Kennett James P, LeCompte Malcolm A, Moore Christopher R, Kletetschka Gunther, Johnson John R, Wolbach Wendy S, Mitra Siddhartha, Maiorana-Boutilier Abigail, Adedeji Victor, Young Marc D, Witwer Timothy, Langworthy Kurt, Razink Joshua J, Brogden Valerie, van Devener Brian, Perez Jesus Paulo, Polson Randy, West Allen
Department of Earth Science and Marine Science Institute, University of California, Santa Barbara, California, United States of America.
Elizabeth City State University, Center of Excellence in Remote Sensing Education and Research, Elizabeth City, North Carolina, United States of America.
PLoS One. 2025 Sep 10;20(9):e0319840. doi: 10.1371/journal.pone.0319840. eCollection 2025.
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.
冲击石英颗粒是陨石坑形成的宇宙撞击事件的公认指标,这类事件通常还会沿着裂缝产生无定形二氧化硅。此外,先前的研究表明,当核爆炸、小行星和彗星产生近地表或“触地”气爆时,也会形成冲击石英。当宇宙气爆以足够的能量在足够低的高度引爆时,产生的相对较小的高速碎片可能以足够高的压力撞击地球表面,从而产生热冲击和机械冲击,使石英颗粒破裂,并将熔融二氧化硅引入裂缝中。在此,我们报告在美国西南部三个经典考古序列中发现了可追溯至新仙女木期(YD)开始(12800年前)的一层冲击石英颗粒,这些序列位于亚利桑那州的默里泉、新墨西哥州的黑水凹地和加利福尼亚州的阿灵顿峡谷。这些遗址对于证明许多大型动物物种的灭绝或观察到的种群瓶颈,以及北美克洛维斯技术复合体在同一时期的崩溃/重组在YD开始时或其附近同时发生具有重要意义。我们使用了一套全面的10种分析技术,包括电子显微镜(透射电子显微镜、扫描电子显微镜、阴极发光显微镜和电子背散射衍射),我们识别出了具有玻璃填充裂缝的颗粒,这些颗粒类似于与核爆炸相关的冲击颗粒,以及27个已被认可的不同年代的撞击坑(例如,5万年前的陨石坑;3500万年前的切萨皮克湾;6600万年前的希克苏鲁伯;2.14亿年前的马尼夸根),并且是在11次实验室冲击实验中产生的。此外,我们使用流体动力学编码模型来探索与一颗100米大小的彗星碎片气爆相关的温度、压力和冲击波速度,并得出结论,它们足以产生冲击石英。这些冲击颗粒与先前报道的铂、熔融玻璃、烟灰和纳米金刚石的峰值浓度同时出现,还有微球粒,类似于在约28个微球粒层中发现的那些,这些微球粒层被公认为是宇宙撞击事件的证据,即使在没有已知陨石坑的情况下也是如此。在这三个关键考古遗址发现明显经过热改变的冲击石英颗粒,支持了宇宙撞击是新仙女木期开始时大型动物灭绝和克洛维斯技术复合体崩溃的一个主要促成因素这一观点。