人类世系列的全球边界层型剖面和点的候选地点和其他参考剖面

C. Waters, S. Turner, J. Zalasiewicz, M. Head
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引用次数: 25

摘要

我们审查并比较了提交给国际第四纪地层学小组委员会人类世工作组的12个参考剖面的提案,其中一个将被推荐为全球边界地层类型剖面和点(GSSP),以将人类世的基底定义为地质时间标度内的一个系列。这些地点横跨五大洲,位于不同的环境中,除一个外,其余都是通过取芯采样的。许多位点显示出每年解析的薄层(这里被认为是GSSP选择的最佳选择),可以通过放射测量法独立确定其年代,以确认在临界区间内的完整序列。分析了一系列广泛的代理,记录了20世纪中期左右人类对地球系统的深刻修改。机载信号(如放射性同位素、飞灰、稳定的碳和氮同位素)提供了适用于大多数环境的最广泛和接近等时代理。其他相关手段包括微塑料和持久性有机污染物的出现,以及重金属浓度和铅同位素比率的变化。海洋、河口和湖泊环境中微体化石(和一些大型化石)的组合变化反映了环境变化和生物引入。这些系统而全面的数据集,以及各部分之间建立的相关性,为正式化人类世的提议提供了基础。
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Candidate sites and other reference sections for the Global boundary Stratotype Section and Point of the Anthropocene series
We review and compare proposals for 12 reference sections submitted to the Anthropocene Working Group of the International Subcommission on Quaternary Stratigraphy, of which one will be recommended as the Global boundary Stratotype Section and Point (GSSP) to define the base of the Anthropocene as a series within the Geological Time Scale. The sites span five continents and are located in diverse environments, with all but one sampled by coring. Many sites show annually resolved laminae (here considered optimal for GSSP selection) that can be independently dated radiometrically to confirm a complete succession over the critical interval. An extensive range of proxies, documenting profound human modification of the Earth System at around the mid-20th century interval, has been analysed. Airborne signals (e.g. radioisotopes, fly ash, stable carbon and nitrogen isotopes) provide the most widespread and near-isochronous proxies, applicable across most environments. Additional means of correlation include the appearance of microplastics and persistent organic pollutants, and shifts in heavy metal concentrations and lead isotope ratios. Assemblage changes of microfossils (and some macrofossils) in marine, estuarine and lake settings reflect environmental changes and biological introductions. These systematic and comprehensive datasets, with correlation established between sections, provide the basis for a proposal to formalize the Anthropocene.
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