Press Release: Increased climate change risk from methane…

17 April 2014

Increased climate change risk from methane suggested by proof of redox cycling of humic substances

• Reversible microbial redox cycling of humic substances shown to occur in anoxic environments

• Climate change may disrupt the process, leading to release large quantities of methane into atmosphere, so causing vicious circle of worsening climate change

Image credit: Klaus-Holger Knorr, University of Münster

The recent Yokahama IPCC meeting painted a stark warning on the possible effects of gases such as methane – which has a greenhouse effect 32 times that of carbon dioxide. Now a team of Swiss-German researchers have shown that humic substances act as fully regenerable electron acceptors which helps explain why large amount of methane are held in wetlands instead of being released to the atmosphere. However, there are worries that if this system is disrupted it may enter into a vicious cycle to release large amounts of methane back into the atmosphere.

Wetlands, such as peatlands, have a high content of organic-compound rich humic soils, which are formed during the breakdown of biological organisms such as plants. When water levels are high, these soils remain wet, and so are starved of oxygen, causing the organic compounds to accept electrons from respiring bacteria – rather like the charging of a giant battery. This prevents these electrons from being used by methane-forming bacteria, and so prevents these bacteria from releasing methane into the atmosphere.

The researchers now found that this giant electrical reaction can also go into reverse, like the charging and discharging of a giant battery. As water levels drop due to periodic variations in weather, then the humic soils will tend to release the electrons to oxygen forming harmless water. However, there is a danger is that climate change could lead to higher water levels, causing these soils remaining submerged for a greater period, and so and the discharging process disappears thus leading to more methane formation.

Potentially even worse, increasing global temperatures may cause permafrost to melt, leading to the soils being charged by microbial activity with electrons but not discharged. This could release vast quantities of methane from the wetlands. This in turn causes a greater greenhouse effect, and so on in a potentially vicious cycle.

One of the two lead researchers, Andreas Kappler (Tübingen), who is also the Secretary of the European Association of Geochemistry, said:

From a scientific point of view, our study is a step forward in understanding the geochemistry of how the humic material in the world’s wetlands store electrons and prevent the release of a massive amount of methane. It also shows that reversible electrochemical processes have the potential to have a large effect on the environment. There are uncertainties as to the exact extent, but we estimate anywhere between an extra 10% up to an extra 166% methane could be released. What it also shows is that these are fragile ecosystems and that slight changes in their geochemical conditions could have dramatic consequences for the environment.”

The world’s wetlands cover around 5% of the planet‘s ice-free land surface, meaning that they are roughly equivalent in size to Australia: but they have a disproportionate effect on the planet’s methane metabolism – contributing between 15 and 40% of the global methane flux into the atmosphere. Wetlands include areas such as marches, swamps, bogs, and fens, and in fact the largest wetlands in the world are swamp forests of the Amazon and the peatlands of Siberia.

Commenting on the potential climate effect, Professor Ralf Conrad (Marburg, Germany) said:

The study shows that humic substances can act as rechargable oxidants in flooded environments in the same way as it is known for inorganic nitrogen, sulfur, iron and manganese. Humic substances are ubiquitous constituents in the terrestrial biosphere and form a huge carbon reservoir. Now it has been shown that humic substances also control the microbially mediated electron flux in wetland ecosystems. This role has so far not been considered in models of global carbon cycling and climate change, but has a potentially great impact.”

This work has recently been published (see below*), but the European Association of Geochemistry wishes to highlight it because of its potential importance.


Notes for Editors

Please mention the European Association of Geochemistry in any press story.

*The paper describing this work was published in Nature Geoscience on 27 February 2014 (doi: 10.1038/NGEO2084, Humic substances as fully regenerable electron acceptors in recurrently anoxic environments. Authors: Laura Klüpfel, Annette Piepenbrock, Andreas Kappler1, and Michael Sander2.

The researchers confirmed that the results of the study need to be confirmed in larger scale, real world experiments, and that they needed better estimates of the amount of methane which can be bound or released by this method.

For more information please contact the EAG press officer, Tom Parkhill, at or on mobile phone +39 349 238 8181.

1Professor Andreas Kappler (EAG Secretary) can be contacted at

2Dr Michael Sander (Senior Scientist, Department of Environmental Systems Science, ETH Zurich, Switzerland) can be contacted at

Professor Ralk Conrad can be reached at

The European Association of Geochemistry is the major European society devoted to the study of the chemical and biochemical processes which shape the earth and other planetary bodies. The EAG website is at:

The EAG is a co-organiser of the forthcoming Goldschmidt conference (Sacramento, June 2014), see

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