privately owned skeleton is currently at the Museum für Naturkunde in Berlin, Germany. Discovered in 2010 in Montana’s famed Hell Creek Formation of the late Cretaceous, the 40-foot-long fossil took four years to excavate and prepare.

Photography by Gerd Ludwig

But that notion depends a lot on more precise dating of the Deccan Traps and the Chicxulub crater. In 2019, two independent studies looked at geochemical clues from Deccan Traps lava and came to slightly different conclusions, with one paper suggesting the volcanoes played a supporting role in the dinosaurs’ demise by causing pre-impact declines, and the other saying the eruptions came after the impact event and may have played only a small role in ushering along their end.

This debate may rage for years, as scientists dig up new clues and develop new techniques for understanding the past. But whether space invaders or loads of lava are to blame, it’s clear that scientists studying the dinosaurs’ last gasp are revealing vital lessons about the effects of dramatic climate change on Earth’s inhabitants.

What theory explains the extinction of dinosaurs and other plants and animals that ended the Cretaceous period?

The Alvarez hypothesis was initially controversial, but it is now the most widely accepted theory for the mass extinction at the end of the Mesozoic Era.

What is the theory of the extinction of dinosaurs?

For decades, the prevailing theory about the extinction of the dinosaurs was that an asteroid from the belt between Mars and Jupiter slammed into the planet, causing cataclysmic devastation that wiped out most life on the planet.

What are the 3 theories of dinosaur extinction?

Today, paleontologists have discerned that most dinosaur lineages disappeared by about 66 million years ago after intense volcanic activity, climate change and a catastrophic asteroid impact triggered one of the worst mass extinctions in our planet's history.

What are the two main theories of dinosaur extinction?

Over the years, paleontologists have proposed several theories for this extensive die-off. One early theory was that small mammals ate dinosaur eggs, thereby reducing the dinosaur population until it became unsustainable. Another theory was that dinosaurs' bodies became too big to be operated by their small brains.