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    Unearthing the Present

    What is the new geological epoch made of? Unearthing the Present connected the geological analysis of the present with a discussion of the changing scope for social and political agency.

    Strontium synchrotron radiation X-ray fluorescence map of annually laminated stalagmite acquired at the XFM beamline of the Australian Synchrotron. Image by Andreas Borsato © All Rights Reserved

    How does a new geological epoch take shape? What do the sediments of Earth tell us about the present and about the actions and decisions we have to take today? The planet has entered the first stage of the Anthropocene: a highly disruptive transitional period of “global weirding” within which ecological patterns and societal structures are changing radically. Between 2020–22, the Anthropocene Working Group was assembling stratigraphic evidence for the geological reality of the new Earth epoch. Unearthing the Present connected these analyses with a discussion of the changing scope for social and political agency. In collaborative Core Readings, scientists, researchers, artists and activists deciphered stratigraphic samples from pacific corals, from lake deposits in northeastern China and from speleothems found in an Italian cave. They examined the microscopic traces left in Earth’s archives by the burning of fossil fuels, atmospheric nuclear bomb testing and the disruption of marine ecosystems to jointly identify ways and means of responding to these signals.

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