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5 Min Read

NASA’s Hubble Uncovers Case of Missing Oxygen in Nearby Dwarf Galaxies

NASA’s Hubble Space Telescope just revealed a mystery in our cosmic neighborhood. In a paper published Monday in The Astrophysical Journal, researchers using Hubble studied 37 nearby dwarf galaxies — small galaxies containing a few thousand to hundreds of millions of stars — and found that much of the oxygen they expected to see is missing. 

Simulations predict that significantly more oxygen, a tracer of a wider set of heavy elements, should reside in these galaxies. So where did it go? 

“Oxygen is produced by stars, which are inside of galaxies. We know that the oxygen had to be inside of the galaxies at some point in the past, so the oxygen must have been ejected,” said co-investigator Grace Telford, assistant professor in the Department of Physics and Astronomy at the University of Utah. “And to do that, you need energy from massive stars and supernova explosions to drive material out of the host galaxies and into the space between galaxies.”

Galactic winds unleashed by supernovae are apparently more effective at removing oxygen from low-mass galaxies than current models predict, according to the new study. The findings show that dwarf galaxies can hold onto only a small fraction of the oxygen made by stars. 

In the Galaxies Losing Oxygen via Winds (GLOW) project, funded by NASA and the National Science Foundation, scientists traced the oxygen to understand how it is distributed inside stars, in the gas between stars, and in the space between galaxies. But, of all the elements in the galaxies, why study oxygen?

Oxygen, the most abundant element after hydrogen and helium, is relatively easy to detect and measure, and its production is well understood — making it a reliable indicator of how chemical elements are distributed in a galaxy. 

“So, it’s really for practical reasons that we’ve chosen oxygen,” said Kristen Wingfield McQuinn, GLOW principal investigator and mission head of the Science Operations Center for NASA’s newly launched, panoramic Nancy Grace Roman Space Telescope at the Space Telescope Science Institute in Baltimore, Maryland. She also is an associate professor at Rutgers University in New Brunswick, New Jersey. 

“Oxygen is one of the primary elements formed by stars. Being able to trace how much oxygen gets made, and then how much is distributed inside and outside of galaxies, helps us understand galaxy evolution,” said McQuinn. “It also helps us learn where and how much galaxies are enriching the space between galaxies, called the intergalactic medium.” 

The study used archival optical imaging data from Hubble to resolve stellar populations and determine star-formation histories and compositions. Along with data from NASA’s retired Spitzer Space Telescope as well as the ground-based Very Large Array and Australian Telescope Compact Array, the researchers analyzed 37 nearby dwarf galaxies to trace oxygen atoms produced by stars. 

The team wanted to understand how oxygen is distributed across the stars, gas, and dust in the galaxies. These dwarf galaxies were selected because their masses fall in the range where simulations and theory predict that an increasing amount of their oxygen will be expelled from the galaxies via supernovae explosions. These 37 galaxies also are all close enough for Hubble to resolve their individual stars. That’s not true for the vast majority of known dwarf galaxies, which are too far away for this kind of study.

Although astronomers already suspected that galaxies expel a large fraction of oxygen and other heavy elements, an open question has been where these metals end up. A previous study from 2014 addressed this question for Milky Way-like, star-forming galaxies, finding that these galaxies lost a large fraction of their oxygen, some of which is found in the diffuse haloes of gas surrounding galaxies outside their disks, called the circumgalactic medium.

In the GLOW study, McQuinn and her team extended this research to low-mass galaxies across a wide range of masses and environments. While previous teams have measured oxygen in the circumgalactic medium of dwarf galaxies, it is still unclear if most of the missing oxygen is in this region, or if it has been completely ejected from the galaxy’s surroundings. 

In the future, McQuinn hopes to study even lower-mass galaxies in the nearby universe. She has an approved program to use the Roman Space Telescope to find these faint and tiny systems across a wide swath of sky. Once she’s identified these galaxies, McQuinn hopes to use Hubble and NASA’s James Webb Space Telescope to get deeper observations of their stars. This would allow her to reconstruct the galaxies’ histories to understand how they formed stars across cosmic time. 

Telford’s future work involves using Hubble to zoom in on the individual, massive stars that produce oxygen and eject it from their host galaxies. She’s using some of the nearby GLOW targets to get very detailed observations to characterize how the massive stars are different in these small galaxies.

The Hubble Space Telescope has been operating for over three decades and continues to make ground-breaking discoveries that shape our fundamental understanding of the universe. Hubble is a project of international cooperation between NASA and ESA (European Space Agency). NASA’s Goddard Space Flight Center in Greenbelt, Maryland, manages the telescope and mission operations. Lockheed Martin Space, based in Denver, also supports mission operations at Goddard. The Space Telescope Science Institute in Baltimore, which is operated by the Association of Universities for Research in Astronomy, conducts Hubble science operations for NASA.

Related Multimedia

Dwarf Galaxy NGC 4449

This is an image from NASA’s Hubble Space Telescope of NGC 4449, one of the dwarf galaxies in the Galaxies Losing Oxygen via Winds (GLOW) study. Researchers found that dwarf galaxies can hold onto only a small fraction of the oxygen made by their stars.

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North-central Pennsylvania is canyon country with an Appalachian flair. Pine Creek Gorge reaches depths of about 1,500 feet (460 meters) along its gently curving path through the forests of the Allegheny Plateau. Instead of the steep rock walls characteristic of canyons in the desert Southwest, lushly vegetated slopes outline the dramatic topography. In autumn, greens give way to a palette of reds and golds sought out by leaf peepers.

Nicknamed the “Grand Canyon of Pennsylvania,” the gorge runs for some 45 miles (72 kilometers) from Ansonia south to Pine Creek’s confluence with the West Branch Susquehanna River, reaching its greatest depths around Waterville. The OLI (Operational Land Imager) on the NASA-USGS Landsat 8 satellite captured this image of Pine Creek Gorge on October 25, 2026, when colorful fall foliage was on display.

Glaciers played a key role in the canyon’s formation, though ice itself did not carve it. Pine Creek once flowed to the north, opposite of what it does today. As glaciers advanced into the region from the northeast during the last ice age, they dammed the river and filled the valley with lakes. Those lakes eventually overflowed, sending water streaming to the south.

When the ice receded, Pine Creek was already becoming entrenched in its southward course. Rocks and sand left behind by the melting ice further prevented the water from turning back north. Glacial meltwater continued to rush through the valley, deepening and shaping it into its current form.

Today, the hillsides around the gorge are blanketed in northern hardwood and mixed oak forest, sprinkled with hemlock and white pine. In autumn, the deciduous trees impart red and gold hues to the landscape akin to the rock of the famous Arizona canyon.

October 9

October 25

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Image Details

Foliage in the northern hardwood and oak forests around Pennsylvania’s Pine Creek Gorge takes on fall color between October 9, 2026 (left), and October 25, 2026 (right). The images were acquired with the OLI (Operational Land Imager) on Landsat 8. NASA Earth Observatory images by Michala Garrison.

This seasonal change around Pine Creek Gorge has not always been so visually pleasing. With increasing demand for wood products in early 19th-century America, loggers found their way to the area’s stately trees. At the time, white pine and hemlock several feet in diameter and towering hardwoods populated the slopes around Pine Creek Gorge. The pines were especially valued for making ship masts, and hemlock bark was used to tan leather. Before railroads, logs were floated down Pine Creek to the Susquehanna in massive drives. By the early 20th century, decades of logging left the land so barren that the area earned the moniker “Pennsylvania Desert.”

The forest has since returned, and with it, wild inhabitants such as black bears, coyotes, bobcats, timber rattlesnakes, and a diversity of songbirds. In 1968, an area of 30,000 acres (12,000 hectares) was designated a National Natural Landmark. Visitors can experience the gorge’s natural splendor at many points along its path, including from multiple state parks and the Pine Creek Rail Trail.

NASA Earth Observatory images by Michala Garrison, using Landsat data from the U.S. Geological Survey. Photo by fishhawk, via Flickr. Story by Lindsey Doermann.

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October 9, 2026

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October 25, 2026

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References & Resources

• Lumber Heritage Region, The Lumber Era of Pine Creek Gorge. Accessed October 30, 2026.
• NASA Earth Observatory (2026, October 26) Hunting Red Leaves With Satellites. Accessed October 30, 2026.
• Pennsylvania Department of Conservation and Natural Resources (2026, October 22) 2026 Fall Foliage Report: Week of October 22-28. Accessed October 30, 2026.
• Pennsylvania Department of Conservation and Natural Resources, Pine Creek Gorge Natural Area. Accessed October 30, 2026.
• Pennsylvania Geological Survey (2016) Pine Creek Gorge (PA Grand Canyon), Tioga and Lycoming Counties. Accessed October 30, 2026.

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