1 History of Geology & Anthropocene
Sunday, 19 March 2017
8:00 AM - 10:00 AM
Allegheny, 17th Floor
A STRATIGRAPHER’S PERSPECTIVES ON THE ANTHROPOCENE
Paper number: 1-4
Program: Technical Sessions
Time: 9:00 AM – 9:20 AM
Authors
Abstract
Time is a continuum. Humans like to compartmentalize time and to choose specific words to do so. A goal is to make it easier to communicate information about strata, events, and patterns in time.
The International Chronostratigraphic Chart is a tool for unambiguous communication. Each horizontal line on it indicates a boundary that is studied, deliberated upon, and accepted as a physical point at a specific location to serve as an agreed-upon standard. Once chosen, no transition is allowed.
The word “Anthropocene” is very popular now. Is it a concept? Is it a philosophy? Is it a hypothesis? Is it an adjective that conveys a stratigraphic record? Is it an adjective that conveys a specific segment in the continuum of time? Does it include the future?
The short answer is that, currently, the word “Anthropocene” sits at a crossroad. It could be used exclusively for that interval of time that includes the present and a little bit back in the past; it could be used exclusively for a concept of human domination over environment.
Who owns the Anthropocene? If one’s premise is that humans have so profoundly altered the planet on which they live that a new geologic epoch has begun, then geologists get to define it and own it. If one’s premise is that humans have so profoundly altered the planet on which they live that these same humans need to stop, think, and perhaps change their ways, then maybe geologists shouldn’t own it.
The question is not “Can the Anthropocene be put on the International Chronostratigraphic Chart?” but rather “Should it?” Putting it as an adjective on the Chart comes with rules and regulations. This presentation will help Quaternarists see both advantages and disadvantages of these limitations with respect to their varied perceptions of the Anthropocene.
Geological Society of America Abstracts with Programs. Vol. 49, No. 2
doi: 10.1130/abs/2017NE-290079
© Copyright 2017 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.