Global Boundary Stratotype Section and Point (GSSP) for the Anthropocene Series: Where and how to look for potential candidates

• Published in: Earth-Science Reviews
• Main Authors: Waters, Colin N., Zalasiewicz, Jan, Summerhayes, Colin, Fairchild, Ian J., Rose, Neil L., Loader, Neil J., Shotyk, William, Cearreta, Alejandro, Head, Martin J., Syvitski, James P. M., Williams, Mark, Wagreich, Michael, Barnosky, Anthony D., Zhisheng, An, Leinfelder, Reinhold, Jeandel, Catherine, Galuszka, Agnieszka, do Sul, Juliana A. Ivar, Gradstein, Felix, Steffen, Will, McNeill, John R., Wing, Scott, Poirier, Clement, Edgeworth, Matt
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2018
• Subjects: Anthropocene; Global Boundary Stratotype Sections And Points; Chronostratigraphy; Palaeoenvironments; Science & Technology; Physical Sciences; WATER-USE EFFICIENCY; SANTA-BARBARA-BASIN; ANTHROPOGENIC NITROGEN DEPOSITION; SPHEROIDAL CARBONACEOUS PARTICLES; ATMOSPHERIC MERCURY DEPOSITION; SCOTTISH MOUNTAIN LAKE; ANTARCTIC SNOW RECORD; OMBROTROPHIC PEAT BOG; LAWRENCE NORTH SHORE; SEA GORGONIAN CORALS; Geology; Geosciences; Multidisciplinary; Antarctic; Antarc*
• Online Access: http://ir.ieecas.cn/handle/361006/5156; https://doi.org/10.1016/j.earscirev.2017.12.016

The Anthropocene as a potential new unit of the International Chronostratigraphic Chart (which serves as the basis of the Geological Time Scale) is assessed in terms of the stratigraphic markers and approximate boundary levels available to define the base of the unit. The task of assessing and selecting potential Global Boundary Stratotype Section and Point (GSSP) candidate sections, a required part of the process in seeking formalisation of the term, is now being actively pursued. Here, we review the suitability of different stratified palaeoenvironmental settings and facies as potential hosts for a candidate GSSP and auxiliary sections, and the relevant stratigraphical markers for correlation. Published examples are evaluated for their strengths and weaknesses in this respect. A marked upturn in abundance of radioisotopes of Pu-239 or C-14, approximately in 1952 and 1954 CE respectively, broadly coincident with a downturn in delta C-13 values, is applicable across most environments. Principal palaeoenvironments examined include: settings associated with accumulations of anthropogenic material, marine anoxic basins, coral reefs, estuaries and deltas, lakes at various latitudes, peat bogs, snow/ice layers, speleothems and trees. Together, many of these geographically diverse palaeoenvironments offer annual/subannual laminae that can be counted and independently dated radiometrically (e.g. by Pb-210). Examples of possible sections offer the possibility of correlation with annual/seasonal resolution. From among such examples, a small number of potentially representative sites require the acquisition of more systematic and comprehensive datasets, with correlation established between sections, to allow selection of a candidate GSSP and auxiliary stratotypes. The assessments in this paper will help find the optimal locations for these sections.