Whereas proponents of the theory have offered “carbonaceous spherules” and nanodiamonds—both of which they claimed were formed by intense heat—as evidence of the impact, a new study concludes that those supposed clues are nothing more than fossilized balls of fungus, charcoal, and fecal pellets.
Moreover, these naturally-occurring organic materials, some of which had likely been subjected to normal cycles of wildfires, date from a period of thousands of years both before and after the time that the Younger Dryas period began – further suggesting that there was no sudden impact event.
“People get very excited about the idea of a major impact causing a catastrophic fire and the abrupt climate change in that period, but there just isn’t the evidence to support it,” says Andrew C. Scott of the Department of Earth Sciences at Royal Holloway, University of London, who led the research.
The findings by Scott and his colleagues have been accepted for publication in Geophysical Research Letters, a journal of the American Geophysical Union (AGU). The research team included scientists from England, Switzerland, and the United States.
The Younger Dryas impact event theory holds that a very large meteor struck Earth or exploded in the atmosphere about 12,900 years ago, causing a vast fire over most of North America, which contributed to extinctions of most of large animals on the continent and triggered a thousand-year-long cold period. While there is much previous evidence for the abrupt onset of a cooling period at that time, other researchers have theorized that the climatic change resulted from increased freshwater in the ocean, changes in ocean and atmospheric circulation patterns, or other causes unrelated to impacts.
The impact-theory proponents point to a charred layer of sediment filled with organic material that they say is unique to that period as evidence of such an event. These researchers described carbon spheres, carbon cylinders, and charcoal pieces that they conclude are melted and charred organic matter created in the intense heat of a widespread fire.
Scott and his fellow researchers analyzed sediment samples to determine the origins of the carbonaceous particles. After comparing the fossil particles with modern fungal ones exposed to low to moderate heat (less than 500 degrees Celsius, or 932 degrees Fahrenheit), Scott’s group concludes that the particles are actually balls of fungal material and other ordinary organic particles, such as fecal pellets from insects, plant or fungal galls, and wood, some of which may have been exposed to regularly-occurring low-intensity wildfires.
The researchers used microscopic analysis of particles from the Pleistocene-Holocene sediments collected from the California Channel Islands and compared them with modern soil samples that had been subjected to wildfires, as well as balls of stringy fungal material, called sclerotia, some of which were also subjected to a range of temperatures in a laboratory. Many soil and plant fungi produce sclerotia – tough balls of cells that are usually 0.5 millimeters to 2 millimeters in size (0.02 inches to 0.08 inches) – as a way to survive periods of harsh conditions. Their shape can vary from spherical to elongated, and their internal structures, which can take on a spongy or honeycomb pattern, matches the descriptions given by Dryas- impact event proponents.
Further, the group studied the amount of light reflected by the fossil spherules and wood charcoal from the sediment layers that included the Dryas period. The researchers used the reflectance of the organic material to determine the amount of heat to which it had been subjected. They found that the fossilized matter was unlikely to have been exposed to temperatures above 450 degrees Celsius (842 degrees Fahrenheit). Radiocarbon dating also showed that the particles, taken from several layers, ranged in age from 16,821 to 11,467 years ago. Proponents of the impact theory had reported that the spherules they found in the Younger Dryas sediment layer dated to a very narrow time period of 12,900 to 13,000 years before present.
“There is a long history of fire in the fossil record, and these fungal samples are common everywhere, from ancient times to the present,” Scott says. “These data support our conclusion that there wasn’t one single intense fire that triggered the onset of the cold period.”
Funding for this research was provided by the National Geographic Society, the National Science Foundation, the Royal Society of London, the Royal Holloway strategy fund, the Natural Environmental Research Council, and the Integrated Infrastructure Initiative on Synchrotrons and Free Electron Lasers.
AGU Media Contact: Kathleen O’Neil, Public Information Specialist: 202.777.7524, firstname.lastname@example.org
Kathleen O’Neil | American Geophysical Union
Greenland ice flow likely to speed up: New data assert glaciers move over sediment, which gets more slippery as it gets wetter
17.08.2017 | Swansea University
Climate change: In their old age, trees still accumulate large quantities of carbon
17.08.2017 | Universität Hamburg
Whether you call it effervescent, fizzy, or sparkling, carbonated water is making a comeback as a beverage. Aside from quenching thirst, researchers at the University of Illinois at Urbana-Champaign have discovered a new use for these "bubbly" concoctions that will have major impact on the manufacturer of the world's thinnest, flattest, and one most useful materials -- graphene.
As graphene's popularity grows as an advanced "wonder" material, the speed and quality at which it can be manufactured will be paramount. With that in mind,...
Physicists at the University of Bonn have managed to create optical hollows and more complex patterns into which the light of a Bose-Einstein condensate flows. The creation of such highly low-loss structures for light is a prerequisite for complex light circuits, such as for quantum information processing for a new generation of computers. The researchers are now presenting their results in the journal Nature Photonics.
Light particles (photons) occur as tiny, indivisible portions. Many thousands of these light portions can be merged to form a single super-photon if they are...
For the first time, scientists have shown that circular RNA is linked to brain function. When a RNA molecule called Cdr1as was deleted from the genome of mice, the animals had problems filtering out unnecessary information – like patients suffering from neuropsychiatric disorders.
While hundreds of circular RNAs (circRNAs) are abundant in mammalian brains, one big question has remained unanswered: What are they actually good for? In the...
An experimental small satellite has successfully collected and delivered data on a key measurement for predicting changes in Earth's climate.
The Radiometer Assessment using Vertically Aligned Nanotubes (RAVAN) CubeSat was launched into low-Earth orbit on Nov. 11, 2016, in order to test new...
A study led by scientists of the Max Planck Institute for the Structure and Dynamics of Matter (MPSD) at the Center for Free-Electron Laser Science in Hamburg presents evidence of the coexistence of superconductivity and “charge-density-waves” in compounds of the poorly-studied family of bismuthates. This observation opens up new perspectives for a deeper understanding of the phenomenon of high-temperature superconductivity, a topic which is at the core of condensed matter research since more than 30 years. The paper by Nicoletti et al has been published in the PNAS.
Since the beginning of the 20th century, superconductivity had been observed in some metals at temperatures only a few degrees above the absolute zero (minus...
16.08.2017 | Event News
04.08.2017 | Event News
26.07.2017 | Event News
21.08.2017 | Medical Engineering
21.08.2017 | Materials Sciences
21.08.2017 | Life Sciences