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spud - size metal nodules strewn across the Pacific Ocean seafloor produce oxygen in complete dark and without any assistance from living organisms , new research let on .

The discovery of this recondite - sea O , dubbed " dark atomic number 8 , " is the first time scientist have ever observed oxygen being generated without the involvement of organisms and challenges what we roll in the hay about the emergence of life on Earth , researchers say .

A picture of the seafloor off the eastern U.S. coast covered in metallic nodules rich in manganese.

So-called polymetallic nodules are potato-size lumps of oxides of iron and manganese that also contain precious metals like cobalt and rare earth elements.

" When we first stimulate this data , we thought the sensors were faulty , because every study ever done in the deep sea has only seen oxygen being run through rather than get , " study lead story authorAndrew Sweetman , a prof and loss leader of the seafloor ecology and biogeochemistry research group at the Scottish Association for Marine Science ( SAMS ) , said in astatement . But when the instruments kept read the same resolution , Sweetman and his workfellow know they " were onto something land - breaking and unhoped-for - of , " he said .

The termination , published Monday ( July 22 ) in the journalNature Geoscience , evoke that small metallic nodule ascertain in the north Pacific ’s Clarion - Clipperton Zone ( CCZ ) produce O through seawater electrolysis , where seawater splits into oxygen and hydrogen in the bearing of an galvanizing charge . This charge may come from the difference in electric potential that survive between metal ions within the nodules , which lead to a redistribution of electrons , accord to the cogitation .

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A close-up image of a manganese nodule from the Clarion-Clipperton Zone in the Pacific Ocean. The nodule is jet black, potato-sized and rough on the outside.

Polymetallic nodules were deposited on the seafloor millions of years ago and grow about 2 millimeters every million years.

So - called polymetallic nodules are common on the sea ’s abyssal plains , which are flavourless neighborhood of the seafloor between 10,000 and 20,000 feet ( 3,000 to 6,000 m ) below the sea surface . These nodules mostly contain oxide of smoothing iron and Mn , but they also admit metal like cobalt , nickel and lithium , as well asrare earth elementssuch as Ce that are essential components of electronics and scurvy - carbon technology .

Sweetman and his colleagues originally typeset out to study the potential wallop of excavation polymetallic nodules on the seafloor ecosystem in the CCZ , an abyssal plainspanning 1.7 million square miles(4.5 million straight kilometers ) between Hawaii and Mexico . As part of this assessment , the team measured changes in O concentrations using special experimental chambers at multiple locations . Typically , atomic number 8 levels slump the deep in the sea scientist look , as less igniter is available , meaning there are fewer photosynthetic organisms and therefore lower oxygen production . But instead of the await declivity in oxygen , the data evince steady emissions from the ocean floor .

The breakthrough of dark oxygen 13,000 foot ( 4,000 m ) below the waves , where no light can penetrate , challenge scientists ' notion that Earth ’s oxygen is only of course make throughphotosynthesis(andthrough oxidizing ammonia water , but this results in tiny amounts that are immediately consumed ) . That , in turn , raise new questions about the origins of life on Earth more or less 3.7 billion years ago , Sweetman said .

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" For aerobic life to begin on the planet , there has to be oxygen and our understanding has been that Earth ’s atomic number 8 supplying lead off with photosynthetic organism , " he said . " But we now recognise that there is O produce in the deep ocean , where there is no light . I think we therefore ask to revisit query like : where could aerobic lifetime have begun ? "

The results also erect new business concern about potentiallymining polymetallic nodules , which could stand for a critical source of O for thick - ocean ecosystem , Sweetman enounce .

" Through this discovery , we have generated many unrequited questions and I consider we have a mountain to think about in term of how we mine these modules , which are in effect batteries in a careen . "

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