Author: Daisy Dunne | Published: August 25, 2017
The study, which maps where soil carbon has been lost and gained since 10,000BC, shows that crop production and cattle grazing have contributed almost equally to global losses.
Understanding how agriculture has altered soil carbon stocks is critical to finding ways to restore lost carbon to the ground, another scientist tells Carbon Brief, which could help to buffer the CO2 accumulating in the atmosphere.
Soil as a carbon sink
The top metre of the world’s soils contains three times as much carbon as the entire atmosphere, making it a major carbon sink alongside forests and oceans.
Soils play a key role in the carbon cycle by soaking up carbon from dead plant matter. Plants absorb CO2 from the atmosphere through photosynthesis, and pass carbon to the ground when dead roots and leaves decompose.
But human activity, in particular agriculture, can cause carbon to be released from the soil at a faster rate than it is replaced. This net release of carbon to the atmosphere contributes to global warming.
New research, published in the Proceedings of the National Academy of Sciences (pdf), estimates the total amount of carbon that has been lost since humans first settled into agricultural life around 12,000 years ago.
The research finds that 133bn tonnes of carbon, or 8% of total global soil carbon stocks, may have been lost from the top two metres of the world’s soil since the dawn of agriculture. This figure is known as the total “soil carbon debt”.
Around two-thirds of lost carbon could have ended up in the atmosphere, while the rest may have been transported further afield before being deposited back into the soil.
And since the industrial revolution, the rate of soil carbon loss has increased, says lead author Dr Jonathan Sanderman, a scientist at the Woods Hole Research Center in Massachusetts. He tells Carbon Brief:
“Considering humans have emitted about 450bn tonnes of carbon since the industrial revolution, soil carbon losses to the atmosphere may represent 10 to 20% of this number. But it has hard to calculate exactly how much of this has ended up in the atmosphere versus how much has been transported due to erosion.”
‘Hotspots’ for carbon loss
As part of the study, the researchers designed an artificially intelligent model that used an existing global soil dataset to estimate past levels of soil carbon stocks, Sanderman says.
“We used a dataset which defines 10,000BC as a world without a human footprint. What we did was develop a model that could explain the current distribution of soil carbon across the globe as a function of climate, topography [physical features], geology and land use. Then we replaced current land use with historic reconstructions including the ‘no land use’ case to get predictions of soil carbon levels back in time.”
To calculate an overall soil carbon debt, the researchers subtracted the amount of current global soil carbon from the amount of soil carbon predicted to have existed in the era before human agriculture. The model also allowed the researchers to estimate global soil carbon stocks at different points throughout history, including at the advent of the industrial revolution.
The results allow scientists to get a clearer picture on how 12,000 years of human agriculture have affected the world’s soil stocks, says Sanderman.
“More carbon has been lost due to agriculture than has generally been recognised and a lot of this loss predated the industrial revolution. This loss isn’t equally distributed across agricultural land. Some regions stand out as having lost the most carbon.”
Map B below shows the regions that have experienced the most soil carbon loss, and includes the US corn belt and western Europe. The red shading represents the very highest level of soil carbon loss since 10,000BC, while blue shows the highest level of carbon gain.
The US corn belt and western Europe are likely to have experienced high levels of soil carbon loss as a result of long periods of intense crop production, says Sanderman.
However, the analysis also reveals a number of regions which have seen high levels of soil carbon loss despite having relatively little farming. These “hot spots” – including the rangelands of Argentina, southern Africa and parts of Australia – are considered to be particularly vulnerable to land degradation driven by agriculture, says Sanderman.
“Semi-arid and arid grasslands [the hotspots] are particularly vulnerable to potentially irreversible degradation if grazing intensity is too high. That’s because there isn’t a lot of soil carbon to start with and there can often be a complete shift in vegetation cover leading to lots of erosion.”
Map A shows the distribution and intensity of crop production (red) and cattle grazing (green) across the world. Both have contributed almost equally to loss of soil carbon stocks, Sanderman says.
