The chronostratigraphy of the Anthropocene in southern Africa: Current status and potential

Abstract The process for the formal ratification of proposed Anthropocene Epoch involves identification a globally isochronous stratigraphic signal to mark its starting point. search Global Boundary Stratotype Section and Point (GSSP), unique reference sequence that would be used fix start epoch, is in progress but none candidate sections are located Africa. We assessed currently available evidence possible markers southern Africa found that, although most have been identified region, robustly dated, high resolution records required GSSP very sparse. then extent range potential natural archives conclude small number permanent lakes, as well marine sediments, corals peats from selected locations could provide temporal required. With sufficient chronological control multi-proxy analyses, one these useful auxiliary stratotype thereby helping confirm global reach, extending utility, GSSP.