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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​encedi​rect​.com/​j​o​u​r​n​a​l​/​a​n​t​h​r​o​p​ocene
3https://​stratig​ra​phy​.org/​n​e​w​s/152
4https://​earth​arx​iv​.org/​r​e​p​o​s​i​t​o​r​y​/​v​i​e​w​/​6954/

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