Study finds reduced feeding activity of soil detritivores under warmer and drier conditions

December 21, 2017, German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig
Woodlice (isopods) are important detrivores in the soil. Credit: Sarah Zieger

When the soil warms up, it releases more carbon dioxide (CO2)—an effect that fuels climate change. Until now, it had been assumed that this was mainly due to the presence of small soil-dwelling animals and microorganisms that would eat and breathe more in warmer temperatures. However, a new study in Nature Climate Change has shown that this is not the case. If warmth is accompanied by drought, the soil animals eat even less. In order to improve the predictive power of climate models, it is now crucial to understand biological processes in the soil better, say the scientists.

The fact that the world's is changing is mainly due to the burning of fossil fuel. As a consequence, large quantities of (CO2) are released into the Earth's atmosphere. However, additionally, climate change is also intensifying on its own, because global warming is also causing the natural carbon cycle to change. Although on Earth, carbon is constantly converted from solid compounds into gaseous CO2 and vice versa, warmer temperatures can enhance carbon losses in form of CO2 from the . As a result, more CO2 is introduced into the Earth's atmosphere: a positive feedback.

Scientists had previously assumed that this effect was mainly due to the presence of small animals and microorganisms in the soil, which feed on dead organic matter (for example, fallen leaves). Because when they 'burn' their food, CO2 is released ('respiration'). It was assumed that at warmer temperatures, insects and worms with decomposing roles would eat more, and the dead organic matter in the soil would be decomposed at faster rates. After all, these animals are poikilotherms whose body temperature and activity depend on the environment.

Bacteria and unicellular fungi in the soil should also be more active at warmer temperatures, based on the current understanding. But now, a new study questions this assumption. A team of researchers led by the German Centre for Integrative Biodiversity Research (iDiv) and Leipzig University carried out an experiment to simulate the warming of the soil in the forest and discovered that the warmer temperatures have no influence on the feeding activity of the . When the researchers simulated a second effect of climate change in addition to warming, namely drought, the results were the opposite of expectations: The soil animals ate less, and the microorganisms living in the soil showed a decline in respiration—an indication that they also consumed less food.

The scientists used so-called bait lamina strips to measure how much the soil animals were eating. Credit: Julia Siebert

Dr. Madhav P. Thakur, first author of the study, explains why these results are of great relevance: "The feedback effect of climate warming via the greater release of CO2 from the soil is a crucial assumption in models predicting our future climate. Therefore, it is important to know what it causing this effect. Our results indicate that it may not be the soil animals, on the contrary: Their role may actually be the opposite of what we expected, at least when warming and drought occur together."

Professor Nico Eisenhauer, the senior author of the study, says, "It is most likely that instead of soil animals and microorganisms, the plants are responsible for the feedback effect because they also breathe with their roots. In order to improve the validity of , we now urgently need to understand the in the soil better." After all, soil is the major reservoir of carbon on earth, the scientist says.

With these heating elements the scientists warmed up the soil in the forests in the B4WarmED experiment. Credit: Artur Stefanski

The study was conducted as part of a long-term experiment in Minnesota, U.S. In the Boreal Forest Warming at an Ecotone in Danger (B4WarmED) experiment, scientists are heating plots of boreal forest land artificially by 3.4°C. In addition, they also reduce rainfall by 40 percent in some places by setting up tents in rainy weather. The scientists measured how much the soil animals ate using bait lamina strips: small sticks with holes the researchers filled with substrate that resembled the organic matter in the soil. These sticks were stuck deep into the ground. Every two weeks, the scientists checked how much of the substrate was eaten. The researchers carried out more than 40 such measurements over a period of four years. It is the first study of this scale to investigate the effects of and drought on decomposer soil . In addition, the researchers checked the respiration of soil microorganisms by excluding plant roots with a metal ring in small soil areas and then measuring how much CO2 was released from the soil with a gas analyser.

Explore further: Carbon feedback from forest soils will accelerate global warming, 26-year study projects

More information: Madhav P. Thakur et al, Reduced feeding activity of soil detritivores under warmer and drier conditions, Nature Climate Change (2017). DOI: 10.1038/s41558-017-0032-6

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