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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​.sci​en​ce​dir​ect​.com/​j​o​u​r​n​a​l​/​a​n​t​h​r​o​p​ocene
3https://​strati​graphy​.org/​n​e​w​s/152
4https://​eartharx​iv​.org/​r​e​p​o​s​i​t​o​r​y​/​v​i​e​w​/​6954/

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