Humans change their environment. Today this is a determining factor for the entire geosystem – from climate change to biodiversity. But is that enough for us to speak of a “geological epoch of humans”, the Anthropocene, (from Ancient Greek ánthropos, meaning man)?
“Stop using the word Holocene. We’re not in the Holocene any more. We’re in the Anthropocene!” With these words atmospheric chemist Paul Crutzen interrupted a conference in 2000. But what was the Nobel prize laureate and discoverer of the hole in the ozone layer making such a fuss about?
Holocene is the name of the epoch in the Earth’s history that started 11,700 years ago with the end of the last Ice Age. The climate in this period was unusually stable. Many scientists think that’s a key requirement for the development of human civilisations. But that seems to be where it ended: since the beginning of industrialisation the global average temperature has risen significantly. The vast majority of scientists are convinced that the reasons for this lie in human action, including intensive agriculture, the global growth economy and increasing traffic.
The Great Acceleration
Humans have been engaging with their local environment for thousands of years. Large-scale use of fossil fuels began with the Industrial Revolution in around 1800. But it’s only since the 1950s that the influence of humans has been developing much faster than ever before all over the world. That’s why many Anthropocene researchers consider the beginning of the “Age of Humans” to be the mid-20th century: the world population is growing as fast as the use of fossil energy. And along with that the amount of the greenhouse gas carbon dioxide (CO2) in the atmosphere. This development is referred to as the “Great Acceleration”.
Further information on the “Great Acceleration” is available from the interactive dossier “Anthropocene” from the Bundeszentrale für politische Bildung (Federal Agency for Civic Education; bpb).
Did you know?
1 in a thousand | Bananas
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There are many different varieties of banana, but not all are edible. In total cultivated forms of bananas and plantains account for more than 1000 hybrids and variants. But in Europa and the USA you often find just one particular variety: “Cavendish”. This banana tastes very mild. It’s harvested green and can therefore be transported easily – so it’s practical for the export trade.
In Germany as well as in Europe there’s an ever-decreasing number of birds. Bird species that live in agricultural environments are particularly under threat. The number of breeding pairs in agricultural regions in the European Union dropped by 300 million between 1980 and 2010.
80 per cent | Mobile phone “junk”
Around 200 million old mobile phones are lying around unused – in German households alone. Each one contains around 60 different substances that are far too valuable to waste: copper, aluminium and gold, scarce metals such as cobalt and tungsten, and around 17 of the “rare earths” that are so important to technology. Around 80 per cent of the components of old telephones could be reused.
35 per cent | Microplastics
Microplastics are everywhere. Plastic particles are for instance released from clothing during washing. 35 per cent of the microplastics in the oceans come from that source. Discarded plastic packaging breaks up into increasingly tiny particles, but only disappears completely after centuries. There are even microplastics in the air – the wind spreads it all around the world.
300 years | Phosphate fertiliser
Without phosphorus, nothing can live – no people, no animals and no plants. That’s why phosphate fertilisers are very important in agriculture. According to current estimates, global reserves will last for at least another 300 years. However, we should be considering right now how to handle this finite resource.
0.04 per cent | CO2
Carbon dioxide only accounts for 0.04 per cent of the air volume. But it has a special property: it allows short-wave solar radiation to pass through the Earth’s atmosphere and at the same time it prevents the long-wave heat rays from escaping into space. As a result the Earth is heating up. That’s why they call it a “greenhouse gas”. CO2 is not the only greenhouse gas, but it’s a very important one.
Composition of the air: nitrogen around 78 %, oxygen around 21 %, argon 0.93 %, carbon dioxide 0.04 %, other gases at trace level.
1.5 degrees | Meat
What can we do to slow down global warming? Eating significantly less meat would be a start. The biggest problem for the climate in this context is cattle farming. The animals need a lot of feed, which has to be cultivated on large areas of land using fertiliser and water. And: when cows chew the cud, they belch out methane, a greenhouse gas.