研究者らが古典的クロービス遺跡で宇宙衝突の痕跡を発見(Researchers find evidence of cosmic impact at classic Clovis archaeological sites)

2025-09-17 カリフォルニア大学サンタバーバラ校(UCSB)

Web要約 の発言:
カリフォルニア大学サンタバーバラ校のKennett教授らは、米国の代表的クロヴィス遺跡(アリゾナ州Murray Springs、ニューメキシコ州Blackwater Draw、カリフォルニア州Arlington Canyon)で「ショック石英」を発見した。これは極端な高温高圧で変形した石英粒であり、火山活動や人類活動では説明できず、約1.3万年前に分裂した彗星が地表上空で爆発した「タッチダウン大気爆発」による衝撃を示す証拠とされる。衝撃は広範な火災や煙塵を生じ、「インパクト冬」を引き起こし、マンモスなど大型動物の絶滅やクロヴィス文化の消滅に寄与した可能性が高い。本成果はPLOS Oneに発表された。

研究者らが古典的クロービス遺跡で宇宙衝突の痕跡を発見(Researchers find evidence of cosmic impact at classic Clovis archaeological sites)Photo CreditCourtesy Image
The three classic Clovis archaeological sites in the study

<関連情報>

ヤングドライアス期(1万2800年前)の衝撃石英は、北米巨大動物群絶滅とクロービス技術複合体の崩壊に寄与した宇宙起源の空中爆発/衝突を裏付ける 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,Timothy Witwer,Kurt Langworthy,Joshua J. Razink, [ … ],Allen West
PLOS One  Published: September 10, 2025
DOI:https://doi.org/10.1371/journal.pone.0319840

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.

1702地球物理及び地球化学
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