fcb6d20346f86f6804396700_dr3397c.jpg Dean Rohrer

Can We Survive the “Anthropocene” Period?

For the past three centuries, humans’ effects on the global environment have escalated. The consequences are numerous and profound: acid precipitation, photochemical “smog,” and global warming being the most widely acknowledged - but that's just the start.

For the past three centuries, humans’ effects on the global environment have escalated. Most importantly, our emissions of carbon dioxide may cause global climate patterns to depart significantly from their natural course for many millennia to come.

It seems appropriate to assign the term “Anthropocene” to the current, in many ways human-dominated, geological epoch, supplementing the Holocene – the warm period of the past 10–12 millennia. The Anthropocene Period could be said to have started in the latter part of the eighteenth century, when analyses of air trapped in polar ice showed the beginning of growing global concentrations of CO2 and methane. This date also happens to coincide with James Watt’s design of the steam engine in 1784.

Mankind’s growing influence on the environment was recognized as long ago as 1873, when the Italian geologist Antonio Stoppani referred to the “anthropozoic era,” defined by a “new telluric force, which in power and universality may be compared to the greater forces of earth.”

In 1926, V. I. Vernadsky similarly acknowledged the increasing impact of mankind on “[t]he direction in which the processes of evolution must proceed, namely towards increasing consciousness and thought, and forms having greater and greater influence on their surroundings.” Vernadsky and Teilhard de Chardin used the term “noösphere” – the world of thought – to mark the growing role of human brain-power in shaping its own future and environment.

Humans’ rapid expansion in terms of population and per capita use of Earth’s resources has continued apace. During the past three centuries, the human population has increased ten-fold, to more than six billion, and is expected to reach 10 billion in this century. As a result, 30–50% of the planet’s land surface is now exploited by humans.

At the same time, the methane-producing cattle population has risen to 1.4 billion, contributing to the increasing rate of destruction of tropical rainforests, which releases carbon dioxide and contributes to faster species extinction. Land conversion for grazing (and construction), together with crop tillage, has also caused soil erosion at 15 times its natural rate. Indeed, at its current pace, anthropogenic soil erosion would fill the Grand Canyon in 50 years.

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Similarly, dam building and river diversion have become commonplace, as humans’ water consumption has risen nine-fold over the past century, to the point that mankind now uses more than half of all accessible fresh water – roughly two-thirds of it for agriculture. Fisheries remove more than 25% of the primary production in upwelling ocean regions and 35% in the temperate continental shelf.

Moreover, energy use has grown 16-fold during the twentieth century, causing 160 million tons of atmospheric sulfur-dioxide emissions per year – more than twice the total of natural emissions. Likewise, more nitrogen fertilizer is applied in agriculture than is fixed naturally in all terrestrial ecosystems, and nitric-oxide production from the burning of fossil fuels and biomass also surpasses natural emissions.

At the same time, of course, human consumption of fossil fuels, together with our agricultural activities, have caused substantial increases in concentrations of “greenhouse” gases – CO2 by 30% and methane by more than 100%. Indeed, these concentrations are higher than at any point in the past 400 millennia, with more growth to follow, because so far these effects have largely been caused by only 25% of the world population.

The consequences are numerous and profound: acid precipitation, photochemical “smog” and global warming, among others. Hence, according to the latest estimates by the Intergovernmental Panel on Climate Change (IPCC), Earth will warm by 1.4–5.8 °C during this century. Many toxic substances are released into the environment, even some that are not toxic but nonetheless are highly damaging – for example, the chlorofluorocarbons that caused the Antarctic ozone hole (and which are now regulated).

Things could have become much worse: the ozone-destroying properties of halogens have been studied since the mid-1970’s. If it had turned out that chlorine behaved chemically like bromine, the ozone hole would by then have been a global, year-round phenomenon, not just an event of the Antarctic spring. More by luck than by wisdom, this catastrophic situation did not develop.

Unless there is a global catastrophe – a meteorite impact, a world war, or a pandemic – mankind will remain a major environmental force for many millennia. As a result, scientists and engineers face a daunting task during the Anthropocene era: to guide us towards environmentally sustainable management. This will require appropriate human behavior at all levels, and may well involve internationally accepted, large-scale geo-engineering projects to “optimize” climate. At this stage, however, we are still largely treading on terra incognita .