The Triassic-Jurassic extinction event occurred during the warming of ~7.4 °C at a rate >10 °C/Myr 17, while the Frasnian-Famennian and the Cretaceous-Paleogene mass extinctions were associated ...The coincidence of a mass extinction at the Cretaceous/Paleogene (K–Pg) boundary and the iridium (sourced from the asteroid) layer of the Chicxulub impact were demonstrated using marine ...Deep-sea limestones exposed in Italy, Denmark, and New Zealand show iridium increases of about 30, 160, and 20 times, respectively, above the background level at precisely the time of the Cretaceous-Tertiary extinctions, 65 million years ago. Reasons are given to indicate that this iridium is of extraterrestrial origin, but did not come from a ...In their Review “The Chicxulub Asteroid impact and mass extinction at the Cretaceous-Paleogene boundary” (5 March, p. 1214), P. Schulte et al. analyzed the 30-year-old controversy over the cause of the end-Cretaceous mass extinction and concluded that the original theory of 1980 was right: A large asteroid impact on Yucatan …Asteroid impacts: one large impact is associated with a mass extinction, that is, the Cretaceous–Paleogene extinction event; there have been many smaller impacts but they are not associated with significant …In their Review “The Chicxulub Asteroid impact and mass extinction at the Cretaceous-Paleogene boundary” (5 March, p. 1214), P. Schulte et al. analyzed the 30-year-old controversy over the cause of the end-Cretaceous mass extinction and concluded that the original theory of 1980 was right: A large asteroid impact on Yucatan …One of the “Big Five” mass extinctions in the Phanerozoic Eon occurred at the Cretaceous–Paleogene (K–Pg) boundary (66.0 million years ago). The K–Pg mass …The Cretaceous-Tertiary extinction The most famous of all mass extinctions marks the end of the Cretaceous Period, about 65 million years ago. As everyone knows, this was the great extinction in which the dinosaurs died out, except for the birds, of course.Ordovician-Silurian extinction (439 Ma) victims: 60 % percent of marine genera. - global cooling, then rapid warming - rapid sea level fall followed by rapid sea level rise Different mass extinctions, different causes ? Mass Extinctions: Summary of “The Big Five” (numbered according to severity) “Today, we may be losing up to 30,000 ...The main contender for the Cretaceous mass extinction event is a huge asteroid striking Earth about 66 million years ago. Eleven other impact structures are known from the Cretaceous, but none rival the terminal event of the Cretaceous. The asteroid that hit Earth north of the Yucatan Peninsula in what is now the Gulf of Mexico was 6-12 miles ...Mar 15, 2023 · The three mass extinction events are highlighted in red with stars: P/Tr = end-Permian event, Tr/J = end-Triassic event, K/Pg = end-Cretaceous event. We further highlight the end-Cenomanian event (OAE2) and the Palaeocene–Eocene thermal maximum (PETM). The black arrows indicate the composition of the PCA components, with each arrow indicating ... Timeline of Cretaceous–Paleogene extinction event research. Since the 19th century, a significant amount of research has been conducted on the Cretaceous–Paleogene extinction event, the mass extinction that ended the dinosaur -dominated Mesozoic Era and set the stage for the Age of Mammals, or Cenozoic Era.A new compilation of fossil data on invertebrate and vertebrate families indicates that four mass extinctions in the marine realm are statistically distinct from background extinction levels. These four occurred late in the Ordovician, Permian, Triassic, and Cretaceous periods. A fifth extinction event in the Devonian stands out from the ...Nov 30, 2022 · But in fact, they were killed off at the end of the Cretaceous period – the fifth of the ‘Big Five’. End Cretaceous (65 mya) – the event that killed off the dinosaurs. Finally, at the end of the timeline we have the question of what is to come. Perhaps we are headed for a sixth mass extinction. But we are currently far from that point. Mass-extinction events have a relatively long history of investigation regarding their effects on biodiversity. As a result, a distinct nomenclature has arisen describing the various phases and taxa present across extinction intervals (Fig. 2). A mass extinction can be divided into four main intervals: pre-extinction, extinction, recovery, and ...Cretaceous-Paleogene extinction. Perhaps the most famous of the major mass extinctions is the Cretaceous-Paleogene, or K–Pg, extinction, which occurred some 66 million years ago. It marked the end of about 67 percent of all species living immediately beforehand, including the non-avian dinosaurs. As a result, mammals and birds (avian ... Cretaceous-Paleogene extinction. Perhaps the most famous of the major mass extinctions is the Cretaceous-Paleogene, or K–Pg, extinction, which occurred some 66 million years ago. It marked the end of about 67 percent of all species living immediately beforehand, including the non-avian dinosaurs. As a result, mammals and birds (avian ...Jan 15, 2021 · Mass extinction is an event in which a considerable portion of the world’s biodiversity is lost. An extinction event can have many causes. There have been at least 5 major extinction events since the Cambrian explosion, each taking a large portion of the biodiversity with it. Mass extinction theories have developed from the simple death-by-sea-level-change hypothesis first proposed almost fifty years ago (Newell, 1967) into ever more complex, multicausal scenarios. The body of evidence associated with mass extinctions lends much support to proximal kill mechanisms that include anoxia ... End Cretaceous: …Sep 12, 2022 · Each mass extinction ended a geologic period — that’s why researchers refer to them by names such as End-Cretaceous. But it’s not all bad news: Mass extinctions topple ecological hierarchies, and in that vacuum, surviving species often thrive, exploding in diversity and territory. 1. End-Ordovician: The 1-2 Punch. These latest Cretaceous Hg peaks may correlate with massive, distal, Deccan-sourced lava flows (> 1000 km long) that traversed the Indian subcontinent and flowed into the Bay of Bengal, bracketing the mass extinction. Results support Deccan volcanism as the primary driver of the end-Cretaceous mass extinction. Your personalized FREE Share Link:The mother of all mass extinctions, the Permian-Triassic Extinction Event was a true global catastrophe, wiping out an unbelievable 95 percent of ocean-dwelling animals and 70 percent of terrestrial animals. So extreme was the devastation that it took life 10 million years to recover, to judge by the early Triassic fossil record.The end-Cretaceous mass extinction at the Cretaceous-Paleogene boundary (KPB; 66.016 Ma) is perhaps the most easily explained environmental catastrophe due to a bolide impact on Yucatan and Deccan Traps volcanism in India. However, the relative importance of these events in driving extinctions is controversial. For the past 40 …26.10.2016 г. ... 66 million years ago, the Cretaceous mass extinction wiped out three quarters of the world's plant and animal species, including all ...The Cretaceous-Paleogene event was the last mass extinction event, yet its impact and long-term effects on species-level marine vertebrate diversity remain la rgely uncharacterized. We quantified elasmobranch (sharks, skates, and rays) speciation, extinction, and ecological change resulting from the end-CretaceousIn the early Cretaceous, many of the southern continents were still joined together as part of the southern landmass called Gondwana. Northern continents formed the great landmass Laurasia. These two supercontinents shared many plants and animals dating from an earlier time when they were joinedEnd-Cretaceous Extinction. Home / Understanding Extinction / Mass Extinctions / End-Cretaceous Extinction. The end-Cretaceous extinction is best known of the “ Big Five ” because it was the end of all dinosaurs except birds (the non-avian dinosaurs ). It also created opportunities for mammals. During the Mesozoic Era dinosaurs dominated all ...At the beginning Cretaceous of Period (145 million to 66 million years ago) sharks were once again widely common and varied in the ancient seas, before experiencing their fifth mass extinction event. While much of life became extinct during the End-Cretaceous extinction event, including all non-avian dinosaurs, sharks once again persisted.The last and probably most well-known of the mass-extinction events happened during the Cretaceous period, when an estimated 76% of all species went extinct, including the non-avian dinosaurs.15.04.2022 г. ... ... Cretaceous periods. Because the fifth extinction occurred at the boundary between the Cretaceous (K) and subsequent Palaeogene (Pg) period ...The Cretaceous period was the last and longest segment of the Mesozoic era. It lasted approximately 79 million years, from the minor extinction event that closed the Jurassic period about 145 ...Dinosaur - Extinction Causes, Evidence, & Theory: The mass extinction of dinosaurs 66 million years ago remains a misconception; the fossil record shows that dinosaurs were already in decline during the late …25.06.2003 г. ... The extinction separates the Cretaceous Period of the dinosaurs from the mammal-dominated Paleocene Period; yet, fossils and sediments nearest ...Mass extinction of birds at the Cretaceous–Paleogene (K–Pg) boundary Nicholas R. Longricha,1, Tim Tokarykb, and Daniel J. Fielda aDepartment of Geology and Geophysics, Yale University, New Haven, CT 06520-8109; and bRoyal Saskatchewan Museum Fossil Research Station, Eastend, SK, Canada S0N 0T0 Edited by David Jablonski, University …We find that (1) improved geochronology in the last decade has shown that nearly all well-dated LIPs erupted in < 1 Ma, irrespective of tectonic setting; (2) for well-dated LIPs with correspondingly well-dated mass extinctions, the LIPs began several hundred ka prior to a relatively short duration extinction event; and (3) for LIPs with a ...Yet the mass extinction, known as the Cretaceous-Palaeogene or “K–Pg” event, was just as important for what it created as for what it destroyed.Cretaceous Period - Climate, Extinction, Dinosaurs: In general, the climate of the Cretaceous Period was much warmer than at present, perhaps the warmest on a worldwide basis than at any other time during the Phanerozoic Eon. The climate was also more equable in that the temperature difference between the poles and the Equator was about …Cretaceous–Paleogene Extinction. 65 million years ago; Brontosaurs looking upon the meteors raining down that preceded the larger asteroid strike that would lead to the extinction of the dinosaurs 65 million years ago. Image credit Aunt Spray via Shutterstock. Of the five mass extinction events, the Cretaceous-Paleogene is probably the most ...The Cretaceous-Tertiary Mass Extinction ... Mass Extinctions: Summary of “The Big Five” (numbered according to severity) “Today, we may be losing up to 30,000 species a year -- a rate much faster than at any time since the last great extinction 65 million years ago that wiped out most of the dinosaurs. If we continue on this course, we will destroy …Sep 22, 2023 · •The disappearance of non-avian dinosaurs was just one part of a larger event: the Cretaceous-Paleogene (K/Pg) mass extinction (formerly called the Cretaceous-Tertiary or K/T extinction). •Diverse groups of land and sea organisms died out at this time, 66.05 million years ago. The extinction that occurred 65 million years ago wiped out some 50 percent of plants and animals. The event is so striking that it signals a major turning point in Earth's history, marking the end of the geologic period known as the Cretaceous and the beginning of the Tertiary period. Explore the great change our planet has experienced: five ... The Alvarezes along with Asaro and Michel published their seminal 1980 paper in Science: “Extraterrestrial Cause for the Cretaceous-Tertiary Extinction.” This paper was immediately resisted by scientific critics who argued that volcanic eruptions were behind the demise of the dinosaurs and cited as evidence the thousands of miles of volcanic rock in an area of India known as the Deccan Traps.Timeline of Cretaceous–Paleogene extinction event research. Since the 19th century, a significant amount of research has been conducted on the Cretaceous–Paleogene extinction event, the mass extinction that ended the dinosaur -dominated Mesozoic Era and set the stage for the Age of Mammals, or Cenozoic Era.The coincidence of a mass extinction at the Cretaceous/Paleogene (K–Pg) boundary and the iridium (sourced from the asteroid) layer of the Chicxulub impact were demonstrated using marine ...Scientists have estimated the eruptions—possibly set off by a meteorite—wiped out as much as three-quarters of the planet’s animals and plants. For decades, scientists have debated what caused the globe’s fifth mass extinction, which marked...K–T extinction, abbreviation of Cretaceous–Tertiary extinction, also called K–Pg extinction or Cretaceous–Paleogene extinction, a global mass extinction event responsible for eliminating approximately 80 percent of all species of animals at or very close to the boundary between the Cretaceous and Paleogene periods, about 66 million ...They suggested that this layer was evidence of an impact event that triggered worldwide climate disruption and caused the Cretaceous–Paleogene extinction event, a mass extinction in which …protists called foraminifera (or forams).Their observations mirror those made by researchers documenting a mass extinction event at the end of the Cretaceous period about 66 million years ago. KEY CONCEPTS AND LEARNING OBJECTIVES • There is a relationship between the geological time scale and the layered patterns of exposed rocks in theMass extinction event, any circumstance that results in the loss of a significant portion of Earth’s living species across a wide geographic area within a relatively short period of geologic time. Mass extinction events are extremely rare. They cause drastic changes to Earth’s biosphere, and in.Each mass extinction ended a geologic period — that’s why researchers refer to them by names such as End-Cretaceous. But it’s not all bad news: Mass extinctions topple ecological hierarchies, and in that vacuum, surviving species often thrive, exploding in diversity and territory. 1. End-Ordovician: The 1-2 Punch.Yet the mass extinction, known as the Cretaceous-Palaeogene or “K–Pg” event, was just as important for what it created as for what it destroyed.The Late Ordovician mass extinction (LOME) occurred in two phases and in terms of species loss was the second-greatest extinction event in Earth’s history 1,2,3.The Late Ordovician is ...66 Million Years Ago: Cretaceous-Paleogene Extinction . ... “Many of the past mass extinction events are mysterious in some ways because we really don’t know the cause,” says Michael Novacek, the Museum’s provost of science and a curator in the Division of Paleontology. "But we have a good idea of what the cause of the current changes ...Abstract. The Cretaceous/Palaeogene mass extinction eradicated 76% of species on Earth 1, 2. It was caused by the impact of an asteroid 3, 4 on the Yucatán carbonate platform in the southern Gulf ...Lowery and Dr. Fraass studied foram fossils from a time period covering roughly 20 million years, beginning around the end of the Cretaceous mass extinction and extending through the ensuing ...The Cretaceous-Paleogene boundary approximately 65.5 million years ago marks one of the three largest mass extinctions in the past 500 million years. The extinction event coincided with a large asteroid impact at Chicxulub, Mexico, and occurred within the time of Deccan flood basalt volcanism in Ind …The Cretaceous Period, spanning 65.5-146 million years ago (Mya), was a world different from what we are familiar with today. Planetary changes during this period included the extinction of dinosaurs and drastic global warming. The breakup of the super continent Pangea had started about 30 Mya, and seaways had begun to form and cover landmass ...Jul 8, 2022 · The Cretaceous ended with perhaps the most famous mass-extinction event of all, but there were other extinctions of note during the period. There were two minor mass-extinctions during the middle Cretaceous. The later of the two, at around 94 million years ago, is notable for the extinction of the ichthyosaurs. The two biggest extinctions were at the end of the Permian Period, about 250 million years ago, and at the end of the Cretaceous, some 65 million years ago. The Permian extinction saw the loss of ...The Cretaceous-Paleogene (K-Pg or K-T) mass extinction — the event in which the non-avian dinosaurs, along with about 70% of all species in the fossil record went extinct — was probably caused by the Chicxulub …Best known for killing off the dinosaurs, the end-Cretaceous mass extinction also caused many other casualties.Ammonoids (marine mollusks), pterosaurs (gliding reptiles), mosasaurs (swimming reptiles), and a host of other plants and animals died out completely or suffered heavy losses. However, some that did survive the extinction—including …1. Introduction. The Cretaceous–Paleogene (K–Pg) mass extinction event of 66 Ma is not only the most recent of the Phanerozoic ‘Big Five’ mass extinctions (Bambach, 2006), but also the most well-known and best-studied.If we assume that all vanishing Cretaceous species became extinct at the K/T boundary and their presence in Tertiary sediments is due to reworking, then the extinction rate exceeds 100 species per year, compared to an average of 1.5 species per million years (m.y.) and 5% per m.y. estimated by Perch-Nielsen (1986) and Roth (1987), respectively, …Many theories have been proposed to explain the Late Cretaceous mass extinction. Since the early 1980s, much attention has been focused on the asteroid theory formulated by American scientists Walter and Luis Alvarez.This theory states that the impact of an asteroid on Earth may have triggered the extinction event by ejecting a huge quantity of rock debris into the atmosphere, enshrouding ...Mass extinctions; Cretaceous period; Want to write? Write an article and join a growing community of more than 172,400 academics and researchers from 4,768 institutions. Register now.The Cretaceous–Paleogene (K–Pg) boundary marks Earth’s most recent mass extinction, when >75% of species, including nonavian dinosaurs, went extinct . In the terrestrial realm, the mass extinction was followed by a radiation of modern clades, particularly placental mammals ( 2 ), crown birds ( 3 ), and angiosperms ( 4 ). Jan 8, 2020 · The fifth major mass extinction event is perhaps the best-known, despite it not being the biggest. The Cretaceous-Tertiary Mass Extinction (or K-T Extinction) became the dividing line between the final period of the Mesozoic Era—the Cretaceous Period—and the Tertiary Period of the Cenozoic Era. It is also the event that wiped out the dinosaurs. January, 2018: The end-Cretaceous mass extinction — the event in which the non-avian dinosaurs, along with about 70% of all species in the fossil record went extinct — was …Nature (2023) Palaeontologists recognize five major extinction events from the fossil record, with the most recent, the Cretaceous mass extinction, ending some 65 million years ago. Given the many ...The Late Ordovician mass extinction (LOME), sometimes known as the end-Ordovician mass extinction or the Ordovician-Silurian extinction, is the first of the "big five" major mass extinction events in Earth's history, occurring roughly 443 Mya. It is often considered to be the second-largest known extinction event, in terms of the percentage of genera …That some mass extinction events have changed the course of evolution is clear, but it is equally obvious that there is no apparent relationship between the magnitude of an extinction and its ecological or evolutionary impact. ... N MacLeod Cretaceous–Tertiary Mass Extinctions, eds N MacLeod, G Keller (Norton, New York), …Five major mass extinctions are recognized: Late Ordovician, Late Devonian, Late Permian, Late Triassic, and Late Cretaceous (Figure 6.27). Of these, the Permian extinction rate is highest, with a mean family extinction rate of 61% for all life, 63% for terrestrial organisms, and 49% for marine organisms ( Benton, 1995 ).Indeed, weak geographic range selectivity appears to be a general pattern with the major mass extinctions, being also observed at the end-Triassic and the end-Cretaceous 45 (Fig. 1a).The Cretaceous is perhaps best known for the mass extinction event that exterminated the dinosaurs and many other species, bringing the period, and the Mesozoic Era, to a close. The Cretaceous was part of an important interval between ancient life-forms and those that dominate Earth today. Following the Permian mass extinction, life was abundant but there was a low diversity of species. However, through the Triassic, Jurassic, and Cretaceous, ...Sep 13, 2023 · The most recent of these events was the Cretaceous–Palaeogene mass extinction (K-Pg) that occurred approximately 66 million years ago (Mya) and is associated with the Chicxulub Impact Event . This event led to the demise of non-avian dinosaurs and high extinction rates of vertebrate species [1,3–6]. The Cretaceous–Paleogene (K–Pg) boundary marks Earth’s most recent mass extinction, when >75% of species, including nonavian dinosaurs, went extinct . In the terrestrial realm, the mass extinction was followed by a radiation of modern clades, particularly placental mammals ( 2 ), crown birds ( 3 ), and angiosperms ( 4 ). The mass extinction at the boundary (KPB) between the Cretaceous and Paleogene periods, ~66 million years ago (Ma), likely involved the catastrophic effects of a bolide impact (), although other factors may have played an important role (2-5).To a large extent, ambiguity between the possible causes stems from inadequate age resolution of relevant events near KPB time.End of the Cretaceous (66 million years ago): Extinction of many species in both marine and terrestrial habitats including pterosaurs, mosasaurs and other marine reptiles, many insects, and all non-Avian dinosaurs. The scientific consensus is that this mass extinction was caused by environmental consequences from the impact of a large asteroid ...The Cretaceous–Paleogene (K–Pg) mass extinction at 66 Ma is the most intensively studied of the ‘Big Five’ crises to have affected life during the Phanerozoic 1,2,3,4,5,6,7,8.The ...Dinosaur - Extinction Causes, Evidence, & Theory: The mass extinction of dinosaurs 66 million years ago remains a misconception; the fossil record shows that dinosaurs were already in decline during the late Cretaceous. Proposed causes for the extinction of dinosaurs have included everything from disease, heat waves, cold spells, faunal changes, and an asteroid collision during the K–T boundary.See full list on britannica.com The extinction that occurred 65 million years ago wiped out some 50 percent of plants and animals. The event is so striking that it signals a major turning point in Earth's history, marking the end of the geologic period known as the Cretaceous and the beginning of the Tertiary period. Explore the great change our planet has experienced: five ...Mass extinction event, any circumstance that results in the loss of a significant portion of Earth’s living species across a wide geographic area within a relatively short period of geologic time. Mass extinction events are extremely rare. They cause drastic changes to Earth’s biosphere, and in.Best known for killing off the dinosaurs, the end- Cretaceous mass extinction also caused many other casualties. Ammonoids ( marine mollusks ), pterosaurs (gliding reptiles), mosasaurs (swimming reptiles), and a host of other plants and animals died out completely or suffered heavy losses. However, some that did survive the extinction ... The contribution of the Deccan Traps (west-central India) volcanism in the Cretaceous-Paleogene (KPg) crisis is still a matter of debate. Recent U-Pb dating of zircons interbedded within the Deccan lava flows indicate that the main eruptive phase (>1.1 × 10 6 km 3 of basalts) initiated ∼250 k.y. before and ended ∼500 k.y. after the KPg boundary. . …Cretaceous-tertiary Extinction: (65.5 mya) 65 million years ago: a mass extinction Scientists refer to the major extinction that wiped out non-avian dinosaurs as the K-T extinction, because it happened at the end of the Cretaceous period and the beginning of the Tertiary period. Why not C-T? Geologists use "K" as a shorthand for Cretaceous.Many theories have been proposed to explain the Late Cretaceous mass extinction. Since the early 1980s, much attention has been focused on the asteroid theory formulated by American scientists Walter and Luis Alvarez. This theory states that the impact of an asteroid on Earth may have triggered the extinction event by ejecting a huge quantity ...
January, 2018: The end-Cretaceous mass extinction — the event in which the non-avian dinosaurs, along with about 70% of all species in the fossil record went extinct — was probably caused by the Chicxulub meteor impact in Yucatán, México. However, scientists have long wondered about the massive volcanic eruptions that were occurring in .... Warframe plague kripath
Sep 14, 2021 · Mass extinctions have repeatedly shaped global biodiversity. The Cretaceous-Paleogene (K-Pg) mass extinction caused the demise of numerous vertebrate groups, and its aftermath saw the rapid ... 3. The extinction rate that is normal in the fossil record is known as background extinction. Background extinction rates are constant within clades but vary greatly between clades. Extinction events are relatively short (in terms of geological time) periods with greatly increased extinction rates. A mass extinction event must eliminate …Each mass extinction ended a geologic period — that’s why researchers refer to them by names such as End-Cretaceous. But it’s not all bad news: Mass extinctions topple ecological hierarchies, and in that vacuum, surviving species often thrive, exploding in diversity and territory. 1. End-Ordovician: The 1-2 Punch.The last and probably most well-known of the mass-extinction events happened during the Cretaceous period, when an estimated 76% of all species went extinct, including the non-avian dinosaurs.65.5. The Ordovician-Silurian extinction event is the first recorded mass extinction and the second largest. During this period, about 85 percent of marine species (few species lived outside the oceans) became extinct. The main hypothesis for its cause is a period of glaciation and then warming.Mass-extinction events have a relatively long history of investigation regarding their effects on biodiversity. As a result, a distinct nomenclature has arisen describing the various phases and taxa present across extinction intervals (Fig. 2). A mass extinction can be divided into four main intervals: pre-extinction, extinction, recovery, and ...However, Renne and his colleagues have now discovered the Chicxulubimpact and the end-Cretaceous mass extinction event happened no more than 33,000 years apart.The end-Cretaceous mass extinction, 66 Ma, is the most recent of Raup and Sepkoski's "Big Five" extinction events ().Non-avian dinosaurs, along with many other groups that had dominated the Earth for 150 My, went extinct.The Cretaceous-Paleogene ( K-Pg) extinction event, [a] also known as the Cretaceous-Tertiary (K-T) extinction, [b] was a sudden mass extinction of three-quarters of the plant and animal species on Earth, [2] [3] approximately 66 million years ago. The event caused the extinction of all non-avian dinosaurs.The most famous mass extinction happened at the end of the Cretaceous, some 65 million years ago, when 76% of all species went extinct, including the dinosaurs.Best known for killing off the dinosaurs, the end- Cretaceous mass extinction also caused many other casualties. Ammonoids ( marine mollusks ), pterosaurs (gliding reptiles), mosasaurs (swimming reptiles), and a host of other plants and animals died out completely or suffered heavy losses. However, some that did survive the extinction ...The Cretaceous mass extinction event occurred 66 million years ago, killing 78% of all species, including the remaining non-avian dinosaurs. This was most likely caused by an asteroid hitting the Earth in what is now Mexico, potentially compounded by ongoing flood volcanism in what is now India. Triceratops was one of the last non-bird ....
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