The idea that humanity has driven the planet into a new geological epoch has been around for a century or more. But recently, it has begun to gain momentum.
Earth is about 4.5 billion years old. Geologists break this history down into blocks of time known as eras, epochs, periods, ages. Eras and epochs are usually separated by a major change.
The epoch we are in is the Holocene. It began as the last Ice Age began to shrink, around 12,000 years ago.
Modern humans first stepped out onto African plains 200,000 years ago. But it has only been during the Holocene that human civilization has developed.
Throughout our history, humans have had significant local effects on the environment. That has now changed. Since the industrial revolution in 1750 have humans have grown into a global force to be reckoned with.
The notion that we have entered a new epoch and that it should be known as the Anthropocene was first suggested in 2000 in an article appearing in the IGBP Global Change Newsletter. The authors of the article, IGBP Vice Chair at the time, Nobel Laureate Paul Crutzen, and Eugene Stoermer argued that Earth had recently crossed a threshold into a new epoch.
Crutzen followed this original article with a commentary in the journal Nature in 2002, the Geology of Mankind.
In this article Crutzen says, “The Anthropocene could be said to have started in the late Eighteenth century when analysis of air trapped in polar ice showed the beginning of growing global concentrations of carbon dioxide and methane.
In the video below, former IGBP Executive Director Will Steffen discusses the Anthropocene.
The planet is now dominated by human activities. Human changes to the Earth system are multiple, complex and interacting. They are often exponential in rate and globally significant in magnitude. They affect every Earth system component – land, coastal zone, atmosphere, cryosphere and oceans.
The human driving forces for these changes are equally complex, interactive and frequently teleconnected across the globe. The magnitude, spatial scale, and pace of human-induced change are unprecedented in human history and perhaps in the history of the Earth. The Earth system is now operating in a “no-analogue state”.
Until the industrial revolution humans and their activities played an insignificant force in the dynamics of the Earth system. Today, humankind has begun to match and even exceed nature in terms of changing the biosphere and affecting other facets of Earth system functioning.
The magnitude and pace of human-induced change are unprecedented. The speed of these changes is on the order of decades to centuries, not the centuries to millennia pace of comparable change in the natural dynamics of the Earth system.
Over the past two centuries, both the human population and the economic wealth of the world have grown rapidly. These two factors have led to a massive hike in consumption. We can see this in agriculture and food production, forestry, industrial development, transport and international commerce, energy production, urbanisation and even recreational activities.
Almost seven billion people now live on Earth. All share basic human needs: water, food, shelter, good health and employment. The ways in which these needs are met are critical determinants of the environmental consequences at all scales.
In the developed world, affluence, and more importantly the demand for a broad range of goods and services such as entertainment, mobility, and communication, is placing significant demands on global resources.
Between 1970 and 1997, the global consumption of energy increased by 84%, and consumption of materials also increased dramatically.
While the global population more than doubled in the second half of the last century, grain production tripled, energy consumption quadrupled, and economic activity quintupled.
Although much of this accelerating economic activity and energy consumption occurred in developed countries, the developing world is beginning to play a larger role in the global economy and hence is having increasing impacts on resources and environment.
Almost all activities in all countries demand energy. Fossil fuels provide the bulk of this energy, which leads to emissions of carbon dioxide, other trace gases and small particles (aerosols).
Industrialisation has led to considerable air and water pollution associated with the extraction, production, consumption and disposal of goods.
Over the past three centuries, the amount of land used for agriculture has increased five-fold.
Furthermore, large areas of land area have been lost to degradation, due, for example, to soil erosion, chemical contamination and salinisation.
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