Evidence map›Paper›PMID 40929082›Full record

ArticlePloS one2025

RETRACTED: Shocked quartz at the Younger Dryas onset (12.8 ka) supports cosmic airbursts/impacts contributing to North American megafaunal extinctions and collapse of the Clovis technocomplex.

James P Kennett, Malcolm A LeCompte, Christopher R Moore, Gunther Kletetschka, John R Johnson, Wendy S Wolbach, Siddhartha Mitra, Abigail Maiorana-Boutilier, Victor Adedeji, Marc D Young and 8 more

RetractedAbstract readRetracted Publication
In one paragraph

Article in PloS one, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. It has been retracted, and should not be counted. Cited by 2 papers.

0numbers the graph read from it
0cells of the map it votes in
2citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

2 citing papers in PubMed.

  1. Article
  2. Article
4 · The record

Corrections and comments

5 · Who and what money

Authors and funding

18 authors.

James P KennettDepartment of Earth Science and Marine Science Institute, University of California, Santa Barbara, California, United States of America.
Malcolm A LeCompteElizabeth City State University, Center of Excellence in Remote Sensing Education and Research, Elizabeth City, North Carolina, United States of America.
Christopher R MooreSouth Carolina Institute of Archaeology and Anthropology, University of South Carolina, Columbia, South Carolina, United States of America.ORCID 0009-0009-3961-7626
Gunther KletetschkaGeophysical Institute, University of Alaska, Fairbanks, Alaska, United States of America.ORCID 0000-0002-0645-9037
John R JohnsonSanta Barbara Museum of Natural History, Santa Barbara, California, United States of America.ORCID 0000-0002-3920-9923
Wendy S WolbachDepartment of Chemistry and Biochemistry, DePaul University, Chicago, Illinois, United States of America.
Siddhartha MitraVirginia Institute of Marine Science, Gloucester Point, Virginia, United States of America.
Abigail Maiorana-BoutilierBrody School of Medicine, East Carolina University, Greenville, North Carolina, United States of America.
Victor AdedejiDepartment of Natural Sciences, Elizabeth City State University, Elizabeth City, North Carolina, United States of America.
Marc D YoungCollege of Humanities, Arts and Social Sciences, Flinders University, Bedford Park, South Australia.
Timothy WitwerComet Research Group, Prescott, Arizona, United States of America.
Kurt LangworthyCAMCOR, University of Oregon, Eugene, Oregon, United States of America.
Joshua J RazinkCAMCOR, University of Oregon, Eugene, Oregon, United States of America.
Valerie BrogdenCAMCOR, University of Oregon, Eugene, Oregon, United States of America.
Brian van DevenerElectron Microscopy and Surface Analysis Lab, Nanofab, University of Utah, Salt Lake City, Utah, United States of America.
Jesus Paulo PerezElectron Microscopy and Surface Analysis Lab, Nanofab, University of Utah, Salt Lake City, Utah, United States of America.
Randy PolsonElectron Microscopy and Surface Analysis Lab, Nanofab, University of Utah, Salt Lake City, Utah, United States of America.
Allen WestComet Research Group, Prescott, Arizona, United States of America.ORCID 0000-0003-3576-4847

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Shocked quartz grains are an accepted indicator of crater-forming cosmic impact events, which also typically produce amorphous silica along the fractures. Furthermore, previous research has shown that shocked quartz can form when nuclear detonations, asteroids, and comets produce near-surface or "touch-down" airbursts. When cosmic airbursts detonate with enough energy and at sufficiently low altitude, the resultant relatively small, high-velocity fragments may strike Earth's surface with high enough pressures to generate thermal and mechanical shock that can fracture quartz grains and introduce molten silica into the fractures. Here, we report the discovery of shocked quartz grains in a layer dating to the Younger Dryas (YD) onset (12.8 ka) in three classic archaeological sequences in the Southwestern United States: Murray Springs, Arizona; Blackwater Draw, New Mexico; and Arlington Canyon, California. These sites were foundational in demonstrating that the extinction or observed population bottlenecks of many megafaunal species and the coeval collapse/reorganization of the Clovis technocomplex in North America co-occurred at or near the YD onset. Using a comprehensive suite of 10 analytical techniques, including electron microscopy (TEM, SEM, CL, and EBSD), we have identified grains with glass-filled fractures similar to shocked grains associated with nuclear explosions and 27 accepted impact craters of different ages (e.g., Meteor Crater, 50 ka; Chesapeake Bay, 35 Ma; Chicxulub, 66 Ma; Manicouagan, 214 Ma) and produced in 11 laboratory shock experiments. In addition, we used hydrocode modeling to explore the temperatures, pressures, and shockwave velocities associated with the airburst of a 100-m fragment of a comet and conclude that they are sufficient to produce shocked quartz. These shocked grains co-occur with previously reported peak concentrations in platinum, meltglass, soot, and nanodiamonds, along with microspherules, similar to those found in ~28 microspherule layers that are accepted as evidence for cosmic impact events, even in the absence of a known crater. The discovery of apparently thermally-altered shocked quartz grains at these three key archaeological sites supports a cosmic impact as a major contributing factor in the megafaunal extinctions and the collapse of the Clovis technocomplex at the YD onset.

Indexed as

QuartzArchaeologyNorth AmericaQuartz

Identifiers

PMID40929082
PMCPMC12422476

What OpenQuestion holds

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LicenceCC BY
Read underepoch 390

Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.