Microbes have skins that react to the environment, much in the same way that our skin sweats when it is hot, or shivers when it is cold outside. Fossilized microbial skins can give us a glimpse of how the climate was in the deep geological past. By discovering the ‘missing link’ between such fossil skins and the skins of living bacteria, Diana Sahonero, a microbiologist at Royal Netherlands Institute for Sea Research (NIOZ), has greatly improved the accuracy of climate reconstructions and predictions.
Microbial skins are made out of lipids—fatty molecules—which can be preserved as fossils telling us stories about how these microbes lived in the past. “Some microbial lipids are widely used to reconstruct past climates. They have always been surrounded by mystery, as we did not know which microbes were making them and under which conditions. This lack of information limits the predictive power of these molecules to reconstruct past environmental conditions,” says Sahonero.
Now, her study shows which bacteria make these lipids and also how they have evolved their lipid skin to adapt to environmental changes—another step towards reconstructing and predicting climate change in more detail.
Lipids form the membrane of a microbe. Image: Diana Sahonero, NIOZ. © Diana Sahonero, NIOZ
Climate reconstructions
Lipids, the molecular building blocks of the cell membrane, are unique for each microbial species. “It works just like fingerprints, they can be used to identify microbial remains,” says Laura Villanueva, associate professor in the Faculty of Geosciences in Utrecht University and senior scientist at NIOZ.
The lipids of ancient microbes can be found in old sediments. Once these molecules from the past are separated, identified and related to currently living groups of bacteria, the lipids can work like ‘biomarkers’. These markers can tell us about the atmospheric and oceanic conditions of the ancient earth, because we know from the living relatives of the microbes how they interact with their environment.
Set-up of the growth experiments in serum bottles without oxygen for obtaining samples for omics analysis (lipidomic, transcriptomic and proteomics). Photo: Diana Sahonero, NIOZ. © Diana Sahonero, NIOZ
Who made these molecules and how?
For long, it was unclear precisely which bacteria were making these specific lipids, called branched Glycerol Dialkyl Glycerol Tetraethers (GDGTs). This type of lipids are often used in climate reconstructions. Diana and her colleagues have finally discovered the bacteria forming these lipids. And also how these bacteria actually make the lipids.
“It was like looking for a needle in a haystack”, says Sahoreno. “From the start, we knew we had to answer this question with a massive approach. We needed to investigate more than 1850 proteins to identify microbes making these lipid molecules.”
Once researchers know which currently living bacteria make these lipid molecules, they can be used to make more accurate climate reconstructions. Researchers can measure the interactions of these living bacteria with their surrounding seawater or atmosphere. This information leads to ‘proxies’—keys to correlate details of the lipid molecules (abundance for instance) to values of the environment. This is an important step in reconstructing past environmental and climate conditions, based on old sediment samples.
Set-up of the growth experiments in serum bottles without oxygen for obtaining samples for omics analysis (lipidomic, transcriptomic and proteomics). Photo: Diana Sahonero, NIOZ. © Diana Sahonero, NIOZ
Early evolution of life
“Our study indicates that there are many species of currently living bacteria that can make these type of membrane lipids. Also, we found that those bacteria are all limited to environments where oxygen is absent,” says Sahonero.
“This study into archaeal-like lipids of bacteria shows how this group of microbes that produces them evolved their lipid membrane billions of years ago. It is fantastic to get a glimpse of this part of life’s history. It was mostly a mystery until now.”
What next?
The work of Sahonero and her colleagues is still ongoing. “Now we know which bacteria form these molecular building blocks and we understand how they do that. Next, we need to find out how the production of these molecules depends on environmental factors like water temperature or pH,” says Villanueva. “Then, the proxy based on these bacterial lipids can be used more confidently by (paleo)climatologists. This gives them new possibilities to reconstruct and predict climate change in more detail.”
The research was published in Science Advances.
More information:
Laura Villanueva et al, Disentangling the lipid divide: Identification of key enzymes for the biosynthesis of membrane-spanning and ether lipids in Bacteria, Science Advances (2022). DOI: 10.1101/2022.04.21.487849v1
Provided by
Royal Netherlands Institute for Sea Research
Citation:
Linking fossil climate proxies to living bacteria helps climate predictions (2022, December 16)
