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How Earth’s Future Supercontinent Will Get Hot Enough To Wipe Us Out

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Earth‘s mass extinctions have come for the dinosaurs and a whopping 95 percent of ocean species.

Mammals, like us, may be next — eventually.

In intriguing new research published in the science journal Nature Geoscience, scientists used a supercomputer to simulate the climate on our planet’s next supercontinent, Pangea Ultima, which is expected to form in some 250 million years. The continent’s monthly average temperatures skyrocket to between some 104 to 122 degrees Fahrenheit (40 to 50 Celsius), and in the warmest summer months, temperatures would average up to a deadly 158 Fahrenheit (70 C).

For reference, today Earth’s average temperature is 59 F (15 C).

Much of the landmass wouldn’t have water to drink or grow food. Mammals — those who stay on Earth’s surface, that is — wouldn’t be able to physiologically withstand such a relentless onslaught of heat, the study’s authors conclude.

“Humans – along with many other species – would expire due to their inability to shed this heat through sweat, cooling their bodies,” Alexander Farnsworth, the study’s lead author who researches past, present and future climate at the University of Bristol, said in a statement.

The projected monthly temperatures on Earth’s future supercontinent, Pangea Ultima.

Extreme heating on Pangea Ultima

Mammalian life may still survive on the outer fringes of the supercontinent, meaning the higher latitudes where temperatures are moderate. But most of this future land, some 84 to 92 percent, would be hellish and uninhabitable. Researchers used a widely employed climate model, one of the UK Meteorological Office’s HadCM3 models, to simulate conditions on Pangea Ultima. (Climate models like HadCM3 have proven incredibly accurate at predicting Earth’s recent warming.)

Here’s why it would get so hot:

Carbon dioxide would skyrocket in the atmosphere: The amount of heat-trapping carbon dioxide gas in the atmosphere largely controls Earth’s climate. That’s why the planet’s temperature is currently increasing. Fortunately, this is controllable heating — the burning of fossil fuels drives today’s heating. But when the continents collide, geologists expect rampant volcanism to ramp up (as it likely has before), relentlessly releasing carbon dioxide into the skies.

“We think CO2 could rise from around 400 parts per million (ppm) today to more than 600 ppm many millions of years in the future,” Benjamin Mills, a biogeochemical modeller at the University of Leeds who worked on the research, said in a statement. “Of course, this assumes that humans will stop burning fossil fuels, otherwise we will see those numbers much, much sooner.”

– The supercontinent’s location: Pangea Ultima is expected to primarily form in the hottest part of Earth: the sweltering tropics where Earth receives the most sunlight. It’s also humid there, owing to warm ocean water evaporating into the tropical atmosphere. Crucially, humidity, which means more moisture in the air, makes air temperatures feel hotter while making it difficult (or impossible) to evaporate away body heat.

– The continentality effect: The interior of continents are far from the moderating influence of the ocean. Los Angeles, for example, experiences a cool marine breeze that California’s inland deserts don’t. Much of Pangea Ultima, as all seven of Earth’s continents scrunched together, won’t be exposed to oceanic influences, allowing the vast, singular inner continent to bake.

– Sun’s increased brightness: Although our star is stable, it’s slowly growing brighter. Every 100 million years, the sun‘s luminosity increases by about 1 percent. In 250 million years, this added brightness will further exacerbate heating on Pangea Ultima.

“With the Sun also anticipated to emit about 2.5 percent more radiation and the supercontinent being located primarily in the hot, humid tropics, much of the planet could be facing temperatures of between 40 to 70°C,” Farnsworth said.

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The distant future climate of Pangea Ultima is an intriguing study in where our planet, and species, are headed. But the news isn’t all bad. After all, 250 million years is awfully far away. By that time, we’d almost certainly have a plan, like we’re developing for incoming asteroids.

And if we’re still around in 250 million years to face the coming onslaught of supercontinental heat, that means we deftly navigated our way through the likes of human-caused climate change, threatening space rocks, and worldwide plagues. What an achievement that would be.





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Where Did Earth’s Oceans Come From? Scientists Say They Originated From Comets

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Scientists have long debated how Earth became rich in liquid water after the planet formed about 4.5 billion years ago. Now a new research published in Science Advances suggests that comets, particularly those from the Jupiter family, may have played a significant role in delivering water to Earth.

The study focused on Comet 67P/Churyumov-Gerasimenko, a celestial body that belongs to the Jupiter family of comets.

Using data from the European Space Agency‘s (ESA) Rosetta mission, researchers analysed the molecular structure of water on the comet and found striking similarities to the water in Earth’s oceans. This discovery strengthens the theory that icy comets and asteroids crashing into Earth contributed to the formation of its oceans.

The ratio of deuterium to regular hydrogen in the water is a key signature which is the basis of the study. Deuterium is a heavier isotope of hydrogen and it forms heavy water.

Previous studies had shown that the levels of deuterium in the water vapour of many Jupiter-family comets closely matched those found in Earth’s water. To explore this connection further, NASA planetary scientist Kathleen Mandt and her team used advanced statistical techniques to analyse data from Comet 67P.

The findings revealed that deuterium-rich water was more closely associated with dust grains around the comet than previously understood. Because water with deuterium is more likely to form in cold environments, there’s a higher concentration of the isotope on objects that formed far from the Sun, such as comets, than in objects that formed closer to the Sun, like asteroids.

Measurements within the last couple of decades of deuterium in the water vapor of several other Jupiter-family comets showed similar levels to Earth’s water.

This discovery not only strengthens the idea that comets helped deliver water to Earth but also provides valuable insight into how the early solar system formed. By studying the molecular makeup of comets like 67P, scientists can better understand the processes that shaped our planet and its oceans billions of years ago.

Mandt expressed her excitement about the results, saying, “This is just one of those very rare cases where you propose a hypothesis and actually find it happening.” The research also shows how studying comets can help unravel mysteries about the building blocks of the solar system.

ALSO SEE: Uranus Is Hiding 8000-Km Deep Ocean? New Study Presents Thrilling Hints

ALSO SEE: Webb Telescope Sees World That Could Reek Of Burnt Matches And Rotten Eggs

(Image: NASA)





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Chainalysis permanently parts ways with its founding CEO

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Michael Gronager, the co-founder and longtime CEO of Chainalysis, has agreed to leave the company permanently, two months after taking a temporary personal leave of absence.

Chainalysis, a buzzy 10-year-old, New York-based blockchain data platform, will now be led by co-founder Jonathan Levin, as Levin told TechCrunch, explaining that on Tuesday, its board of directors gave him Gronager’s job. But Levin, who has long served as the outfit’s chief strategy officer, will do more than run the company as CEO; he will also maintain his other roles.

“I’ve been running R&D, and I think the CEO should be the chief product officer, so I’m making no changes to our R&D leadership team; it will continue to report directly to me,” he said in an interview on Wednesday.

Levin declined to provide more information about Gronager other than to say that Gronager is also no longer on the Chainalysis board but retains his equity in the company.

A message to Gronager on Wednesday from TechCrunch went unreturned.

Asked about Chainalysis’ financial health, Levin said the startup is “continuing to invest in our growth,” and that “we don’t need to raise capital. We raised $175 million in 2022 and [still] feel strong about the cash position of company.” He added that his focus will be on “executing, the expansion of our risk platform, and going deeper with our government clients across the world to ensure they can deal with the increased demand of crypto.”

Chainalysis, whose early investors include Benchmark, was valued by investors at $8.6 billion during that 2022 funding round. Crypto investor Katie Haun, who first discovered Chainalysis in her capacity as federal prosecutor, reportedly began buying up secondary shares of the company at a valuation of $2.5 billion this past April.

Considered a “crypto detective,” one whose clients include the U.S. government and a wide range of corporations, Chainalysis in late 2023 laid off slightly more than 15% of its staff of 900, with plans to focus more squarely on government contracting, according to The Block.

The entire crypto industry has been in bounce-back mode in more recent weeks, as the incoming Trump administration signals a far friendlier stance toward digital currencies. The most obvious proof point: The price of bitcoin reached a record high of $100,000 on Wednesday.

Above: Levin at a StrictlyVC event hosted by TechCrunch in November 2024.



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Zopa, the UK neobank, snaps up $87M at a $1B+ valuation, eschewing the IPO route

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Some believe Klarna’s planned IPO in 2025 could set the stage for other fintech startups to go public. But with the tech IPO market still sluggish, one of the candidates hotly tipped to follow suit has instead just announced a fundraise, and its CEO says going public is “not a priority.” Zopa, the U.K. neobank […]

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