Latest paper by Johan Rockström and colleagues.
Abstract
While the term “Anthropocene” is well established across scientific disciplines and social spheres, interpretations are diverse. Taking account of the 2024 rejection by a geological commission to accept the Anthropocene as a geological epoch and the related scientific debate, here we offer a future-oriented perspective from the viewpoint of Earth system science. We describe different pathways in the Anthropocene up to the year 3,000, systematically characterizing them according to impacts and causes. We discuss the enormous global consequences of anthropogenic pressures on the Earth system and quantify the corresponding long-term commitment to change. Regarding the causes, we conservatively explore best-case and middle-of-the road emission scenarios, in combination with climate sensitivities drawn from within the IPCC likely range. We also discuss implications for Earth system resilience that could result in what we call worst case scenarios for Anthropocene outcomes. We conclude that, beyond the slow pace of natural climate recovery spanning many millennia, even minimal, unavoidable residual emissions like from the food sector risk perpetuating global warming in the absence of other human forcing. One implication is that if climate or carbon cycle feedbacks shift toward reinforcing warming, they risk not only exacerbating climate impacts but to also surpassing human forcing in relevance. At that point, human influence on the Anthropocene would no longer play the dominant role.
Plain Language Summary
Most people have a general, intuitive understanding of the term “Anthropocene.” And while it has not formally been declared as a new geological epoch, it is scientifically clear that these new times have only begun to fully unfold. The Anthropocene stresses both the enormity of the human imprint on Earth, as well as its long-term nature. That latter aspect, however, is highly underappreciated among the public. We describe several qualitatively different Anthropocene pathways for the next millennium, some of them depending on our cumulative actions as humanity, some on how the Earth system responds to these human pressures. We highlight how much we are already stuck in a figurative “Anthropocene quicksand”, where only an active pull can free us from consequences like global heating—while even a very modest continuation of greenhouse gas emissions will keep us at high warming levels. Should Earth system resilience, the natural buffering capacity, significantly decline, the impacts of our actions would become even stronger. In a worst-case scenario, shifts in Earth system feedbacks could even surpass human forcing in relevance. But we are not there yet and can still pull ourselves out of the quicksand.
We Are in the Anthropocene—Now What? - Rockström - 2026 - Earth's Future - Wiley Online Library
https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025EF007730