When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal

Autor(en)

Jan Zalasiewicz, Colin N. Waters, Mark Williams, Anthony D. Barnosky, Alejandro Cearreta, Paul Crutzen, Erle Ellis, Michael A. Ellis, Ian J. Fairchild, Jacques Grinevald, Peter K. Haff, Irka Hajdas, Reinhold Leinfelder, John McNeill, Eric O. Odada, Clement Poirier, Daniel Richter, Will Steffen, Colin Summerhayes, James P.M. Syvitski, Davor Vidas, Michael Wagreich, Scott L. Wing, Alexander P. Wolfe, An Zhisheng, Naomi Oreskes

Abstrakt

We evaluate the boundary of the Anthropocene geological time interval as an epoch, since it is useful to have a consistent temporal definition for this increasingly used unit, whether the presently informal term is eventually formalized or not. Of the three main levels suggested - an 'early Anthropocene' level some thousands of years ago; the beginning of the Industrial Revolution at ~1800 CE (Common Era); and the 'Great Acceleration' of the mid-twentieth century - current evidence suggests that the last of these has the most pronounced and globally synchronous signal. A boundary at this time need not have a Global Boundary Stratotype Section and Point (GSSP or 'golden spike') but can be defined by a Global Standard Stratigraphic Age (GSSA), i.e. a point in time of the human calendar. We propose an appropriate boundary level here to be the time of the world's first nuclear bomb explosion, on July 16th 1945 at Alamogordo, New Mexico; additional bombs were detonated at the average rate of one every 9.6 days until 1988 with attendant worldwide fallout easily identifiable in the chemostratigraphic record. Hence, Anthropocene deposits would be those that may include the globally distributed primary artificial radionuclide signal, while also being recognized using a wide range of other stratigraphic criteria. This suggestion for the Holocene-Anthropocene boundary may ultimately be superseded, as the Anthropocene is only in its early phases, but it should remain practical and effective for use by at least the current generation of scientists.

Organisation(en)

Institut für Geologie

Externe Organisation(en)

University of Leicester, British Geological Survey, University of California, Berkeley, University of the Basque Country, Max-Planck-Institut für Chemie (Otto-Hahn-Institut), University of Maryland, Baltimore, University of Birmingham, Hochschulinstitut für internationale Studien und Entwicklung (IHEID), Durham University, Eidgenössische Technische Hochschule Zürich, Freie Universität Berlin (FU), Georgetown University, Kenyatta University, Université Caen-Normandie, Duke University, Australian National University, University of Cambridge, University of Colorado, Boulder, Fridtjof Nansen Institute, Smithsonian National Museum of Natural History, University of Alberta, Chinese Academy of Sciences (CAS), Harvard University

Journal

Quaternary International

Band

383

Seiten

196-203

Anzahl der Seiten

8

ISSN

1040-6182

DOI

https://doi.org/10.1016/j.quaint.2014.11.045

Publikationsdatum

10-2015

Peer-reviewed

Ja

ÖFOS 2012

105205 Klimawandel, 105123 Stratigraphie, 601003 Archäologie

Schlagwörter

ASJC Scopus Sachgebiete

Earth-Surface Processes

Sustainable Development Goals

SDG 13 – Maßnahmen zum Klimaschutz

Link zum Portal

https://ucrisportal.univie.ac.at/de/publications/when-did-the-anthropocene-begin-a-midtwentieth-century-boundary-level-is-stratigraphically-optimal(28f12b5c-c7a3-4624-a8b6-bacad6b6baba).html