The East Gotland Basin (Baltic Sea) as a candidate Global boundary Stratotype Section and Point for the Anthropocene series

J. Kaiser, Serena M. Abel, H. Arz, A. Cundy, O. Dellwig, P. Gaca, G. Gerdts, I. Hajdas, M. Labrenz, J. Milton, M. Moros, S. Primpke, S. Roberts, N. Rose, S. Turner, M. Voss, J. A. Ivar do Sul
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引用次数: 1

Abstract

The short sediment core EMB201/7-4 retrieved from the East Gotland Basin, central Baltic Sea, is explored here as a candidate to host the stratigraphical basis for the Anthropocene series and its equivalent Anthropocene epoch, still to be formalized in the Geological Time Scale. The core has been accurately dated back to 1840 CE using a well-established event stratigraphy approach. A pronounced and significant change occurs at 26.5 cm (dated 1956 ± 4 CE) for a range of geochemical markers including 239+240Pu, 241Am, fly-ash particles, DDT (organochlorine insecticide), total organic carbon, and bulk organic carbon stable isotopes. This stratigraphic level, which corresponds to a change in both lithology and sediment colour related to early anthropogenic-triggered eutrophication of the central Baltic Sea, is proposed as a Global boundary Stratotype Section and Point for the Anthropocene series.
东哥特兰盆地(波罗的海)作为人类世系列的候选全球边界层型剖面和点
本文对波罗的海中部东哥特兰盆地的EMB201/7-4短沉积物岩心进行了研究,认为该岩心可作为人类世系列及其对应的人类世期的地层基础,但在地质时间尺度上仍有待确定。利用一种成熟的事件地层学方法,地核可以精确地追溯到公元1840年。在26.5 cm(1956±4 CE)处,一系列地球化学标志(239+240Pu、241Am、粉煤灰颗粒、DDT(有机氯杀虫剂)、总有机碳和体积有机碳稳定同位素)发生了显著变化。该地层水平对应于与波罗的海中部早期人类活动引发的富营养化有关的岩性和沉积物颜色变化,被认为是人类世系列的全球边界层型剖面和点。
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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