First evidence of life colonizing deep into the bedrock of Greenland
A new international research study, led by Henrik Drake, Associate Professor of Environmental Science at Linnaeus University, shows that microorganisms lived deep in the bedrock of Greenland 75 million years ago.
Beneath our feet lies a habitat called the deep biosphere. In this harsh environment, without sunlight and without dissolved oxygen, microorganisms have lived for millions of years. However, how long life has existed in the bedrock and how widespread it is, is less known. This is because we have only made needle pricks in this unexplored environment. But more and more pieces of the puzzle are being found.
In connection with investigations in western Greenland, researchers have drilled deep into the bedrock near the ice sheet. At several hundred meters depth, they found minerals lining bedrock fractures, which serve as important geochemical archives for ancient life.
“We used high-resolution geochronology of the calcium carbonate, a method where you examine how much uranium has decayed into lead. The datings gave ages of 64-75 million years”, Henrik Drake says.
Opening of the Atlantic Ocean gave rise to life in the deep biosphere
These ages overlap with tectonic events related to the early stages, or precursors, of the opening of the Atlantic and the Labrador Sea. This suggests that deep fracture networks in western Greenland opened up and were colonized by microorganisms, such as sulfate reducers, during these events. The movements of the continents have thus influenced how the deep biosphere has been colonized.
Henrik Drake explain the researchers drill core findings as chemical fingerprints, indicating that life existed in this harsh environment. Also, biological traces in form of bacterial fatty acids was discovered, which were preserved inside calcium carbonate crystals.
“When we retrieved the drill cores, we conducted thorough analyses of different sulfur isotopes in minerals formed in the bedrock fractures. The results clearly show that the minerals were formed by bacteria (microbial sulfate reduction).”
More information
- The study is published in the journal Geochemistry, Geophysics, Geosystems - https://doi.org/10.1029/2024GC011646
- High resolution pictures for download >> (Photo: Henrik Drake)
Contact
Henrik Drake, Associate Professor, +46 70-289 26 46, henrik.drake@lnu.se
Ulrika Bergström, Press Officer, +46 70-259 36 29, ulrika.bergstrom@lnu.se