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Why the Anthropocene has divided the scientific community

Jan Piotrowski
Jan Piotrowski
Professor of Quaternary Geology at Aarhus University and Nicolaus Copernicus University in Toruń
Michel Magny
Michel Magny
Emeritus Research Director at CNRS
Erle Ellis
Erle Ellis
Professor of Geography and Environmental Systems at the University of Maryland
Key takeaways
  • The concept of the Anthropocene refers to a new geological era, characterised by the significant and worldwide impact of human activity on the planet.
  • In 2023, a working group dedicated to the Anthropocene set its “golden spike” (the landmark that marks the boundary between two geological periods) in 1952, in the sediment of Crawford Lake, Canada, notably because of nuclear markers.
  • Although this term is widely used by the scientific community, it is the subject of debate in geology and has been rejected by the International Commission on Stratigraphy.
  • Among the reasons for this rejection are the difficulty of rigorously defining the beginning of the Anthropocene and the fact that the proposed golden spike does not meet the standards of the geological time scale.
  • However, the concept is still widely used, not least because it underlines the urgent need to act in the face of climate change and highlights a society in which the global transformations of the planet are caused by humans.

The term is eve­ryw­here : from the École de l’Anthropocène in Lyon to a dedi­ca­ted IGN atlas1 and even two dedi­ca­ted scien­ti­fic jour­nals2, eve­ryone – scien­tists inclu­ded – is using the concept of the Anthro­po­cene. This new geo­lo­gi­cal era is cha­rac­te­ri­sed by a signi­fi­cant glo­bal human foot­print on the pla­net. But the term is not offi­cial­ly reco­gni­sed. In March 2024, the Inter­na­tio­nal Com­mis­sion on Stra­ti­gra­phy – the orga­ni­sa­tion res­pon­sible for defi­ning the geo­lo­gi­cal time scale – rejec­ted the offi­cial addi­tion of a new geo­lo­gi­cal era3. We are the­re­fore still offi­cial­ly in the Holo­cene era, as we have been for the past 11,700 years. None­the­less, this deci­sion has not put an end to the debate within the scien­ti­fic community.

#1 THE ANTHROPOCENE EXISTS.

True : Part of the scientific community recognises its existence.

Erle Ellis. The Anthro­po­cene, as defi­ned in dic­tio­na­ries, exists and is wide­ly used in science to define a time when humans are trans­for­ming the pla­net. Howe­ver, there is no offi­cial era in the geo­lo­gi­cal timeline.

Michel Magny. A large part of the inter­na­tio­nal scien­ti­fic com­mu­ni­ty reco­gnises the term. When it was first pro­po­sed in our team, which works on the recons­truc­tion of past envi­ron­ments in rela­tion to socie­ties, we had the impres­sion that all our work incor­po­ra­ted the concept of the Anthro­po­cene ! We have seen the major impact of human­kind on eco­sys­tems since the first agri­cul­tu­ral socie­ties. Many geo­lo­gists also reco­gnise the exis­tence of the Anthropocene.

Without dis­pu­ting the fact that rapid and far-rea­ching cli­mate changes may have occur­red in the past, the Anthro­po­cene marks a sud­den change in the cli­mate pat­tern. Whe­reas for a mil­lion years, cli­ma­tic oscil­la­tions were main­ly dri­ven by the Earth’s orbi­tal fac­tors, now it is the rate of human green­house gas emis­sions that is cau­sing the cli­mate to warm up by a simi­lar amount.

False : The International Committee for Stratigraphy has rejected the adoption of the Anthropocene as a geological epoch.

Jan Pio­trows­ki. There is no jus­ti­fi­ca­tion for ending the Holo­cene. The end of the last Ice Age – rough­ly coin­ci­ding with the begin­ning of the Holo­cene – was mar­ked by envi­ron­men­tal changes that were signi­fi­cant­ly grea­ter than those that would have mar­ked the begin­ning of the Anthro­po­cene. For example, the tem­pe­ra­ture rose by 1°C per decade in Wales 15,000 years ago ; 11,700 years ago in Green­land, a war­ming of 7°C occur­red in just 50 years ; and 14,000 years ago, the docu­men­ted rise in sea level in Bar­ba­dos was 40 mm/year. These rates of change are grea­ter than those our pla­net has expe­rien­ced since 1950.

Unclear : There are other alternatives for characterising humanity’s footprint on the planet.

JP. The only valid alter­na­tive to the Anthro­po­cene is to des­cribe it not as an epoch but as an event. Events are ele­ments that are well esta­bli­shed in stra­ti­gra­phy : we find, for example, the Great Oxi­da­tion 2.4 bil­lion years ago, or the Ordo­vi­cian bio­lo­gi­cal explo­sion 500 mil­lion years ago. An event can be dia­chro­nic, as is the case with the Anthro­po­cene. [Edi­tor’s note : The Anthro­po­cene wor­king group says it has consi­de­red this pos­si­bi­li­ty in detail, and concludes that it is incom­pa­tible with the stra­ti­gra­phic data4.]

#2 : IT IS POSSIBLE TO DEFINE THE ANTHROPOCENE PRECISELY.

True : Scientists have defined a marker for the start of the Anthropocene.

MM. A wor­king group dedi­ca­ted to the Anthro­po­cene was set up in 2009 at the request of the Inter­na­tio­nal Union of Geo­lo­gi­cal Sciences. In 2019, this group pro­po­sed adop­ting the term Anthro­po­cene. In 2023, it even defi­ned a gol­den spike in the sedi­ments of Lake Craw­ford, in Cana­da. Here, and across the globe, there has been a rapid increase in the concen­tra­tions of two iso­topes of plu­to­nium, cor­res­pon­ding to the first nuclear tests on land. The begin­ning of the Anthro­po­cene would thus be defi­ned in 1952. Apart from the nuclear mar­ker, many other indi­ca­tors show an abrupt change at this time : green­house gas levels rising, bio­di­ver­si­ty fal­ling, pol­lu­tion piling up, man-made waste (such as plas­tic) accumulating.

Some have cri­ti­ci­sed the choice of Lake Craw­ford to define the gol­den spike mar­king the begin­ning of the Anthro­po­cene, main­ly because of its lack of acces­si­bi­li­ty. But what about the site offi­cial­ly cho­sen for the Gol­den Spike at the start of the Holo­cene ? It’s a bore­hole in the Green­land ice cap, which is in dan­ger of disap­pea­ring because of glo­bal warming…

False : It is not possible to precisely define the beginning of the Anthropocene.

JP. There are geo­lo­gi­cal traces of human pre­sence well before the pro­po­sed start of the Anthro­po­cene (begin­ning of agri­cul­ture, set­tle­ment of the Ame­ri­cas, indus­trial revo­lu­tion, etc.). Among the argu­ments against reco­gni­sing the Anthro­po­cene as a geo­lo­gi­cal epoch, seve­ral concern the begin­ning of the Anthro­po­cene. It can­not be pre­ci­se­ly defi­ned because it began at dif­ferent times and in dif­ferent places on Earth. What’s more, the pro­po­sed date (1952) makes no sense, as humanity’s impact on the Earth goes back much fur­ther than that. This would make the Second World War pre-Anthro­po­cene ! Final­ly, the pro­po­sed gol­den spike – Lake Craw­ford – does not meet the stan­dards of the geo­lo­gi­cal time­line : it is not very acces­sible and geo­lo­gi­cal­ly unstable.

EE. It’s poten­tial­ly pos­sible to pre­ci­se­ly define a date and mar­ker for the Anthro­po­cene, but there’s no obvious scien­ti­fic point to it, espe­cial­ly if it’s recent. There are bet­ter ways of unders­tan­ding the Anthro­po­cene as an ongoing pro­cess and event, rather than an abrupt glo­bal change that occur­red in 1952.

Uncertain : Conflicting positions remain, not always based on scientific evidence.

MM. The deci­sion by the Inter­na­tio­nal Com­mis­sion on Stra­ti­gra­phy to refuse to reco­gnise the Anthro­po­cene may seem sur­pri­sing. In fact, in 2023, the dedi­ca­ted wor­king group had recom­men­ded the adop­tion of the Anthro­po­cene and pro­po­sed a gol­den spike.

But I unders­tand the geo­lo­gists’ mis­gi­vings. First, it should be remem­be­red that the Anthro­po­cene epoch was pro­po­sed in 2000 by Paul Josef Crut­zen. This che­mist, who works on stra­tos­phe­ric ozone, is reco­gni­sed by the inter­na­tio­nal scien­ti­fic com­mu­ni­ty and has been awar­ded the Nobel Prize for Che­mis­try. But he is not a geo­lo­gist. The fact that a che­mist is pro­po­sing to revi­sit the geo­lo­gi­cal time­line can be a source of dif­fi­cul­ty. Final­ly, geo­lo­gi­cal time­lines are very long, often mil­lions of years. The change of scale here is radi­cal, with the Anthro­po­cene star­ting in 1952, i.e. only 72 years ago !

#3 : WE CAN STILL TALK ABOUT THE ANTHROPOCENE.

True : The term unites many scientists.

MM. The inter­na­tio­nal scien­ti­fic com­mu­ni­ty sei­zed on the term as soon as it was pro­po­sed. There are dedi­ca­ted jour­nals, and major scien­ti­fic jour­nals such as Nature and The Holo­cene have devo­ted spe­cial issues to the Anthro­po­cene. The term brings toge­ther scien­tists from the natu­ral and human sciences, and it is a ban­ner that car­ries weight with the autho­ri­ties that govern us, and we will conti­nue to use it. In my view, refu­sing offi­cial recog­ni­tion sends out a nega­tive signal to scien­tists, but above all to poli­ti­cal and eco­no­mic lea­ders and to public opi­nion. I fear that it will serve as an ali­bi for inac­tion in the face of cli­mate change. It’s a real source of confu­sion, which is to be deplored.

EE. I think that scien­tists will conti­nue to dis­cuss the mea­ning of the “human era” using the term Anthro­po­cene, and pro­ba­bly others. Human socie­ties are not the first or only glo­bal change to the pla­net cau­sed by orga­nisms, but it is the most recent and is dif­ferent from pre­vious ones in many ways. There is no need to for­mal­ly define the Anthro­po­cene epoch for the dis­cus­sion to continue.

Uncertain : Debate is part of the scientific method, and this decision is not final.

MM. Des­pite the deci­sion of the Inter­na­tio­nal Com­mis­sion on Stra­ti­gra­phy, the debate conti­nues. As scien­tists, we are used to seeing nar­ra­tives and inter­pre­ta­tions evolve as the data pro­gresses, and I think that as the eco­lo­gi­cal cri­sis inten­si­fies, the break mar­ked by the Anthro­po­cene will become more and more obvious.

JP. There’s nothing wrong with using the Anthro­po­cene as a scien­ti­fic term, but it should be cal­led an event rather than an epoch. If the Anthro­po­cene star­ted only 70 years ago, then its future impact is based on pre­dic­tions and not on avai­lable geo­lo­gi­cal data. Conse­quent­ly, its sta­tus should be confir­med by future gene­ra­tions of geologists.

Anaïs Marechal
1https://​www​.ign​.fr/​a​t​l​a​s​-​i​g​n​-​d​e​s​-​c​a​r​t​e​s​-​d​e​-​l​a​n​t​h​r​o​p​o​c​e​n​e​-​2​0​2​4​-​i​n​t​e​l​l​i​g​e​n​c​e​-​a​r​t​i​f​i​c​ielle
2https://​www​.scien​ce​di​rect​.com/​j​o​u​r​n​a​l​/​a​n​t​h​r​o​p​ocene
3https://​stra​ti​gra​phy​.org/​n​e​w​s/152
4https://​ear​tharxiv​.org/​r​e​p​o​s​i​t​o​r​y​/​v​i​e​w​/​6954/

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