Department of Statistics, School of Mathematics, University of Leeds, Leeds, UK.
CEREGE, Aix-Marseille University, CNRS, IRD, INRAE, Collège de France, Technopole de l'Arbois BP 80, Aix en Provence Cedex 4, France.
Nature. 2024 Sep;633(8029):306-317. doi: 10.1038/s41586-024-07679-4. Epub 2024 Sep 11.
Radiocarbon (C) is essential for creating chronologies to study the timings and drivers of pivotal events in human history and the Earth system over the past 55,000 years. It is also a fundamental proxy for investigating solar processes, including the potential of the Sun for extreme activity. Until now, fluctuations in past atmospheric C levels have limited the dating precision possible using radiocarbon. However, the discovery of solar super-storms known as extreme solar particle events (ESPEs) has driven a series of advances with the potential to transform the calendar-age precision of radiocarbon dating. Organic materials containing unique C ESPE signatures can now be dated to annual precision. In parallel, the search for further storms using high-precision annual C measurements has revealed fine-scaled variations that can be used to improve calendar-age precision, even in periods that lack ESPEs. Furthermore, the newly identified C fluctuations provide unprecedented insight into solar variability and the carbon cycle. Here, we review the current state of knowledge and share our insights into these rapidly developing, diverse research fields. We identify links between radiocarbon, archaeology, solar physics and Earth science to stimulate transdisciplinary collaboration, and we propose how researchers can take advantage of these recent developments.
放射性碳 (C) 对于创建年代表至关重要,可用于研究过去 55000 年来人类历史和地球系统中关键事件的时间和驱动因素。它也是研究太阳过程的基本指标,包括太阳发生极端活动的可能性。到目前为止,过去大气 C 水平的波动限制了使用放射性碳进行可能的测年精度。然而,被称为极端太阳粒子事件 (ESPE) 的太阳超级风暴的发现,推动了一系列进展,有可能改变放射性碳测年的日历年精度。现在可以对含有独特 ESPE 特征 C 的有机材料进行年度精度的测年。与此同时,使用高精度年度 C 测量值寻找进一步的风暴,揭示了可以提高日历年精度的精细尺度变化,即使在缺乏 ESPE 的时期也是如此。此外,新发现的 C 波动提供了对太阳变化和碳循环的前所未有的深入了解。在这里,我们回顾了当前的知识状况,并分享了我们对这些快速发展的、多样化的研究领域的见解。我们确定了放射性碳、考古学、太阳物理学和地球科学之间的联系,以激发跨学科合作,并提出了研究人员如何利用这些最新进展的方法。