Saturday, August 28, 2021

US achieves laser-fusion record: what it means for nuclear-weapons research

People inside the NIF Target Chamber

The US National Ignition Facility (target chamber shown) is the size of three American football fields.Credit: Lawrence Livermore National Laboratory

Scientists at the US Department of Energy’s flagship laser facility shattered their own record earlier this month by generating more than 10 quadrillion watts of fusion power for a fraction of a second — roughly 700 times the generating capacity of the entire US electrical grid at any given moment. News of the breakthrough has revived hopes that the long-troubled National Ignition Facility (NIF) might yet attain its goal of producing more energy than it consumes in a sustained fusion reaction.

Housed at Lawrence Livermore National Laboratory, the US$3.5-billion facility wasn’t designed to serve as a power-plant prototype, however, but rather to probe fusion reactions at the heart of thermonuclear weapons. After the United States banned underground nuclear testing at the end of the cold war in 1992, the energy department proposed the NIF as part of a larger science-based Stockpile Stewardship Program, designed to verify the reliability of the country’s nuclear weapons without detonating any of them.

With this month’s laser-fusion breakthrough, scientists are cautiously optimistic that the NIF might live up to its promise, helping physicists to better understand the initiation of nuclear fusion — and thus the detonation of nuclear weapons. “That's really the scientific question for us at the moment,” says Mark Herrmann, Livermore’s deputy director for fundamental weapons physics. “Where can we go? How much further can we go?”

Here Nature looks at the NIF’s long journey, what the advance means for the energy department’s stewardship programme and what lies ahead.

How does the NIF achieve nuclear fusion?

Ten storeys high and spanning the area of three American football fields, the NIF houses an array of optics and mirrors that amplify and split an initial pulse of photons into 192 ultraviolet laser beams, ultimately focusing them onto a target that is smaller than a pencil eraser. The beams hit the target — a gold cylinder — with around 1.9 megajoules of energy in less than 4 billionths of a second, creating temperatures and pressures seen only in stars and thermonuclear bombs.

Faced with this pulse power, the cylinder, which holds a frozen pellet of deuterium and tritium, collapses as the hydrogen isotopes at the pellet’s core heat up, fuse and generate helium nuclei, neutrons and electromagnetic radiation. The goal is to unleash a cascade of particles that leads to more fusion and more particles, thus creating a sustained fusion reaction; by definition, ‘ignition’ occurs when the fusion reaction generates more energy than it consumes. Preliminary results from the experiment on 8 August indicate that fusion reactions generated a record-shattering 70% of the power that went into the experiment — nearly achieving ignition.

The NIF began operations in 2009. Why has it taken so long to (nearly) achieve ignition?

Nobody said it would be easy, but building the NIF proved to be a more complex endeavour than officials originally thought. Construction began in 1997 and ended more than a decade later, several years behind schedule and at least $2.4 billion over budget.

The NIF missed its goal of achieving ignition by 2012; scientists have spent the years since fine-tuning the facility and introducing optimized targets into the reaction chamber. The recent success was achieved after multiple changes to the massive system, including new diagnostics, improved target-fabrication techniques and enhancements to the precision of the lasers.

NIF Target Positioner

The NIF focuses 192 laser beams onto a target, creating temperatures and pressures like those inside thermonuclear bombs.Credit: Lawrence Livermore National Laboratory

Long before the NIF fired its first shot, it was surrounded by controversy. Independent scientists raised questions about both the design and management of the facility. As recently as May 2016, the US National Nuclear Security Administration (NNSA), a branch of the Department of Energy (DOE) that oversees nuclear weapons and funds the NIF to the tune of around $350 million per year, questioned whether the facility would ever achieve its ignition goal.

But even long-time critics of the facility have acknowledged the recent breakthrough as a significant step forward. Stephen Bodner, a plasma physicist who formerly worked at the US Naval Research Laboratory in Washington DC, said he is both “surprised and pleased” with the result — assuming it’s reproducible. “I look forward to reading the scientific report that explains it,” he says.

The Livermore team and its collaborators are just beginning to pore over results, but preliminary data suggest an eight-fold increase in energy yield compared with experiments conducted several months ago, and a 25-fold increase compared with the previously reported record, set in 2018. Laboratory officials said they made the announcement about the experiment before peer-reviewed publication because news of the results was already spreading through the fusion community.

If the NIF achieves full ignition, what could the results teach scientists about nuclear weapons?

In theory, the NIF could offer a better understanding of the precise conditions necessary to initiate and sustain a fusion reaction — which is, in a sense, what the facility’s scientists have been working out as they’ve optimized the system over the past 12 years. This question is also at the heart of the stockpile stewardship programme.

Since 1992, physicists have been building a comprehensive programme to study the US nuclear arsenal with increasingly powerful supercomputers and dozens of other research facilities designed to test everything from nuclear materials and components to explosives. Although the NIF is not detonating miniature bombs, says Herrmann, its experiments could help scientists improve the computer models they use to simulate how weapons will detonate, potentially reducing uncertainties. Other experiments might test how the electronics and other components in a weapon hold up in the face of intense bursts of radiation expected in a hostile war environment.

Many scientists argue that the facility also bolsters confidence in the nation’s weapons stockpile — and wards off external threats — by helping to attract young researchers to the nuclear field and maintaining a broader scientific enterprise. “There is an overall element of showing scientific prowess that is important as well,” says Herrmann.

But is the NIF essential to the US stockpile stewardship programme?

Some critics have questioned whether scientists need the facility to maintain the United States’ nuclear weapons. They say the stewardship programme has already bolstered confidence in the stockpile within the NNSA, and point out that the agency is now proposing to build what are effectively new nuclear weapons, rather than simply maintaining the current cache with minimal changes.

“That shows either an enormous amount of hubris, or an incredible confidence that you can build a lot of what we need for the next 50 years, even without a functioning NIF,” says Hans Kristensen, who heads the nuclear information project at the Federation of American Scientists in Washington DC.

Herrmann argues that the NIF can still help, though. He says nuclear weapons scientists are constantly extrapolating from limited experimental data as they evaluate their computer simulations. Information gathered from more energetic fusion reactions at the NIF, he says, will allow them to test the models more directly, hopefully reducing uncertainties and making it easier for the NNSA to certify that weapons in the arsenal will detonate if needed, and not before.

So what happens next for the NIF?

The ultimate test — whether the team can replicate its 8 August success — could come as early as October, say laboratory officials. Meanwhile, scientists are rushing to understand and publish their findings. Because the facility is operating at the scientific edge of what is possible, even slight variations in the manufacture of the target capsule or the tuning of the lasers could cause the system to produce more, or less, energy than the earlier experiment, says Herrmann. “We can’t do the exact same target experiment, because we blew the target up,” he says. But with time, he adds, the science team should be able to repeat and build on this success — and push the facility even further.

doi: https://doi.org/10.1038/d41586-021-02338-4

 

Why Nuclear Fusion Is Still The Holy Grail Of Clean Energy

Just 100 years ago, when English mathematician and astronomer Arthur Eddington suggested that the stars power themselves through a process of merging atoms to create energy, heat, and light, the idea was an unthinkable novelty. Now, in 2021, we’re getting remarkably close to recreating the process of nuclear fusion here on Earth.  Over the last century, scientists have been steadily chasing commercial nuclear fusion, ‘the holy grail of clean energy.’ The first direct demonstration of fusion in a lab took place just 12 years after it was conceptualized, at Cambridge University in 1932, followed by the world’s first attempt to build a fusion reactor in 1938. In 1950, Soviet scientists Andrei Sakharov and Igor Tamm propelled the pursuit forward with their development of the tokamak, a fusion device involving massive magnets which is still at the heart of many major fusion pursuits today, including the world’s biggest nuclear fusion experiment ITER.

Since that breakthrough, scientists have been getting closer and closer to achieving nuclear fusion. While fusion has indeed been achieved in labs throughout this timeline, it has always required far more energy than it emits, defeating the purpose of the commercial fusion initiative. If unlocked, commercial nuclear fusion would change life as we know it. It would provide an infinite source of clean energy requiring no fossil fuels and leaving behind no hazardous waste products. 

Nuclear fission, the process which powers all of our nuclear energy production now, requires the use of radioactive isotopes to achieve the splitting of atoms, and leaves behind waste products which remain hazardous to human and ecological health for up to tens of thousands of years. Not only does nuclear fusion leave nothing behind, it is many times more powerful. Yet, it has remained elusive despite decades of attempts and considerable investment and collaboration from both public and private entities around the world. 

Related: Oil Glut In Asia Worsens

But just this month there was an incredible breakthrough that may indicate that we are getting close. “For an almost imperceptible fraction of a second on Aug. 8, massive lasers at a government facility in Northern California re-created the power of the sun in a tiny hot spot no wider than a human hair,” CNET reported in August. This breakthrough occurred at the National Ignition Facility, where scientists used lasers to set off a fusion reaction that emitted a stunning 10 quadrillion watts of power. Although the experiment lasted for just 100 trillionths of a second, the amount of energy it produced was equal to about “6% of the total energy of all the sunshine striking Earth's surface at any given moment.”

Even more importantly than the stunning power of the reaction, however, was the fact that scientists observed that this hotspot was able to “ ignite a self-sustaining chain reaction.” This means that the fusion caused by the lasers was able to cause additional fusion reactions in a continuous chain of energy production, a breakthrough that lies at the heart of commercially successful nuclear fusion. While this experiment still was unable to produce more energy than went into its production, it marks a monumentally important milestone in the journey to finally creating net energy with human-created nuclear fusion.

"This phenomenal breakthrough brings us tantalizingly close to a demonstration of 'net energy gain' from fusion reactions -- just when the planet needs it," said Arthur Turrell, physicist and nuclear fusion expert. What’s more, scientists and experts are hopeful that the rate of fusion breakthroughs will continue to speed up, and commercial nuclear fusion could be achieved sooner than ever seemed possible before. At a time when it has never been more important or more urgent to find a powerful and affordable means of producing clean energy, commercial nuclear fusion can’t come fast enough. 

By Haley Zaremba for Oilprice.com


Martian cave entrances may offer the perfect radiation shelter for human settlements

Mars is bombarded by a ton of radiation. But cave entrances block most of these dangerous rays.



   
The entrance of a Martian cavern. Credit: NASA, JPL and University of Arizona.

There are very good reasons why Mars is such a desolate, barren landscape. With no thick atmosphere nor a magnetic field, the Red Planet’s surface is bombarded daily by radiation up to 900 times higher than seen on Earth. However, some places are sheltered. New research has found that cave entrances are shielded from the harmful radiation that normally hits Mars. This may make them ideal as both sites for future settlements and robotic missions meant to scour for signs of alien life.

Despite amazing advances in space exploration in the last decade, if we’re going to take the idea of settling Mars sometime during this century seriously, there are many challenges that need to be overcome. That’s unless we’re content with one-way suicide missions.

There’s no shortage of environmental hazards out to kill any astronaut bold enough to dare set foot on Mars. For one, the planet only has 0.7% of Earth’s sea-level pressure, meaning any human on Mars must wear a full pressure suit or stay barricaded inside a pressure-controlled chamber, otherwise oxygen wouldn’t flow through the bloodstream and the body could swell and bleed out.


Then there’s the issue of radiation. Mars is farther away from the Sun than Earth, receiving roughly 60% of the power per square meter seen on a similar site on Earth. But since Mars doesn’t have a magnetic field to deflect energetic particles, coupled with the paper-thin atmosphere, its surface is exposed to much higher levels of radiation than Earth. Furthermore, besides regular exposure to cosmic rays and solar wind, it receives occasional, lethal radiation blasts due to strong solar flares.

Measurements performed by the Mars Odyssey probe suggest that ongoing radiation levels on Mars are at least 2.5 times higher than what astronauts experience on the International Space Station. That’s about 22 millirads per day, which works out to 8000 millirads (8 rads) per year. For comparison, the people in the U.S. are exposed to roughly 0.62 rads/year on average.

Any attempt to colonize the Red Planet will require measures to ensure radiation exposure is kept to a minimum. Some of the proposed ideas thus far involve habitats built directly into the ground or even above-ground habitats using inflatable modules encased in ceramics.

But a better idea may be to take advantage of the natural shelters already in place. Mars is dotted with deep pits, caves, and lava tube structures across its surface. According to a new study performed by researchers led by Daniel Viúdez-Moreiras at Spain’s National Institute for Aerospace Technology, many of these caverns could offer ample protection to human settlers.

“Caves and their entrances have been proposed as habitable environments and regions that could have preserved evidence of life, mostly due to their natural shielding from the damaging ionizing and non-ionizing radiation present on the surface. However, no studies to date have quantitatively determined the shielding offered by these voids on Mars,” the researchers wrote in the journal Icarus.

The researchers found that the levels of UV radiation inside Martian caverns were, in some cases, ~2% of those values found on the surface.

“Numerical simulations of cave entrances show a reduction even more than two orders of magnitude in UV radiation, both in the maximum instantaneous and cumulative doses, throughout the year and at any location of the planet,” the researchers found.

What’s more, the amount of active radiation is still higher than the minimum required for Earth-like photosynthesis. In other words, cave entrances could shelter both humans and their plant food source. However, it’s unclear whether ionizing radiation — the kind of electromagnetic radiation associated with cancer — is blocked in the same way as UV radiation.

“Ionizing radiation doesn’t present exactly the same behavior as UV radiation,” Viúdez-Moreiras. told New Scientist. “However, it is expected that ionizing radiation will also be strongly attenuated in pit craters and cave skylights.”   






Tharsis caves from the MGC3 catalog. Credit: G. Cushing and USGS.

High-resolution surface imaging data recorded over the past couple of decades by instruments like the Mars Reconnaissance Orbiter Context Camera system (CTX), together with Mars Odyssey’s thermal emission imaging system (THEMIS), suggest that the Tharsis bulge may be the best region for cave candidates on Mars. More than 1,000 suitable caves have been identified in this region, which also contains three enormous shield volcanoes, Arsia Mons, Pavonis Mons, and Ascraeus Mons.

Tharsis city sounds like an awesome name for the first human settlement on Mars. Remember the name.

 

Bacterial bloom as the Earth thawed

Bacterial bloom as the Earth thawed
Changes in Earth's environment and lifeforms during the Snowball Earth and its aftermath 650-630 million years ago. Black arrows show changes. The appearance of a supercontinent caused a decrease in ocean volcanism, which resulted in a decrease in atmospheric CO2 and the Snowball Earth. Red words show new findings in this paper. Credit: Kunio Kaiho

Around 650 million years ago, the Earth entered into the Marinoan glaciation that saw the entire planet freeze. The "Snowball Earth" impeded the evolution of life. But as it warmed, biotic life began to flourish. A research team from Tohoku University has analyzed rock samples from China to tell us more about this transition.

Some researchers hypothesize that ice sheets enveloped the earth during the Marinoan glaciation (650–535 million years ago) in what is dubbed the "Snowball Earth." The glaciation also impacted the climate and chemical compositions of the oceans, restraining the evolution of early life. Yet, as the earth warmed, and the Ediacaran period dawned, biotic life began to evolve.

A research team from Tohoku University has unveiled more about the evolutionary process of the Marinoan-Ediacaran transition. Using biomarker evidence, they revealed possible photosynthetic activity during the Marinoan glaciation. This was followed by photosynthetic organisms and bacteria entering a period of low productivity. However, as eukaryotes expanded during the early Ediacaran period, they blossomed.

Dr. Kunio Kaiho, who co-authored a paper with Atena Shizuya, said, "Our findings help clarify the evolution of primitive to complex animals in the aftermath of the Snowball Earth." Their paper online was published in the journal Global and Planetary Change on August 8, 2021.

The late Neoproterozoic era (650–530 million years ago) witnessed one of the most severe ice ages in the Earth's 4.6-billion-year history. Researchers believe that ice sheets covered the entire  since glaciogenic units, such as ice-rafted debris, are distributed globally. Overlaying these glaciogenic formations are cap carbonates. These precipitate under warm conditions and therefore suggest that the glacial environment changed rapidly into a greenhouse environment.

The Snowball Earth hypothesis purports the atmospheric carbon dioxide concentration controlled the change from a frozen state to an ice-free state. Ice sheet-covered oceans prevented the dissolution of carbon dioxide into seawater during the Marinoan ice age, meaning greenhouse gas concentration, emitted by volcanic activity, increased gradually. Once the extreme greenhouse effect kicked in, glaciers melted and excess carbon dioxide precipitated on glaciogenic sediments as cap carbonates.

Whilst the Snowball Earth theory explains the wide distributions of glacial formations, it fails to shed light on the survival of living organisms. To counteract this, some researchers argue that sedimentary organic molecules, a molecular clock, and fossils from the late Neoproterozoic era are evidence that primitive eukaryotes such as sponges survived this severe ice age. Alternative models also propose that an ice-free open sea existed during the glaciation and acted as an oasis for marine life

But what is understood is that the Marinoan glaciation and the succeeding extreme climatic transition likely had a marked impact on the biosphere. Shortly after the ice age, the Lantian biota, the earliest-known complex macroscopic multicellular eukaryotes, emerged. The Lantian biota includes macrofossils that are phylogenetically uncertain but morphologically and taxonomically diverse. Meanwhile, pre-Marinoan species have simple body plans with limited taxonomic variety.

Bacteria and eukaryote biomarkers demonstrate that bacteria dominated before the glaciation, whereas steranes/hopanes ratios illustrate that eukaryotes dominated just before it. However, the relationship between the biosphere changes and the Marinoan glaciation is unclear.

In 2011, Kaiho and his team traveled to Three Gorges, China under the guidance of China University of Science's Dr. Jinnan Tong to take sedimentary rock samples from the deeper outcrops of marine sedimentary rocks. From 2015 onwards, Shizuya and Kaiho analyzed the biomarkers of algae, photosynthetic activity, bacteria, and eukaryotes from the rock samples.

They found photosynthetic activity based on n-C17 + n-C19 alkanes for algae and pristane + phytane during the Marinoan . Hopanes within the early and late carbonate deposition showed  and other bacteria entering a state of low productivity before recovering. And steranes from carbonates and mudstones after the cap carbonate deposition from the early Ediacaran period indicated the expansion of eukaryotes. The expansion of eukaryotes corresponded to the Lantian biota being morphologically diverse when compared to pre-Marinoan species.

Kaiho believes we are one step closer to understanding the evolutionary process that occurred before and after Snowball Earth. "The environmental stress of closed ocean environments for the atmosphere followed by high temperatures around 60°C may have produced more complex animals in the aftermath." Their findings show that bacterial recovery preceded eukaryotes' domination.

Kaiho's team is doing further studies to clarify the relationship between climate change and the biosphere in other locations. They are also studying the relationship between atmospheric oxygen increases and animal evolution from the late Cryogenian to early Cambrian (650 to 500 million years ago).

Changes in Earth's orbit enabled the emergence of complex life

More information: Atena Shizuya et al, Marine biomass changes during and after the Neoproterozoic Marinoan global glaciation, Global and Planetary Change (2021). DOI: 10.1016/j.gloplacha.2021.103610

Provided by Tohoku University 

6 mysterious structures hidden beneath the Greenland ice sheet

By Stephanie Pappas 

Nearly 2 miles thick in places, the ice sheet hides a landscape of canyons, mountains, fjords and gem-like lakes.

There are many hidden wonders beneath Greenland's ice sheet. (Image credit: Martin Zwick/REDA&CO/Universal Images Group)

Fridtjof Nansen, the leader of the first expedition to cross Greenland, once described what he found in the Arctic as "the great adventure of the ice, deep and pure as infinity." Nansen, who made his journey in 1888, could not have known of the wonders hidden below the icy landscape beneath his skis.

Today, thanks to radar and other technologies, the part of Greenland that sits below its 9,800-foot-thick(3,000 meters) ice sheet is coming into focus. These new tools reveal a complex, invisible landscape that holds clues to the past and future of the Arctic.
The world's longest canyon

3D view of the subglacial canyon, looking northwest from central Greenland. (Image credit: J. Bamber, University Bristol)


The Greenland ice sheet hides the longest canyon in the world.

Discovered in 2013, the canyon stretches 460 miles (740 kilometers) from the highest point in central Greenland to Petermann Glacier on the northwest coast. That's significantly longer than China's 308-mile-long (496 km) Yarlung Tsangpo Grand Canyon, the longest canyon on the planet that you can actually see.

The canyon plunges up to 2,600 feet (800 m) deep in places and is 6 miles (10 km) wide. For comparison, the Grand Canyon in Arizona averages about 1 mile (1.6 km) deep and 10 miles (16 km) across.

Parts of the canyon may route meltwater from beneath the ice sheet to the sea. It probably formed before the ice sheet and was once the channel for a mighty river.


Invisible mountains

As ice in Greenland melts at the surface, water carves fissures and reaches the base, where ice meets land. This sub-glacial ice can lubricate a glacier, causing it to flow to the ocean faster and be depleted more quickly. (Image credit: Ashley Cooper via Getty Images)


The canyon isn't the only rugged part of Greenland's under-ice landscape. Decades of mapping the island by ice-penetrating radar (which is usually mounted on airplanes) have revealed rugged mountain ranges and plunging fjords beneath the ice sheet.

A 2017 map of Greenland stripped of its ice shows a bowl-like depression in the center of the island. A circle of coastal mountain ranges rings this depression. The map revealed the topography underlying Greenland's flowing glaciers, which can help scientists predict how fast the glaciers will move in warming conditions and how quickly they will calve icebergs into the ocean.

A primeval lake

Ice seems to go on forever at Humboldt Glacier in northwest Greenland. (Image credit: VWPics/Universal Images Group via Getty Images)


Hundreds of thousands or millions of years ago, before Greenland was covered with ice, it was home to a lake the size of Rhode Island and Delaware combined.

Today, the lake is a depression filled with sediment. But it was once filled with water 800 feet (250 m) deep in some places. The lake basin covers 2,700 square miles (7,100 square km) and was fed by at least 18 different streams.

The lake bed could hold valuable clues to the climate of the Arctic in the distant past, though discovering these secrets would require drilling through the 1.1 miles (1.8 km) of ice that now caps the ancient site.

Hidden gems

The blue rivers and splotches are Greenland's surface meltwaters. (Image credit: Andrew Sole/University of Sheffield)


Greenland's ice sheet also hides a landscape of jewel-like lakes filled with crystalline meltwater. There are at least 60 of these small lakes, mostly clustered in northern and eastern Greenland, Stephen Livingstone, a senior lecturer in physical geography at the University of Sheffield in the United Kingdom and co-researcher of a study into the lakes, Live Science previously reported.

The lakes range in size from 656 feet (200 m) across to 3.7 miles (5.9 km) across. The meltwater in these lakes may flow from the surface of the ice sheet, or it may melt because of friction from the movement of ice or geothermal energy from below.
Evidence of meteor impacts

Crater in Greenland below the ice sheet. (Image credit: NASA's Goddard Space Flight Center/ Cynthia Starr)



Not all the topography below the ice sheet is of Earthly origin. Scientists have found at least two likely meteor craters buried beneath the ice. Both are in northwest Greenland: One sits below Hiawatha Glacier, while the other is 114 miles (183 km) away from the first. The Hiawatha crater sits under about a half-mile (930 m) of ice, while the second crater is buried under 1.2 miles (2 km) of ice. The second crater is 22 miles (36 km) across, making it the 22nd-largest impact crater ever found on Earth. The first is a bit smaller at 19 miles (31 km) across.

Perfectly preserved fossil plants


Greenland's ice sheet may have disappeared far more recently than once thought, enabling plants and trees to thrive. (Image credit: Joshua Brown/UVM)


An ice core dug up during a Cold War-era attempt at building a nuclear weapons base was rediscovered in a freezer in 2017 and found to hold the perfectly preserved fossils of plants dating to a million years ago.

"The best way to describe them is freeze-dried," Andrew Christ, lead author of a study into the core and a postdoctoral fellow and lecturer in the Department of Geology at The University of Vermont in Burlington, told Live Science at the time. "When we pulled these out and put a little water on them, they kind of unfurled, so they looked like they died yesterday."

The core came from northwestern Greenland, and the plants held within may have grown in a boreal forest. Such a forest could only grow in largely ice-free conditions, suggesting that parts of Greenland's ice sheet may be younger than researchers previously believed.

Originally published on Live Science

 

Newly identified mosasaur was fish-hunting monster

Newly identified mosasaur was fish-hunting monster
The Smoky Hill Chalk Member is a fossil-rich region of western Kansas where a new species of mosasaur was discovered. Credit: Takuya Konishi

Researchers at the University of Cincinnati identified a new species of mosasaur—an 18-foot-long fish-eating monster that lived 80 million years ago.

UC assistant professor-educator Takuya Konishi and his student, UC graduate Alexander Willman, named the mosasaur Ectenosaurus everhartorum after paleontologists Mike and Pamela Everhart. The mosasaur inhabited the Western Interior Seaway in what today is western Kansas.

The discovery was announced this week in the Canadian Journal of Earth Sciences.

The newly identified mosasaur marks only the second species in the genus Ectenosaurus.

"Mosasaurs in western Kansas have been well sampled and well researched. Those two factors create tall odds when you try to find something new," Konishi said.

Mosasaurs were enormous marine reptiles, some as big as school buses. They inhabited oceans around the world during the Cretaceous period around the time of Tyrannosaurus rex. If Ectenosaurus clidastoides with its long, slender jaws resembles a gharial crocodile, Konishi said the new species is closer to a false gharial crocodile with notably blunter jaws.

Konishi, who teaches in the Biological Sciences Department of UC's College of Arts and Sciences, first encountered the fossil in 2004 while working as a graduate student in systematics and evolution. Konishi was studying fossils of Platecarpus, a different genus of mosasaur in storage at Fort Hays State University's Sternberg Museum of Natural History, when he recognized something odd about one specimen.

Newly identified mosasaur was fish-hunting monster
UC paleontologist Takuya Konishi helped identify a new species of mosasaur from a specimen he first saw in 2004. Here he stands in front of another mosasaur skull. Credit: Joseph Fuqua II/UC Creative

"It wasn't a platecarpus. The frontal bone above the eye socket was much longer. The bones of Platecarpus should have had a broader triangle," he said. "That was one telltale sign."

Konishi suspected the specimen was a type of ectenosaur, only one species of which had been identified. But the teeth seemed all wrong. The now-empty sockets that would have contained the mosasaur's sharp, curved teeth in the unidentified specimen would have extended around the front of its mouth, unlike other recognized species that has a toothless rostrum, the bony protuberance at the front of the mouth.

For years, the fossils puzzled him.

"Some things just stick in your mind and they're hard to let go," he said.

But the mystery would have to wait because Konishi was busy finishing his  and launching an academic career that would bring him to UC's College of Arts and Sciences.

The first mosasaur fossils were found in the Netherlands a half-century before anyone used the term "dinosaur." Mosasaurs began to capture the nation's attention after the Civil War when the nation's premier paleontologists, Othniel Charles Marsh and Edward Drinker Cope, began to study Cretaceous limestone in Kansas in a partnership that became a bitter public feud. Since then, Kansas has become world-renowned for mosasaur research.

Generations of experts have come to Kansas to study its specimens, which are on display at museums around the world.

Newly identified mosasaur was fish-hunting monster
University of Cincinnati graduate Alexander Willman was lead author of a study identifying a new species of mosasaur. Credit: Takuya Konishi

"It's a famous place for mosasaur research. It's quite well known," Konishi said. "So I thought I don't have to be the guy to place a stake. I'm sure someone will catch it. But nobody did."

Ectenosaur is unusual for how few specimens have been found in the genus compared to other mosasaurs, Konishi said.

"In western Kansas we have over 1,500 mosasaur specimens. Out of those we can only find one specimen each representing these two species of ectenosaur," Konishi said. "That's sort of crazy."

When Konishi confirmed with the Sternberg Museum that no other researchers were studying the specimen, he asked them to ship the fossils to UC. When he opened the carefully bubble-wrapped contents, his initial impressions were confirmed.

"By then I had looked at all the other known Platecarpus specimens under the sun, as it were. And this specimen was distinct from the others," he said. "To me it was so obvious."

At the same time, Konishi's student Willman inquired about working on a research project. He received a UC Undergraduate STEM Experience grant to help with the taxonomic identification.

"I was beyond excited to be part of the discovery," Willman said.

Newly identified mosasaur was fish-hunting monster
UC researchers identified the mosasaur as belonging to the same genus as Ectenosaurus clidastoides, pictured. The above specimen was found in Kansas in 1953. Credit: Mike Everhart

The third author on the study, Michael Caldwell, is a professor of biology at the University of Alberta, Edmonton.

Willman illustrated the fossils in painstaking detail to help scientists understand the morphological differences that make the mosasaur unique.

"I was very happy with how he brought these broken bones to life," Konishi said. "It helped make our case very convincing to anyone that this is something new that warrants the establishment of a new taxon."

The researchers dedicated the project to the late Dale Russell, whose work has had a profound impact in North American mosasaur paleontology, Konishi said. But they named the  for the Everharts, a Kansas couple who have spent more than 30 years sharing their fossils with museums and leading research field trips in the fossil-rich Smoky Hill Chalk.

"We're still in a little bit of shock at the news. It's very exciting," Pamela Everhart said.

"It's a great honor," said Mike Everhart, author of "Oceans of Kansas" about mosasaurs and other prehistoric life that inhabited the Western Interior Seaway during the Cretaceous Period.

Mosasaurs are very special to him, he said.

"The oceans would not have been a safe place for swimming in the Cretaceous," he said. "Mosasaurs were the top predator in the ocean during those times."

Did mosasaurs hunt like killer whales?

More information: Alexander J. Willman et al, A new species of Ectenosaurus (Mosasauridae: Plioplatecarpinae) from western Kansas, USA, reveals a novel suite of osteological characters for the genus, Canadian Journal of Earth Sciences (2021). DOI: 10.1139/cjes-2020-0175

Journal information: Canadian Journal of Earth Sciences 

Provided by University of Cincinnati 

Newly identified mosasaur was fish-hunting monster


Researchers name species for husband-wife paleontologists in Kansas

Peer-Reviewed Publication

UNIVERSITY OF CINCINNATI

Konishi 

IMAGE: UC PALEONTOLOGIST TAKUYA KONISHI HELPED IDENTIFY A NEW SPECIES OF MOSASAUR FROM A SPECIMEN HE FIRST SAW IN 2004. HERE HE STANDS IN FRONT OF ANOTHER MOSASAUR SKULL. view more 

CREDIT: JOSEPH FUQUA II/UC CREATIVE

Researchers at the University of Cincinnati identified a new species of mosasaur — an 18-foot-long fish-eating monster that lived 80 million years ago.

UC assistant professor-educator Takuya Konishi and his student, UC graduate Alexander Willman, named the mosasaur Ectenosaurus everhartorum after paleontologists Mike and Pamela Everhart. The mosasaur inhabited the Western Interior Seaway in what today is western Kansas.

The discovery was announced this week in the Canadian Journal of Earth Sciences.

The newly identified mosasaur marks only the second species in the genus Ectenosaurus.

“Mosasaurs in western Kansas have been well sampled and well researched. Those two factors create tall odds when you try to find something new,” Konishi said.

Mosasaurs were enormous marine reptiles, some as big as school buses. They inhabited oceans around the world during the Cretaceous period around the time of Tyrannosaurus rex. If Ectenosaurus clidastoides with its long, slender jaws resembles a gharial crocodile, Konishi said the new species is closer to a false gharial crocodile with notably blunter jaws.

Konishi, who teaches in the Biological Sciences Department of UC's College of Arts and Sciences, first encountered the fossil in 2004 while working as a graduate student in systematics and evolution. Konishi was studying fossils of Platecarpus, a different genus of mosasaur in storage at Fort Hays State University's Sternberg Museum of Natural History, when he recognized something odd about one specimen.

“It wasn’t a platecarpus. The frontal bone above the eye socket was much longer. The bones of Platecarpus should have had a broader triangle,” he said. “That was one telltale sign.”

Konishi suspected the specimen was a type of ectenosaur, only one species of which had been identified. But the teeth seemed all wrong. The now-empty sockets that would have contained the mosasaur’s sharp, curved teeth in the unidentified specimen would have extended around the front of its mouth, unlike other recognized species that has a toothless rostrum, the bony protuberance at the front of the mouth.

For years, the fossils puzzled him.

“Some things just stick in your mind and they’re hard to let go,” he said.

But the mystery would have to wait because Konishi was busy finishing his doctoral degree and launching an academic career that would bring him to UC’s College of Arts and Sciences.

The first mosasaur fossils were found in the Netherlands a half-century before anyone used the term “dinosaur.” Mosasaurs began to capture the nation’s attention after the Civil War when the nation’s premier paleontologists, Othniel Charles Marsh and Edward Drinker Cope, began to study Cretaceous limestone in Kansas in a partnership that became a bitter public feud. Since then, Kansas has become world-renowned for mosasaur research.

Generations of experts have come to Kansas to study its specimens, which are on display at museums around the world.

“It’s a famous place for mosasaur research. It’s quite well known,” Konishi said. “So I thought I don’t have to be the guy to place a stake. I’m sure someone will catch it. But nobody did.”

Ectenosaur is unusual for how few specimens have been found in the genus compared to other mosasaurs, Konishi said.

“In western Kansas we have over 1,500 mosasaur specimens. Out of those we can only find one specimen each representing these two species of ectenosaur,” Konishi said. “That’s sort of crazy.”

When Konishi confirmed with the Sternberg Museum that no other researchers were studying the specimen, he asked them to ship the fossils to UC. When he opened the carefully bubble-wrapped contents, his initial impressions were confirmed.

“By then I had looked at all the other known Platecarpus specimens under the sun, as it were. And this specimen was distinct from the others,” he said. “To me it was so obvious.”

At the same time, Konishi’s student Willman inquired about working on a research project. He received a UC Undergraduate STEM Experience grant to help with the taxonomic identification.

“I was beyond excited to be part of the discovery,” Willman said.

The third author on the study, Michael Caldwell, is a professor of biology at the University of Alberta, Edmonton.

Willman illustrated the fossils in painstaking detail to help scientists understand the morphological differences that make the mosasaur unique.

“I was very happy with how he brought these broken bones to life,” Konishi said. “It helped make our case very convincing to anyone that this is something new that warrants the establishment of a new taxon.”

The researchers dedicated the project to the late Dale Russell, whose work has had a profound impact in North American mosasaur paleontology, Konishi said. But they named the mosasaur for the Everharts, a Kansas couple who have spent more than 30 years sharing their fossils with museums and leading research field trips in the fossil-rich Smoky Hill Chalk.

“We’re still in a little bit of shock at the news. It’s very exciting,” Pamela Everhart said.

“It’s a great honor,” said Mike Everhart, author of “Oceans of Kansas” about mosasaurs and other prehistoric life that inhabited the Western Interior Seaway during the Cretaceous Period.

Mosasaurs are very special to him, he said.

“The oceans would not have been a safe place for swimming in the Cretaceous,” he said. “Mosasaurs were the top predator in the ocean during those times.”

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