When a plant dies, its leaves and branches fall to the ground. Decomposition¹ of soil organic matter is then mainly carried out by fungi² and bacteria, which convert dead plant materials into carbon dioxide and mineral nutrients³. Until now, scientists have thought that high quality organic materials, such as leaves that are rich in soluble⁴ sugars, are mainly decomposed⁵ by bacteria. Lower quality materials, such as cellulose and lignin that are found in wood, are mainly broken down by fungi. 

 

Previous research has also shown that organic material that is broken down by fungi results in a reduced leakage⁶ of carbon dioxide and nutrients compared to material decomposed by bacteria. 

 

This has consequences for climate models, since more loss of carbon dioxide and mineral nitrogen would have a direct bearing on the soil's contribution to greenhouse gases and eutrophication.

 

In a 23-year experiment, researchers from Lund University and USA have examined the relative significance of fungal and bacterial⁷ decomposition.

 

"In contrast with expectations, there was no evidence that high quality organic material was mainly broken down by bacteria. In fact, the data strongly suggested the contrary", says Johannes Rousk, researcher in Microbial Ecology at Lund University in Sweden.

 

"There was also no evidence to suggest that organic material broken down by fungi reduced the leakage of carbon dioxide into the atmosphere, or the leakage of nutrients. Once again, the results tended to suggest the contrary", says Johannes Rousk.

 

The results could have consequences not only for future climate models, but may also impact current policies on land use intended to promote fungi. This may be based on flawed assumptions regarding the fungal role in reducing negative environmental effects.

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