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Geomicrobiology

This Project Page presents the scientific work I have done in the field of Geomicrobiology

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Chemodenitrification

Press release Tübingen University - 2019

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written by Dr. Karl Guido Rijkhoek

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Press release:

Coastal marine sediment contribute to the formation of greenhouse gases

From Dr. Karl Guido Rijkhoek

University of Tübingen research team investigates microbial and chemical processes as a natural source
of laughing gas


Nitrous oxide – or laughing gas – is a greenhouse gas nearly 300 times as harmful as carbon dioxide. Much of it is
released by human activity, for example from fertilizers and in vehicle and industrial exhaust. But there are natural
sources of nitrous oxide, too. For a long time, scientists had little idea of all the processes which lead to the formation of
nitrous oxide or their magnitude. Now, a team of geomicrobiologists, headed by Professor Andreas Kappler and Dr.
Caroline Schmidt, from the University of Tübingen’s Center for Applied Geoscience has identified an important source of
nitrous oxide which is harmful to the environment. The team discovered that it is not solely bacterial activity which
causes laughing gas formation – it is also due to chemical processes in coastal marine sediments. This source may well
be responsible for the production of up to one quarter of all nitrous oxide formation. It is important to find out more
about how climate-damaging gases are produced – and in what amounts – if we want to properly assess future climate
developments. The study is published in the latest edition of Scientific Reports.


"Previously, it was assumed that nitrous oxide was mainly created as an intermediate product in the conversion of
nitrate by bacteria in typical coastal marine sediments," says Andreas Kappler. However, this did not explain the full
extent of the formation of laughing gas. Unexplained sources of nitrous oxide had been reported in various studies of
natural systems such as river sediments and soils in rice fields. In the new study, the team took coastal sediment
samples from the Danish Baltic Sea and simulated environmental conditions in artificial microcosms in the laboratory.
In this controlled experiment, the different nitrous oxide formation process could be identified and quantified.
Microorganisms only produce the ingredients
.


This study showed that chemical denitrification is responsible for a considerable part of nitrous oxide production.
Denitrification refers to the microbial conversion of nitrogen bound in nitrate into molecular nitrogen and nitrous oxide.
"The raw materials for chemodenitrification, ferrous iron and nitrite, are formed by microbial processes in the
sediment," explains Caroline Schmidt. However, microbes play no part in the conversion to nitrous oxide. The chemical
reaction takes place spontaneously. "Laughing gas is produced and released extremely quickly," Schmidt says. The
extent to which laughing gas is formed as a result of this reaction could explain its mysterious origin.
"We need to understand all the man-made and natural sources of greenhouse gases to be able to assess future climate
developments," Kappler says. Schmidt adds: "The study illustrates how processes on the smallest scale – interactions
between microorganisms and sediment chemistry – can have massive effects on global environment phenomena such
as greenhouse gas emissions.”

01

Sterilization of microbes

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02

Chemodenitrification in marine sediment

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03

Distribution of iron-cycling microbes in sediment

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04

Cable bacteria

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