That's deep: life found 11km below sea level in deepest known point on the surface of the Earth
Bacteria discovered in Mariana Trench, a gigantic chasm in the seabed which is big enough to swallow Mount Everest entirely
Steve Connor is the Science Editor of The Independent. He has won many awards for his journalism, including five-times winner of the prestigious British science writers’ award; the David Perlman Award of the American Geophysical Union; twice commended as specialist journalist of the year in the UK Press Awards; UK health journalist of the year and a special merit award of the European School of Oncology for his investigative journalism. He has a degree in zoology from the University of Oxford and has a special interest in genetics and medical science, human evolution and origins, climate change and the environment.
Sunday 17 March 2013
Scientist have found a thriving community of microbes living at the deepest known point on the surface of the Earth – a massive underwater canyon in the Pacific Ocean 11km (6.8 miles) below sea level.
The bacteria were recovered from muddy sediments at a point underneath the central west Pacific called Challenger Deep in the huge Mariana Trench, a gigantic chasm in the seabed which is big enough and deep enough to swallow Mount Everest entirely.
Marine biologists said they were astonished to find such an abundance of microbial life-forms living off the dead and decaying matter that sinks to the deepest parts of the ocean where pressures are more than a thousand times greater than at sea level.
“These microbes may in fact be the ones that are the closest to the centre of the Earth, the deepest living organisms that we have seen. They are probably the deepest observed community of microbes below sea level,” said Professor Ronnie Glud of the University of Southern Denmark.
“We expected to see microbes there but we didn’t expect them to flourish and to be so efficient. What is really surprising is that we have seen bacteria that operate so efficiently at these depths,” Professor Glud said.
The microbes are feeding off the constant stream of organic matter that sinks to the seabed in the Pacific Ocean. In doing so, they play a crucial role in the global carbon cycle, which affects the amount of carbon dioxide circulating in the atmosphere, he said.
“We know very little about what is going on down there or what impact the deep-sea trenches have on the global carbon cycle as well as climate regulation,” he added
A deep-sea submersible robot that can analyse life-forms in situ discovered the microbial community in sediment samples taken in 2010 from the Mariana Trench. The sediment has built up over tens of thousands of years and is probably several hundreds of metres deep, Professor Glud said.
“If we retrieve samples from the seabed to investigate them in the laboratory, many of the microorganisms that have adapted to life at these extreme conditions will die, due to the changes in temperature and pressure,” he said.
“Therefore, we have developed instruments that can autonomously perform pre-programmed measuring routines directly on the seabed at the extreme pressure of the Mariana Trench….We find a world dominated by microbes that are adapted to function effectively at conditions highly inhospitable to most higher organisms,” he said.
The scientists found 10 times as many microbes living in the sediment of the trench than in the surrounding abyssal plain of the Pacific seabed, which lies in relatively shallower depths of between five and six kilometres.
The discovery, detailed in a study published in the journal Nature Geoscience, is the latest in a string of finds showing that life can exist in some of the most extreme environments on Earth, from the dry, intensely cold regions of Antarctica to the hot springs and geysers of Iceland.
Mark Lever of Aarhus University in Denmark announced last week in the journal Science that he had discovered microbial life-forms living on the chemical energy trapped in volcanic rocks at the bottom of the sea – the first time microbes were found living deep inside the Earth’s oceanic crust.
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