148 Adieu to the Anthropocene? Debating the Formality of Geologic Time in the Face of Accelerating Changes in Earth Processes (a late-breaking session sponsored by the Geochronology Division)

Monday, 23 September 2024
1:30 PM - 5:30 PM
204A


BEYOND THE EPOCHAL ANTHROPOCENE: EARTH SCIENCE FOR A HUMAN-TRANSFORMED PLANET

Paper number: 148-6
Program: Special and Late Breaking Sessions
Time: 2:55 PM – 3:15 PM


Authors

  • Erle Ellis Presenting Author
    University of Maryland, Baltimore County (UMBC), Baltimore, MD

Abstract

The Anthropocene has inspired decades of discussion and research aimed at better understanding the dynamics of our increasingly human-transformed planet. Recently, the decision by geologists not to define the Anthropocene as an epoch in the Geological Time Scale has left some Earth scientists and others concerned that the term remains without any formal scientific definition. This presentation explains the general scientific utility of informally defining the Anthropocene as a geological event, or more specifically, as an ongoing, complex, socially differentiated, and spatially and temporally heterogenous planet-transforming event, itself made up of manifold events, that has been unfolding across the planet since prehistoric times. Geologists, geographers, environmental scientists, archaeologists and other scholars have long collaborated in their efforts to understand the interacting material, biological, and social processes that have formed and continue to shape Earth’s surface conditions since humans first emerged as a species more than 300,000 years ago. The Anthropocene event expands this common ground for collaboration to better understand planetary changes beyond the shallow sedimentary evidence and narrow temporal confines of a formal epoch definition, to focus instead on the Anthropocene as a complex and ongoing planetary event analogous to the Great Oxidation Event and others.

Geological Society of America Abstracts with Programs. Vol. 56, No. 5

doi: 10.1130/abs/2024AM-406425

© Copyright 2024 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.