High-resolution analysis of the varved succession at Crawford lake across the base of the proposed Crawfordian stage and Anthropocene series.

The anthropocene review Pub Date : 2025-03-31 eCollection Date: 2025-08-01 DOI:10.1177/20530196251315454
Francine Mg McCarthy, R Timothy Patterson, Carling Walsh, Krysten M Lafond, Brian F Cumming, Andy B Cundy, Karin Hain, Pawel Gaca, Peter Steier, Arnoud Boom, Paul B Hamilton, Michael Fj Pisaric, Martin J Head, Joseph I Boyce, Neil L Rose, Simon D Turner
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Abstract

Four years after the Anthropocene Working Group (AWG) voted to work toward defining the Anthropocene series/epoch with a base in the mid-20th C, the varved sediments of Crawford Lake (Milton, ON, Canada) were selected as the Global boundary Stratotype Section and Point (GSSP) candidate. The initial major rise in activity of 239 + 240Pu had been selected as the primary chronostratigraphic marker to define the base of the Anthropocene, but the precise year when this occurred could not be determined from measurements of samples combining multiple varves. Individual varves from freeze cores collected in April 2023 provide annual resolution for bomb radionuclides, allowing the varve age model to be refined, former assignments determined to have been 1 year too old. The increase in 239 + 240Pu activities (calculated from atom concentrations of 239Pu and 240Pu measured using Accelerated Mass Spectrometry) of 0.0031 Bq/g between varves now assigned to 1951 and 1952 is consistent with the onset of thermonuclear weapons testing on November 1, 1952, so the proposed base for the Anthropocene is at the contact between the light- and dark-coloured laminae deposited in 1952 CE (17.5 cm in core CRA23-BC-1F-B). Sharply lower 239 + 240Pu and 137Cs activities capture the moratorium from November 1958 to September 1961 before rising quickly to peak activities of 239 + 240Pu in 1963 CE. Analysis of individual varves with varying amounts of organic matter and inorganic calcite illustrates the influence of lithology on organic proxies, but the upcore trend toward depleted values of δ15N through the 20th C reflects increased fossil fuel combustion worldwide. An inflection point in δ15N around 1911 CE is attributed the global impact of the Haber-Bosch process and establishment of nearby steel mills, and another in the early 1950s attributed to the Great Acceleration to which the tipping point in the Earth system is attributed.

克劳福德湖跨克劳福德阶段和人类世系列基底的变异演替的高分辨率分析。
在人类世工作组(AWG)投票决定以20世纪中期为基准确定人类世系列/时代的四年后,克劳福德湖(Milton, ON, Canada)的变分沉积物被选为全球边界层型剖面和点(GSSP)候选者。239 + 240Pu的活动最初的主要上升被选为确定人类世基础的主要年代地层标志,但这种情况发生的确切年份无法通过结合多个阀门的样品测量来确定。从2023年4月收集的冷冻岩心中收集的单个阀门提供了核弹放射性核素的年度分辨率,从而使阀门年龄模型得以改进,以前的分配确定为1岁。239 + 240Pu活度的增加(通过加速质谱法测量239 + 240Pu的原子浓度计算)在1951年和1952年之间增加了0.0031 Bq/g,这与1952年11月1日热核武器试验的开始是一致的,因此人类世的建议基地是在1952年沉积的浅色和深色纹层之间的接触处(在CRA23-BC-1F-B岩心17.5 cm)。急剧下降的239 + 240Pu和137Cs活动在1958年11月至1961年9月期间暂停,然后在1963年CE迅速上升至239 + 240Pu的峰值。对不同有机质和无机方解石含量的单个样品的分析表明,岩性对有机代用物的影响,但到20℃,δ15N值下降的上核趋势反映了全球范围内化石燃料燃烧的增加。1911年前后δ15N的一个拐点归因于哈伯-博世过程的全球影响和附近钢厂的建立,另一个在20世纪50年代初归因于地球系统临界点的大加速度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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