Microbiologist Laura Villanueva studies the membranes that surround microbes. ‘A microorganism’s membrane is effectively its skin. Just like our skin, the membrane responds strongly to the environment. Our skin becomes darker if more sunlight falls on it or shivers if it is cold. Similarly, changes also take place in the membranes of microorganisms. These can tell you something about the climate under which the organism is living or has lived.’
‘In particular, the possibility to derive conditions from the past based on the composition of a membrane offers many interesting possibilities. By searching for fossils of membranes in seafloors – the lipid molecules from these membranes can remain intact for millions of years – we can learn what the sea temperature was in a certain period. However, to do that we first need to investigate “modern” species to find out how their composition changes when allowed to grow at different temperatures. Ultimately, this research could contribute to understanding the earth’s climate in the past and therefore to prognoses for the climate of the future.’
From an evolutionary viewpoint, I am particularly interested in the “archaea”, more commonly known as ancient bacteria. This is a separate domain of unicellular organisms that can survive under extreme conditions. By searching for archaea that can live at considerable depth without oxygen and under extreme pressure, or under extreme temperatures in the vicinity of hot water springs, I also hope to learn what that does to the composition of their membranes.’
‘The study of membranes also has particularly practical applications. Some medicines can only be delivered to the right location in the body if the active substances are packaged in the right membrane. So besides understanding the climate from the past and the present, membranes can also teach us something about how we can improve medicines.’
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Molecular Geomicrobiology is the molecular level understanding of microbial activities both in past and present ecosystems. I combine molecular microbiology & organic biogeochemistry techniques to determine:
The re-mineralization of organic matter in anoxic sediments is mainly driven by fermentative microorganisms, sulfate reducers, and methanogens. However, there is a general lack of knowledge on the diversity, abundance and activity of the anaerobic microorganisms involved (directly or indirectly) in organic matter recycling in anoxic sediments.
Methanogens (strictly anaerobic archaea) biologically produce methane, a trace greenhouse gas in the earth’s atmosphere the concentration of which has doubled since industrialization. On its way to the atmosphere, methane travels through anaerobic sediments, passing through zones dominated by different regimes of anaerobic respiration before reaching the aerobic sediment or oxic water column. Along this route methane can be oxidized, which significantly decreases/mitigates the effective emission of this greenhouse gas to the atmosphere. However, it is unclear how ecosystems to different physicochemical conditions with respect to methane production, consumption and thus ultimately emissions to the atmosphere.
Our aim is to improve our understanding of the microbial players involved in anaerobic organic matter remineralization and also specifically focus on those involved in the methane cycle. We also want to assess their individual niches, metabolic pathways, environmental significance, interactions, and their response to environmental changes. Ultimately this information will be key to explore their potential use in biotechnology and to design mitigation strategies for greenhouse gas emission.
This research is conducted in the framework of the Soehngen Institute for Anaerobic Microbiology SIAM (Gravitation grant- Zwaartekracht, from the Dutch Ministry of Education, Culture and Science, read more here) in which the Radboud University, Wageningen University, Delft University of Technology, and NIOZ Royal Netherlands Institute for Sea Research participate.
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