Wednesday, December 10, 2025

 

A new study reveals how oxygen first reached Earth’s oceans



Researchers use vanadium isotopes to track the rise of oxygen in ancient seas



Woods Hole Oceanographic Institution

Sample 

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South Africa’s exceptionally preserved ancient rocks hold key evidence for the rise ofatmospheric oxygen. Within them, researchers see the disappearance of sulfur mass-independent fractionation, evidence for a GOE.

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Credit: Photo by Daniel Hentz, ©Woods Hole Oceanographic Institution




Woods Hole, Mass (December 9, 2025) –  For roughly two billion years of Earth’s early history, the atmosphere contained no oxygen, the essential ingredient required for complex life. Oxygen began building up during the period known as the Great Oxidation Event (GOE), but when and how it first entered the oceans has remained uncertain.

A new study published in Nature Communications shows that oxygen was absorbed from the atmosphere into the shallow oceans within just a few million years—a geological blink of an eye. Led by researchers at Woods Hole Oceanographic Institution (WHOI), the work provides new insight into one of the most important environmental shifts in Earth’s history.

“At that point in Earth’s history, nearly all life was in the oceans. For complex life to develop, organisms first had to learn not only to use oxygen, but simply to tolerate it,” said Andy Heard, lead author of the study and assistant scientist at WHOI. “Understanding when oxygen first accumulated in Earth’s atmosphere and oceans is essential to tracing the evolution of life. And because ocean oxygenation appears to have followed atmospheric oxygen surprisingly quickly, it suggests that if we detect oxygen in the atmosphere of a distant exoplanet, there’s a strong chance its oceans also contain oxygen.”

Researchers used new chemical analyses of black shales, organic-rich marine sedimentary rocks from South Africa, that formed in the ocean during the ongoing Great Oxidation Event. They found that the trace metal vanadium saw a shift in the relative abundance of its stable isotopes in shales formed before and after the stratigraphic level marking the occurrence of oxygenation in the atmosphere.

“South Africa is one of the few places on Earth with exceptionally well-preserved rock records from this pivotal time in our planet’s history. These sedimentary rocks play host to some of our strongest indicators for the rise of atmospheric oxygen,” said Chad Ostrander, one of the study’s co-authors and an isotope geochemist at the University of Utah. “These rocks have relatively tight age constraints, and within them we see the disappearance of sulfur mass-independent fractionation—the traditional ‘smoking gun’ evidence for a GOE.”

“Vanadium is especially powerful because it responds to relatively high levels of dissolved oxygen compared to other geochemical proxies used for this period of Earth’s history. That means we can detect when oxygen in the oceans first rose above roughly 10 micromoles per liter—a few percent of modern levels,” said Sune Nielsen, one of the study's co-authors and adjunct scientist at WHOI. Nielsen is also noted as one of the first scientists to use the vanadium isotope redox method to study past ocean oxygen levels. “For context, today’s oceans average about 170 micromoles of dissolved oxygen per liter. It’s not much by modern standards, but in oceans that were previously almost entirely oxygen-free, it represents a major step in Earth’s oxygenation.”

These findings show that Earth’s oceans began accumulating oxygen far earlier, and more rapidly, than previously thought, reshaping our understanding of how the planet became habitable for complex life.

“This study helps clarify one of the biggest turning points in Earth’s history,” Heard continued. “By tracing when oxygen first reached the oceans, we’re getting closer to understanding how the conditions for complex life emerged on our planet—and how they might arise elsewhere.”

This work was funded by NASA Exobiology, the WHOI postdoctoral scholar program, the Agouron Institute Fellowship in Geobiology, Discovery and Accelerator Grants from the Natural Sciences and Engineering Research Council of Canada, ACS Petroleum Fund, and the Natural Environmental Research Council.

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About Woods Hole Oceanographic Institution

Woods Hole Oceanographic Institution (WHOI) is a private, non-profit organization on Cape Cod, Massachusetts, dedicated to marine research, engineering, and higher education. Founded in 1930, its mission is to understand the ocean, its interactions with the Earth, and its role in a changing global environment. WHOI’s pioneering discoveries arise from a unique blend of science and engineering that has made it one of the world’s most trusted leaders in ocean research and exploration. Known for its multidisciplinary approach, advanced ship operations, and unmatched deep-sea robotics, WHOI also operates the most extensive suite of ocean data-gathering platforms worldwide. More than 800 concurrent projects—driven by top scientists, engineers, and students—push the boundaries of knowledge to inform people and policy for a healthier planet. Behind the scenes, ship captains, mates, craftsmen, marine operations, and other skilled professionals provide essential support that makes this work possible. Learn more at whoi.edu.

 

Ocean current and seabed shape influence warm water circulation under ice shelves




University of East Anglia

Boaty McBoatface 

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Autonomous underwater vehicle Boaty McBoatface was used to gather data from underneath the Dotson Ice Shelf.

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Credit: Hannah Wyles





New research reveals how the speed of ocean currents and the shape of the seabed influence the amount of heat flowing underneath Antarctic ice shelves, contributing to melting.

Scientists at the University of East Anglia (UEA) used an autonomous underwater vehicle to survey beneath the Dotson Ice Shelf in the Amundsen Sea, an area of rapid glacial ice loss largely due to increasing ocean heat around and below ice shelves.

The circulation of warm water and the heat transport within ice shelf cavities - significant areas beneath ice shelves - remains mostly unknown. To address this the team collected data from over 100 kilometres of dive tracks the underwater robot made along the seabed in the Dotson cavity.

The findings are published today in the journal Ocean Sciences.

Lead author Dr Maren Richter, from UEA’s Centre for Ocean and Atmospheric Sciences, said: “Upward transport of deep warm water to the shallower ice-ocean boundary in ice shelf cavities is what drives melting at the underside of the ice shelf. This melting makes the ice shelf thinner, and therefore less strong.

“We found that while there is mixing of warm water with other, cooler, water, under the Dotson Ice Shelf most of the warm water is not mixed upward. Instead, it flows horizontally to the grounding line, the point where the glacier loses contact with the seabed and starts to float.

“This means that the water stays warm all the way to the grounding line, where it can melt the glacier directly. This can cause the glacier to retreat, speed up and lose more ice into the ocean. Together, the retreat, increased speed, and increased melt contribute to sea level rise globally.”

During the mission, the first of its kind under the Dotson Ice Shelf, the researchers found warm, salty water below colder, fresher water. It is already known that warm water is transported upward by mixing, however this study shows that the mixing and upward transport of warm water are strongest in the inflow areas to the east of the ice shelf, where the currents are faster and the seabed is steep, with the gradient of the bedrock being particularly significant.

Current speeds recorded in this area by the Autosub Long Range (ALR) autonomous underwater vehicle - named Boaty McBoatface and operated by the National Oceanography Centre - were around five centimetres per second up to 10 centimetres per second. The gradient was about 45 degrees in the steepest areas.

Dr Richter added: “We were expecting the influence of current speed on the mixing to be much higher than what we found. Instead, the shape of the seabed seems to be really important.

“We also found water in the deepest part of the cavity that was surprisingly warm, and we are now working to explain how and when it got there.” 

The data was collected over four missions in 2022 when Boaty, equipped with sensors to measure properties of the water including temperature, current, turbulence (mixing) and oxygen, travelled along the bottom of the ice shelf cavity, staying about 100 metres above the seabed. Boaty was in the cavity for approximately 74 hours.

Missions to send a robot into an ice shelf cavity and then get it back at the end are very difficult, and ones with an instrument that can measure mixing are especially rare.

“This mission was the first of its kind under the Dotson Ice Shelf,” said Dr Richter. “We gained very valuable baseline measurements which can now be compared to assumptions about mixing in regional and global models of ice shelf-ocean interactions, and to measurements under other ice shelf cavities, helping us understand how these cavities are similar or different from each other.”

Warm deep water that is mixed upward not only increases the temperature in the upper ocean, it can also transport nutrients and trace-metals upward, which is very important for local algae blooms and the creatures that depend on them for food.

While this study did not measure nutrient transports through mixing, the data can be used by other researchers who want to calculate the effects of mixing in the cavity. 

The work was carried out as part of a project for the International Thwaites Glacier Collaboration, a major five-year research programme aiming to understand what is causing ice loss and better predict how this could contribute to sea level rise. It was funded by the UK’s Natural Environment Research Council and the US National Science Foundation.

‘Observations of turbulent mixing in the Dotson Ice Shelf cavity’, Maren Richter, Karen Heywood, Rob Hall and Peter Davis, is published in Ocean Sciences on December 10.


The Dotson Ice Shelf, Antarctica

Credit

Anna WÃ¥hlin, University of Gothenburg


Autonomous underwater vehicle Boaty McBoatface was used to gather data from underneath the Dotoson Ice Shelf in Antarctica.

Credit

Hannah Wyles

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