Bacteria can survive multiple extreme conditions. However, as a rule, these microorganisms need a steady source of carbon and oxygen or some other oxygen alternative in the case of anaerobic bacteria.
Such sources are rare in some regions of the world – for example, in-depth of the ocean. The lowest levels of the seafloor are often referred to as low productivity areas as there is almost no access to sunlight or potential nutrients. Nevertheless, colonies of bacteria can be found even there.
A team of Japanese researchers has decided to study the area called South Pacific Gyre[7] . This area is sometimes called a “biological desert “. It is located very far from all continents. This area is said to have some of the most transparent water on the planet – and that is not a good thing for supporting life.
This part of the ocean is low on nutrients and chlorophyll, which means a low chance of photosynthesis . Considering how little food the upper layers of water contain, the ocean floor has even fewer feeding opportunities. There is also an added pressure of water above.
The scientists have taken probes from this ocean floor, composed of various sediments – a material made from multiple dead organisms and particles falling down on the ocean floor. The analysis of these sediments has shown that:
There were bacterial cells trapped in the sediments. As the pores in the sediments were microscopic, the access to oxygen and other nutrients for the bacteria was very low. The bacteria were probably trapped millions ago – as the sediment itself was dated to be around 100 million years old. The quantity of the trapped bacteria was low – around 1000 microbial cells per probe. There were two types of bacteria present: those that rely on oxygen (aerobic) and that live without oxygen (anaerobic). When aerobic bacteria were put into a nutritive medium, they could grow and divide quickly. As a result, their colonies grew about 4 times in size. Anaerobic bacteria had minimal growth in their own media. These new data show that aerobic bacteria can grow in extremely poor conditions and under high pressure for a million years and still retain their ability to divide and grow if the conditions change.
This discovery has long-term implications, as global warming can cause the release of such bacteria from ice or ocean floor, and the properties of these microorganisms are unknown.
Sources
Reference : “Aerobic microbial life persists in oxic marine sediment as old as 101.5 million years | Nature Communications” . Accessed May 22, 2022. Link .