Jumat, 23 September 2022

Undersea volcano eruption in Tonga was a "once-in-a-lifetime event" that could warm Earth's surface, scientists say - CBS News

When an undersea volcano erupted in Tonga in January, its watery blast was huge and unusual — and scientists are still trying to understand its impacts.

The volcano, known as Hunga Tonga-Hunga Ha'apai, shot millions of tons of water vapor high up into the atmosphere, according to a study published Thursday in the journal Science.

The researchers estimate the eruption, which dwarfed the power of the Hiroshima atomic bomb, raised the amount of water in the stratosphere - the second layer of the atmosphere, above the range where humans live and breathe - by around 5%.

Now, scientists are trying to figure out how all that water could affect the atmosphere, and whether it might warm Earth's surface over the next few years.

"This was a once-in-a-lifetime event," said lead author Holger Voemel, a scientist at the National Center for Atmospheric Research in Colorado.

FILE PHOTO: Satellite view of the eruption of an underwater volcano off Tonga
The eruption of an underwater volcano off Tonga is seen in an image from a NOAA GOES-West satellite taken on January 15, 2022. CIRA / NOAA / Handout via REUTERS

Big eruptions usually cool the planet. Most volcanoes send up large amounts of sulfur, which blocks the sun's rays, explained Matthew Toohey, a climate researcher at the University of Saskatchewan who was not involved in the study.

The Tongan blast was much soggier: The eruption started under the ocean, so it shot up a plume with much more water than usual. And since water vapor acts as a heat-trapping greenhouse gas, the eruption will probably raise temperatures instead of lowering them, Toohey said.

It's unclear just how much warming could be in store.

Karen Rosenlof, a climate scientist at the National Oceanic and Atmospheric Administration who was not involved with the study, said she expects the effects to be minimal and temporary.

"This amount of increase might warm the surface a small amount for a short amount of time," Rosenlof said in an email.

In August, scientists said it broke "all records" for the injection of water vapor since satellites began recording such data -- enough water vapor to fill 58,000 Olympic-sized swimming pools.

The water vapor will stick around the upper atmosphere for a few years before making its way into the lower atmosphere, Toohey said. In the meantime, the extra water might also speed up ozone loss in the atmosphere, Rosenlof added.

But it's hard for scientists to say for sure, because they've never seen an eruption like this one.

The stratosphere stretches from around 7.5 miles to 31 miles above Earth and is usually very dry, Voemel explained.

Voemel's team estimated the volcano's plume using a network of instruments suspended from weather balloons. Usually, these tools can't even measure water levels in the stratosphere because the amounts are so low, Voemel said.

Another research group monitored the blast using an instrument on a NASA satellite. In their study, published earlier this summer, they estimated the eruption to be even bigger, adding around 150 million metric tons of water vapor to the stratosphere - three times as much as Voemel's study found.

In that study, scientists also concluded that the unprecedented plume could temporarily affect Earth's global average temperature. 

Voemel acknowledged that the satellite imaging might have observed parts of the plume that the balloon instruments couldn't catch, making its estimate higher.

Either way, he said, the Tongan blast was unlike anything seen in recent history, and studying its aftermath may hold new insights into our atmosphere.

e2-tonga-ash-plume-width-1320.jpg
An image from the ISS from Jan. 16, 2022, shows the ash plume from the Hunga Tonga-Hunga Ha'apai volcanic eruption that occurred the day before.  NASA

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2022-09-23 11:02:00Z
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Kamis, 22 September 2022

Tonga volcano blast was unusual, could even warm the Earth - mySA

NEW YORK (AP) — When an undersea volcano erupted in Tonga in January, its watery blast was huge and unusual — and scientists are still trying to understand its impacts.

The volcano, known as Hunga Tonga-Hunga Ha’apai, shot millions of tons of water vapor high up into the atmosphere, according to a study published Thursday in the journal Science.

The researchers estimate the eruption raised the amount of water in the stratosphere — the second layer of the atmosphere, above the range where humans live and breathe — by around 5%.

Now, scientists are trying to figure out how all that water could affect the atmosphere, and whether it might warm Earth’s surface over the next few years.

“This was a once-in-a-lifetime event,” said lead author Holger Voemel, a scientist at the National Center for Atmospheric Research in Colorado.

Big eruptions usually cool the planet. Most volcanoes send up large amounts of sulfur, which blocks the sun’s rays, explained Matthew Toohey, a climate researcher at the University of Saskatchewan who was not involved in the study.

The Tongan blast was much soggier: The eruption started under the ocean, so it shot up a plume with much more water than usual. And since water vapor acts as a heat-trapping greenhouse gas, the eruption will probably raise temperatures instead of lowering them, Toohey said.

It’s unclear just how much warming could be in store.

Karen Rosenlof, a climate scientist at the National Oceanic and Atmospheric Administration who was not involved with the study, said she expects the effects to be minimal and temporary.

“This amount of increase might warm the surface a small amount for a short amount of time,” Rosenlof said in an email.

The water vapor will stick around the upper atmosphere for a few years before making its way into the lower atmosphere, Toohey said. In the meantime, the extra water might also speed up ozone loss in the atmosphere, Rosenlof added.

But it’s hard for scientists to say for sure, because they’ve never seen an eruption like this one.

The stratosphere stretches from around 7.5 miles to 31 miles (12 km to 50 km) above Earth and is usually very dry, Voemel explained.

Voemel's team estimated the volcano’s plume using a network of instruments suspended from weather balloons. Usually, these tools can’t even measure water levels in the stratosphere because the amounts are so low, Voemel said.

Another research group monitored the blast using an instrument on a NASA satellite. In their study, published earlier this summer, they estimated the eruption to be even bigger, adding around 150 million metric tons of water vapor to the stratosphere — three times as much as Voemel's study found.

Voemel acknowledged that the satellite imaging might have observed parts of the plume that the balloon instruments couldn’t catch, making its estimate higher.

Either way, he said, the Tongan blast was unlike anything seen in recent history, and studying its aftermath may hold new insights into our atmosphere.

___

The Associated Press Health and Science Department receives support from the Howard Hughes Medical Institute’s Department of Science Education. The AP is solely responsible for all content.

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2022-09-22 18:10:55Z
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James Webb space telescope captures Neptune rings and moons - Sky News

NASA has released new images capturing Neptune and its rings, taken by the James Webb space telescope in July.

Neptune is the solar system's outermost planet which has thin rings with faint dust bands around it.

These have been observed in infrared for the first time, allowing for seven of Neptune's 14 moons to be captured.

The seven that can be viewed from the newly-released shots are Galatea, Naiad, Thalassa, Despina, Proteus, Larissa, and Triton.

Triton is Neptune's largest and most unusual moon, which dominates the James Webb image of Neptune as a beaming point of light, creating signature diffraction spikes that are seen in many images.

Webb recently showed Jupiter at its clearest in photos publicised last month.

The new telescope was launched last Christmas and experts are hope to be able to look back to the beginning of time when stars and galaxies were formed.

James Webb Space Telescope  captures  view of  Neptune's  rings 
Credit: NASA, ESA, CSA, STScI

NASA's Voyager 2 was the first spacecraft to view the icy, blue planet of Neptune in a 1989 flyby.

Heidi Hammel, of the Space Science Institute, said it had been three decades since astronomers last saw the rings from Neptune in detail.

And Ms Hammel wrote on Twitter: "More than 20 years in the making, and the James Webb Space Telescope delivered.

"...And that bright blue "star"? That's no star! That's Neptune's fantastic moon Triton! It looks brighter than Neptune because at these near-IR wavelengths, Neptune's atmospheric methane absorbs sunlight, making the planet darker - this is also why the rings pop out."

James Webb is the world's biggest and most powerful telescope and is floating about 930,000 miles above us.

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2022-09-22 11:37:17Z
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Trending on WION | James Webb telescope captures stunning image of Neptune and its rings - WION

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2022-09-22 09:24:15Z
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Rabu, 21 September 2022

Blinding light of Mars spotted by Webb telescope - CTV News

The James Webb Space Telescope's main goal is to detect faint light from distant galaxies, but it recently observed one of the brightest objects in the night sky: Mars.

The space observatory captured its first images and data of the red planet on September 5.

Multiple orbiters above Mars, and the land-bound rovers Curiosity and Perseverance, roam the surface, regularly send back insights. Webb's infrared capabilities contribute another perspective that could reveal details about the Martian surface and atmosphere.

Webb, located a million miles (1.6 million kilometres) from Earth, can spot the sunlit side of Mars that faces the space telescope, which puts the observatory in the perfect position to spy the planet's seasonal changes, dust storms and weather all at once.

The telescope is so sensitive that astronomers had to make adjustments to prevent the blinding infrared light of Mars from saturating Webb's detectors. Instead, Webb observed Mars using very short exposures.

The new images depict Mars' eastern hemisphere in different wavelengths of infrared light. To the left is a reference map of the hemisphere captured by the Mars Global Surveyor mission, which ended in 2006.

The top-right image from Webb shows reflected sunlight on the Martian surface, showcasing Martian features like the Huygens Crater, dark volcanic rock and the Hellas Planitia, a massive impact crater on the red planet that stretches for more than 1,200 miles (2,000 kilometres).

The lower-right image shows the thermal emission of Mars, or the light emitted by the planet as it loses heat. The brightest areas indicate the warmest spots. Additionally, astronomers spotted something else in the thermal emission image.

When this thermal light passes through the Martian atmosphere, some of it is absorbed by carbon dioxide molecules. This phenomenon has caused the Hellas Planitia to appear darker.

"This is actually not a thermal effect at Hellas," said Geronimo Villanueva, a planetary scientist at NASA's Goddard Space Flight Center, in Greenbelt, Maryland, in a statement.

"The Hellas Basin is a lower altitude, and thus experiences higher air pressure," said Villanueva, who is also the principal investigator of Mars and Ocean Worlds studies for Webb. "That higher pressure leads to a suppression of the thermal emission at this particular wavelength range due to an effect called pressure broadening. It will be very interesting to tease apart these competing effects in these data."

With Webb's powerful capabilities, Villanueva and his team also captured the first near-infrared spectrum of Mars.

The spectrum indicates more subtle differences in brightness across the planet, which could highlight aspects of the Martian surface and atmosphere. An initial analysis has revealed information about icy clouds, dust, rock types on the surface and the composition of the atmosphere contained in the spectrum. There are also signatures of water, carbon dioxide and carbon monoxide.

The NASA research team will share more about Webb's observations of Mars in a study that will be submitted for peer review and publication in the future. And the Mars team is looking forward to using Webb's capabilities to pick out the differences between regions on the red planet and search for gases like methane and hydrogen chloride in the atmosphere.

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2022-09-21 15:11:51Z
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Exoplanets study reveals uniqueness of Earth's climate - Innovation News Network

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  1. Exoplanets study reveals uniqueness of Earth's climate  Innovation News Network
  2. Earth-like exoplanets unlikely to be another 'pale blue dot'  Phys.org
  3. View Full coverage on Google News

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2022-09-21 09:32:06Z
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Selasa, 20 September 2022

Philadephia’s Diatom Archive Is a Way, Way, Wayback Machine - Hakai Magazine

Article body copy

Nestled in the heart of Philadelphia, Pennsylvania, the Academy of Natural Sciences of Drexel University emanates the aura of a sprawling cabinet of curiosities. Its neoclassical facade is covered in natural motifs—doorways flanked by ammonites, handrails that curl into ferns, bronze door handles shaped like ibis skulls. As the oldest natural science institution in the western hemisphere, the academy has accumulated a trove of remarkable specimens. Among the 19 million or so specimens housed here are plants procured on the Lewis and Clark Expedition, blue marlin reeled in by Ernest Hemingway, and America’s first mounted dinosaur skeleton.

Many of the academy’s most unassuming yet impactful treasures are filed away on its second floor, in an office space crowded with hulking cabinets and microscopes. Next to one of these microscopes, curator Marina Potapova pops open a notebook-sized plastic container brimming with glass slides. To the untrained eye, these unremarkable slides seem filthy—each looks like it’s been smudged by dirty fingers.

But as soon as Potapova slips one under a microscope lens, the slide’s contents dazzle. Dozens of diatoms—microscopic, single-celled algae encased in sturdy silica walls and found wherever there is water—are fixed to the slides in a myriad of shapes.

container of microscope slides

With over four million specimens, the Academy of Natural Sciences of Drexel University’s diatom collection in Philadelphia, Pennsylvania, is the second largest in the world. Photo by Jack Tamisiea

Some are elongated like baguettes or flattened into saucers while others hook together to resemble translucent centipedes. Others are barbed like harpoons or shaped like pudgy sea stars. Some even resemble ornate stained-glass windows. Under a microscope, a few drops of murky pond water become a kaleidoscope of diatom diversity.

The beauty of diatoms is impressive. But their ecological significance is staggering. Diatoms anchor marine food webs by feeding everything from minuscule zooplankton to mammoth filter feeders. (Case in point: scientists have deduced that the rise of whales some 30 million years ago mirrors a spike in diatom diversity.) Diatoms also have an outsized atmospheric impact. As one of the planet’s most prolific organisms, diatoms siphon harmful gases like carbon dioxide out of the air and produce massive stores of oxygen as they photosynthesize. It is estimated that roughly one-quarter of the air we breathe is created by diatoms.

More than four million specimens of these essential algae are plastered onto hundreds of thousands of slides and housed in the academy’s diatom herbarium. Only London’s Natural History Museum stores more slides of diatoms.

Although the academy’s diatoms no longer feed the planktonic masses or pump oxygen into the atmosphere, they do hold clues about how the aquatic world is changing. As their tough shells sink to the bottom of a body of water, they are stored in the sediment for millennia. When researchers use a sediment core to drill down into the muddy bottom of an estuary, they are collecting diatoms deposited over the eons.

In addition to being plentiful and hardy, diatoms are also a crucial barometer for a variety of environmental conditions. The existence of certain diatom species can help scientists pinpoint everything from industrial pollution to oxygen depletion. Potapova and her colleagues have recently used these water condition time capsules to gauge how accelerating sea level rise is endangering New Jersey’s coastal wetlands.

diatoms

Diatoms, a type of phytoplankton made of silica and coming in myriad shapes and forms, underpin marine food webs and have an outsized impact on the health of Earth’s atmosphere. Photo by Scenics & Science/Alamy Stock Photo

Thanks to a relative dearth of environmental monitoring, the historical decline of these crucial marshes—which hoard carbon, provide nursery grounds for fish, and buffer the coast from storms—has largely been obscured, making restoration efforts little more than guesswork.

However, the millions of diatoms stored at the academy are helping the researchers track the fall of the coastal wetlands as the ocean rises, which may help anticipate the coast’s future. “Diatoms are absolutely invaluable environmental archives,” Potapova says. “You can infer the future from what they tell you about the past.”


Considering the academy’s history, it is no wonder that the storied institution has become a hub for diatoms. With the advent of accessible microscopy in the 1850s, many of Philadelphia’s gentleman naturalists were captivated by the realm of minute microbes, eventually establishing the Microscopical Society of Philadelphia at the academy.

Because of their striking beauty, diatoms took the microscopical society by storm. To satiate their interest, many of these diatomists headed east to the New Jersey coastline to collect samples, which they mounted onto glass slides using a steady hand and a brush brimming with pig eyelashes. The hobbyists would then gather at the academy to show off their slides at gourmet luncheons.

The academy’s early members were clearly enthusiastic about diatoms, but most were amateurs and published little research on the myriad of specimens they collected. Organizing the mountains of slides compiled by each collector into a cohesive collection proved to be quite the task for Ruth Patrick when she arrived at the academy in 1933. The daughter of an amateur diatomist who received her first microscope at the age of seven, Patrick gravitated toward diatoms early in her childhood and eventually completed her PhD studying the microscopic organisms. Despite her scientific credentials, she was relegated to setting up microscopes and slides for the untrained hobbyists. It took her years to even gain membership in the male-dominated academy. But her persistence paid off, and in 1937 she became curator of the nascent diatom herbarium.

Patrick’s first goal was organizing the amalgamation of different collections into a unified and comprehensive source for taxonomic research. When she was not mounting and organizing slides, she was wading into nearby ponds and streams to collect new specimens in the field, where she gradually gained an appreciation for the ecological importance of diatoms.

Ruth Patrick

Ruth Patrick, the first curator of the academy’s diatoms, works on the collection in the 1940s. Photo courtesy of Academy of Natural Sciences Archives coll. 457

This crystalized during a 1948 expedition to Pennsylvania’s Conestoga River—a body of water heavily polluted by sewage and industrial runoff. As her team collected samples from throughout the creek, she recognized patterns in the diatom composition. Some species’ densities exploded in areas contaminated with sewage, while others thrived in spots tainted with chemicals. Soon, Patrick became adept at using the existence of certain diatoms as a key for diagnosing pollution in lakes and rivers. This supported the idea that greater diatom diversity correlated with healthier freshwater ecosystems—an insight ecologists coined the Patrick Principle.

Patrick revolutionized the use of diatoms to monitor freshwater systems, but using them in coastal wetlands lagged behind. The brackish fusion of fresh and salt water in coastal zones such as estuaries creates habitats that are dynamic and complex with a mixture of inland and oceanic diatoms, according to Mihaela Enache, a research scientist at the New Jersey Department of Environmental Protection (NJDEP).

However, in recent decades, the sea has dominated the once-dynamic coastal margin, propelling farther inland as sea levels rise. Over the last century, the sea level along New Jersey has risen by 0.45 meters, more than double the global average of 0.18 meters. By 2100, the sea could rise by over a meter.

This dramatic rise in sea level has proven disastrous for the patchwork of marshes along New Jersey’s coastline, several of which have already succumbed to the sea. However, the full extent of the loss of these wetlands is difficult to parse because environmental monitoring only dates back a few decades.

Without a sense of a wetland’s natural conditions, ecological restoration is daunting. Having that information is crucial, says Enache. “Without [it], you are in the dark.” Thankfully, some of this missing data is recorded in the academy’s cache of diatoms.


Like most coastal margins, New Jersey is familiar with sea level rise. During the Pleistocene, when New Jersey was blanketed by ice and home to mastodons, sea ice slurped up stores of seawater. Around 18,000 years ago, sea levels sank more than 130 meters below their current levels—extending the New Jersey coastline 110 kilometers farther into the Atlantic Ocean.

The end of the last ice age sparked a steady climb in sea levels. Retreating ice sheets caused parts of New Jersey to sink. This subsidence, combined with glacial melt, proved a potent mix for rapid sea level rise according to Jennifer Walker, a sea level researcher at Rutgers University.

In a study published last year, Walker turned to the past to put New Jersey’s current bout of sea level rise in context. “If we can understand how temperatures, atmosphere, and sea level changes are all interconnected in the past, that’s what we can use to project changes in the future.”

To gauge fluctuating sea levels over the past 2,000 years, her team examined the shells of single-celled protists called foraminifera that are finely calibrated to specific environmental conditions. This makes them a valuable proxy for reconstructing shifts in sea levels. By identifying the presence of certain foraminifera species throughout sediment cores collected from different spots along the Jersey shore, her team concluded that New Jersey’s coast is experiencing the fastest rise of sea level in 2,000 years.

The NJDEP hoped diatoms could serve as a similar tool for understanding how coastal marshes responded to the rising sea. Like foraminifera, each diatom species is extremely sensitive to environmental conditions. For example, species like the rolling pin–shaped Nitzschia microcephala thrive in nitrogen-rich environments, making their shells a common sign of nutrient pollution. Other species, like Diploneis smithii, whose segmented shell resembles a slender trilobite, prefer saline waters. Their existence inland is a good indication of past sea level intrusion and helps researchers deduce which marshes have been prone to flooding in the past.

To pinpoint where these microscopic indicators once existed, the NJDEP deployed a team of researchers into several marshes along the coastline, ranging from heavily polluted wetlands in the north to near-pristine tidal marshes in the south. At each site, they cored into the marsh muck, sampling as deep as two meters in certain spots. Enache compares this method to slicing into a stack of pancakes—as you cut deeper, you are essentially going back in time from the steaming pancake just off the griddle to the soggy pancake deposited at the bottom of the stack. As they dug deeper, the researchers were traveling back decades. In total, they collected nine cores from five wetlands.

The NJDEP then sent the sediment cores to Philadelphia, where Potapova and her master’s student Nina Desianti gauged the diatom diversity of New Jersey’s coastal wetlands through time. Desianti began processing the diatom specimens by soaking the sediment samples in strong acid to dissolve everything but the silica shell before adhering them to slides. The result was an environmental history of each of the five marshes mounted onto thousands of glass slides. Then, by using the specimens already cataloged at the academy, they played a microscopic game of who’s who. But even the sprawling diatom herbarium lacked all the answers—Desianti estimates that over one-third of the 900-odd species they collected from the wetlands are new to science.

Marina Potapova

Marina Potapova, curator at the Academy of Natural Sciences of Drexel University, samples for diatoms. Photo courtesy of Academy of Natural Sciences of Drexel University

The monumental effort yielded the tome Diatom Flora of the New Jersey Coastal Wetlands in 2019. To the uninitiated, it is an overwhelming mix of intimidating Latinized names and dramatic electron microscope photographs that portray the diatoms in all their infinitesimal glory. To Enache, it’s the key to decoding the decline of New Jersey’s wetlands. By punching the composition of diatom species and modern wetland conditions into modeling programs, Enache is able to illustrate what a wetland once looked like. “Diatom species are a very precious environmental archive because we can go back in time—when nobody could take measurements of nutrients, nobody could take measurements of pH—and actually use the diatom species to get complete numbers,” she says. These figures help her record the increase of everything from agricultural nutrients to industrial chemicals in New Jersey’s water all the way back to the mid-1600s, when Europeans arrived and began to dramatically alter the state.

But while diatoms offer a window into the decline of New Jersey’s marshes, they also offer a glimpse of environmental resiliency to Desianti. Just as the team used the salt tolerance of different diatoms to map past episodes of sea level rise, they could also use the microscopic algae to deduce how these marshes responded to saltwater intrusion.

When it comes to habitats, marshes are particularly dynamic. As the boggy barriers between land and sea, coastal marshes hoard sediment, building vertically to stay above the rising ocean. When sea level rise outpaces their accumulation of sediment, the marshes retreat inland by spilling into coastal forests. As the marsh’s briny water percolates into the groundwater, it kills the trees, creating what ecologists call “ghost forests” of desiccated tree husks.

Marina Potapova at a microscope

Potapova examines diatoms sampled from the coast in an Academy of Natural Sciences of Drexel University lab. Photo by Jack Tamisiea

While coastal marshes are naturally pliable, anthropogenic impacts have rendered them brittle. In New Jersey, dams strain out sediment, robbing the marsh of construction material, and retreating marshes butt up against paved roads and vacation homes. “Salt marshes have to compete with us in establishing habitat,” says Desianti, who now uses diatoms to track nutrient pollution for the Wisconsin State Laboratory of Hygiene. “As a result, these salt marshes are squeezed between sea level rise and human pressures.”


The diatoms Potapova and Desianti collected and identified will help the NJDEP not only understand how New Jersey’s coastal wetlands have responded to past bouts of sea level rise but also inform what can be done to restore these vibrant ecosystems.

The deeper you core into the pond muck, the more diverse the diatoms tend to be, which, as Ruth Patrick deduced decades ago, is the trademark of a healthy ecosystem. As you examine a core’s more recent chapters, this diatomic diversity often decreases as certain specialists, like salt-loving marine diatoms, dominate. Understanding where these saline-specializing species persist reveals which ecosystems have succumbed to sea level rise and where restoration efforts, like an influx of sediment, are needed the most.

Diatoms are not a cure for threats like sea level rise and pollution. Instead, they are a key to help combat them. They reveal what pristine habitats were once like long before anyone paid attention and illustrate what has gone awry over the centuries. To enact successful wetland restoration measures, it would be wise to consult these microscopic algae.

Which is why the diatom specimens Potapova and Desianti collected in New Jersey’s coastal marshes are being filed away alongside Patrick’s specimens in the diatom herbarium’s steel cabinets. Similarly to how they persist in sediment for millennia, the diatom specimens stored at the academy will offer invaluable data points for future researchers to make sense of pollution and shifting sea levels.

“The diatom herbarium is an invaluable resource for diatom research,” says Desianti. “I’m sure that in the future, even when I’m gone, people will still access this collection and continue to investigate environmental issues.” She is confident that within the tens of thousands of slides deposited in the recesses of the academy are environmental breakthroughs waiting to be decoded.

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