Working Group on the ‘Anthropocene’

Results of binding vote by AWG

Released 21st May 2019

Following guidance from the Subcommission on Quaternary Stratigraphy and the International Commission on Stratigraphy, the AWG have completed a binding vote to affirm some of the key questions that were voted on and agreed at the IGC Cape Town meeting in 2016. The details are as follows:

No. of potential voting members: 34        No. required to be quorate (60%): 21     No. of votes received: 33 (97% of voting membership)

Q1.  Should the Anthropocene be treated as a formal chrono-stratigraphic unit defined by a GSSP?

29  voted in favour (88% of votes cast); 4 voted against; no abstentions

Q2. Should the primary guide for the base of the Anthropocene be one of the stratigraphic signals around the mid-twentieth century of the Common Era?

29  voted in favour (88% of votes cast); 4 voted against; no abstentions

Both votes exceed the 60% supermajority of cast votes required to be agreed by the Anthropocene Working Group as the official stance of the group and will guide their subsequent analysis.

 

What is the Anthropocene? – current definition and status

  • The ‘Anthropocene’ is a term widely used since its coining by Paul Crutzen and Eugene Stoermer in 2000 to denote the present geological time interval, in which many conditions and processes on Earth are profoundly altered by human impact. This impact has intensified significantly since the onset of industrialization, taking us out of the Earth System state typical of the Holocene Epoch that post-dates the last glaciation.
  • The ‘Anthropocene’ has developed a range of meanings among vastly different scholarly communities. Here we examine the Anthropocene as a geological time (chronostratigraphic) unit and potential addition to the Geological Time Scale, consistent with Crutzen and Stoermer’s original proposal. The Anthropocene Working Group (AWG) is charged with this task as a component body of the Subcommission on Quaternary Stratigraphy (SQS) which is itself a constituent body of the International Commission on Stratigraphy (ICS).
  • Phenomena associated with the Anthropocene include: an order-of-magnitude increase in erosion and sediment transport associated with urbanization and agriculture; marked and abrupt anthropogenic perturbations of the cycles of elements such as carbon, nitrogen, phosphorus and various metals together with new chemical compounds; environmental changes generated by these perturbations, including global warming, sea-level rise, ocean acidification and spreading oceanic ‘dead zones’; rapid changes in the biosphere both on land and in the sea, as a result of habitat loss, predation, explosion of domestic animal populations and species invasions;  and the proliferation and global dispersion of many new ‘minerals’ and ‘rocks’ including concrete, fly ash and plastics, and the myriad ‘technofossils’ produced from these and other materials.
  • Many of these changes will persist for millennia or longer, and are altering the trajectory of the Earth System, some with permanent effect. They are being reflected in a distinctive body of geological strata now accumulating, with potential to be preserved into the far future.
  • The Anthropocene is not currently a formally defined geological unit within the Geological Time Scale; officially we still live within the Meghalayan Age of the Holocene Epoch. A proposal to formalise the Anthropocene is being developed by the AWG. Based on preliminary recommendations made by the AWG in 2016, this proposal is being developed on the following basis:
    1. It is being considered at series/epoch level (and so its base/beginning would terminate the Holocene Series/Epoch as well as Meghalayan Stage/Age);
    2. It would be defined by the standard means for a unit of the Geological Time Scale, via a Global boundary Stratotype Section and Point (GSSP), colloquially known as a ‘golden spike’;
    3. Its beginning would be optimally placed in the mid-20th century, coinciding with the array of geological proxy signals preserved within recently accumulated strata and resulting from the ‘Great Acceleration’ of population growth, industrialization and globalization;
    4. The sharpest and most globally synchronous of these signals, that may form a primary marker, is made by the artificial radionuclides spread worldwide by the thermonuclear bomb tests from the early 1950s.

    Analyses of potential ‘golden spike’ locations are underway. The resultant proposal, when made, would need supermajority (>60%) agreement by the AWG and its parent bodies (successively the SQS and ICS) and ratification by the Executive Committee of the International Union of Geological Sciences. The success of any such proposal is not guaranteed.

  • Broadly, to be accepted as a formal geological time term the Anthropocene needs to be (a) scientifically justified, i.e. the ‘geological signal’ currently being produced in strata now forming must be significantly large, clear and distinctive; sufficient evidence has now been gathered to demonstrate this phenomenon (b) useful as a formal term to the scientific community. In terms of (b), the currently informal term ‘Anthropocene’ has already proven highly useful to the global change and Earth System science research communities and thus will continue to be used. Its value as a formal geological time term to other communities continues to be discussed.
  • The Anthropocene has emerged as a popular scientific term used by scientists, the scientifically engaged public and the media to designate the period of Earth’s history during which humans have a decisive influence on the state, dynamics and future of the Earth System. It is widely agreed that the Earth is currently in such a state. The term has also been used in a non-chronostratigraphic context to be an informal term to denote a broader interpretation of anthropogenic impact on the planet that is markedly diachronous, reaching back many millennia. In geology, such an interpretation is already encompassed by lithostratigraphy, in which the character of stratified rocks is based solely on their physical features and not by age. Such an interpretation represents a concept sharply distinct from the Anthropocene as a chronostratigraphic unit, though it can be complementary with it.

Working group convenors:

Colin Waters (Chair) e-mail: cw398@leicester.ac.uk
Simon Turner (Secretary) e-mail: simon.turner@ucl.ac.uk

Members:

An Zhisheng e-mail: anzs@loess.llqg.ac.cn
Anthony Barnosky e-mail: tonybarnosky@stanford.edu
Alejandro Cearreta e-mail: alejandro.cearreta@ehu.eus
Paul Crutzen e-mail: paul.crutzen@mpic.de
Andy Cundy e-mail: A.Cundy@noc.soton.ac.uk
Matt Edgeworth e-mail: me87@leicester.ac.uk
Erle Ellis e-mail: ece@umbc.edu
Ian Fairchild e-mail: i.j.fairchild@bham.ac.uk
Agnieszka Gałuszka e-mail: aggie@ujk.edu.pl
Philip Gibbard (Secretary-General, ICS) e-mail: plg1@cam.ac.uk
Jacques Grinevald e-mail: jacques.grinevald@graduateinstitute.ch
Peter Haff e-mail: haff@duke.edu
Irka Hajdas e-mail: hajdas@phys.ethz.ch
Han Yongming e-mail: yongming@ieecas.cn
Martin J. Head (Vice-Chair, SQS) email: mjhead@brocku.ca
Juliana Assunção Ivar do Sul email: juliana.ivardosul@io-warnemuende.de
Catherine Jeandel e-mail: catherine.jeandel@legos.obs-mip.fr
Reinhold Leinfelder e-mail: reinhold.leinfelder@fu-berlin.de
Francine McCarthy e-mail: fmccarthy@brocku.ca
John McNeill e-mail: mcneillj@georgetown.edu
Eric Odada e-mail: eodada@uonbi.ac.ke
Naomi Oreskes e-mail: oreskes@fas.harvard.edu
Clément Poirier e-mail: clement.poirier@unicaen.fr
Dan Richter e-mail drichter@duke.edu
Neil Rose e-mail: n.rose@ucl.ac.uk
Yoshiki Saito e-mail: ysaito@soc.shimane-u.ac.jp
Bill Shotyk e-mail: shotyk@ualberta.ca
Will Steffen e-mail: will.steffen@anu.edu.au
Colin Summerhayes e-mail: cps32@cam.ac.uk
Jaia Syvitski e-mail: jai.syvitski@colorado.edu
Simon Turner (AWG Secretary) e-mail: simon.turner@ucl.ac.uk
Davor Vidas e-mail: dvidas@fni.no
Michael Wagreich e-mail: michael.wagreich@univie.ac.at
Colin Waters (AWG Chair) e-mail: cw398@leicester.ac.uk
Mark Williams e-mail: mri@leicester.ac.uk
Scott Wing e-mail: wings@si.edu
Jan Zalasiewicz (Chair, SQS) e-mail: jaz1@leicester.ac.uk
Jens Zinke e-mail: jz262@leicester.ac.uk

Working Group communications:

Publications of the Working Group on the ‘Anthropocene’

2020

      • Syvitski, J. et al. (in press). Extraordinary human energy consumption and resultant geological impacts beginning around 1950 CE initiated the proposed Anthropocene Epoch. Communications Earth & Environment.
      • Zalasiewicz, J., Waters, C. and Williams, M. (in press). Chapter 31: The Anthropocene. In: Gradstein, F., Ogg, J., Schmitz, M. and Ogg, G. (eds.) A Geologic Time Scale 2020.

2019

      • Williams, M. et al. 2019. Underground metro systems: a durable geological proxy of rapid urban population growth and energy consumption during the Anthropocene. In Craig Benjamin, Esther Quaedakers and David Baker (Eds.) Anthropocene: The Routledge Handbook of Big History (Routledge Companions). Oxon: Taylor & Francis.
      • Zalasiewicz, J., Gabbott, S.E. and Waters C.N. 2019. Chapter 23: Plastic Waste: how plastic has become part of the Earth’s geological cycle. In: Trevor M. Letcher and Dan  A Vallero (eds.) Waste: A Handbook for Management, 2nd edition. Elsevier, New York, 443-452.
      • Zalasiewicz, J. et al. 2019. A formal Anthropocene is compatible with but distinct from its diachronous anthropogenic counterparts: a response to WF Ruddiman’s ‘three flaws in defining a formal Anthropocene’. Progress in Physical Geography, 43(3): 319-333.
      • Zalasiewicz, J, Waters, CN et al. (Eds.) (2019). The Anthropocene as a Geological Time Unit. CUP.The Anthropocene, a term launched into public debate by Nobel Prize winner Paul Crutzen, has been used informally to describe the time interval during which human actions have had a drastic effect on the Earth and its ecosystems, including anthropogenic climate change. This book presents the underpinning geological evidence for defining the Anthropocene as a geological epoch, written by the high-profile international team tasked with analysing its potential addition to the Geological Time Scale. It discusses Anthropocene stratigraphy and ongoing changes to the Earth system, including the climate, oceans and biosphere.
        The evidence for the Anthropocene is examined in detail, ranging from chemical signals arising from pollution, to physical changes to the landscape associated with urbanisation and biological changes associated with species invasion and extinctions. The scale, manner and rate of global environmental change is placed within the context of planetary processes and deep geological time, allowing the reader to appreciate the scale of human-driven change to the Earth system, and compare the global transition taking place today with major transitions in Earth history. Key aspects of the geological background are explained, providing an authoritative review of the Anthropocene for graduate students and academic researchers across a broad range of scientific, social science and humanities disciplines.

2018

2017

2016

2015

2014

2011

2008

      • Zalasiewicz, J, Williams, M, Smith, A, Barry, TL, Coe, AL, Bown, PR, Brenchley, P, Cantrill, D, Gale, A, Gibbard, P, Gregory, FJ, Hounslow, MW, Kerr, AC, Pearson, P, Knox, R, Powell, JH, Waters, CN et al. 2008. Are we living in the Anthropocene? GSA Today, 18(2): 4-8.

2007

2002

2000