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Building Blocks of Life on the Atlantis Massif

JOIDES Resolution

An upcoming expedition aboard the US ocean drilling ship JOIDES Resolution co-led by Susan Q. Lang, a geochemist at WHOI and director NOSAMS Facility, will attempt to shed new light on the processes that likely helped jumpstart the formation of life early in Earth’s history.

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Hydrothermal field discovered at the East Pacific Rise 9°54’N

A new high-temperature, off-axis hydrothermal vent field on Pacific seafloor at 2550 meters depth was discovered in 2021 by a team that included researchers from Lehigh University; Scripps Institution of Oceanography (SIO); the University of Bergen Norway; and Woods Hole Oceanographic Institution (WHOI).

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Origin of Massive Methane Reservoir Identified

New research provides evidence of the formation and abundance of abiotic methane—methane formed by chemical reactions that don’t involve organic matter—on Earth and shows how the gases could have a similar origin on other planets and moons, even those no longer home to liquid water.

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Panel to Discuss Deep-Sea Mining at AAAS Meeting

Panel to Discuss Deep-Sea Mining at AAAS Meeting

Home to an immense diversity of marine life, the deep ocean also contains valuable minerals with metals such as nickel, copper, cobalt, manganese, zinc, and gold, and rare-earth elements used in electronic technology like smart phones and medical imaging machines. As demand for these resources increases and supplies on land decrease, commercial mining operators are looking to the deep ocean as the next frontier for mining.

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Carbon Dioxide Pools Discovered in Aegean Sea

The waters off Greece’s Santorini are the site of newly discovered opalescent pools forming at 250 meters depth. The interconnected series of meandering, iridescent white pools contain high concentrations of carbon dioxide (CO2) and may hold answers to questions related to deepsea carbon storage as well as provide a means of monitoring the volcano for future eruptions.

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Making Organic Molecules in Hydrothermal Vents in the Absence of Life

In 2009, scientists from Woods Hole Oceanographic Institution embarked on a NASA-funded mission to the Mid-Cayman Rise in the Caribbean, in search of a type of deep-sea hot-spring or hydrothermal vent that they believed held clues to the search for life on other planets. They were looking for a site with a venting process that produces a lot of hydrogen because of the potential it holds for the chemical, or abiotic, creation of organic molecules like methane – possible precursors to the prebiotic compounds from which life on Earth emerged.   

For more than a decade, the scientific community has postulated that in such an environment, methane and other organic compounds could be spontaneously produced by chemical reactions between hydrogen from the vent fluid and carbon dioxide (CO2).  The theory made perfect sense, but showing that it happened in nature was challenging.

Now we know why:  an analysis of the vent fluid chemistry proves that for some organic compounds, it doesn’t happen that way.

New research by geochemists at Woods Hole Oceanographic Institution, published June 8 in the Proceedings of the National Academy of Sciences, is the first to show that methane formation does not occur during the relatively quick fluid circulation process, despite extraordinarily high hydrogen contents in the waters.  While the methane in the Von Damm vent system they studied was produced through chemical reactions (abiotically), it was produced on geologic time scales deep beneath the seafloor and independent of the venting process. Their research further reveals that another organic abiotic compound is formed during the vent circulation process at adjacent lower temperature, higher pH vents, but reaction rates are too slow to completely reduce the carbon all the way to methane.

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Study Finds Deep Ocean is Source of Dissolved Iron in Central Pacific

A new study led by scientists at the Woods Hole Oceanographic Institution (WHOI) points to the deep ocean as a major source of dissolved iron in the central Pacific Ocean. This finding highlights the vital role ocean mixing plays in determining whether deep sources of iron reach the surface-dwelling life that need it to survive.

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Long-Distance Larvae Speed to New Undersea Vent Homes

Working in a rare, ?natural seafloor laboratory? of hydrothermal vents that had just been rocked by a volcanic eruption, scientists from the Woods Hole Oceanographic Institution (WHOI) and other institutions have discovered what they believe is an undersea superhighway carrying tiny life forms unprecedented distances to inhabit the post-eruption site.

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Lost City pumps life-essential chemicals at rates unseen at typical black smokers

Hydrocarbons?molecules critical to life?are routinely generated by the simple interaction of seawater with the rocks under the Lost City hydrothermal vent field in the Atlantic Ocean. The production of such building blocks of life makes Lost City-like vents strong contenders as places where life might have originated on Earth, according to research led by the University of Washington and the Woods Hole Oceanographic Institution.

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