气泡中的生命:附近的超新星如何在宇宙射线光谱上留下短暂的足迹,并在生命上留下不可磨灭的印记

Caitlyn Nojiri, Noémie Globus and Enrico Ramirez-Ruiz
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摘要

地球位于一个300个人电脑宽的空间内,这个空间是由几千万年前一系列超新星爆炸形成的,这些爆炸推开了星际气体,形成了一个泡沫状的结构。在深海地壳中发现的60Fe峰矿床被解释为大约2-3和5-6万年前发生的超新星爆炸所留下的印记。大约2-3迈的60Fe峰值很可能来自发生在半人马座上半人马座红斑星系团(≈140 pc)或半人马座天蝎座的tucina - horologium星系团(≈70 pc)的超新星,而≈5-6迈r的峰值可能归因于太阳系进入气泡。在这篇文章中,我们表明,负责合成60Fe峰沉积的超新星源≈2-3 Myr ago可以一致地解释宇宙射线谱和100 TeV和100 PeV之间的大尺度各向异性。宇宙射线膝盖可能完全归因于附近一个单一的“PeVatron”源。匹配宇宙射线光谱的强度和形状使我们能够对超新星的宇宙射线能量含量以及宇宙射线扩散系数施加严格的限制。利用这些限制条件,我们对地球电离宇宙辐射水平的时间变化提供了一个可靠的估计,并讨论了它们对地球上早期生命发展的影响,合理地影响突变率,因此,可以想象,有助于复杂生物体的进化。
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Life in the Bubble: How a Nearby Supernova Left Ephemeral Footprints on the Cosmic-Ray Spectrum and Indelible Imprints on Life
The Earth sits inside a 300 pc-wide void that was carved by a series of supernova explosions that went off tens of millions of years ago, pushing away interstellar gas and creating a bubble-like structure. The 60Fe peak deposits found in the deep-sea crust have been interpreted by the imprints left by the ejecta of supernova explosions occurring about 2–3 and 5–6 Myr ago. It is likely that the 60Fe peak at about 2–3 Myr originated from a supernova occurring in the Upper Centaurus Lupus association in Scorpius Centaurus (≈140 pc) or the Tucana-Horologium association (≈70 pc), whereas the ≈5–6 Myr peak is likely attributed to the solar system's entrance into the bubble. In this Letter, we show that the supernova source responsible for synthesizing the 60Fe peak deposits ≈2–3 Myr ago can consistently explain the cosmic-ray spectrum and the large-scale anisotropy between 100 TeV and 100 PeV. The cosmic-ray knee could then potentially be attributed entirely to a single nearby “PeVatron” source. Matching the intensity and shape of the cosmic-ray spectrum allows us to place stringent constraints on the cosmic-ray energy content from the supernova as well as on the cosmic-ray diffusion coefficient. Making use of such constraints, we provide a robust estimate of the temporal variation of terrestrial ionizing cosmic radiation levels and discuss their implications in the development of early life on Earth by plausibly influencing the mutation rate and, as such, conceivably assisting in the evolution of complex organisms.
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