A distant supernova that exploded 41,000 years ago may have led to the extinction of the mammoth, according to research that will be presented tomorrow (Sept. 24) by nuclear scientist Richard Firestone of the U.S. Department of Energy's Lawrence Berkeley National Laboratory (Berkeley Lab).
Firestone, who conducted this research with Arizona geologist Allen West, will unveil this theory at the 2nd International Conference "The World of Elephants" in Hot Springs, S.D. Their theory joins the list of possible culprits responsible for the demise of mammoths, which last roamed North America roughly 13,000 years ago. Scientists have long eyed climate change, disease, or intensive hunting by humans as likely suspects.
Now, a supernova may join the line-up. Firestone and West believe that debris from a supernova explosion coalesced into low-density, comet-like objects that wreaked havoc on the solar system long ago. One such comet may have hit North America 13,000 years ago, unleashing a cataclysmic event that killed off the vast majority of mammoths and many other large North American mammals. They found evidence of this impact layer at several archaeological sites throughout North America where Clovis hunting artefacts and human-butchered mammoths have been unearthed. It has long been established that human activity ceased at these sites about 13,000 years ago, which is roughly the same time that mammoths disappeared.
They also found evidence of the supernova explosion's initial shockwave: 34,000-year-old mammoth tusks that are peppered with tiny impact craters apparently produced by iron-rich grains travelling at an estimated 10,000 kilometres per second. These grains may have been emitted from a supernova that exploded roughly 7,000 years earlier and about 250 light years from Earth.
"Our research indicates that a 10-kilometer-wide comet, which may have been composed from the remnants of a supernova explosion, could have hit North America 13,000 years ago. This event was preceded by an intense blast of iron-rich grains that impacted the planet roughly 34,000 years ago." - Richard Firestone.
In support of the comet impact, Firestone and West found magnetic metal spherules in the sediment of nine 13,000-year-old Clovis sites in Michigan, Canada, Arizona, New Mexico and the Carolinas. Low-density carbon spherules, charcoal, and excess radioactivity were also found at these sites.
"Armed with only a magnet and a Geiger counter, we found the magnetic particles in the well-dated Clovis layer all over North America where no one had looked before" - Richard Firestone.
Analysis of the magnetic particles by Prompt Gamma Activation Analysis at the Budapest Reactor and by Neutron Activation Analysis at Canada's Becquerel Laboratories revealed that they are rich in titanium, iron, manganese, vanadium, rare earth elements, thorium, and uranium. This composition is very similar to lunar igneous rocks, called KREEP, which were discovered on the moon by the Apollo astronauts, and have also been found in lunar meteorites that fell to Earth in the Middle East an estimated 10,000 years ago.
"This suggests that the Earth, moon, and the entire solar system were bombarded by similar materials, which we believe were the remnants of the supernova explosion 41,000 years ago" - Richard Firestone.
In addition, Berkeley Lab's Al Smith used the Lab's Low-Background Counting Facility to detect the radioactive isotope potassium-40 in several Clovis arrowhead fragments. Researchers at Becquerel Laboratories also found that some Clovis layer sediment samples are significantly enriched with this isotope.
"The potassium-40 in the Clovis layer is much more abundant than potassium-40 in the solar system. This isotope is formed in considerable excess in an exploding supernova, and has mostly decayed since the Earth was formed. We therefore believe that whatever hit the Earth 13,000 years ago originated from a recently exploded supernova" - Richard Firestone.
Firestone and West also uncovered evidence of an even earlier event that blasted parts of the Earth with iron-rich grains. Three mammoth tusks found in Alaska and Siberia, which were carbon-dated to be about 34,000 years old, are pitted with slightly radioactive, iron-rich impact sites caused by high-velocity grains. Because tusks are composed of dentine, which is a very hard material, these craters aren't easily formed. In fact, tests with shotgun pellets travelling 1,000 kilometres per hour produced no penetration in the tusks. Much higher energies are needed: x-ray analysis determined that the impact depths are consistent with grains travelling at speeds approaching 10,000 kilometres per second.
"This speed is the known rate of expansion of young supernova remnants" Richard Firestone.
The supernova's one-two punch to the Earth is further corroborated by radiocarbon measurements. The timeline of physical evidence discovered at Clovis sites and in the mammoth tusks mirrors radiocarbon peaks found in Icelandic marine sediment samples that are 41,000, 34,000, and 13,000 years old. Firestone contends that these peaks, which represent radiocarbon spikes that are 150 percent, 175 percent, and 40 percent above modern levels, respectively, can only be caused by a cosmic ray-producing event such as a supernova.
"The 150 percent increase of radiocarbon found in 41,000-year-old marine sediment is consistent with a supernova exploding 250 light years away, when compared to observations of a radiocarbon increase in tree rings from the time of the nearby historical supernova SN 1006" - Richard Firestone.
It would take 7,000 years for the supernova's iron-rich grains to travel 250 light years to the Earth, which corresponds to the time of the next marine sediment radiocarbon spike and the dating of the 34,000-year-old mammoth tusks. The most recent sediment spike corresponds with the end of the Clovis era and the comet-like bombardment.
"It's surprising that it works out so well" - Richard Firestone.
The riddle of the greatest life extinction on earth will likely be solved shortly, according to Wei Jiayong, a Chinese geologist. Since 1988, geologists from Britain, Australia, Germany and the United States, have made spot inspections at a mountainous area in Luodian County in southwest China's Guizhou Province, hoping to find evidence for the mass extinction 251 million years ago among fossils from the late Permian and early Triassic periods.
There have been six mass extinctions on earth. Among them, the most massive and influential was the extinction that occurred at the end of the Permian Period some 250 million years ago, when more than 90 percent of marine life perished in a short period of time - The Great Dying. Only a small amount of primitive life remained.
The precise cause of that extinction remains a mystery.
In Loudian County, frequented by both Chinese and foreign geologists, the core area called Big Guizhoutan, or Big Guizhou Shoal, is praised as a "treasure land for Triassic Period research."
Geologists have found that prior to the Permian extinction, the earth experienced a major environmental change. However, areas around the Big Guizhoutan were barely affected. Michael J. Orchard, president of the Triassic stratum department of the International Commission on Stratigraphy, said, "A variety of factors conspired toward the Permian extinction. China has provided unique fossils for research in this case and has made productive research in this field."
"The Triassic history of the vast, attached Yangtze platform (YP), as recorded near Hongyan, Guizhou, China, started with a retreat of the margin following a regional transgression initiated during the latest Permian. A condensed sequence of laminated lime mudstones spread across the Permian platform that was submerged to form a ramp. The platform-interior deposits are characterized by dolomitic shoaling-upward cycles. Carbonate breccia wedges within the basin may represent lowstand aprons corresponding to possible exposure surfaces." Source
Meteor strikes may have led to the extinction of some life on Earth, but they may have also contributed to the creation of life, according to a study released on Monday. Geologists researching the crater left when the Haughton meteor slammed into what is now Canada's Arctic 23 million years ago found the impact created hydrothermal springs in the cracked rock and other conditions that would have made it easier for microbes to survive and evolve. The impact of a meteor hitting the Earth may have caused the extinction of the dinosaurs, according to some theories that posit it sparked huge fires and a gigantic dust cloud.
"Most people put impacts with mass extinction... What we're trying to say is that following the impact, the impact sites are actually more favourable than the surrounding terrain" - Gordon Osinski, of the Canadian Space Agency.
Researchers found that in addition to hydrothermal springs, meteor impacts would have allowed microbes easier access to minerals in a protected environment. The shocked rocks are also more translucent, which would be beneficial to organisms that possessing with any photosynthetic capabilities. A crater shape might also serve as a protective environment. As such, impact craters are also good places to store evidence of past life. The craters fill with water and become lakes that in turn accumulate sediments; the layers of which are a geological archive of the time after the crater formed. The Haughton Impact crater on Devon Island, for instance, contains the only Miocene-age sediments in the entire Canadian Arctic.
The heaviest meteor bombardment of Earth happened about 3.8 billion years ago, around the same time that life on the planet is believed to have started.
The researchers reported their study on the biological effects of impacts on Monday in Calgary, Alberta, during a joint meeting of the Geological Society of America and the Geological Association of Canada.
Scientists have long suspected that certain features of the Jeerinan Formation in the area known as the Pilbara Craton were signs of a large meteor impact.
However, until now, the only evidence for this had been small splatters of melted rock called spherules, between 3.4 and 2.6 billion years old; the area had lacked the indisputable hallmarks of a Meteorite impact: high iridium levels and shocked quartz.
A cluster of at least three asteroids between 20 and 50 kilometres across colliding with Earth over 3.2 billion years ago caused a massive change in the structure and composition of the earth’s surface, according to new research by Australian National University(ANU) earth scientists. According to Dr Andrew Glikson and Mr John Vickers from the Department of Earth and Marine Sciences at ANU, the impact of these asteroids triggered major earthquakes, faulting, volcanic eruption and deep-seated magmatic activity and interrupted the evolution of parts of the Earth’s crust. The research extends the original discovery of extraterrestrial impact deposits, discovered in South Africa by two US scientists, D.R. Lowe and G.R. Byerly, identifying their effects in the Pilbara region in Western Australia.
"Our findings are further evidence that the seismic aftershocks of these massive impacts resulted in the abrupt termination of an over 300 million years-long evolutionary stage dominated by basaltic volcanic activity and protracted accretion of granitic plutons" - Dr Andrew Glikson.
The identification of impact ejecta is based on unique minerals and chemical and isotopic compositions indicative of extraterrestrial origin, including iridium anomalies.
The impact ejecta from the Barberton region in the eastern Transvaal indicate the formation of impact craters several hundred kilometres in diameter in oceanic regions of the earth, analogous to the lunar maria basins (large dark impressions on the surface of the moon). The seismic effects of the impacts included vertical block movements, exposure of deep-seated granites and onset of continental conditions on parts of the earth surface.
In the Pilbara, the formation of fault escarpments and fault troughs is represented by collapse of blocks up to 250-metres wide and 150-metres high, buried canyons and a major volcanic episode 3240 million years ago.
"The precise coincidence of the faulting and igneous activity with the impact deposits, coupled with the sharp break between basaltic crust and continental formations, throws a new light on the role of asteroid impacts in terrestrial evolution" - Dr Andrew Glikson.
Preliminary indications suggest that at about the same time the Moon was also affected by asteroid impacts and by resurgent volcanic activity. Dr Glikson and Mr Vickers will continue to investigate the extent and effects of large asteroid impacts by studying early terrains in other parts of the world, including India and Canada.