Two years ago a team of scientists visited Costa Rica’s subduction zone, where the ocean floor sinks beneath the continent and volcanoes tower above the surface. They wanted to find out if microbes can affect the cycle of carbon moving from Earth’s surface into the deep interior. According to their new study in Nature, the answer is affirmatively - yes they can.
Albuquerque/New Mexico – According to a study, published in Nature, microbes consume and — crucially — help trap a small amount of sinking carbon in this zone. This finding has important implications for understanding Earth’s fundamental processes and for revealing how nature can potentially help mitigate climate change.
At a subduction zone there is communication between Earth’s surface and interior. Two plates collide and the denser plate sinks, transporting material from the surface into Earth’s interior. Showing that the microbes at the near-surface are playing a fundamental role in how carbon and other elements are being locked up into the crust provides a profound new understanding of Earth processes and helps researchers model how Earth’s interior may develop over time.
The scientists have shown that in areas that are critically important for putting chemicals back down into the planet – these big subduction zones – life is sequestering carbon. On geological timescales life might be controlling the chemicals at the surface and storing elements like carbon in the crust, explains co-author, Professor Chris Ballentine, Head of the Department of Earth Sciences at the University of Oxford.
This is the first evidence that subterranean life plays a role in removing carbon from subduction zones. It has been well established that microbes are capable of taking carbon dissolved in water and converting it into a mineral within the rocks. This study demonstrates that the process is happening on a large scale across a subduction zone. It is a natural CO2 sequestration process which can control the availability of carbon on Earth’s surface. Lead author, Dr Peter Barry, who carried out the research while at the Department of Earth Sciences, Oxford University, said that a substantial amount of carbon is being trapped in non-volcanic areas instead of escaping through volcanoes or sinking into Earth’s interior. Until this point scientists had assumed that life plays little to no role in whether this oceanic carbon is transported all the way into the mantle, but they found that life and chemical processes work together to be the gatekeepers of carbon delivery to the mantle.
During the 12-day expedition, the 25-person group of multi-disciplinary scientists collected water samples from thermal springs throughout Costa Rica. Scientists have long predicted that these thermal waters spit out ancient carbon molecules, subducted millions of years before. By comparing the relative amounts of two different kinds of carbon — called isotopes — the scientists showed that the predictions were true and that previously unrecognized processes were at work in the crust above the subduction zone, acting to trap large amounts of carbon.
Following their analyses, the scientists estimated that about 94 % of that carbon transforms into calcite minerals and microbial biomass. The researchers now plan to investigate other subduction zones to see if this trend is widespread. If these biological and geochemical processes occur worldwide, they would translate to 19 % less carbon entering the deep mantle than previously estimated.
Reference: ‘Forearc carbon sink reduces long-term volatile recycling into the mantle’ in Nature when the embargo ends on Wednesday 24 April at 1800 London time (BST): https://doi.org/10.1038/s41586-019-1131-5.