A new study, which has been published in the journal Anthropocene, examines the evidence that we now live in the Anthropocene, an epoch where humans dominate the Earth's surface geology, and suggests that the surface of the planet is being noticeably altered by the production of long-lasting human-made materials, resulting in us entering an 'Age of Plastic'.
Jan Zalasiewicz, Professor of Palaeobiology from the University of Leicester's Department of Geology explained, "Plastics were more or less unknown to our grandparents, when they were children. But now, they are indispensable to our lives. They're everywhere -wrapping our food, being containers for our water and milk, providing cartons for eggs and yoghourt and chocolate, keeping our medicines sterile. They now make up most of the clothes that we wear, too.”
"Plastics are also pretty well everywhere on Earth, from mountain tops to the deep ocean floor -and can be fossilized into the far future. We now make almost a billion tons of the stuff every three years. If all the plastic made in the last few decades was clingfilm, there would be enough to put a layer around the whole Earth. With current trends of production, there will be the equivalent of several more such layers by mid-century."
The study suggests that plastics have such a long-lasting impact on the planet's geology because they are inert and hard to degrade. As a result, when plastics litter the landscape they become a part of the soil, often ending up in the sea and being consumed by and killing plankton, fish and seabirds.
Plastics can travel thousands of miles, caught up in the 'great oceanic garbage patches', or eventually being washed up on distant beaches. Plastics can eventually sink to the sea floor, to become a part of the strata of the future.
The rise of plastics since the mid-20th century, both as a material element of modern life and as a growing environmental pollutant, has been widely described. Their distribution in both the terrestrial and marine realms suggests that they are a key geological indicator of the Anthropocene, as a distinctive stratal component.