New pieces in the puzzle of first life on Earth

A drill core sample from the Barberton greenstone belt used in the study. The da
A drill core sample from the Barberton greenstone belt used in the study. The dark layers contain particles of carbonaceous matter, the altered remains from Palaeoarchaean microorganisms. Photo: Manuel Reinhardt

Research team discovers complex microbial communities in ecosystems over 3 billion years ago

Microorganisms were the first forms of life on our planet. The clues are written in 3.5 billion-year-old rocks by geochemical and morphological traces, such as chemical compounds or structures that these organisms left behind. However, it is still not clear when and where life originated on Earth and when a diversity of species developed in these early microbial communities. Evidence is scarce and often disputed. Now, researchers led by the University of Göttingen and LinnÓ•us University in Sweden have uncovered key findings about the earliest forms of life. In rock samples from South Africa, they found evidence dating to around 3.42 billion years ago of an unprecedentedly diverse carbon cycle involving various microorganisms. This research shows that complex microbial communities already existed in the ecosystems during the Palaeoarchaean period. The results were published in the journal Precambrian Research.

The researchers analysed well-preserved particles of carbonaceous matter - the altered remains of living organisms - and the corresponding rock layers from samples of the Barberton greenstone belt, a mountain range in South Africa whose rocks are among the oldest on the Earth’s surface. The scientists combined macro and micro analyses to clearly identify original biological traces and distinguish them from later contamination. They identified geochemical "fingerprints" of various microorganisms, including those that must have used sunlight for energy, metabolised sulphate and probably also produced methane. The researchers determined the respective role of the microorganisms in the carbon cycle of the ecosystem at the time by combining geochemical data with findings on the texture of the rocks obtained from thin section analysis with a microscope. "By discovering carbonaceous matter in primary pyrite crystals and analysing carbon and sulphur isotopes in these materials, we were able to distinguish individual microbial metabolic processes," explains the senior author of the study, Dr Henrik Drake from LinnÓ•us University.


First author Dr Manuel Reinhardt, from Göttingen University’s Geosciences Centre, adds: "We didn’t expect to find traces of so many microbial metabolic processes. It was like the proverbial search for a needle in a haystack." The study provides a rare glimpse into the Earth’s early ecosystems. "Our findings significantly advance the understanding of ancient microbial ecosystems and open up new avenues for research in the field of palaeobiology."


Original publication: Reinhardt, M. et al. Aspects of the biological carbon cycle in a ca. 3.42-billion-year-old marine ecosystem. Precambrian Research (2024). DOI: 10.1016/j.precamres.2024.107289