1 00:00:02,000 --> 00:00:07,120 Speaker 1: Welcome to brain Stuff from How Stuff Works, Hey, brain Stuff, 2 00:00:07,200 --> 00:00:10,079 Speaker 1: Lauren Vogel bomb Here on the northern coast of the 3 00:00:10,119 --> 00:00:13,159 Speaker 1: Yucatan Peninsula, near the town of Chichi Lob, Mexico, is 4 00:00:13,200 --> 00:00:15,440 Speaker 1: a crater about a hundred and twenty miles in diameter. 5 00:00:15,680 --> 00:00:19,560 Speaker 1: That's about a hundreds The asteroid that created this crater 6 00:00:19,720 --> 00:00:22,400 Speaker 1: was about six miles that's ten kilometers wide and hit 7 00:00:22,440 --> 00:00:25,959 Speaker 1: the Earth sixty five million years ago. In spite of 8 00:00:26,000 --> 00:00:28,800 Speaker 1: these immense measurements, the crater is hard to see, even 9 00:00:28,800 --> 00:00:30,960 Speaker 1: if you're standing right on its rim. To get a 10 00:00:30,960 --> 00:00:35,440 Speaker 1: good map, NASA researchers examined it from space. Ten years 11 00:00:35,479 --> 00:00:39,000 Speaker 1: before the discovery of the Chichi Lob crater, physicist Louise 12 00:00:39,040 --> 00:00:42,680 Speaker 1: Alvarez and geologist Walter Alvarez, a father son team, proposed 13 00:00:42,720 --> 00:00:45,400 Speaker 1: a theory about the impact that we know today created it. 14 00:00:46,040 --> 00:00:49,120 Speaker 1: They noted increased concentrations of the element a ridium in 15 00:00:49,159 --> 00:00:52,760 Speaker 1: sixty five million year old clay. A Ridium is rare 16 00:00:52,800 --> 00:00:55,560 Speaker 1: on Earth, but it's more common in some objects from space, 17 00:00:55,640 --> 00:00:59,200 Speaker 1: like meteors and asteroids. According to the Alvarez theory, a 18 00:00:59,240 --> 00:01:02,000 Speaker 1: massive asteroid it had hit the Earth, blanketing the world 19 00:01:02,000 --> 00:01:05,000 Speaker 1: in a ridium. But a shower of particles wasn't the 20 00:01:05,040 --> 00:01:08,640 Speaker 1: only effect of the collision. The impact caused fires, climate change, 21 00:01:08,640 --> 00:01:12,600 Speaker 1: and widespread extinctions. At the same time, dinosaurs, which until 22 00:01:12,640 --> 00:01:14,880 Speaker 1: then had managed to survive for a hundred and eighty 23 00:01:14,920 --> 00:01:18,880 Speaker 1: million years, died out. Geo Physicist Doug Robertson of the 24 00:01:18,959 --> 00:01:22,559 Speaker 1: University of Colorado at Boulder theorizes the impact heated Earth's 25 00:01:22,560 --> 00:01:26,360 Speaker 1: atmosphere dramatically, causing most big dinosaurs to die within hours. 26 00:01:27,560 --> 00:01:31,280 Speaker 1: This mass extinction definitely happened. Fossil evidence shows that about 27 00:01:31,280 --> 00:01:34,360 Speaker 1: seventy of species living on Earth at that time became extinct. 28 00:01:35,120 --> 00:01:37,640 Speaker 1: The massive die off marks the border between the Cretaceous 29 00:01:37,640 --> 00:01:40,800 Speaker 1: and Tertiary periods of Earth's history, which are also known 30 00:01:40,800 --> 00:01:44,720 Speaker 1: as the Age of Reptiles and the Age of Mammals, respectively. Today, 31 00:01:44,840 --> 00:01:48,320 Speaker 1: scientists call the extinction the KT event, after the German 32 00:01:48,400 --> 00:01:52,560 Speaker 1: spellings of Cretaceous and Tertiary. The KT event had an 33 00:01:52,720 --> 00:01:55,640 Speaker 1: enormous effect on life on Earth. But what would have 34 00:01:55,640 --> 00:01:58,520 Speaker 1: happened if the asteroid had missed. Would it have led 35 00:01:58,560 --> 00:02:01,120 Speaker 1: to a world where people and dine sours would coexist 36 00:02:01,600 --> 00:02:05,800 Speaker 1: or one in which neither could live? In a world 37 00:02:05,880 --> 00:02:08,760 Speaker 1: where an asteroid whizzed past Earth instead of crashing down 38 00:02:08,800 --> 00:02:11,280 Speaker 1: with the force of a hundred million tons of TNT, 39 00:02:11,880 --> 00:02:15,760 Speaker 1: life could have progressed much differently sixty five million years ago. 40 00:02:15,880 --> 00:02:17,840 Speaker 1: Some of the animals and plants that are common today 41 00:02:17,880 --> 00:02:21,280 Speaker 1: we're just getting started. These include placental mammals, which are 42 00:02:21,400 --> 00:02:25,000 Speaker 1: mammals that develop inside a placenta in the womb, and angiosperms, 43 00:02:25,040 --> 00:02:28,520 Speaker 1: which are flowering plants. Insects that rely on flowers, such 44 00:02:28,560 --> 00:02:32,280 Speaker 1: as bees, were also relatively new. Many of these life 45 00:02:32,280 --> 00:02:35,480 Speaker 1: forms thrived after the KT event, and without that mass 46 00:02:35,480 --> 00:02:37,919 Speaker 1: reptilian extinction to clear the way, they may not have 47 00:02:37,960 --> 00:02:42,200 Speaker 1: found ecological niches to fill. In this scenario, today's world 48 00:02:42,280 --> 00:02:45,360 Speaker 1: might be full of reptiles and short on mammals, including people. 49 00:02:46,639 --> 00:02:49,400 Speaker 1: But even if the asteroid hadn't hit, dinosaurs and other 50 00:02:49,440 --> 00:02:53,200 Speaker 1: Cretaceous life forms might have become extinct anyway. Some dinosaur 51 00:02:53,200 --> 00:02:56,280 Speaker 1: species had started to dwindle long before the asteroids impact. 52 00:02:56,840 --> 00:02:59,240 Speaker 1: This has led many researchers to conclude that the asteroid 53 00:02:59,280 --> 00:03:02,920 Speaker 1: was just one spect of a complex story. Other global 54 00:03:02,960 --> 00:03:06,240 Speaker 1: catastrophes like massive volcanic eruptions in what is now India 55 00:03:06,520 --> 00:03:10,120 Speaker 1: most likely played a role. Also, the Earth's changing landscape 56 00:03:10,160 --> 00:03:14,160 Speaker 1: as the supercontinent Pangaea broke up into today's continence probably 57 00:03:14,240 --> 00:03:17,919 Speaker 1: had something to do with it too. Then, there's another 58 00:03:18,040 --> 00:03:21,400 Speaker 1: argument that the Chicktullub asteroid hit the Earth too early 59 00:03:21,440 --> 00:03:25,480 Speaker 1: to have caused the extinction. Researchers GERTA. Keller and Marcus 60 00:03:25,520 --> 00:03:28,919 Speaker 1: Harding both conclude that the impact took place three thousand 61 00:03:29,000 --> 00:03:32,880 Speaker 1: years before the end of the Cretaceous period. Keller theorizes 62 00:03:33,000 --> 00:03:36,280 Speaker 1: the Chicktullub impact was one of at least three massive collisions. 63 00:03:36,840 --> 00:03:39,200 Speaker 1: Harding argues that the iridium layer didn't come from the 64 00:03:39,280 --> 00:03:42,160 Speaker 1: Chichillub asteroid, but from another event, such as a series 65 00:03:42,160 --> 00:03:46,360 Speaker 1: of meteors burning up in the atmosphere. He bases this 66 00:03:46,440 --> 00:03:50,320 Speaker 1: theory on spheroid particles ejected during the impact. Most of 67 00:03:50,360 --> 00:03:52,080 Speaker 1: these are in an older layer of the Earth than 68 00:03:52,120 --> 00:03:55,640 Speaker 1: the Katie irridium layer. According to both of these points 69 00:03:55,640 --> 00:03:58,160 Speaker 1: of view, the absence of the chick Tallub asteroid strike 70 00:03:58,320 --> 00:04:00,880 Speaker 1: may not have had a big effect on the Hayti extinction. 71 00:04:02,080 --> 00:04:04,040 Speaker 1: Earth was a warm planet for most of the time 72 00:04:04,080 --> 00:04:07,080 Speaker 1: that dinosaurs lived. After the end of the Cretaceous period, 73 00:04:07,200 --> 00:04:10,120 Speaker 1: the world got a lot colder and experienced several ice ages. 74 00:04:10,480 --> 00:04:13,040 Speaker 1: Whether dinosaurs could have survived such a change in climate 75 00:04:13,120 --> 00:04:17,200 Speaker 1: is debatable. It's hard to come to a definitive conclusion 76 00:04:17,279 --> 00:04:19,120 Speaker 1: about what the world would look like today without the 77 00:04:19,160 --> 00:04:22,240 Speaker 1: Chick to Love impact, but the question of whether people 78 00:04:22,240 --> 00:04:25,440 Speaker 1: and dinosaurs could have coexisted is a captivating one. The 79 00:04:25,520 --> 00:04:28,080 Speaker 1: idea is present in everything from the congo legend of 80 00:04:28,160 --> 00:04:31,440 Speaker 1: mokol Ambenbe to King Kong to the pervading kitch of 81 00:04:31,480 --> 00:04:35,360 Speaker 1: the Flintstones. Then, of course, there's the prevailing scientific theory 82 00:04:35,400 --> 00:04:38,080 Speaker 1: about the origin of birds that they are, in essence, 83 00:04:38,200 --> 00:04:46,680 Speaker 1: dinosaurs that we are coexisting with today. Today's episode was 84 00:04:46,720 --> 00:04:49,120 Speaker 1: written by Tracy V. Wilson and produced by Tyler Klang. 85 00:04:49,520 --> 00:04:51,400 Speaker 1: Brain Stuff is a production of I Heart Radio as 86 00:04:51,400 --> 00:04:53,720 Speaker 1: How Stuff Works. To hear more from Tracy, check out 87 00:04:53,720 --> 00:04:55,880 Speaker 1: the podcast Stuff You Missed in History Class, and for 88 00:04:55,920 --> 00:04:58,120 Speaker 1: more on this and lots of other historic topics, visit 89 00:04:58,160 --> 00:05:00,880 Speaker 1: our home planet how Stuff Works dot com. And for 90 00:05:00,960 --> 00:05:03,320 Speaker 1: more podcasts from my heart Radio, visit the I heart 91 00:05:03,400 --> 00:05:06,080 Speaker 1: Radio app, Apple Podcasts, or wherever you listen to your 92 00:05:06,080 --> 00:05:06,760 Speaker 1: favorite shows.