Researchers identify oxygen produced by seabed metals as ‘dark oxygen’

Researchers identify oxygen produced by seabed metals as ‘dark oxygen’

Scientists have made a groundbreaking discovery in the deep sea that challenges our understanding of the origins of oxygen on Earth. Dr. Sweetman, a researcher leading the study, and his team have found evidence of oxygen production in the deep sea, where no light reaches. This discovery raises important questions about where aerobic life could have begun on our planet.

During fieldwork in the Clarion–Clipperton Zone, an area known for its metal-rich nodules, the researchers observed a mysterious phenomenon. The seafloor ecosystem in this region was found to be producing oxygen, contrary to the belief that oxygen was solely produced by photosynthetic organisms on the surface.

The mechanism behind this oxygen production remains a mystery, but the researchers have ruled out sensor malfunctions, confirming their findings through alternative techniques. The sequestered water in the deep sea was found to be richer in oxygen than surface waters with abundant algae.

This discovery has significant implications for the mining industry, as the Clarion–Clipperton Zone is a prime target for companies like The Metals Company. The nodules in this region contain valuable metals such as cobalt, nickel, copper, and lithium, crucial for green technologies like solar panels and electric car batteries.

Despite the potential economic benefits, shares of The Metals Company fell following the news of the discovery. However, scientists estimate that deep-sea mining could meet up to 45% of the world’s critical metal needs by 2065. The implications of this discovery extend beyond the scientific realm, shaping the future of both industry and our understanding of life on Earth.

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