La Administración De Los Recursos Naturales

INVITED PAPER

The Anthropocene: From Global Change to Planetary

Stewardship

Will Steffen, A ° sa Persson, Lisa Deutsch, Jan Zalasiewicz, Mark Williams, Katherine Richardson,

Carole Crumley, Paul Crutzen, Carl Folke, Line Gordon, Mario Molina, Veerabhadran Ramanathan,

Johan Rockstro¨m, Marten Scheffer, Hans Joachim Schellnhuber, Uno Svedin

Received: 29 June 2011 / Accepted: 29 June 2011

Abstract Over the past century, the total material wealth

of humanity has been enhanced. However, in the twentyfirst

century, we face scarcity in critical resources, the

degradation of ecosystem services, and the erosion of the

planet’s capability to absorb our wastes. Equity issues

remain stubbornly difficult to solve. This situation is novel

in its speed, its global scale and its threat to the resilience

of the Earth System. The advent of the Anthropence, the

time interval in which human activities now rival global

geophysical processes, suggests that we need to fundamentally

alter our relationship with the planet we inhabit.

Many approaches could be adopted, ranging from geoengineering

solutions that purposefully manipulate parts of

the Earth System to becoming active stewards of our own

life support system. The Anthropocene is a reminder that

the Holocene, during which complex human societies have

developed, has been a stable, accommodating environment

and is the only state of the Earth System that we know for

sure can support contemporary society. The need to

achieve effective planetary stewardship is urgent. As we go

further into the Anthropocene, we risk driving the Earth

System onto a trajectory toward more hostile states from

which we cannot easily return.

Keywords Earth System  Anthropocence 

Planetary stewardship  Ecosystem services  Resilience

PEOPLE AND THE PLANET: HUMANITY

AT A CROSSROADS IN THE TWENTY-FIRST

CENTURY

The twin challenges of ‘‘peak oil’’—decreasing petroleum

resources and increasing demand—and climate change are

redefining the pathways of human development in the

twenty-first century (Sorrell et al. 2009; ASPO 2010;

Richardson et al. 2011). Less well known is the potential

shortage of the mineral phosphorus and the increasing

competition for land—sometimes referred to as the ‘‘land

grab’’ in relation to Africa—as the new economic giants of

Asia move to secure food resources in non-Asian territories.

The pathways of development followed by today’s

wealthy countries after the Second World War—built on

plentiful, cheap fossil fuel energy resources, an abundance

of other material resources, and large expanses of productive

land to be developed—cannot be followed by the

75–80% of the human population who are now at various

stages of their trajectories out of poverty, and are beginning

to compete with today’s wealthy countries for increasingly

scarce resources.

A large fraction of our population of nearly 7000 million

people needs more access to food, water and energy to

improve their material standard of living, and the prospect

of an additional 2000 million by 2050 intensifies the need

for basic resources. These challenges come at a time when

the global environment shows clear signs of deterioration

and, as a consequence, questions the continuing ability of

the planet to provide the same accommodating environment

that has facilitated human development over the past

10 000 years.

Climate change is a prominent sign of human-driven

changes to the global environment. The evidence that the

Earth is warming is unequivocal, and human emissions of

greenhouse gases, most importantly carbon dioxide (CO2),

have been responsible for most of the warming since the

middle of the twentieth century (IPCC 2007). The manmade

greenhouse gases have already trapped enough

infrared energy to warm the planet by more than 2C

(Ramanathan and Feng 2008). Although many uncertainties

still surround the risks associated with climate change,

 Royal Swedish Academy of Sciences 2011

www.kva.se/en 123

AMBIO

DOI 10.1007/s13280-011-0185-x

impacts are already observable at today’s mean global

surface

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