News Release

Newly discovered microbial communities beneath the Atacama Desert

Thanks to a new technique of molecular DNA analysis, viable microbes have been detected down to depths of 4.20 metres. This also has implications for the search for life on other planets.

Peer-Reviewed Publication

GFZ GeoForschungsZentrum Potsdam, Helmholtz Centre

The Yungay-Playa

image: 

The Yungay-Playa, one of the driest areas in the Chilean Atacama Desert.


 

view more 

Credit: Photo: D. Wagner, GFZ

Summary

For a long time, the extremely dry soils of the Chilean Atacama Desert were considered completely lifeless. In one of its driest regions, a team of scientists around Lucas Horstmann and Dirk Wagner from the GFZ German Research Centre for Geosciences, together with colleagues from the TU Berlin and the University of Antofagasta, Chile, has now uncovered a previously unexplored underground habitat. This was based on newly developed methods of molecular DNA analysis, which allow the focussed extraction and analysis of intracellular DNA. This comes from intact cells of living or dormant organisms, making it possible to detect viable and potentially active microbial communities which inhabit hyperarid soils down to a depth of 4.20 metres. The study, published in the journal PNAS Nexus, thus expands our understanding of biodiversity of a region where extreme conditions of drought, salinity and nutrient deficiency are close to the limits of life. The results also have implications for the search for life on other planets.

Background: The extreme desert habitat

Deserts are one of the largest and most fragile ecosystems on Earth. Although the conditions there are among the harshest and most life-threatening, they harbour microbial life. In the absence of regular rainfall, microorganisms are the most important ecological component mediating nutrient flows by utilising soil components such as minerals and salts as well as atmospheric gases as a source of energy and water.

“The study of microbial diversity and distribution is crucial to fully understand the central role of microbial processes in maintaining the ecological balance and functionality of desert ecosystems, especially in regard of their future development in the context of climate change,” says Dirk Wagner, head of the GFZ Geomicrobiology Section and one of the leaders of the study.

The 105,000 square kilometre Atacama Desert in northern Chile is considered the driest hot desert in the world. It is therefore an extremely relevant and suitable location for research into this habitat. Shallow areas down to a depth of around one metre have already been investigated. Here we know that it is a niche habitat that protects against UV radiation and where water is still available so that microbial life can thrive.

New approach: analysing deep soils in the Atacama Desert with special DNA analysis

The deeper layers of desert soils, on the other hand, have only been analysed in a few studies to date. They were therefore the focus of a team led by Lucas Horstmann, PhD student, and Daniel Lipus, post-doctoral researcher, both in the GFZ Geomicrobiology Section, and Dirk Wagner, head of the same section and Professor of Geomicrobiology and Geobiology at the University of Potsdam. Other colleagues came from the TU Berlin and the University of Antofagasta in Chile. The researchers wanted to test whether the deeper sediments of the hyperarid Atacama Desert could also be a habitat for specialised microbes.

The research team studied a soil profile in the Yungay area, about 60 kilometres south-east of Antofagasta, to analyse the microbial diversity and its interaction with soil properties along a depth profile that included both the sediments of the playa and the alluvial fan deposits below, reaching down to a depth of 4.2 metres. To do this, they dug a soil profile and took soil samples every 10 centimetres down to a depth of three metres, then every 30 centimetres, which were taken to the GFZ laboratories for analysis.

In order to detect traces of life in the samples, the scientists used a new technique of molecular DNA analysis, which was developed by Dirk Wagner and others at the GFZ: Using a special extraction method, it is possible to filter out only intracellular DNA from a sample, i.e. DNA that originates from intact and potentially active cells. Various chemicals, centrifuges and filters are used for this.

“This approach represents a significant improvement for studies on microbial diversity in extreme environments, as it effectively excludes bias generated by the DNA from dead cells and still provides valid data even when the detection limit for other methods has been reached due to the low amount of biomass,” emphasises Wagner. 

Discovery of a potentially viable microbial community down to a depth of 4.2 metres

Through intracellular DNA extraction and subsequent gene sequencing of the samples, the researchers were able to identify potentially viable microbes down to a depth of 4.2 metres. In the upper 80 centimetres, they mainly found microbes of the Firmicutes phylum, but their numbers decreased with increasing depth and thus also increasing amounts of soluble salts. The researchers suspect that the high salt concentration and increasing water scarcity could also be responsible for the fact that the microbial colonisation in the lower part of the playa sediments ceases. In this respect, their findings are consistent with earlier studies.

However, Horstmann and Wagner's team once again discovered a microbial community in the alluvial fan deposits below two metres. It is more diverse than the surface community and is probably completely isolated from the surface. It consisted mainly of bacteria belonging to the phylum Actinobacteriota, a group with specialised members that are often found in dry or pristine soils.

The existence of these microbes could be related to the presence of vesicular gypsum, which may provide an alternative water source by dissolving into anhydrite. The organisms observed in this study belonged to species that can use trace gases such as hydrogen as an energy source to utilise CO2 as a carbon source for their growth.

“This type of metabolism, called chemolithoautotrophy, has been suggested in other studies to be important for hyper arid soils where organic matter is extremely limited as a carbon source. It therefore, could also be essential for the isolated subterranean niches investigated in this study,” says first author Lucas Horstmann.

Summary and outlook: Astonishing desert biodiversity and implications for extraterrestrial life

Horstmann concludes: “The discovery of this subsurface community, which thrives in alluvial fan sediments below two metres depth and shows an astonishing diversity and ecological stability, challenges our current understanding of desert ecosystems.”

The authors suggest that this community might have colonized the soil already 19,000 years ago, before its burial by playa deposits, and hypothesize that it could continue downwards for an unknown distance, representing a previously unknown deep biosphere under hyper-arid desert soils.

“Given the wide distribution of drylands on our planet, the presence of potentially carbon-binding communities in previously unexplored subsurface soils has profound implications not only for biodiversity in deserts, but also for element cycling on a global scale,” says co-author Dirk Wagner. “This indicates that the importance of these habitats has been underestimated so far. And it emphasises the importance of subsurface habitats for a comprehensive understanding of desert ecosystems in the future.”

The researchers emphasise that the results of this study not only have implications for our planet Earth, but are also relevant to ongoing discussions about the search for life on other planets: “The presence of gypsum deposits on Mars, similar to those found in alluvial fan sediments, is of great interest to astrobiology. The association of these subsurface communities with gypseous substrates in the Atacama may provide further evidence that gypsum deposits on Mars not only indicate the possibility of liquid water in the past, but could also serve as a habitable niche for microbial life in the present.”

 


Disclaimer: AAAS and EurekAlert! are not responsible for the accuracy of news releases posted to EurekAlert! by contributing institutions or for the use of any information through the EurekAlert system.