The New Zealand Herald

Team to drill into undersea volcano

Brothers expedition will probe life forms able to survive in extreme environmen­t

- Jamie Morton

Dscience eep in the ocean, several hundred kilometres northeast of New Zealand, lies the world’s most hydrotherm­ally active volcano.

The Brothers volcano is huge — it’s about three times the size of White Island and its summit rises to within 1200m of sea level — and it sits in one of the most active regions of the planet, the Kermadec Arc.

In a bold first, scientists will soon attempt to drill directly into the beast’s belly, encounteri­ng rocks as hot as 400C as they go.

The two-month-long internatio­nal expedition, setting out from Auckland this week, will drill three boreholes into Brothers. One is planned to reach a depth of about 800m in a cone growing up inside the submarine volcano’s caldera.

The others will reach depths between 400m and 570m at the top and base of the caldera walls.

Led by the 23-nation Internatio­nal Ocean Discovery Programme (IODP), the $21 million project aims to learn more about how metals move through the Earth’s crust, while gaining new insights into local life forms somehow able to survive in such extreme environmen­ts.

The expedition’s co-chief scientist, Dr Cornel de Ronde, of GNS Science, has visited Brothers 12 times before, using surface ships and remotely operated vehicles, or ROVs.

All magmas contained small amounts of metals, he explained, but the magma and resultant volcanic rock at Brothers was unusually rich in metals such as copper, gold, silver and molybdenum.

“We don’t really know the full range of metals and in what quantities we will find at Brothers, or even how they are distribute­d within the volcano,” he said. “But if the chimneys sitting on the seafloor are anything to go by, we suspect we will see networks of veins beneath the seafloor that will be host to significan­t copper, zinc and gold mineralisa­tion.

“This voyage will increase our understand­ing of where these metals come from and how they accumulate in submarine volcanoes, which may help in the extraction of these economical­ly important and critical metals in similar settings worldwide.”

Co-chief scientist Susan Humphris, of US-based Woods Hole Oceanograp­hic Institutio­n, said the expedition would also help scientists better understand what regulates the chemical compositio­n of seawater.

“Chemical reactions between rocks and seawater at depth in the volcano change the chemistry of the fluid that is released through hydrotherm­al vents into the ocean.”

The team was also likely to find microbes completely new to science.

The hundreds of vents and chimneys, some as tall as 20m, that discharge fluids ranging in temperatur­e from 10C to 310C were focal points for a wide range of marine life, from microbes to tubeworms.

As well as tolerating temperatur­es as high as 120C, some of the microorgan­isms lived in fluids as corrosive as battery acid — and examining their tolerance could help biologists better understand how life began on Earth.

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